Sample records for activity direction sheet

  1. Ice stream activity scaled to ice sheet volume during Laurentide Ice Sheet deglaciation.

    PubMed

    Stokes, C R; Margold, M; Clark, C D; Tarasov, L

    2016-02-18

    The contribution of the Greenland and West Antarctic ice sheets to sea level has increased in recent decades, largely owing to the thinning and retreat of outlet glaciers and ice streams. This dynamic loss is a serious concern, with some modelling studies suggesting that the collapse of a major ice sheet could be imminent or potentially underway in West Antarctica, but others predicting a more limited response. A major problem is that observations used to initialize and calibrate models typically span only a few decades, and, at the ice-sheet scale, it is unclear how the entire drainage network of ice streams evolves over longer timescales. This represents one of the largest sources of uncertainty when predicting the contributions of ice sheets to sea-level rise. A key question is whether ice streams might increase and sustain rates of mass loss over centuries or millennia, beyond those expected for a given ocean-climate forcing. Here we reconstruct the activity of 117 ice streams that operated at various times during deglaciation of the Laurentide Ice Sheet (from about 22,000 to 7,000 years ago) and show that as they activated and deactivated in different locations, their overall number decreased, they occupied a progressively smaller percentage of the ice sheet perimeter and their total discharge decreased. The underlying geology and topography clearly influenced ice stream activity, but--at the ice-sheet scale--their drainage network adjusted and was linked to changes in ice sheet volume. It is unclear whether these findings can be directly translated to modern ice sheets. However, contrary to the view that sees ice streams as unstable entities that can accelerate ice-sheet deglaciation, we conclude that ice streams exerted progressively less influence on ice sheet mass balance during the retreat of the Laurentide Ice Sheet.

  2. Environmental Education Activity Sheets 1-11.

    ERIC Educational Resources Information Center

    Halsey, Clifton F.; And Others

    These activity sheets, developed by personnel of the Agricultural Extension Service of the University of Minnesota, were designed for youth group campers but may be used by other populations and individuals. Each activity sheet focuses on a separate topic: (1) Selecting Suitable Uses for Land, (2) Measuring the Steepness of Land, (3) Determining…

  3. Lateral dimension-dependent antibacterial activity of graphene oxide sheets.

    PubMed

    Liu, Shaobin; Hu, Ming; Zeng, Tingying Helen; Wu, Ran; Jiang, Rongrong; Wei, Jun; Wang, Liang; Kong, Jing; Chen, Yuan

    2012-08-21

    Graphene oxide (GO) is a promising precursor to produce graphene-family nanomaterials for various applications. Their potential health and environmental impacts need a good understanding of their cellular interactions. Many factors may influence their biological interactions with cells, and the lateral dimension of GO sheets is one of the most relevant material properties. In this study, a model bacterium, Escherichia coli ( E. coli ), was used to evaluate the antibacterial activity of well-dispersed GO sheets, whose lateral size differs by more than 100 times. Our results show that the antibacterial activity of GO sheets toward E. coli cells is lateral size dependent. Larger GO sheets show stronger antibacterial activity than do smaller ones, and they have different time- and concentration-dependent antibacterial activities. Large GO sheets lead to most cell loss after 1 h incubation, and their concentration strongly influences antibacterial activity at relative low concentration (<10 μg/mL). In contrast, when incubating with small GO sheets up to 4 h, the inactivation rate of E. coli cells continues increasing. The increase of small GO sheet concentration also results in persistent increases in their antibacterial activity. In this study, GO sheets with different lateral sizes are all well dispersed, and their oxidation capacity toward glutathione is similar, consistent with X-ray photoelectron spectroscopy and ultraviolet-visible absorption spectroscopy results. This suggests the lateral size-dependent antibacterial activity of GO sheets is caused by neither their aggregation states, nor oxidation capacity. Atomic force microscope analysis of GO sheets and cells shows that GO sheets interact strongly with cells. Large GO sheets more easily cover cells, and cells cannot proliferate once fully covered, resulting in the cell viability loss observed in the followed colony counting test. In contrast, small GO sheets adhere to the bacterial surfaces, which cannot

  4. Loading direction-dependent shear behavior at different temperatures of single-layer chiral graphene sheets

    NASA Astrophysics Data System (ADS)

    Zhao, Yang; Dong, Shuhong; Yu, Peishi; Zhao, Junhua

    2018-06-01

    The loading direction-dependent shear behavior of single-layer chiral graphene sheets at different temperatures is studied by molecular dynamics (MD) simulations. Our results show that the shear properties (such as shear stress-strain curves, buckling strains, and failure strains) of chiral graphene sheets strongly depend on the loading direction due to the structural asymmetry. The maximum values of both the critical buckling shear strain and the failure strain under positive shear deformation can be around 1.4 times higher than those under negative shear deformation. For a given chiral graphene sheet, both its failure strain and failure stress decrease with increasing temperature. In particular, the amplitude to wavelength ratio of wrinkles for different chiral graphene sheets under shear deformation using present MD simulations agrees well with that from the existing theory. These findings provide physical insights into the origins of the loading direction-dependent shear behavior of chiral graphene sheets and their potential applications in nanodevices.

  5. Experimental Method for Characterizing Electrical Steel Sheets in the Normal Direction

    PubMed Central

    Hihat, Nabil; Lecointe, Jean Philippe; Duchesne, Stephane; Napieralska, Ewa; Belgrand, Thierry

    2010-01-01

    This paper proposes an experimental method to characterise magnetic laminations in the direction normal to the sheet plane. The principle, which is based on a static excitation to avoid planar eddy currents, is explained and specific test benches are proposed. Measurements of the flux density are made with a sensor moving in and out of an air-gap. A simple analytical model is derived in order to determine the permeability in the normal direction. The experimental results for grain oriented steel sheets are presented and a comparison is provided with values obtained from literature. PMID:22163394

  6. Distribution and directional fabric of ash-flow sheets in the northwestern Mogollon Plateau, New Mexico.

    NASA Technical Reports Server (NTRS)

    Rhodes, R. C.; Smith, E. I.

    1972-01-01

    Individual ash-flow sheets distributed over wide areas in the Mogollon-Datil volcanic province can be delineated and related by flow direction techniques to specific source cauldrons. Two major mid-Tertiary ash flows in the Mogollon Plateau have measurable microscopic directional fabric indicative of primary flow direction imprinted in the ash-flow sheets during late-stage laminar flow. Regional stratigraphic relationships and flow patterns of the ash-flow sheets indicate a late Tertiary origin of the Mogollon Plateau depression. They also show that Basin-Range faulting in southwestern New Mexico was not initiated until after emplacement of the younger ash flow (23 m.y. B.P.). Directional fabric is an inherent property of many calc-alkalic ash-flow sheets and measurement of preferred orientation provides a powerful tool in unravelling the geologic history of complex volcanic terrane.

  7. Properties of Rolled AZ31 Magnesium Alloy Sheet Fabricated by Continuous Variable Cross-Section Direct Extrusion

    NASA Astrophysics Data System (ADS)

    Liu, Yang; Li, Feng; Li, Xue Wen; Shi, Wen Yong

    2018-03-01

    Rolling is currently a widely used method for manufacturing and processing high-performance magnesium alloy sheets and has received widespread attention in recent years. Here, we combined continuous variable cross-section direct extrusion (CVCDE) and rolling processes. The microstructure and mechanical properties of the resulting sheets rolled at different temperatures from CVCDE extrudate were investigated by optical microscopy, scanning electron microscope, transmission electron microscopy and electron backscatter diffraction. The results showed that a fine-grained microstructure was present with an average grain size of 3.62 μm in sheets rolled from CVCDE extrudate at 623 K. Dynamic recrystallization and a large strain were induced by the multi-pass rolling, which resulted in grain refinement. In the 573-673 K range, the yield strength, tensile strength and elongation initially increased and then declined as the CVCDE temperature increased. The above results provide an important scientific basis of processing, manufacturing and the active control on microstructure and property for high-performance magnesium alloy sheet.

  8. Detection of oppositely directed reconnection jets in a solar wind current sheet

    NASA Astrophysics Data System (ADS)

    Davis, M. S.; Phan, T. D.; Gosling, J. T.; Skoug, R. M.

    2006-10-01

    We report the first two-spacecraft (Wind and ACE) detection of oppositely directed plasma jets within a bifurcated current sheet in the solar wind. The event occurred on January 3, 2003 and provides further direct evidence that such jets result from reconnection. The magnetic shear across the bifurcated current sheet at both Wind and ACE was ~150°, indicating that the magnetic shear must have been the same at the reconnection site located between the two spacecraft. These observations thus provide strong evidence for component merging with a guide field ~ 30% of the antiparallel field. The dimensionless reconnection rate based on the measured inflow was 0.03, implying fast reconnection.

  9. Detection of oppositely directed reconnection jets in a solar wind current sheet

    NASA Astrophysics Data System (ADS)

    Davis, M. S.; Phan, T. D.; Gosling, J. T.; Skoug, R. M.

    2006-12-01

    We report the first two-spacecraft (Wind and ACE) detection of oppositely directed plasma jets within a bifurcated current sheet in the solar wind. The event occurred on January 3, 2003 and provides further direct evidence that such jets result from reconnection. The magnetic shear across the bifurcated current sheet at both Wind and ACE was approximately 150 degrees, indicating that the magnetic shear must have been the same at the reconnection site located between the two spacecraft. These observations thus provide strong evidence for component merging with a guide field approximately 30% of the antiparallel field. The dimensionless reconnection rate based on the measured inflow was 0.03, implying fast reconnection.

  10. Petroleum Refineries New Source Performance Standards (NSPS) Direct Final Amendments Fact Sheet

    EPA Pesticide Factsheets

    This page contains a December 2013 fact sheet with information regarding the direct final rule for the NSPS for Petroleum Refineries. This document provides a summary of the information for this NSPS.

  11. Active volcanism beneath the West Antarctic ice sheet and implications for ice-sheet stability

    USGS Publications Warehouse

    Blankenship, D.D.; Bell, R.E.; Hodge, S.M.; Brozena, J.M.; Behrendt, John C.; Finn, C.A.

    1993-01-01

    IT is widely understood that the collapse of the West Antarctic ice sheet (WAIS) would cause a global sea level rise of 6 m, yet there continues to be considerable debate about the detailed response of this ice sheet to climate change1-3. Because its bed is grounded well below sea level, the stability of the WAIS may depend on geologically controlled conditions at the base which are independent of climate. In particular, heat supplied to the base of the ice sheet could increase basal melting and thereby trigger ice streaming, by providing the water for a lubricating basal layer of till on which ice streams are thought to slide4,5. Ice streams act to protect the reservoir of slowly moving inland ice from exposure to oceanic degradation, thus enhancing ice-sheet stability. Here we present aerogeophysical evidence for active volcanism and associated elevated heat flow beneath the WAIS near the critical region where ice streaming begins. If this heat flow is indeed controlling ice-stream formation, then penetration of ocean waters inland of the thin hot crust of the active portion of the West Antarctic rift system could lead to the disappearance of ice streams, and possibly trigger a collapse of the inland ice reservoir.

  12. Direct Laser Writing of Single-Material Sheets with Programmable Self-Rolling Capability

    NASA Astrophysics Data System (ADS)

    Bauhofer, Anton; KröDel, Sebastian; Bilal, Osama; Daraio, Chiara; Constantinescu, Andrei

    Direct laser writing, a sub-class of two-photon polymerization, facilitates 3D-printing of single-material microstructures with inherent residual stresses. Here we show that controlled distribution of these stresses allows for fast and cost-effective fabrication of structures with programmable self-rolling capability. We investigate 2D sheets that evolve into versatile 3D structures. Precise control over the shape morphing potential is acquired through variations in geometry and writing parameters. Effects of capillary action and gravity were shown to be relevant for very thin sheets (thickness <1.5um) and have been analytically and experimentally quantified. In contrast to that, the deformations of sheets with larger thickness (>1.5um) are dominated by residual stresses and adhesion forces. The presented structures create local tensions up to 180MPa, causing rolling curvatures of 25E3m-1. A comprehensive analytical model that captures the relevant influence factors was developed based on laminate plate theory. The predicted curvature and directionality correspond well with the experimentally obtained data. Potential applications are found in drug encapsulation and particle traps for emulsions with differing surface energies. This work was supported by the Swiss National Science Foundation.

  13. Stable subcutaneous cartilage regeneration of bone marrow stromal cells directed by chondrocyte sheet.

    PubMed

    Li, Dan; Zhu, Lian; Liu, Yu; Yin, Zongqi; Liu, Yi; Liu, Fangjun; He, Aijuan; Feng, Shaoqing; Zhang, Yixin; Zhang, Zhiyong; Zhang, Wenjie; Liu, Wei; Cao, Yilin; Zhou, Guangdong

    2017-05-01

    In vivo niche plays an important role in regulating differentiation fate of stem cells. Due to lack of proper chondrogenic niche, stable cartilage regeneration of bone marrow stromal cells (BMSCs) in subcutaneous environments is always a great challenge. This study explored the feasibility that chondrocyte sheet created chondrogenic niche retained chondrogenic phenotype of BMSC engineered cartilage (BEC) in subcutaneous environments. Porcine BMSCs were seeded into biodegradable scaffolds followed by 4weeks of chondrogenic induction in vitro to form BEC, which were wrapped with chondrocyte sheets (Sheet group), acellular small intestinal submucosa (SIS, SIS group), or nothing (Blank group) respectively and then implanted subcutaneously into nude mice to trace the maintenance of chondrogenic phenotype. The results showed that all the constructs in Sheet group displayed typical cartilaginous features with abundant lacunae and cartilage specific matrices deposition. These samples became more mature with prolonged in vivo implantation, and few signs of ossification were observed at all time points except for one sample that had not been wrapped completely. Cell labeling results in Sheet group further revealed that the implanted BEC directly participated in cartilage formation. Samples in both SIS and Blank groups mainly showed ossified tissue at all time points with partial fibrogenesis in a few samples. These results suggested that chondrocyte sheet could create a chondrogenic niche for retaining chondrogenic phenotype of BEC in subcutaneous environment and thus provide a novel research model for stable ectopic cartilage regeneration based on stem cells. In vivo niche plays an important role in directing differentiation fate of stem cells. Due to lack of proper chondrogenic niche, stable cartilage regeneration of bone marrow stromal cells (BMSCs) in subcutaneous environments is always a great challenge. The current study demonstrated that chondrocyte sheet generated by

  14. Direct nucleation of silver nanoparticles on graphene sheet.

    PubMed

    Singh, Manoj K; Titus, E; Krishna, R; Hawaldar, R R; Goncalves, G; Marques, P A A P; Gracio, J

    2012-08-01

    Silver (Ag) nanoparticles were synthesized on the surface of graphene sheet by the simultaneous reduction of Ag+ and graphene oxide (GO) in the presence of simple reducing agent, hydrazine hydrate (N2H4 x H2O). Both the Ag+ and GO were reduced and Ag+ was nucleated onto graphene. GO flakes were prepared by conventional chemical exfoliation method and in the presence of strong acidic medium of potassium chlorate. Silver nanoparticles were prepared using 0.01 M AgNO3 solution. The reduced GO sheet decorated with Ag is referred as G-Ag sample. G-Ag was characterized by FTIR (Fourier transform infrared) spectroscopy using GO as standard. An explicit alkene peak appeared around 1625 cm(-1) was observed in G-Ag sample. Besides, the characteristic carbonyl and hydroxyl peaks shows well reduction of GO. The FTIR therefore confirms the direct interaction of Ag into Graphene. SEM (scanning electron microscopy) and TEM (transmission electron microscopy) analysis were performed for morphological probing. The average size of Ag nanoparticles was confirmed by around 5-10 nm by the high-resolution TEM (HRTEM). The Ag quantum dots incorporated nanocomposite material could become prominent candidate for diverse applications including photovoltaic, catalysis, and biosensors etc.

  15. Development and evaluation of adsorption sheet (HD safe sheet-U) using active carbon for the purpose of the preventing the contamination diffusion of urinary excreted anticancer drug.

    PubMed

    Sato, Junya; Ohkubo, Haruka; Sasaki, Yuki; Yokoi, Makoto; Hotta, Yasunori; Kudo, Kenzo

    2017-01-01

    Certain amount of anticancer drugs is excreted in the urine of patients receiving anticancer drugs, and urinary scattering including anticancer drugs at excretion has become a route of anticancer drug contamination. Therefore, we developed an active carbon sheet (HD safe sheet-U) that prevented diffusion by adsorbing anticancer drugs including that excreted in urine. The present study conducted a performance evaluation of this sheet. The adsorption performance of active carbon to anticancer drug in the urine was evaluated by determining concentration changes in the active carbon suspension (5 mg/mL) of 14 kinds of anticancer drugs (cyclophosphamide, ifosfamide, carboplatin, cisplatin, methotrexate, 5-fluorouracil, cytarabine, gemcitabine, doxorubicin, epirubicin, paclitaxel, docetaxel, etoposide, and irinotecan) diluted with artificial urine. Adhesion of the anticancer drug dropping on the sheet to a slipper sole was evaluated because urine including anticancer drugs is scattered on the floor, which can spread by adhering to shoe soles of patients and healthcare workers. The performance of the active carbon sheet was compared with two other types of medical adsorption sheets used as control sheets. Anticancer drugs diluted with artificial urine (1 mL) were dropped on the active carbon sheet and the two control sheets. The sheets were trod with slippers made by polyvinyl chloride. The adhered anticancer drug was wiped off and its quantity was determined. A remarkable decrease in anticancer drug concentrations, except for cisplatin, was detected by mixture of active carbon in the artificial urine (0-79.6%). The quantity of anticancer drug adhesion to slipper soles from the active carbon sheet was significantly lower compared with that observed for the two control sheets for eight kinds of anticancer drugs (cyclophosphamide, ifosfamide, carboplatin, methotrexate, cytarabine, gemcitabine, doxorubicin, and docetaxel). There was no adhesion in cyclophosphamide and

  16. Zinc oxide nanorod clusters deposited seaweed cellulose sheet for antimicrobial activity.

    PubMed

    Bhutiya, Priyank L; Mahajan, Mayur S; Abdul Rasheed, M; Pandey, Manoj; Zaheer Hasan, S; Misra, Nirendra

    2018-06-01

    Seaweed cellulose was isolated from green seaweed Ulva fasciata using a common bleaching agent. Sheet containing porous mesh was prepared from the extracted seaweed crystalline cellulose along with zinc oxide (ZnO) nanorod clusters grown over the sheet by single step hydrothermal method. Seaweed cellulose and zinc oxide nanorod clusters deposited seaweed cellulose sheet was characterized by FT-IR, XRD, TGA, and SEM-EDX. Morphology showed that the diameter of zinc oxide nanorods were around 70nm. Zinc oxide nanorod clusters deposited on seaweed cellulose sheet gave remarkable antibacterial activity towards gram-positive (Staphylococcus aureus, Bacillus ceresus, Streptococcus thermophilis) and gram-negative (Escherichia coli, Pseudomonas aeruginous) microbes. Such deposited sheet has potential applications in pharmaceutical, biomedical, food packaging, water treatment and biotechnological industries. Copyright © 2018 Elsevier B.V. All rights reserved.

  17. Electric fields measured by ISEE-1 within and near the neutral sheet during quiet and active times

    NASA Technical Reports Server (NTRS)

    Cattell, C. A.; Mozer, F. S.

    1982-01-01

    An understanding of the physical processes occurring in the magnetotail and plasmasheet during different interplanetary magnetic field orientations and differing levels of ground magnetic activity is crucial for the development of a theory of energy transfer from the solar wind to the particles which produce auroral arcs. In the present investigation, the first observations of electric fields during neutral sheet crossings are presented, taking into account the statistical correlations of the interplanetary magnetic field direction and ground activity with the character of the electric field. The electric field data used in the study were obtained from a double probe experiment on the ISEE-1 satellite. The observations suggest that turbulent electric and magnetic fields are intimately related to plasma acceleration in the neutral sheet and to the processes which create auroral particles.

  18. Salt-assisted direct exfoliation of graphite into high-quality, large-size, few-layer graphene sheets.

    PubMed

    Niu, Liyong; Li, Mingjian; Tao, Xiaoming; Xie, Zhuang; Zhou, Xuechang; Raju, Arun P A; Young, Robert J; Zheng, Zijian

    2013-08-21

    We report a facile and low-cost method to directly exfoliate graphite powders into large-size, high-quality, and solution-dispersible few-layer graphene sheets. In this method, aqueous mixtures of graphite and inorganic salts such as NaCl and CuCl2 are stirred, and subsequently dried by evaporation. Finally, the mixture powders are dispersed into an orthogonal organic solvent solution of the salt by low-power and short-time ultrasonication, which exfoliates graphite into few-layer graphene sheets. We find that the as-made graphene sheets contain little oxygen, and 86% of them are 1-5 layers with lateral sizes as large as 210 μm(2). Importantly, the as-made graphene can be readily dispersed into aqueous solution in the presence of surfactant and thus is compatible with various solution-processing techniques towards graphene-based thin film devices.

  19. Criminal investigations and the Superfund program. Fact sheet (Final)

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Not Available

    1990-09-01

    The fact sheet, directed toward any one who witnesses fraudulent activity in EPA programs, discusses areas in which fraud and abuse can occur and provides an understanding of the criminal investigation process that results from reports of suspicious activity.

  20. Controllable curvature from planar polymer sheets in response to light.

    PubMed

    Hubbard, Amber M; Mailen, Russell W; Zikry, Mohammed A; Dickey, Michael D; Genzer, Jan

    2017-03-22

    The ability to change shape and control curvature in 3D structures starting from planar sheets can aid in assembly and add functionality to an object. Herein, we convert planar sheets of shape memory polymers (SMPs) into 3D objects with controllable curvature by dictating where the sheets shrink. Ink patterned on the surface of the sheet absorbs infrared (IR) light, resulting in localized heating, and the material shrinks locally wherever the temperature exceeds the activation temperature, T a . We introduce two different mechanisms for controlling curvature within SMP sheets. The 'direct' mechanism uses localized shrinkage to induce curvature only in regions patterned with ink. The 'indirect' mechanism uses localized shrinkage in regions patterned with ink to induce curvature in neighboring regions without ink through a balance of internal stresses. Finite element analysis predicts the final shape of the polymer sheets with excellent qualitative agreement with experimental studies. Results from this study show that curvature can be controlled by the distribution and darkness of the ink pattern on the polymer sheet. Additionally, we utilize the direct and indirect curvature mechanisms to demonstrate the formation and actuation of gripper devices, which represent the potential utility of this approach.

  1. Sheet production apparatus for removing a crystalline sheet from the surface of a melt using gas jets located above and below the crystalline sheet

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Kellerman, Peter L.; Thronson, Gregory D.

    In one embodiment, a sheet production apparatus comprises a vessel configured to hold a melt of a material. A cooling plate is disposed proximate the melt and is configured to form a sheet of the material on the melt. A first gas jet is configured to direct a gas toward an edge of the vessel. A sheet of a material is translated horizontally on a surface of the melt and the sheet is removed from the melt. The first gas jet may be directed at the meniscus and may stabilize this meniscus or increase local pressure within the meniscus.

  2. Clouds enhance Greenland ice sheet meltwater runoff

    PubMed Central

    Van Tricht, K.; Lhermitte, S.; Lenaerts, J. T. M.; Gorodetskaya, I. V.; L'Ecuyer, T. S.; Noël, B.; van den Broeke, M. R.; Turner, D. D.; van Lipzig, N. P. M.

    2016-01-01

    The Greenland ice sheet has become one of the main contributors to global sea level rise, predominantly through increased meltwater runoff. The main drivers of Greenland ice sheet runoff, however, remain poorly understood. Here we show that clouds enhance meltwater runoff by about one-third relative to clear skies, using a unique combination of active satellite observations, climate model data and snow model simulations. This impact results from a cloud radiative effect of 29.5 (±5.2) W m−2. Contrary to conventional wisdom, however, the Greenland ice sheet responds to this energy through a new pathway by which clouds reduce meltwater refreezing as opposed to increasing surface melt directly, thereby accelerating bare-ice exposure and enhancing meltwater runoff. The high sensitivity of the Greenland ice sheet to both ice-only and liquid-bearing clouds highlights the need for accurate cloud representations in climate models, to better predict future contributions of the Greenland ice sheet to global sea level rise. PMID:26756470

  3. Clouds enhance Greenland ice sheet meltwater runoff.

    PubMed

    Van Tricht, K; Lhermitte, S; Lenaerts, J T M; Gorodetskaya, I V; L'Ecuyer, T S; Noël, B; van den Broeke, M R; Turner, D D; van Lipzig, N P M

    2016-01-12

    The Greenland ice sheet has become one of the main contributors to global sea level rise, predominantly through increased meltwater runoff. The main drivers of Greenland ice sheet runoff, however, remain poorly understood. Here we show that clouds enhance meltwater runoff by about one-third relative to clear skies, using a unique combination of active satellite observations, climate model data and snow model simulations. This impact results from a cloud radiative effect of 29.5 (±5.2) W m(-2). Contrary to conventional wisdom, however, the Greenland ice sheet responds to this energy through a new pathway by which clouds reduce meltwater refreezing as opposed to increasing surface melt directly, thereby accelerating bare-ice exposure and enhancing meltwater runoff. The high sensitivity of the Greenland ice sheet to both ice-only and liquid-bearing clouds highlights the need for accurate cloud representations in climate models, to better predict future contributions of the Greenland ice sheet to global sea level rise.

  4. Ohm's law for a current sheet

    NASA Technical Reports Server (NTRS)

    Lyons, L. R.; Speiser, T. W.

    1985-01-01

    The paper derives an Ohm's law for single-particle motion in a current sheet, where the magnetic field reverses in direction across the sheet. The result is considerably different from the resistive Ohm's law often used in MHD studies of the geomagnetic tail. Single-particle analysis is extended to obtain a self-consistency relation for a current sheet which agrees with previous results. The results are applicable to the concept of reconnection in that the electric field parallel to the current is obtained for a one-dimensional current sheet with constant normal magnetic field. Dissipated energy goes directly into accelerating particles within the current sheet.

  5. Basic Residues of β-Sheet A Contribute to Heparin Binding and Activation of Vaspin (Serpin A12).

    PubMed

    Ulbricht, David; Oertwig, Kathrin; Arnsburg, Kristin; Saalbach, Anja; Pippel, Jan; Sträter, Norbert; Heiker, John T

    2017-01-20

    Many members of the serine protease inhibitor (serpin) family are activated by glycosaminoglycans (GAGs). Visceral adipose tissue-derived serpin (vaspin), serpin A12 of the serpin family, and its target protease kallikrein 7 (KLK7) are heparin-binding proteins, and inhibition of KLK7 by vaspin is accelerated by heparin. However, the nature of GAG binding to vaspin is not known. Here, we measured vaspin binding of various glycosaminoglycans and low molecular weight heparins by microscale thermophoresis and analyzed acceleration of protease inhibition by these molecules. In addition, basic residues contributing to heparin binding and heparin activation were identified by a selective labeling approach. Together, these data show that vaspin binds heparin with high affinity (K D = 21 ± 2 nm) and that binding takes place at a basic patch on top of β-sheet A and is different from other heparin-binding serpins. Mutation of basic residues decreased heparin binding and activation of vaspin. Similarly, reactive center loop insertion into sheet A decreased heparin binding because it disturbs the basic cluster. Finally, using vaspin-overexpressing keratinocyte cells, we show that a significant part of secreted vaspin is bound in the extracellular matrix on the cell surface. Together, basic residues of central β-sheet A contribute to heparin binding and activation of vaspin. Thus, binding to GAGs in the extracellular matrix can direct and regulate vaspin interaction with target proteases or other proteins and may play an important role in the various beneficial functions of vaspin in different tissues. © 2017 by The American Society for Biochemistry and Molecular Biology, Inc.

  6. FSA future directions: FSA technology activities in FY86

    NASA Technical Reports Server (NTRS)

    Leipold, M. H.

    1985-01-01

    The silicon material, advanced silicon sheet, device research, and process research activities are explained. There will be no new initiatives. Many activities are targeted for completion and the emphasis will then be on technology transfer. Industrial development of the fluidized-bed reactor (FBR) deposition technology is proceeding. Technology transfer and industry funding of sheet development are continuing.

  7. Current status of solar cell performance of unconventional silicon sheets

    NASA Technical Reports Server (NTRS)

    Yoo, H. I.; Liu, J. K.

    1981-01-01

    It is pointed out that activities in recent years directed towards reduction in the cost of silicon solar cells for terrestrial photovoltaic applications have resulted in impressive advancements in the area of silicon sheet formation from melt. The techniques used in the process of sheet formation can be divided into two general categories. All approaches in one category require subsequent ingot wavering. The various procedures of the second category produce silicon in sheet form. The performance of baseline solar cells is discussed. The baseline process included identification marking, slicing to size, and surface treatment (etch-polishing) when needed. Attention is also given to the performance of cells with process variations, and the effects of sheet quality on performance and processing.

  8. Probing the interactions of phenol with oxygenated functional groups on curved fullerene-like sheets in activated carbon.

    PubMed

    Yin, Chun-Yang; Ng, Man-Fai; Goh, Bee-Min; Saunders, Martin; Hill, Nick; Jiang, Zhong-Tao; Balach, Juan; El-Harbawi, Mohanad

    2016-02-07

    The mechanism(s) of interactions of phenol with oxygenated functional groups (OH, COO and COOH) in nanopores of activated carbon (AC) is a contentious issue among researchers. This mechanism is of particular interest because a better understanding of the role of such groups in nanopores would essentially translate to advances in AC production and use, especially in regard to the treatment of organic-based wastewaters. We therefore attempt to shed more light on the subject by employing density functional theory (DFT) calculations in which fullerene-like models integrating convex or concave structure, which simulate the eclectic porous structures on AC surface, are adopted. TEM analysis, EDS mapping and Boehm titration are also conducted on actual phenol-adsorbed AC. Our results suggest the widely-reported phenomenon of decreased phenol uptake on AC due to increased concentration of oxygenated functional groups is possibly attributed to the increased presence of the latter on the convex side of the curved carbon sheets. Such a system effectively inhibits phenol from getting direct contact with the carbon sheet, thus constraining any available π-π interaction, while the effect of groups acting on the concave part of the curved sheet does not impart the same detriment.

  9. Plasma flow disturbances in the magnetospheric plasma sheet during substorm activations

    NASA Astrophysics Data System (ADS)

    Kozelova, T. V.; Kozelov, B. V.; Turyanskii, V. A.

    2017-11-01

    We have considered variations in fields and particle fluxes in the near-Earth plasma sheet on the THEMIS-D satellite together with the auroral dynamics in the satellite-conjugate ionospheric part during two substorm activations on December 19, 2014 with K p = 2. The satellite was at 8.5 R E and MLT = 21.8 in the outer region of captured energetic particles with isotropic ion fluxes near the convection boundary of electrons with an energy of 10 keV. During substorm activations, the satellite recorded energetic particle injections and magnetic field oscillations with a period of 90 s. In the satellite-conjugate ionospheric part, the activations were preceded by wavelike disturbances of auroral brightness along the southern azimuthal arc. In the expansion phase of activations, large-scale vortex structures appeared in the structure of auroras. The sudden enhancements of auroral activity (brightening of arcs, auroral breakup, and appearance of NS forms) coincided with moments of local magnetic field dipolarization and an increase in the amplitude Pi2 of pulsations of the B z component of the magnetic field on the satellite. Approximately 30-50 s before these moments, the magnetosphere was characterized by an increased rate of plasma flow in the radial direction, which initiated the formation of plasma vortices. The auroral activation delays relative to the times when plasma vortices appear in the magnetosphere decreased with decreasing latitude of the satellite projection. The plasma vortices in the magnetosphere are assumed to be responsible for the observed auroral vortex structures and the manifestation of the hybrid vortex instability (or shear flow ballooning instability) that develops in the equatorial magnetospheric plane in the presence of a shear plasma flow in the region of strong pressure gradients in the Earthward direction.

  10. Effects of Changing Hot Rolling Direction on Microstructure, Texture and Mechanical Properties of Cu-2.7Be Sheets

    NASA Astrophysics Data System (ADS)

    Zhu, Daibo; Liu, Chuming; Yu, Haijun; Han, Tan

    2018-03-01

    A hot rolling scheme (cross-rolling and unidirectional rolling) was adopted to process Cu-2.7Be sheets used as multiplier dynodes in photomultiplier. The effects of changing rolling direction on microstructure, texture and mechanical properties were studied by a combination of XRD, EBSD and TEM. It was found that higher copper-type texture and lower brass texture intensity were obtained in the ultimately cross-rolling (CR) sheet compared with the unidirectional rolling (UR) sheet.The EBSD results indicated that the grain orientation from mainly < {101} > for UR sample turns to random for CR sample. Great enhancements in YS and UTS after unidirectional rolling were attributed to the massive and polygonal γ precipitates. The CR sample exhibited lower anisotropy, because of the increase of S and γ precipitates with spherical and tiny shape.

  11. The Conductive Silver Nanowires Fabricated by Two-beam Laser Direct Writing on the Flexible Sheet.

    PubMed

    He, Gui-Cang; Zheng, Mei-Ling; Dong, Xian-Zi; Jin, Feng; Liu, Jie; Duan, Xuan-Ming; Zhao, Zhen-Sheng

    2017-02-02

    Flexible electrically conductive nanowires are now a key component in the fields of flexible devices. The achievement of metal nanowire with good flexibility, conductivity, compact and smooth morphology is recognized as one critical milestone for the flexible devices. In this study, a two-beam laser direct writing system is designed to fabricate AgNW on PET sheet. The minimum width of the AgNW fabricated by this method is 187 ± 34 nm with the height of 84 ± 4 nm. We have investigated the electrical resistance under different voltages and the applicable voltage per meter range is determined to be less than 7.5 × 10 3  V/m for the fabricated AgNW. The flexibility of the AgNW is very excellent, since the resistance only increases 6.63% even after the stretched bending of 2000 times at such a small bending radius of 1.0 mm. The proposed two-beam laser direct writing is an efficient method to fabricate AgNW on the flexible sheet, which could be applied in flexible micro/nano devices.

  12. All about Me: Reproducible Activity Sheets To Develop Self-Esteem in Your Students.

    ERIC Educational Resources Information Center

    Palomares, Susanna

    This document contains a set of reproducible activity sheets for teachers to use in enhancing the self-esteem of their students. Designed to supplement other approaches being used by teachers, the activities in this book can be used to infuse esteem-building activities into the core curriculum. The activities are organized around several…

  13. Direct observations of evolving subglacial drainage beneath the Greenland Ice Sheet.

    PubMed

    Andrews, Lauren C; Catania, Ginny A; Hoffman, Matthew J; Gulley, Jason D; Lüthi, Martin P; Ryser, Claudia; Hawley, Robert L; Neumann, Thomas A

    2014-10-02

    Seasonal acceleration of the Greenland Ice Sheet is influenced by the dynamic response of the subglacial hydrologic system to variability in meltwater delivery to the bed via crevasses and moulins (vertical conduits connecting supraglacial water to the bed of the ice sheet). As the melt season progresses, the subglacial hydrologic system drains supraglacial meltwater more efficiently, decreasing basal water pressure and moderating the ice velocity response to surface melting. However, limited direct observations of subglacial water pressure mean that the spatiotemporal evolution of the subglacial hydrologic system remains poorly understood. Here we show that ice velocity is well correlated with moulin hydraulic head but is out of phase with that of nearby (0.3-2 kilometres away) boreholes, indicating that moulins connect to an efficient, channelized component of the subglacial hydrologic system, which exerts the primary control on diurnal and multi-day changes in ice velocity. Our simultaneous measurements of moulin and borehole hydraulic head and ice velocity in the Paakitsoq region of western Greenland show that decreasing trends in ice velocity during the latter part of the melt season cannot be explained by changes in the ability of moulin-connected channels to convey supraglacial melt. Instead, these observations suggest that decreasing late-season ice velocity may be caused by changes in connectivity in unchannelized regions of the subglacial hydrologic system. Understanding this spatiotemporal variability in subglacial pressures is increasingly important because melt-season dynamics affect ice velocity beyond the conclusion of the melt season.

  14. A Statistical Model of the Magnetotail Neutral Sheet

    NASA Astrophysics Data System (ADS)

    Xiao, Sudong; Zhang, Tielong; Baumjohann, Wolfgang; Nakamura, Rumi; Ge, Yasong; Du, Aimin; Wang, Guoqiang; Lu, Quanming

    2015-04-01

    The neutral sheet of the magnetotail is characterized by weak magnetic field, strong cross tail current, and a reversal of the magnetic field direction across it. The dynamics of the earth's magnetosphere is greatly influenced by physical processes that occur near the neutral sheet. However, the exact position of the neutral sheet is variable in time. It is therefore essential to have a reliable estimate of the average position of the neutral sheet. Magnetic field data from ten years of Cluster, nineteen years of Geotail, four years of TC 1, and seven years of THEMIS observations have been incorporated to obtain a model of the magnetotail neutral sheet. All data in aberrated GSM (Geocentric Solar Magnetospheric) coordinate system are normalized to the same solar wind pressure condition. The shape and position of the neutral sheet, illustrated directly by the separator of positive and negative Bx on the YZ cross sections, are fitted with a displaced ellipse model. It is consistent with previous studies that the neutral sheet becomes curvier in the YZ cross section when the dipole tilt increases, yet our model shows the curviest neutral sheet compared with previous models. The new model reveals a hinging distance very close to 10 RE at a reference solar wind dynamic pressure of 2 nPa. We find that the earth dipole tilt angle not only affects the neutral sheet configuration in the YZ cross section but also in the XZ cross section. The neutral sheet becomes more tilting in the XZ cross section when the dipole tilt increases. The effect of an interplanetary magnetic field (IMF) penetration is studied, and an IMF By-related twisting of about 3° is found. Anticlockwise twisting of the neutral sheet is observed, looking along the downtail direction, for a positive IMF By, and clockwise twisting of the neutral sheet for a negative IMF By.

  15. Buckling and stretching of thin viscous sheets

    NASA Astrophysics Data System (ADS)

    O'Kiely, Doireann; Breward, Chris; Griffiths, Ian; Howell, Peter; Lange, Ulrich

    2016-11-01

    Thin glass sheets are used in smartphone, battery and semiconductor technology, and may be manufactured by producing a relatively thick glass slab and subsequently redrawing it to a required thickness. The resulting sheets commonly possess undesired centerline ripples and thick edges. We present a mathematical model in which a viscous sheet undergoes redraw in the direction of gravity, and show that, in a sufficiently strong gravitational field, buckling is driven by compression in a region near the bottom of the sheet, and limited by viscous resistance to stretching of the sheet. We use asymptotic analysis in the thin-sheet, low-Reynolds-number limit to determine the centerline profile and growth rate of such a viscous sheet.

  16. Sheet, ligament and droplet formation in swirling primary atomization

    NASA Astrophysics Data System (ADS)

    Shao, Changxiao; Luo, Kun; Chai, Min; Fan, Jianren

    2018-04-01

    We report direct numerical simulations of swirling liquid atomization to understand the physical mechanism underlying the sheet breakup of a non-turbulent liquid swirling jet which lacks in-depth investigation. The volume-of-fluid (VOF) method coupled with adapted mesh refinement (AMR) technique in GERRIS code is employed in the present simulation. The mechanisms of sheet, ligament and droplet formation are investigated. It is observed that the olive-shape sheet structure is similar to the experimental result qualitatively. The numerical results show that surface tension, pressure difference and swirling effect contribute to the contraction and extension of liquid sheet. The ligament formation is partially at the sheet rim or attributed to the extension of liquid hole. Especially, the movement of hairpin vortex exerts by an anti-radial direction force to the sheet surface and leads to the sheet thinness. In addition, droplet formation is attributed to breakup of ligament and central sheet.

  17. Vitamin C treatment promotes mesenchymal stem cell sheet formation and tissue regeneration by elevating telomerase activity.

    PubMed

    Wei, Fulan; Qu, Cunye; Song, Tieli; Ding, Gang; Fan, Zhipeng; Liu, Dayong; Liu, Yi; Zhang, Chunmei; Shi, Songtao; Wang, Songlin

    2012-09-01

    Cell sheet engineering has been developed as an alternative approach to improve mesenchymal stem cell-mediated tissue regeneration. In this study, we found that vitamin C (Vc) was capable of inducing telomerase activity in periodontal ligament stem cells (PDLSCs), leading to the up-regulated expression of extracellular matrix type I collagen, fibronectin, and integrin β1, stem cell markers Oct4, Sox2, and Nanog as well as osteogenic markers RUNX2, ALP, OCN. Under Vc treatment, PDLSCs can form cell sheet structures because of increased cell matrix production. Interestingly, PDLSC sheets demonstrated a significant improvement in tissue regeneration compared with untreated control dissociated PDLSCs and offered an effective treatment for periodontal defects in a swine model. In addition, bone marrow mesenchymal stem cell sheets and umbilical cord mesenchymal stem cell sheets were also well constructed using this method. The development of Vc-mediated mesenchymal stem cell sheets may provide an easy and practical approach for cell-based tissue regeneration. Copyright © 2011 Wiley Periodicals, Inc.

  18. 46 CFR 232.4 - Balance sheet accounts.

    Code of Federal Regulations, 2010 CFR

    2010-10-01

    ... 46 Shipping 8 2010-10-01 2010-10-01 false Balance sheet accounts. 232.4 Section 232.4 Shipping... ACTIVITIES UNIFORM FINANCIAL REPORTING REQUIREMENTS Balance Sheet § 232.4 Balance sheet accounts. (a.... (b) Purpose of balance sheet accounts. The balance sheet accounts are intended to disclose the...

  19. 46 CFR 232.4 - Balance sheet accounts.

    Code of Federal Regulations, 2011 CFR

    2011-10-01

    ... 46 Shipping 8 2011-10-01 2011-10-01 false Balance sheet accounts. 232.4 Section 232.4 Shipping... ACTIVITIES UNIFORM FINANCIAL REPORTING REQUIREMENTS Balance Sheet § 232.4 Balance sheet accounts. (a.... (b) Purpose of balance sheet accounts. The balance sheet accounts are intended to disclose the...

  20. A flexible thermoresponsive cell culture substrate for direct transfer of keratinocyte cell sheets.

    PubMed

    Praveen, Wulligundam; Madathil, Bernadette K; Sajin Raj, R S; Kumary, T V; Anil Kumar, P R

    2017-10-25

    Most cell sheet engineering systems require a support or carrier to handle the harvested cell sheets. In this study, polyethylene terephthalate-based overhead projection transparency sheets (OHPS) were subjected to surface hydrolysis by alkali treatment to increase pliability and hydrophilicity and enable poly(N-isopropylacrylamide-co-glycidylmethacrylate) copolymer (NGMA) coating to impart thermoresponsiveness. NGMA was applied on the modified OHPS by the technique of spin coating using an indigenously designed spin coater. The spin coating had the advantage of using low volumes of the polymer and a reduced coating time. The surface chemistry and thermoresponsive coating was analyzed by Fourier transform infrared spectroscopy and water contact angle. Human keratinocyte cells were cultured on the spin coated surface and scaffold-free cell sheets were successfully harvested by simple variation of temperature. These cell sheets were found to be viable, exhibited epithelial characteristic and cell-cell contact as confirmed by positive immunostaining for ZO-1. The integrity and morphology of the cell sheet was confirmed by stereomicroscopy and E-SEM. These results highlight the potential of the NGMA spin coated modified OHPS to serve as a thermoresponsive culture surface-cum-flexible transfer tool.

  1. H+ and O+ dynamics during ultra-low frequency waves in the Earth's magnetotail plasma sheet

    NASA Astrophysics Data System (ADS)

    De Spiegeleer, Alexandre; Hamrin, Maria; Pitkänen, Timo; Volwerk, Martin; Mouikis, Christopher; Kistler, Lynn; Nilsson, Hans; Norqvist, Patrik; Andersson, Laila

    2017-04-01

    The concentration of ionospheric oxygen (O^+) in the magnetotail plasma sheet can be relatively elevated depending on, for instance, the geomagnetic activity as well as the solar cycle. The dynamics of the tail plasma sheet can be affected by the presence of O+ via for example the generation of instabilities such as the Kelvin-Helmholtz instability. However, the O+ is not always taken into account when studying the dynamics of the tail plasma sheet. We investigate proton (H^+) and O+ during ultra-low frequency waves (period > 5 min) in the mid-tail plasma sheet (beyond 10R_E) using Cluster data. We observe that the velocity of O+ can be significantly different from that of H^+. When occuring, this velocity difference always seems to be in the direction parallel to the magnetic field. The parallel velocity of the two species can be observed to be somewhat out of phase, meaning that while one species flows in the parallel direction, the other flows in the anti-parallel direction. Possible causes for such large discrepancies between the dynamics of O+ and H+ are discussed.

  2. Investigation of the magnetic properties of Si-gradient steel sheet by comparison with 6.5%Si steel sheet

    NASA Astrophysics Data System (ADS)

    Hiratani, T.; Zaizen, Y.; Oda, Y.; Yoshizaki, S.; Senda, K.

    2018-05-01

    In this study, we investigated the magnetic properties of Si-gradient steel sheet produced by CVD (chemical vapor deposition) siliconizing process, comparing with 6.5% Si steel sheet. The Si-gradient steel sheet having silicon concentration gradient in the thickness direction, has larger hysteresis loss and smaller eddy current loss than the 6.5% Si steel sheet. In such a loss configuration, the iron loss of the Si-gradient steel sheet becomes lower than that of the 6.5% Si steel sheet at high frequencies. The experiment suggests that tensile stress is formed at the surface layer and compressive stress is formed at the inner layer in the Si gradient steel sheet. The magnetic anisotropy is induced by the internal stress and it is considered to affect the magnetization behavior of the Si-gradient steel sheet. The small eddy current loss of Si-gradient steel sheet can be explained as an effect of magnetic flux concentration on the surface layer.

  3. Pilot randomized trial of a volitional help sheet-based tool to increase leisure time physical activity in breast cancer survivors.

    PubMed

    Chapman, Janine; Fletcher, Chloe; Flight, Ingrid; Wilson, Carlene

    2018-05-16

    To develop and test a volitional help sheet-based tool to improve physical activity in breast cancer survivors compared to a standard self-generated implementation intention intervention. Pilot randomized trial conducted online over 3 months. Participants were randomized to an online volitional help sheet (n = 50) or implementation intention (n = 51) intervention. Measures were taken at baseline, 1 and 3 months. The main outcome measure was moderate-strenuous leisure time physical activity. Secondary outcomes were health-related quality of life and mood. Participants exposed to the volitional help sheet and implementation intention interventions showed similar effects after 1 month, with both groups reporting a significant increase in moderate-strenuous physical activity. After 3 months, the initial increase in physical activity was maintained by the volitional help sheet group, but not the implementation intention group. Improvements were also found for negative affect and emotional quality of life. While both interventions show promise in promoting physical activity in breast cancer survivors, the volitional help sheet may be more effective for facilitating lasting change and emotional well-being. Findings suggest that the volitional help sheet may have potential to offer a cost-effective contribution to consumer-led tertiary preventive health. Future research should test these initial findings in a definitive trial. Statement of contribution What is already known on this subject? Physical activity is important for optimizing health in breast cancer survivors. Despite this, physical activity in this cohort remains low. Theory-based strategies are needed to help breast cancer survivors independently manage and maintain regular physical activity over the long term. What does this study add? Online planning interventions can improve physical activity in breast cancer survivors. Volitional help sheets, but not implementation intentions, show sustained

  4. Development of the apparatus for measuring magnetic properties of electrical steel sheets in arbitrary directions under compressive stress normal to their surface

    NASA Astrophysics Data System (ADS)

    Maeda, Yoshitaka; Urata, Shinya; Nakai, Hideo; Takeuchi, Yuuya; Yun, Kyyoul; Yanase, Shunji; Okazaki, Yasuo

    2017-05-01

    In designing motors, one must grasp the magnetic properties of electrical steel sheets considering actual conditions in motors. Especially important is grasping the stress dependence of magnetic power loss. This paper describes a newly developed apparatus to measure two-dimensional (2-D) magnetic properties (properties under the arbitrary alternating and the rotating flux conditions) of electrical steel sheets under compressive stress normal to the sheet surface. The apparatus has a 2-D magnetic excitation circuit to generate magnetic fields in arbitrary directions in the evaluation area. It also has a pressing unit to apply compressive stress normal to the sheet surface. During measurement, it is important to apply uniform stress throughout the evaluation area. Therefore, we have developed a new flux density sensor using needle probe method. It is composed of thin copper foils sputtered on electrical steel sheets. By using this sensor, the stress can be applied to the surface of the specimen without influence of this sensor. This paper described the details of newly developed apparatus with this sensor, and measurement results of iron loss by using are shown.

  5. Litter Control Achievement - Ohio 4-H Club Score Sheet [and] Activity Guides 1 through 7. 4-H Pilot Program 918.

    ERIC Educational Resources Information Center

    Ohio State Univ., Columbus. Cooperative Extension Service.

    Seven activity guides, evaluation sheet, and club scoresheet have been prepared for Ohio 4-H clubs' litter education program. Topics of the seven activity guides include: (1) general guidelines and types of activities; (2) little known facts about waste/litter; (3) guidelines for a walking tour; (4) fact sheet (questionnaire) related to garbage;…

  6. New directions in the science and technology of advanced sheet explosive formulations and the key energetic materials used in the processing of sheet explosives: Emerging trends.

    PubMed

    Talawar, M B; Jangid, S K; Nath, T; Sinha, R K; Asthana, S N

    2015-12-30

    This review presents the work carried out by the international community in the area of sheet explosive formulations and its applications in various systems. The sheet explosive is also named as PBXs and is a composite material in which solid explosive particles like RDX, HMX or PETN are dispersed in a polymeric matrix, forms a flexible material that can be rolled/cut into sheet form which can be applied to any complex contour. The designed sheet explosive must possess characteristic properties such as flexible, cuttable, water proof, easily initiable, and safe handling. The sheet explosives are being used for protecting tanks (ERA), light combat vehicle and futuristic infantry carrier vehicle from different attacking war heads etc. Besides, sheet explosives find wide applications in demolition of bridges, ships, cutting and metal cladding. This review also covers the aspects such as risks and hazard analysis during the processing of sheet explosive formulations, effect of ageing on sheet explosives, detection and analysis of sheet explosive ingredients and the R&D efforts of Indian researchers in the development of sheet explosive formulations. To the best of our knowledge, there has been no review article published in the literature in the area of sheet explosives. Copyright © 2015 Elsevier B.V. All rights reserved.

  7. Emittance Measurements for a Thin Liquid Sheet Flow

    NASA Technical Reports Server (NTRS)

    Englehart, Amy N.; McConley, Marc W.; Chubb, Donald L.

    1996-01-01

    The Liquid Sheet Radiator (LSR) is an external flow radiator that uses a triangular-shaped flowing liquid sheet as the radiating surface. It has potentially much lower mass than solid wall radiators such as pumped loop and heat pipe radiators, along with being nearly immune to micrometeoroid penetration. The LSR has an added advantage of simplicity. Surface tension causes a thin (100-300 microns) liquid sheet to coalesce to a point, causing the sheet flow to have a triangular shape. Such a triangular sheet is desirable since it allows for simple collection of the flow at a single point. A major problem for all external flow radiators is the requirement that the working fluid be of very low (approx. 10(sup -8) torr) vapor pressure to keep evaporative losses low. As a result, working fluids are limited to certain oils (such as used in diffusion pumps) for low temperatures (300-400 K) and liquid metals for higher temperatures. Previous research on the LSR has been directed at understanding the fluid mechanics of thin sheet flows and assessing the stability of such flows, especially with regard to the formation of holes in the sheet. Taylor studied extensively the stability of thin liquid sheets both theoretically and experimentally. He showed that thin sheets in a vacuum are stable. The latest research has been directed at determining the emittance of thin sheet flows. The emittance was calculated from spectral transmittance data for the Dow Corning 705 silicone oil. By experimentally setting up a sheet flow, the emittance was also determined as a function of measurable quantities, most importantly, the temperature drop between the top of the sheet and the temperature at the coalescence point of the sheet. Temperature fluctuations upstream of the liquid sheet were a potential problem in the analysis and were investigated.

  8. Imaging a seizure model in zebrafish with structured illumination light sheet microscopy

    NASA Astrophysics Data System (ADS)

    Liu, Yang; Dale, Savannah; Ball, Rebecca; VanLeuven, Ariel J.; Baraban, Scott; Sornborger, Andrew; Lauderdale, James D.; Kner, Peter

    2018-02-01

    Zebrafish are a promising vertebrate model for elucidating how neural circuits generate behavior under normal and pathological conditions. The Baraban group first demonstrated that zebrafish larvae are valuable for investigating seizure events and can be used as a model for epilepsy in humans. Because of their small size and transparency, zebrafish embryos are ideal for imaging seizure activity using calcium indicators. Light-sheet microscopy is well suited to capturing neural activity in zebrafish because it is capable of optical sectioning, high frame rates, and low excitation intensities. We describe work in our lab to use light-sheet microscopy for high-speed long-time imaging of neural activity in wildtype and mutant zebrafish to better understand the connectivity and activity of inhibitory neural networks when GABAergic signaling is altered in vivo. We show that, with light-sheet microscopy, neural activity can be recorded at 23 frames per second in twocolors for over 10 minutes allowing us to capture rare seizure events in mutants. We have further implemented structured illumination to increase resolution and contrast in the vertical and axial directions during high-speed imaging at an effective frame rate of over 7 frames per second.

  9. The Effective Width of Curved Sheet After Buckling

    NASA Technical Reports Server (NTRS)

    Wenzek, W A

    1938-01-01

    This report describes experiments made for the purpose of ascertaining the effective width of circularly curved sheet under pure flexural stress. A relation for the effective width of curved sheets is established. Experiments were made with circular cylinders compressed in longitudinal direction. The sheets were rigidly built in at the sides parallel to the axis of the cylinder.

  10. A comparison of coronal and interplanetary current sheet inclinations

    NASA Technical Reports Server (NTRS)

    Behannon, K. W.; Burlaga, L. F.; Hundhausen, A. J.

    1983-01-01

    The HAO white light K-coronameter observations show that the inclination of the heliospheric current sheet at the base of the corona can be both large (nearly vertical with respect to the solar equator) or small during Cararington rotations 1660 - 1666 and even on a single solar rotation. Voyager 1 and 2 magnetic field observations of crossing of the heliospheric current sheet at distances from the Sun of 1.4 and 2.8 AU. Two cases are considered, one in which the corresponding coronameter data indicate a nearly vertical (north-south) current sheet and another in which a nearly horizontal, near equatorial current sheet is indicated. For the crossings of the vertical current sheet, a variance analysis based on hour averages of the magnetic field data gave a minimum variance direction consistent with a steep inclination. The horizontal current sheet was observed by Voyager as a region of mixed polarity and low speeds lasting several days, consistent with multiple crossings of a horizontal but irregular and fluctuating current sheet at 1.4 AU. However, variance analysis of individual current sheet crossings in this interval using 1.92 see averages did not give minimum variance directions consistent with a horizontal current sheet.

  11. Endogenous Sheet-Averaged Tension Within a Large Epithelial Cell Colony.

    PubMed

    Dumbali, Sandeep P; Mei, Lanju; Qian, Shizhi; Maruthamuthu, Venkat

    2017-10-01

    Epithelial cells form quasi-two-dimensional sheets that function as contractile media to effect tissue shape changes during development and homeostasis. Endogenously generated intrasheet tension is a driver of such changes, but has predominantly been measured in the presence of directional migration. The nature of epithelial cell-generated forces transmitted over supracellular distances, in the absence of directional migration, is thus largely unclear. In this report, we consider large epithelial cell colonies which are archetypical multicell collectives with extensive cell-cell contacts but with a symmetric (circular) boundary. Using the traction force imbalance method (TFIM) (traction force microscopy combined with physical force balance), we first show that one can determine the colony-level endogenous sheet forces exerted at the midline by one half of the colony on the other half with no prior assumptions on the uniformity of the mechanical properties of the cell sheet. Importantly, we find that this colony-level sheet force exhibits large variations with orientation-the difference between the maximum and minimum sheet force is comparable to the average sheet force itself. Furthermore, the sheet force at the colony midline is largely tensile but the shear component exhibits significantly more variation with orientation. We thus show that even an unperturbed epithelial colony with a symmetric boundary shows significant directional variation in the endogenous sheet tension and shear forces that subsist at the colony level.

  12. Plasma Sheet Circulation Pathways

    NASA Technical Reports Server (NTRS)

    Moore, Thomas E.; Delcourt, D. C.; Slinker, S. P.; Fedder, J. A.; Damiano, P.; Lotko, W.

    2008-01-01

    Global simulations of Earth's magnetosphere in the solar wind compute the pathways of plasma circulation through the plasma sheet. We address the pathways that supply and drain the plasma sheet, by coupling single fluid simulations with Global Ion Kinetic simulations of the outer magnetosphere and the Comprehensive Ring Current Model of the inner magnetosphere, including plasmaspheric plasmas. We find that the plasma sheet is supplied with solar wind plasmas via the magnetospheric flanks, and that this supply is most effective for northward IMF. For southward IMF, the innermost plasma sheet and ring current region are directly supplied from the flanks, with an asymmetry of single particle entry favoring the dawn flank. The central plasma sheet (near midnight) is supplied, as expected, from the lobes and polar cusps, but the near-Earth supply consists mainly of slowly moving ionospheric outflows for typical conditions. Work with the recently developed multi-fluid LFM simulation shows transport via plasma "fingers" extending Earthward from the flanks, suggestive of an interchange instability. We investigate this with solar wind ion trajectories, seeking to understand the fingering mechanisms and effects on transport rates.

  13. Polycrystalline silicon sheets for solar cells by the spinning method

    NASA Astrophysics Data System (ADS)

    Maeda, Y.; Yokoyama, T.; Hide, I.

    1984-03-01

    A new method has been developed in which polycrystalline silicon sheets are formed directly from molten silicon on a spinning wheel. The sheet is 5 cm x 5 cm, 0.1-0.5 mm thick, and made at a rate of four sheets per 15 s; power conversion rate of a solar cell assembled with these silicon sheets is more than 10 percent.

  14. kW-class direct diode laser for sheet metal cutting based on commercial pump modules

    NASA Astrophysics Data System (ADS)

    Witte, U.; Schneider, F.; Holly, C.; Di Meo, A.; Rubel, D.; Boergmann, F.; Traub, M.; Hoffmann, D.; Drovs, S.; Brand, T.; Unger, A.

    2017-02-01

    We present a direct diode laser with an optical output power of more than 800 W ex 100 μm with an NA of 0.17. The system is based on 6 commercial pump modules that are wavelength stabilized by use of VBGs. Dielectric filters are used for coarse and dense wavelength multiplexing. Metal sheet cutting tests were performed in order to prove system performance and reliability. Based on a detailed analysis of loss mechanisms, we show that the design can be easily scaled to output powers in the range of 2 kW and to an optical efficiency of 80%.

  15. Lysine-Based Site-Directed Mutagenesis Increased Rigid β-Sheet Structure and Thermostability of Mesophilic 1,3-1,4-β-Glucanase.

    PubMed

    Niu, Chengtuo; Zhu, Linjiang; Zhu, Pei; Li, Qi

    2015-06-03

    1,3-1,4-β-Glucanase is widely applied in the food industry, while its low thermostability often reduces its performance. In a previous study, chemical modification of surface lysine residues was proved to increase the thermostability of β-glucanase. To improve the thermostability, the mesophilic β-glucanase from Bacillus terquilensis was rationally engineered through site-directed mutagenesis of the 12 lysines into serines. The results showed that the K20S, K117S, and K165S mutants could both enhance the specific activities and thermostability of β-glucanase. The triple mutant (K20S/K117S/K165S) could increase the optimal temperature and T50 value by 15 and 14 °C, respectively. Five percent more structured residues were observed in the mutant, which formed new β-sheet structures in the concave side. Molecular dynamics simulation analysis showed that the flexibility in the mutation regions was decreased, which resulted in the overall rigidity of the β-glucanase. Therefore, the lysine-based site-directed mutagenesis is a simple and effective method for improving the thermostability of β-glucanase.

  16. Predicting Hot Deformation of AA5182 Sheet

    NASA Astrophysics Data System (ADS)

    Lee, John T.; Carpenter, Alexander J.; Jodlowski, Jakub P.; Taleff, Eric M.

    Aluminum 5000-series alloy sheet materials exhibit substantial ductilities at hot and warm temperatures, even when grain size is not particularly fine. The relatively high strain-rate sensitivity exhibited by these non-superplastic materials, when deforming under solute-drag creep, is a primary contributor to large tensile ductilities. This active deformation mechanism influences both plastic flow and microstructure evolution across conditions of interest for hot- and warm-forming. Data are presented from uniaxial tensile and biaxial bulge tests of AA5182 sheet material at elevated temperatures. These data are used to construct a material constitutive model for plastic flow, which is applied in finite-element-method (FEM) simulations of plastic deformation under multiaxial stress states. Simulation results are directly compared against experimental data to explore the usefulness of this constitutive model. The effects of temperature and stress state on plastic response and microstructure evolution are discussed.

  17. Visible-light promoted catalytic activity of dumbbell-like Au nanorods supported on graphene/TiO2 sheets towards hydrogenation reaction.

    PubMed

    Dai, Yunqian; Zhu, Mingyun; Wang, Xiaotian; Wu, Yanan; Huang, Chengqian; Fu, Wanlin; Meng, Xiangyu; Sun, Yueming

    2018-06-15

    In this work, the rationally-designed sharp corners on Au nanorods tremendously improved the catalytic activity, particularly in the presence of visible light irradiation, towards the hydrogenation of 4-nitrophenol to 4-aminophenol. A strikingly increased rate constant of 50.6 g -1 s -1 L was achieved in M-Au-3, which was 41.8 times higher than that of parent Au nanorods under dark conditions. The enhanced activities were proportional to the extent of the protruding sharp corners. Furthermore, remarkably enhanced activities were achieved in novel ternary Au/RGO/TiO 2 sheets, which were endowed with a 52.0 times higher rate constant than that of straight Au nanorods. These remarkably enhanced activities were even higher than those of previously reported 3-5 nm Au and 3 nm Pt nanoparticles. It was systematically observed that there are three aspects to the synergistic effects between Au and RGO sheets: (i) electron transfer from RGO to Au, (ii) a high concentration of p-nitrophenol close to dumbbell-like Au nanorods on RGO sheets, and (iii) increased local reaction temperature from the photothermal effect of both dumbbell-like Au nanorods and RGO sheets.

  18. Visible-light promoted catalytic activity of dumbbell-like Au nanorods supported on graphene/TiO2 sheets towards hydrogenation reaction

    NASA Astrophysics Data System (ADS)

    Dai, Yunqian; Zhu, Mingyun; Wang, Xiaotian; Wu, Yanan; Huang, Chengqian; Fu, Wanlin; Meng, Xiangyu; Sun, Yueming

    2018-06-01

    In this work, the rationally-designed sharp corners on Au nanorods tremendously improved the catalytic activity, particularly in the presence of visible light irradiation, towards the hydrogenation of 4-nitrophenol to 4-aminophenol. A strikingly increased rate constant of 50.6 g‑1 s‑1 L was achieved in M-Au-3, which was 41.8 times higher than that of parent Au nanorods under dark conditions. The enhanced activities were proportional to the extent of the protruding sharp corners. Furthermore, remarkably enhanced activities were achieved in novel ternary Au/RGO/TiO2 sheets, which were endowed with a 52.0 times higher rate constant than that of straight Au nanorods. These remarkably enhanced activities were even higher than those of previously reported 3–5 nm Au and 3 nm Pt nanoparticles. It was systematically observed that there are three aspects to the synergistic effects between Au and RGO sheets: (i) electron transfer from RGO to Au, (ii) a high concentration of p-nitrophenol close to dumbbell-like Au nanorods on RGO sheets, and (iii) increased local reaction temperature from the photothermal effect of both dumbbell-like Au nanorods and RGO sheets.

  19. Structure of the Magnetotail Current Sheet

    NASA Technical Reports Server (NTRS)

    Larson, Douglas J.; Kaufmann, Richard L.

    1996-01-01

    An orbit tracing technique was used to generate current sheets for three magnetotail models. Groups of ions were followed to calculate the resulting cross-tail current. Several groups then were combined to produce a current sheet. The goal is a model in which the ions and associated electrons carry the electric current distribution needed to generate the magnetic field B in which ion orbits were traced. The region -20 R(sub E) less than x less than - 14 R(sub E) in geocentric solar magnetospheric coordinates was studied. Emphasis was placed on identifying the categories of ion orbits which contribute most to the cross-tail current and on gaining physical insight into the manner by which the ions carry the observed current distribution. Ions that were trapped near z = 0, ions that magnetically mirrored throughout the current sheet, and ions that mirrored near the Earth all were needed. The current sheet structure was determined primarily by ion magnetization currents. Electrons of the observed energies carried relatively little cross-tail current in these quiet time current sheets. Distribution functions were generated and integrated to evaluate fluid parameters. An earlier model in which B depended only on z produced a consistent current sheet, but it did not provide a realistic representation of the Earth's middle magnetotail. In the present study, B changed substantially in the x and z directions but only weakly in the y direction within our region of interest. Plasmas with three characteristic particle energies were used with each of the magnetic field models. A plasma was found for each model in which the density, average energy, cross-tail current, and bulk flow velocity agreed well with satellite observations.

  20. Structure of the Magnetotail Current Sheet

    NASA Technical Reports Server (NTRS)

    Larson, Douglas J.; Kaufmann, Richard L.

    1996-01-01

    An orbit tracing technique was used to generate current sheets for three magnetotail models. Groups of ions were followed to calculate the resulting cross-tail current. Several groups then were combined to produce a current sheet. The goal is a model in which the ions and associated electrons carry the electric current distribution needed to generate the magnetic field B in which ion orbits were traced. The region -20 R(E) less than x less than -14 R(E) in geocentric solar magnetospheric coordinates was studied. Emphasis was placed on identifying the categories of ion orbits which contribute most to the cross-tail current and on gaining physical insight into the manner by which the ions carry the observed current distribution. Ions that were trapped near z = 0, ions that magnetically mirrored throughout the current sheet, and ions that mirrored near the Earth all were needed. The current sheet structure was determined primarily by ion magnetization currents. Electrons of the observed energies carried relatively little cross-tail current in these quiet time current sheets. Distribution functions were generated and integrated to evaluate fluid parameters. An earlier model in which B depended only on z produced a consistent current sheet, but it did not provide a realistic representation of the Earth's middle magnetotail. In the present study, B changed substantially in the x and z directions but only weakly in the y direction within our region of interest. Plasmas with three characteristic particle energies were used with each of the magnetic field models. A plasma was found for each model in which the density, average energy, cross-tail current, and bulk flow velocity agreed well with satellite observations.

  1. Ice_Sheets_CCI: Essential Climate Variables for the Greenland Ice Sheet

    NASA Astrophysics Data System (ADS)

    Forsberg, R.; Sørensen, L. S.; Khan, A.; Aas, C.; Evansberget, D.; Adalsteinsdottir, G.; Mottram, R.; Andersen, S. B.; Ahlstrøm, A.; Dall, J.; Kusk, A.; Merryman, J.; Hvidberg, C.; Khvorostovsky, K.; Nagler, T.; Rott, H.; Scharrer, M.; Shepard, A.; Ticconi, F.; Engdahl, M.

    2012-04-01

    As part of the ESA Climate Change Initiative (www.esa-cci.org) a long-term project "ice_sheets_cci" started January 1, 2012, in addition to the existing 11 projects already generating Essential Climate Variables (ECV) for the Global Climate Observing System (GCOS). The "ice_sheets_cci" goal is to generate a consistent, long-term and timely set of key climate parameters for the Greenland ice sheet, to maximize the impact of European satellite data on climate research, from missions such as ERS, Envisat and the future Sentinel satellites. The climate parameters to be provided, at first in a research context, and in the longer perspective by a routine production system, would be grids of Greenland ice sheet elevation changes from radar altimetry, ice velocity from repeat-pass SAR data, as well as time series of marine-terminating glacier calving front locations and grounding lines for floating-front glaciers. The ice_sheets_cci project will involve a broad interaction of the relevant cryosphere and climate communities, first through user consultations and specifications, and later in 2012 optional participation in "best" algorithm selection activities, where prototype climate parameter variables for selected regions and time frames will be produced and validated using an objective set of criteria ("Round-Robin intercomparison"). This comparative algorithm selection activity will be completely open, and we invite all interested scientific groups with relevant experience to participate. The results of the "Round Robin" exercise will form the algorithmic basis for the future ECV production system. First prototype results will be generated and validated by early 2014. The poster will show the planned outline of the project and some early prototype results.

  2. Thermoelectric properties of single-layered SnSe sheet.

    PubMed

    Wang, Fancy Qian; Zhang, Shunhong; Yu, Jiabing; Wang, Qian

    2015-10-14

    Motivated by the recent study of inspiring thermoelectric properties in bulk SnSe [Zhao et al., Nature, 2014, 508, 373] and the experimental synthesis of SnSe sheets [Chen et al., J. Am. Chem. Soc., 2013, 135, 1213], we have carried out systematic calculations for a single-layered SnSe sheet focusing on its stability, electronic structure and thermoelectric properties by using density functional theory combined with Boltzmann transport theory. We have found that the sheet is dynamically and thermally stable with a band gap of 1.28 eV, and the figure of merit (ZT) reaches 3.27 (2.76) along the armchair (zigzag) direction with optimal n-type carrier concentration, which is enhanced nearly 7 times compared to its bulk counterpart at 700 K due to quantum confinement effect. Furthermore, we designed four types of thermoelectric couples by assembling single-layered SnSe sheets with different transport directions and doping types, and found that their efficiencies are all above 13%, which are higher than those of thermoelectric couples made of commercial bulk Bi2Te3 (7%-8%), suggesting the great potential of single-layered SnSe sheets for heat-electricity conversion.

  3. A Synthesis of the Basal Thermal State of the Greenland Ice Sheet

    NASA Technical Reports Server (NTRS)

    Macgregor, J. A.; Fahnestock, M. A.; Catania, G. A.; Aschwanden, A.; Clow, G. D.; Colgan, W. T.; Gogineni, S. P.; Morlighem, M.; Nowicki, S. M. J.; Paden, J. D.; hide

    2016-01-01

    Greenland's thick ice sheet insulates the bedrock below from the cold temperatures at the surface, so the bottom of the ice is often tens of degrees warmer than at the top, because the ice bottom is slowly warmed by heat coming from the Earth's depths. Knowing whether Greenland's ice lies on wet, slippery ground or is anchored to dry, frozen bedrock is essential for predicting how this ice will flow in the future. But scientists have very few direct observations of the thermal conditions beneath the ice sheet, obtained through fewer than two dozen boreholes that have reached the bottom. Our study synthesizes several independent methods to infer the Greenland Ice Sheet's basal thermal state -whether the bottom of the ice is melted or not-leading to the first map that identifies frozen and thawed areas across the whole ice sheet. This map will guide targets for future investigations of the Greenland Ice Sheet toward the most vulnerable and poorly understood regions, ultimately improving our understanding of its dynamics and contribution to future sea-level rise. It is of particular relevance to ongoing Operation IceBridge activities and future large-scale airborne missions over Greenland.

  4. Development of a check sheet for collecting information necessary for occupational safety and health activities and building relevant systems in overseas business places.

    PubMed

    Kajiki, Shigeyuki; Kobayashi, Yuichi; Uehara, Masamichi; Nakanishi, Shigemoto; Mori, Koji

    2016-06-07

    This study aimed to develop an information gathering check sheet to efficiently collect information necessary for Japanese companies to build global occupational safety and health management systems in overseas business places. The study group consisted of 2 researchers with occupational physician careers in a foreign-affiliated company in Japan and 3 supervising occupational physicians who were engaged in occupational safety and health activities in overseas business places. After investigating information and sources of information necessary for implementing occupational safety and health activities and building relevant systems, we conducted information acquisition using an information gathering check sheet in the field, by visiting 10 regions in 5 countries (first phase). The accuracy of the information acquired and the appropriateness of the information sources were then verified in study group meetings to improve the information gathering check sheet. Next, the improved information gathering check sheet was used in another setting (3 regions in 1 country) to confirm its efficacy (second phase), and the information gathering check sheet was thereby completed. The information gathering check sheet was composed of 9 major items (basic information on the local business place, safety and health overview, safety and health systems, safety and health staff, planning/implementation/evaluation/improvement, safety and health activities, laws and administrative organs, local medical care systems and public health, and medical support for resident personnel) and 61 medium items. We relied on the following eight information sources: the internet, company (local business place and head office in Japan), embassy/consulate, ISO certification body, university or other educational institutions, and medical institutions (aimed at Japanese people or at local workers). Through multiple study group meetings and a two-phased field survey (13 regions in 6 countries), an information

  5. Ice sheet radar altimetry

    NASA Technical Reports Server (NTRS)

    Zwally, J.

    1988-01-01

    The surface topography of the Greenland and Antarctic ice sheets between 72 degrees north and south was mapped using radar altimetry data from the U.S. Navy GEOSAT. The glaciological objectives of this activity were to study the dynamics of the ice flow, changes in the position of floating ice-shelf fronts, and ultimately to measure temporal changes in ice surface elevation indicative of ice sheet mass balance.

  6. Electromagnetic augmentation for casting of thin metal sheets

    DOEpatents

    Hull, J.R.

    1987-10-28

    Thin metal sheets are cast by magnetically levitating molten metal deposited in a model within a ferromagnetic yoke and between AC conducting coils and linearly displacing the magnetically levitated liquid metal while it is being cooled by the water-cooled walls of the mold to form a solid metal sheet. A conducting shield is electrically coupled to the molten metal sheet to provide a return path for eddy currents induced in the metal sheet by the current in the AC conducting coils. In another embodiment, a DC conducting coil is coupled to the metal sheet for providing a direct current therein which interacts with the magnetic field to levitate the moving metal sheet. Levitation of the metal sheet in both molten and solid forms reduces its contact pressure with the mold walls while maintaining sufficient engagement therebetween to permit efficient conductive cooling by the mold through which a coolant fluid may be circulated. 8 figs.

  7. Multiple-satellite studies of magnetospheric substorms: Plasma sheet recovery and the poleward leap of auroral-zone activity

    NASA Technical Reports Server (NTRS)

    Pytte, T.; Mcpherron, R. L.; Kivelson, M. G.; West, H. I., Jr.; Hones, E. W., Jr.

    1977-01-01

    Particle observations from pairs of satellites (Ogo 5, Vela 4A and 5B, Imp 3) during the recovery of plasma sheet thickness late in substorms were examined. Six of the nine events occurred within about 5 min in locations near the estimated position of the neutral sheet, but over wide ranges of east-west and radial separations. The time of occurrence and spatial extent of the recovery were related to the onset (defined by ground Pi 2 pulsations) and approximate location (estimated from ground mid-latitude magnetic signatures) of substorm expansions. It was found that the plasma sheet recovery occurred 10 - 30 min after the last in a series of Pi bursts, which were interpreted to indicate that the recovery was not due directly to a late, high latitude substorm expansion. The recovery was also observed to occur after the substorm current wedge had moved into the evening sector and to extend far to the east of the center of the last preceding substorm expansion.

  8. TSCA Chemical Data Reporting Fact Sheet: Reporting Manufactured Chemical Substances from Metal Mining and Related Activities

    EPA Pesticide Factsheets

    This fact sheet provides guidance on the Chemical Data Reporting (CDR) rule requirements related to the reporting of mined metals, intermediates, and byproducts manufactured during metal mining and related activities.

  9. Fluctuation dynamics in reconnecting current sheets

    NASA Astrophysics Data System (ADS)

    von Stechow, Adrian; Grulke, Olaf; Ji, Hantao; Yamada, Masaaki; Klinger, Thomas

    2015-11-01

    During magnetic reconnection, a highly localized current sheet forms at the boundary between opposed magnetic fields. Its steep perpendicular gradients and fast parallel drifts can give rise to a range of instabilities which can contribute to the overall reconnection dynamics. In two complementary laboratory reconnection experiments, MRX (PPPL, Princeton) and VINETA.II (IPP, Greifswald, Germany), magnetic fluctuations are observed within the current sheet. Despite the large differences in geometries (toroidal vs. linear), plasma parameters (high vs. low beta) and magnetic configuration (low vs. high magnetic guide field), similar broadband fluctuation characteristics are observed in both experiments. These are identified as Whistler-like fluctuations in the lower hybrid frequency range that propagate along the current sheet in the electron drift direction. They are intrinsic to the localized current sheet and largely independent of the slower reconnection dynamics. This contribution characterizes these magnetic fluctuations within the wide parameter range accessible by both experiments. Specifically, the fluctuation spectra and wave dispersion are characterized with respect to the magnetic topology and plasma parameters of the reconnecting current sheet.

  10. Linear Tidal Vestige Found in the WM Sheet

    NASA Astrophysics Data System (ADS)

    Lee, Jounghun; Kim, Suk; Rey, Soo-Chang

    2018-06-01

    We present a vestige of the linear tidal influence on the spin orientations of the constituent galaxies of the WM sheet discovered in the vicinity of the Virgo Cluster and the Local Void. The WM sheet is chosen as an optimal target since it has a rectangular parallelepiped-like shape whose three sides are in parallel with the supergalactic Cartesian axes. Determining three probability density functions of the absolute values of the supergalactic Cartesian components of the spin vectors of the WM sheet galaxies, we investigate their alignments with the principal directions of the surrounding large-scale tidal field. When the WM sheet galaxies located in the central region within the distance of 2 h ‑1 Mpc are excluded, the spin vectors of the remaining WM sheet galaxies are found to be weakly aligned, strongly aligned, and strongly anti-aligned with the minor, intermediate, and major principal directions of the surrounding large-scale tidal field, respectively. To examine whether or not the origin of the observed alignment tendency from the WM sheet is the linear tidal effect, we infer the eigenvalues of the linear tidal tensor from the axial ratios of the WM sheet with the help of the Zeldovich approximation and conduct a full analytic evaluation of the prediction of the linear tidal torque model for the three probability density functions. A detailed comparison between the analytical and the observational results reveals a good quantitative agreement not only in the behaviors but also in the amplitudes of the three probability density functions.

  11. Modelling the effects of ice-sheet activity on CO2 outgassing by Icelandic volcanoes

    NASA Astrophysics Data System (ADS)

    Armitage, J. J.; Ferguson, D.; Petersen, K. D.; Creyts, T. T.

    2017-12-01

    Glacial cycles may play a significant role in mediating the flux of magmatic CO2 between the Earth's mantle and atmosphere. In Iceland, it is thought that late-Pleistocene deglaciation led to a significant volcanic pulse, evidenced by increased post-glacial lava volumes and changes in melt chemistry consistent with depressurization. Investigating the extent to which glacial activity may have affected volcanic CO2 emissions from Iceland, and crucially over what timescale, requires detailed knowledge of how the magma system responded to the growth and collapse of the ice-sheet before and after the LGM. To investigate this, we coupled a model of magma generation and transport with a history of ice-sheet activity. Our results show that the emplacement and removal of the LGM ice-sheet likely led to two significant pulses of magmatic CO2. The first, and most significant of these, is associated with ice-sheet growth and occurs as the magma system recovers from glacial loading. This recovery happens from the base of the melting region upwards, producing a pulse of CO2 rich magma that is predicted to reach the surface around 20 ka after the loading event, close in time to the LGM. The second peak in CO2 output occurs abruptly following deglaciation as a consequence of increased rates of melt generation and transport in the shallow mantle. Although these post-glacial melts are relatively depleted in CO2, the increase in magma flux leads to a short-lived period of elevated CO2 emissions. Our results therefore suggest a negative feedback, whereby ice-sheet growth produces a delayed pulse of magmatic CO2, which, in addition to increased geothermal heat flux, may contribute towards driving deglaciation, which itself then causes further magmatism and CO2 outgassing. This model is consistent with the seismic structure of the asthenosphere below Iceland, and the established compositional and volumetric trends for sub- and post-glacial volcanism in Iceland. These trends show that

  12. Dynamo-driven plasmoid formation from a current-sheet instability

    DOE PAGES

    Ebrahimi, F.

    2016-12-15

    Axisymmetric current-carrying plasmoids are formed in the presence of nonaxisymmetric fluctuations during nonlinear three-dimensional resistive MHD simulations in a global toroidal geometry. In this study, we utilize the helicity injection technique to form an initial poloidal flux in the presence of a toroidal guide field. As helicity is injected, two types of current sheets are formed from the oppositely directed field lines in the injector region (primary reconnecting current sheet), and the poloidal flux compression near the plasma edge (edge current sheet). We first find that nonaxisymmetric fluctuations arising from the current-sheet instability isolated near the plasma edge have tearingmore » parity but can nevertheless grow fast (on the poloidal Alfven time scale). These modes saturate by breaking up the current sheet. Second, for the first time, a dynamo poloidal flux amplification is observed at the reconnection site (in the region of the oppositely directed magnetic field). This fluctuation-induced flux amplification increases the local Lundquist number, which then triggers a plasmoid instability and breaks the primary current sheet at the reconnection site. Finally, the plasmoids formation driven by large-scale flux amplification, i.e., a large-scale dynamo, observed here has strong implications for astrophysical reconnection as well as fast reconnection events in laboratory plasmas.« less

  13. The Jovian magnetotail and its current sheet

    NASA Technical Reports Server (NTRS)

    Behannon, K. W.; Burlaga, L. F.; Ness, N. F.

    1980-01-01

    Analyses of Voyager magnetic field measurements have extended the understanding of the structural and temporal characteristics of Jupiter's magnetic tail. The magnitude of the magnetic field in the lobes of the tail is found to decrease with Jovicentric distance approximately as r to he-1.4, compared with the power law exponent of -1.7 found for the rate of decrease along the Pioneer 10 outbound trajectory. Voyager observations of magnetic field component variations with Jovicentric distance in the tail do not support the uniform radial plasma outflow model derived from Pioneer data. Voyager 2 has shown that the azimuthal current sheet which surrounds Jupiter in the inner and middle magnetosphere extends tailward (in the anti-Sun direction) to a distance of at least 100 R sub J. In the tail this current sheet consists of a plasma sheet and embedded neutral sheet. In the region of the tail where the sheet is observed, the variation of the magnetic field as a result of the sheet structure and its 10 hr periodic motion is the dominant variation seen.

  14. Magma transport in sheet intrusions of the Alnö carbonatite complex, central Sweden.

    PubMed

    Andersson, Magnus; Almqvist, Bjarne S G; Burchardt, Steffi; Troll, Valentin R; Malehmir, Alireza; Snowball, Ian; Kübler, Lutz

    2016-06-10

    Magma transport through the Earth's crust occurs dominantly via sheet intrusions, such as dykes and cone-sheets, and is fundamental to crustal evolution, volcanic eruptions and geochemical element cycling. However, reliable methods to reconstruct flow direction in solidified sheet intrusions have proved elusive. Anisotropy of magnetic susceptibility (AMS) in magmatic sheets is often interpreted as primary magma flow, but magnetic fabrics can be modified by post-emplacement processes, making interpretation of AMS data ambiguous. Here we present AMS data from cone-sheets in the Alnö carbonatite complex, central Sweden. We discuss six scenarios of syn- and post-emplacement processes that can modify AMS fabrics and offer a conceptual framework for systematic interpretation of magma movements in sheet intrusions. The AMS fabrics in the Alnö cone-sheets are dominantly oblate with magnetic foliations parallel to sheet orientations. These fabrics may result from primary lateral flow or from sheet closure at the terminal stage of magma transport. As the cone-sheets are discontinuous along their strike direction, sheet closure is the most probable process to explain the observed AMS fabrics. We argue that these fabrics may be common to cone-sheets and an integrated geology, petrology and AMS approach can be used to distinguish them from primary flow fabrics.

  15. Magma transport in sheet intrusions of the Alnö carbonatite complex, central Sweden

    PubMed Central

    Andersson, Magnus; Almqvist, Bjarne S. G.; Burchardt, Steffi; Troll, Valentin R.; Malehmir, Alireza; Snowball, Ian; Kübler, Lutz

    2016-01-01

    Magma transport through the Earth’s crust occurs dominantly via sheet intrusions, such as dykes and cone-sheets, and is fundamental to crustal evolution, volcanic eruptions and geochemical element cycling. However, reliable methods to reconstruct flow direction in solidified sheet intrusions have proved elusive. Anisotropy of magnetic susceptibility (AMS) in magmatic sheets is often interpreted as primary magma flow, but magnetic fabrics can be modified by post-emplacement processes, making interpretation of AMS data ambiguous. Here we present AMS data from cone-sheets in the Alnö carbonatite complex, central Sweden. We discuss six scenarios of syn- and post-emplacement processes that can modify AMS fabrics and offer a conceptual framework for systematic interpretation of magma movements in sheet intrusions. The AMS fabrics in the Alnö cone-sheets are dominantly oblate with magnetic foliations parallel to sheet orientations. These fabrics may result from primary lateral flow or from sheet closure at the terminal stage of magma transport. As the cone-sheets are discontinuous along their strike direction, sheet closure is the most probable process to explain the observed AMS fabrics. We argue that these fabrics may be common to cone-sheets and an integrated geology, petrology and AMS approach can be used to distinguish them from primary flow fabrics. PMID:27282420

  16. Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets

    NASA Astrophysics Data System (ADS)

    Heister, Anton; Scheiber, Rolf

    2017-04-01

    Conventional processing of ice-sounder data produces 2-D images of the ice sheet and bed, where the two dimensions are along-track and depth, while the across-track direction is fixed to nadir. The 2-D images contain information about the topography and radar reflectivity of the ice sheet's surface, bed, and internal layers in the along-track direction. Having multiple antenna phase centers in the across-track direction enables the production of 3-D images of the ice sheet and bed. Compared to conventional 2-D images, these contain additional information about the surface and bed topography, and orientation of the internal layers over a swath in the across-track direction. We apply a 3-D SAR tomographic ice-sounding method based on sparse signal reconstruction [1] to the data collected by Center for Remote Sensing of Ice Sheets (CReSIS) in 2008 in Greenland [2] using their multichannel coherent radar depth sounder (MCoRDS). The MCoRDS data have 16 effective phase centers which allows us to better understand the performance of the method. Lastly we offer sparsity improvement by including wavelet dictionaries into the reconstruction.The results show improved scene feature resolvability in across-track direction compared to MVDR beamformer. References: [1] A. Heister, R. Scheiber, "First Analysis of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets". In: Proceedings of EUSAR, pp. 788-791, June 2016. [2] X. Wu, K. C. Jezek, E. Rodriguez, S. Gogineni, F. Rodriguez-Morales, and A. Freeman, "Ice sheet bed mapping with airborne SAR tomography". IEEE Transactions on Geoscience and Remote Sensing, vol. 49, no. 10 Part 1, pp. 3791-3802, 2011.

  17. Collisionless current sheet equilibria

    NASA Astrophysics Data System (ADS)

    Neukirch, T.; Wilson, F.; Allanson, O.

    2018-01-01

    Current sheets are important for the structure and dynamics of many plasma systems. In space and astrophysical plasmas they play a crucial role in activity processes, for example by facilitating the release of magnetic energy via processes such as magnetic reconnection. In this contribution we will focus on collisionless plasma systems. A sensible first step in any investigation of physical processes involving current sheets is to find appropriate equilibrium solutions. The theory of collisionless plasma equilibria is well established, but over the past few years there has been a renewed interest in finding equilibrium distribution functions for collisionless current sheets with particular properties, for example for cases where the current density is parallel to the magnetic field (force-free current sheets). This interest is due to a combination of scientific curiosity and potential applications to space and astrophysical plasmas. In this paper we will give an overview of some of the recent developments, discuss their potential applications and address a number of open questions.

  18. Structurally Oriented Nano-Sheets in Co Thin Films: Changing Their Anisotropic Physical Properties by Thermally-Induced Relaxation

    PubMed Central

    Vergara, José; Favieres, Cristina; Magén, César; de Teresa, José María; Ibarra, Manuel Ricardo

    2017-01-01

    We show how nanocrystalline Co films formed by separated oblique nano-sheets display anisotropy in their resistivity, magnetization process, surface nano-morphology and optical transmission. After performing a heat treatment at 270 °C, these anisotropies decrease. This loss has been monitored measuring the resistivity as a function of temperature. The resistivity measured parallel to the direction of the nano-sheets has been constant up to 270 °C, but it decreases when measured perpendicular to the nano-sheets. This suggests the existence of a structural relaxation, which produces the change of the Co nano-sheets during annealing. The changes in the nano-morphology and the local chemical composition of the films at the nanoscale after heating above 270 °C have been analysed by scanning transmission electron microscopy (STEM). Thus, an approach and coalescence of the nano-sheets have been directly visualized. The spectrum of activation energies of this structural relaxation has indicated that the coalescence of the nano-sheets has taken place between 1.2 and 1.7 eV. In addition, an increase in the size of the nano-crystals has occurred in the samples annealed at 400 °C. This study may be relevant for the application in devices working, for example, in the GHz range and to achieve the retention of the anisotropy of these films at higher temperatures. PMID:29206155

  19. Structurally Oriented Nano-Sheets in Co Thin Films: Changing Their Anisotropic Physical Properties by Thermally-Induced Relaxation.

    PubMed

    Vergara, José; Favieres, Cristina; Magén, César; de Teresa, José María; Ibarra, Manuel Ricardo; Madurga, Vicente

    2017-12-05

    We show how nanocrystalline Co films formed by separated oblique nano-sheets display anisotropy in their resistivity, magnetization process, surface nano-morphology and optical transmission. After performing a heat treatment at 270 °C, these anisotropies decrease. This loss has been monitored measuring the resistivity as a function of temperature. The resistivity measured parallel to the direction of the nano-sheets has been constant up to 270 °C, but it decreases when measured perpendicular to the nano-sheets. This suggests the existence of a structural relaxation, which produces the change of the Co nano-sheets during annealing. The changes in the nano-morphology and the local chemical composition of the films at the nanoscale after heating above 270 °C have been analysed by scanning transmission electron microscopy (STEM). Thus, an approach and coalescence of the nano-sheets have been directly visualized. The spectrum of activation energies of this structural relaxation has indicated that the coalescence of the nano-sheets has taken place between 1.2 and 1.7 eV. In addition, an increase in the size of the nano-crystals has occurred in the samples annealed at 400 °C. This study may be relevant for the application in devices working, for example, in the GHz range and to achieve the retention of the anisotropy of these films at higher temperatures.

  20. Cell Sheet Stiffness Sensing without taking out from culture liquid.

    PubMed

    Uchida, Ryohei; Tanaka, Nobuyuki; Higashimori, Mitsuru; Tadakuma, Kenjiro; Kaneko, Makoto; Kondo, Makoto; Yamato, Masayuki

    2010-01-01

    Stiffness could be an important index for evaluating the vitality of cell sheet. This paper challenges the measurement of stiffness of transparent cell sheet in culture liquid without taking it out from petri dish. The system is composed of a micro air nozzle for supplying an air jet and a regular reflective type laser sensor for measuring the the deformation of transparent cell sheet. This system is called as Cell Sheet Stiffness Sensing system (CS(3) system). When an air jet is given to a cell sheet in culture liquid, it pushes away the liquid toward the outer direction at initial phase and reaches the surface of cell sheet. Without any switching motion, the air jet continuously imparts a force to the surface of cell sheet so that the sensor can measure the stiffness of the cell sheet.

  1. Electromagnetic augmentation for casting of thin metal sheets

    DOEpatents

    Hull, John R.

    1989-01-01

    Thin metal sheets are cast by magnetically levitating molten metal deposited in a mold within a ferromagnetic yoke and between AC conducting coils and linearly displacing the magnetically levitated liquid metal while it is being cooled by the water-cooled walls of the mold to form a solid metal sheet. A conducting shield is electrically coupled to the molten metal sheet to provide a return path for eddy currents induced in the metal sheet by the current in the AC conducting coils. In another embodiment, a DC conducting coil is coupled to the metal sheet for providing a direct current therein which interacts with the magnetic field to levitate the moving metal sheet. Levitation of the metal sheet in both molten and solid forms reduces its contact pressure with the mold walls while maintaining sufficient engagement therebetween to permit efficient conductive cooling by the mold through which a coolant fluid may be circulated. The magnetic fields associated with the currents in the aforementioned coils levitate the molten metal sheet while the mold provides for its lateral and vertical confinement. A leader sheet having electromagnetic characteristics similar to those of the molten metal sheet is used to start the casing process and precedes the molten metal sheet through the yoke/coil arrangement and mold and forms a continuous sheet therewith. The yoke/coil arrangement may be either U-shaped with a single racetrack coil or may be rectangular with a pair of spaced, facing bedstead coils.

  2. A study of thin liquid sheet flows

    NASA Technical Reports Server (NTRS)

    Chubb, Donald L.; Calfo, Frederick D.; Mcconley, Marc W.; Mcmaster, Matthew S.; Afjeh, Abdollah A.

    1993-01-01

    This study was a theoretical and experimental investigation of thin liquid sheet flows in vacuum. A sheet flow created by a narrow slit of width, W, coalesces to a point at a distance, L, as a result of surface tension forces acting at the sheet edges. As the flow coalesces, the fluid accumulates in the sheet edges. The observed triangular shape of the sheet agrees with the calculated triangular result. Experimental results for L/W as a function of Weber number, We, agree with the calculated result, L/W = the sq. root of 8We. The edge cross sectional shape is found to oscillate from elliptic to 'cigar' like to 'peanut' like and then back to elliptic in the flow direction. A theoretical one-dimensional model was developed that yielded only elliptic solutions for the edge cross section. At the points where the elliptic shapes occur, there is agreement between theory and experiment.

  3. Flapping dynamics of a thin liquid sheet

    NASA Astrophysics Data System (ADS)

    Vadivukkarasan, M.; Kumaran, Dhivyaraja; Panchagnula, Mahesh; Multi-phase flow physics Group Team

    2017-11-01

    We attempt to delineate and describe the complete evolution of a thin soap film when air is blown through a nozzle in the normal direction. The sequence of events and its intrinsic dynamics are captured using high speed imaging. By careful observation, it was observed that multiple mechanisms occur in the same system and each event is triggered by an independent mechanism. The events include (a) flapping of a liquid sheet and pinching of the bubble, (b) onset of rupture on the liquid sheet, (c) formation of ligaments and (d) ejection of drops. From this study, it is shown that these events are predominantly governed by Kelvin-Helmholtz instability, Taylor - Culick law, Rayleigh-Taylor instability and capillary instability, respectively. The present experiments can be considered as an extension to the previous studies on soap films as well as thin flapping sheets which has direct relevance to coaxial atomizers used in aircraft applications.

  4. Teen Sexual Activity, Pregnancy and Childbearing among Latinos in the United States. Fact Sheet.

    ERIC Educational Resources Information Center

    National Campaign To Prevent Teen Pregnancy, Washington, DC.

    The Latino population is the fastest-growing major racial/ethnic group in the United States. By 2020, approximately 16 percent of the population will be Latino. This increase will be even more pronounced among teens. This fact sheet summarizes data from the National Vital Statistics Reports on reported sexual activity, pregnancy rates, and…

  5. Solid/melt interface studies of high-speed silicon sheet growth

    NASA Technical Reports Server (NTRS)

    Ciszek, T. F.

    1984-01-01

    Radial growth-rate anisotropies and limiting growth forms of point nucleated, dislocation-free silicon sheets spreading horizontally on the free surface of a silicon melt have been measured for (100), (110), (111), and (112) sheet planes. Sixteen-millimeter movie photography was used to record the growth process. Analysis of the sheet edges has lead to predicted geometries for the tip shape of unidirectional, dislocation-free, horizontally growing sheets propagating in various directions within the above-mentioned planes. Similar techniques were used to study polycrystalline sheets and dendrite propagation. For dendrites, growth rates on the order of 2.5 m/min and growth rate anisotropies on the order of 25 were measured.

  6. Aerogeophysical evidence for active volcanism beneath the West Antarctic Ice Sheet

    NASA Technical Reports Server (NTRS)

    Blankenship, Donald D.; Bell, Robin E.; Hodge, Steven M.; Brozena, John M.; Behrendt, John C.

    1993-01-01

    Although it is widely understood that the collapse of the West Antarctic Ice Sheet (WAIS) would cause a global sea-level rise of 6 m, there continues to be considerable debate about the response of this ice sheet to climate change. The stability of the WAIS, which is characterized by a bed grounded well below sea level, may depend on geologically controlled conditions at the base, which are independent of climate. Ice streams moving up to 750 m/yr disperse material from the interior through to the oceans. As these ice streams tend to buffer the reservoir of slow-moving inland ice from exposure to oceanic degradation, understanding the ice-streaming process is important for evaluating WAIS stability. There is strong evidence that ice streams slide on a lubricating layer of water-saturated till. Development of this basal layer requires both water and easily eroded sediments. Active lithospheric extension may elevate regional heat flux, increase basal melting, and trigger ice streaming. If a geologically defined boundary with a sharp contrast in geothermal flux exists beneath the WAIS, ice streams may only be capable of operating as a buffer over a restricted region. Should ocean waters penetrate beyond this boundary, the ice-stream buffer would disappear, possibly triggering a collapse of the inland ice reservoir. Aerogeophysical evidence for active volcanism and elevated heat flux beneath the WAIS near the critical region where ice streaming begins is presented.

  7. On the balance of stresses in the plasma sheet.

    NASA Technical Reports Server (NTRS)

    Rich, F. J.; Wolf, R. A.; Vasyliunas, V. M.

    1972-01-01

    The stress resulting from magnetic tension on the neutral sheet must, in a steady state, be balanced by any one or a combination of (1) a pressure gradient in the direction along the axis of the tail, (2) a similar gradient of plasma flow kinetic energy, and (3) the tension resulting from a pressure anisotropy within the plasma sheet. Stress balance in the first two cases requires that the ratios h/LX and BZ/BX be of the same order of magnitude, where h is the half-thickness of the neutral sheet, LX is the length scale for variations along the axis of the tail, and BZ and BX are the magnetic field components in the plasma sheet just outside the neutral sheet. The second case requires, in addition, that the plasma flow speed within the neutral sheet be of the order of or larger than the Alfven speed outside the neutral sheet. Stress balance in the third case requires that just outside the neutral sheet the plasma pressure obey the marginal firehose stability condition.

  8. The Direct Loan Reconciliation Game.

    ERIC Educational Resources Information Center

    Department of Education, Washington, DC.

    This training guide for a one-day workshop provides an introduction to the William D. Ford Federal Direct Loan Program for administrative personnel at higher education institutions. The six sections of the guide, each corresponding to a workshop session, include activity sheets, questions for participants to answer, and space for notes. Following…

  9. Switch of flow direction in an Antarctic ice stream.

    PubMed

    Conway, H; Catania, G; Raymond, C F; Gades, A M; Scambos, T A; Engelhardt, H

    2002-10-03

    Fast-flowing ice streams transport ice from the interior of West Antarctica to the ocean, and fluctuations in their activity control the mass balance of the ice sheet. The mass balance of the Ross Sea sector of the West Antarctic ice sheet is now positive--that is, it is growing--mainly because one of the ice streams (ice stream C) slowed down about 150 years ago. Here we present evidence from both surface measurements and remote sensing that demonstrates the highly dynamic nature of the Ross drainage system. We show that the flow in an area that once discharged into ice stream C has changed direction, now draining into the Whillans ice stream (formerly ice stream B). This switch in flow direction is a result of continuing thinning of the Whillans ice stream and recent thickening of ice stream C. Further abrupt reorganization of the activity and configuration of the ice streams over short timescales is to be expected in the future as the surface topography of the ice sheet responds to the combined effects of internal dynamics and long-term climate change. We suggest that caution is needed when using observations of short-term mass changes to draw conclusions about the large-scale mass balance of the ice sheet.

  10. Photocatalytic activity and antimicrobial properties of paper sheets modified with TiO2/Sodium alginate nanocomposites.

    PubMed

    Abdel Rehim, Mona H; El-Samahy, Magda A; Badawy, Abdelrahman A; Mohram, Maysa E

    2016-09-05

    Photocatalytic paper sheets were prepared by addition of different ratios of TiO2/Sodium alginate (TSA) nanocomposite. The modified paper sheets were characterized by XRD, TGA. Their morphology was studied by scanning electron microscope (SEM) and energy dispersive X-ray (EDX). Photocatalytic activity of modified paper has been studied by analysis of chemical oxygen demand (COD) of waste-water. The results confirmed the mineralization of the waste-water and enhanced removal of chemical oxygen demand (COD) by increasing the amount of photocatalyst in the paper. Moreover, the results also confirmed that presence of sodium alginate as biopolymer increased adhesion of nanoparticles to paper fibers and reduced the harmful effect of the photocatalyst on them. The paper sheets containing 7% as well as 15% TSA showed high photocatalytic activity and anti-bacterial effect against Salmonella typhimurium higher than standard antibiotic beside other microorganisms such as Candida albicans. The maximum antimicrobial effect was found in case of specimen loaded with 15% TSA. Moreover, it was found that by adding 20% TSA to the paper matrix, the properties of the paper composite collapse. The obtained results confirm the possible utilization of the modified paper in both hygienic and food packaging applications. Copyright © 2016 Elsevier Ltd. All rights reserved.

  11. Evolution of three-dimensional relativistic current sheets and development of self-generated turbulence

    NASA Astrophysics Data System (ADS)

    Takamoto, M.

    2018-05-01

    In this paper, the temporal evolution of three-dimensional relativistic current sheets in Poynting-dominated plasma is studied for the first time. Over the past few decades, a lot of efforts have been conducted on studying the evolution of current sheets in two-dimensional space, and concluded that sufficiently long current sheets always evolve into the so-called plasmoid chain, which provides a fast reconnection rate independent of its resistivity. However, it is suspected that plasmoid chain can exist only in the case of two-dimensional approximation, and would show transition to turbulence in three-dimensional space. We performed three-dimensional numerical simulation of relativistic current sheet using resistive relativistic magnetohydrodynamic approximation. The results showed that the three-dimensional current sheets evolve not into plasmoid chain but turbulence. The resulting reconnection rate is 0.004, which is much smaller than that of plasmoid chain. The energy conversion from magnetic field to kinetic energy of turbulence is just 0.01 per cent, which is much smaller than typical non-relativistic cases. Using the energy principle, we also showed that the plasmoid is always unstable for a displacement in the opposite direction to its acceleration, probably interchange-type instability, and this always results in seeds of turbulence behind the plasmoids. Finally, the temperature distribution along the sheet is discussed, and it is found that the sheet is less active than plasmoid chain. Our finding can be applied for many high-energy astrophysical phenomena, and can provide a basic model of the general current sheet in Poynting-dominated plasma.

  12. Notched strength of beryllium powder and ingot sheets.

    NASA Technical Reports Server (NTRS)

    Moss, R. G.

    1972-01-01

    The effects of notches in thin beryllium sheets were studied as functions of material variables and notch severity. Double edge notched samples having stress concentration factors of 1.0 to 15.4 were prepared by milling to size, etching, and electrical discharge machining the notches. Strength was not reduced greatly by sharp notches, and duller notches were more deleterious than sharp notches. The trend was for reduced strength for dull notches, increased strength for sharper notches, and reduced strength for very sharp notches. Differences in material purity or source of the sheet had little affect on notch sensitivity. The most important factors appear to be oxide content and directionality of the sheet microstructure; high oxide content and highly directional microstructure tend to give more notch sensitivity than low oxide content, and more bidirectional microstructure. Postulated causes of the change in notched/unnotched strength are given.

  13. SU-F-T-49: Dosimetry Parameters and TPS Commissioning for the CivaSheet Directional Pd-103 Brachytherapy Source

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Rivard, MJ

    2016-06-15

    Purpose: The CivaSheet is a new LDR Pd-103 brachytherapy device offering directional-radiation for preferentially irradiating malignancies with healthy-tissue sparing. Observations are presented on dosimetric characterization, TPS commissioning, and evaluation of the dosesuperposition- principle for summing individual elements comprising a planar CivaSheet Methods: The CivaSheet comprises individual sources (CivaDots, 0.05cm thick and 0.25cm diam.) inside a flexible bioabsorbable substrate with a 0.8cm center-to-center rectangular array. All non-radioactive components were measured to ensure accuracy of manufacturer-provided dimensional information. The Pd spatial distribution was gleaned from radioactive and inert samples, then modeled with the MCNP6 radiation-transport-code. A 6×6 array CivaSheet was modeled tomore » evaluate the dose superposition principle for treatment planning. Air-kerma-strength was estimated using the NIST WAFAC geometry. Absorbed dose was estimated in water with polar sampling covering 0.05≤r≤15cm in 0.05cm increments and 0°≤θ≤180° in 1° increments. These data were entered into VariSeed9.0 and tested for the dose-superposition-principle. Results: The dose-rate-constant was 0.579 cGy/h/U with g(r) determined along the rotational-axis of symmetry (0°) instead of 90°. gP(r) values at 0.1, 0.5, 2, 5, and 10cm were 1.884, 1.344, 0.558, 0.088, and 0.0046. F(r,θ) decreased between 0° and 180° by factors of 270, 23, and 5.1 at 0.1, 1, and 10cm. The highest dose-gradient was at 92°, changing by a factor of 3 within 1° due to Au-foil shielding. TPS commissioning from 0.1≤r≤11cm and 0°≤θ≤180° demonstrated 2% reproducibility of input data except at the high-dose-gradient where interpolations caused 3% differences. Dose superposition of CivaDots replicated a multi-source CivaSheet array within 2% except where another CivaDot was present. Following implantation, the device is not perfectly planar. TPS accuracy utilizing

  14. Are Adolescents Talking with Their Parents about Sex before Becoming Sexually Active? Fact Sheet

    ERIC Educational Resources Information Center

    Leuschner, Kristin

    2010-01-01

    This paper examines parent-child discussions of sexual behavior. It finds consistency in the timing and content of such discussions; however, many parents and children do not discuss key topics, such as birth control, before adolescents become sexually active. [This fact sheet is based on Megan K. Beckett, Marc N. Elliott, Steven Martino, David E.…

  15. Simulation and measurement of melting effects on metal sheets caused by direct lightning strikes

    NASA Technical Reports Server (NTRS)

    Kern, Alexander

    1991-01-01

    Direct lightning strikes melt metal parts of various systems, like fuel and propellant tanks of rockets and airplanes, at the point of strike. Responsible for this melting are the impulse current and, if occurring, the long duration current, both carrying a remarkable charge Q. For studying these meltings the simulation in the laboratory has to be based on the parameters of natural lightnings. International standards exist defining certain threat levels of natural lightnings and giving possible generator circuits for the simulation. The melting caused by both types of lightning currents show different appearance. Their characteristics, their differences in melting and heating of metal sheets are investigated. Nevertheless the simulation of lightning in the laboratory is imperfect. While natural lightning is a discharge without a counter electrode, the simulation always demands a close counter electrode. The influence of this counter electrode is studied.

  16. Exposure age and ice-sheet model constraints on Pliocene East Antarctic ice sheet dynamics.

    PubMed

    Yamane, Masako; Yokoyama, Yusuke; Abe-Ouchi, Ayako; Obrochta, Stephen; Saito, Fuyuki; Moriwaki, Kiichi; Matsuzaki, Hiroyuki

    2015-04-24

    The Late Pliocene epoch is a potential analogue for future climate in a warming world. Here we reconstruct Plio-Pleistocene East Antarctic Ice Sheet (EAIS) variability using cosmogenic nuclide exposure ages and model simulations to better understand ice sheet behaviour under such warm conditions. New and previously published exposure ages indicate interior-thickening during the Pliocene. An ice sheet model with mid-Pliocene boundary conditions also results in interior thickening and suggests that both the Wilkes Subglacial and Aurora Basins largely melted, offsetting increased ice volume. Considering contributions from West Antarctica and Greenland, this is consistent with the most recent IPCC AR5 estimate, which indicates that the Pliocene sea level likely did not exceed +20 m on Milankovitch timescales. The inception of colder climate since ∼3 Myr has increased the sea ice cover and inhibited active moisture transport to Antarctica, resulting in reduced ice sheet thickness, at least in coastal areas.

  17. Gaps and Pathways Project: driving pathways by diagnosis sheets.

    PubMed

    Touchinsky, Susan; Chew, Felicia; Davis, Elin Schold

    2014-04-01

    This paper describes the development and use of information sheets for occupational therapy practitioners to use as guides for evaluation and intervention planning to address their client's driving and community mobility needs. Called Driving Pathways by Diagnosis Sheets, the information assists therapists with direction to connect impairment to driving risk and incorporate intervention to client goals and priorities related to driving and community mobility. An example of one of the sheets for the diagnosis of arthritis is highlighted and implications for use are discussed.

  18. Radar attenuation and temperature within the Greenland Ice Sheet

    USGS Publications Warehouse

    MacGregor, Joseph A; Li, Jilu; Paden, John D; Catania, Ginny A; Clow, Gary D.; Fahnestock, Mark A; Gogineni, Prasad S.; Grimm, Robert E.; Morlighem, Mathieu; Nandi, Soumyaroop; Seroussi, Helene; Stillman, David E

    2015-01-01

    The flow of ice is temperature-dependent, but direct measurements of englacial temperature are sparse. The dielectric attenuation of radio waves through ice is also temperature-dependent, and radar sounding of ice sheets is sensitive to this attenuation. Here we estimate depth-averaged radar-attenuation rates within the Greenland Ice Sheet from airborne radar-sounding data and its associated radiostratigraphy. Using existing empirical relationships between temperature, chemistry, and radar attenuation, we then infer the depth-averaged englacial temperature. The dated radiostratigraphy permits a correction for the confounding effect of spatially varying ice chemistry. Where radar transects intersect boreholes, radar-inferred temperature is consistently higher than that measured directly. We attribute this discrepancy to the poorly recognized frequency dependence of the radar-attenuation rate and correct for this effect empirically, resulting in a robust relationship between radar-inferred and borehole-measured depth-averaged temperature. Radar-inferred englacial temperature is often lower than modern surface temperature and that of a steady state ice-sheet model, particularly in southern Greenland. This pattern suggests that past changes in surface boundary conditions (temperature and accumulation rate) affect the ice sheet's present temperature structure over a much larger area than previously recognized. This radar-inferred temperature structure provides a new constraint for thermomechanical models of the Greenland Ice Sheet.

  19. The mechanistic exploration of porous activated graphene sheets-anchored SnO2 nanocrystals for application in high-performance Li-ion battery anodes.

    PubMed

    Yang, Yingchang; Ji, Xiaobo; Lu, Fang; Chen, Qiyuan; Banks, Craig E

    2013-09-28

    Porous activated graphene sheets have been for the first time exploited herein as encapsulating substrates for lithium ion battery (LIB) anodes. The as-fabricated SnO2 nanocrystals-porous activated graphene sheet (AGS) composite electrode exhibits improved electrochemical performance as an anode material for LIBs, such as better cycle performance and higher rate capability in comparison with graphene sheets, activated graphene sheets, bare SnO2 and SnO2-graphene sheet composites. The superior electrochemical performances of the designed anode can be ascribed to the porous AGS substrate, which improves the electrical conductivity of the electrode, inhibits agglomeration between particles and effectively buffers the strain from the volume variation during Li(+)-intercalation-de-intercalation and provides more cross-plane diffusion channels for Li(+) ions. As a result, the designed anode exhibits an outstanding capacity of up to 610 mA h g(-1) at a current density of 100 mA g(-1) after 50 cycles and a good rate performance of 889, 747, 607, 482 and 372 mA h g(-1) at a current density of 100, 200, 500, 1000, and 2000 mA g(-1), respectively. This work is of importance for energy storage as it provides a new substrate for the design and implementation of next-generation LIBs exhibiting exceptional electrochemical performances.

  20. Preparation of multilayer graphene sheets and their applications for particle accelerators

    NASA Astrophysics Data System (ADS)

    Tatami, Atsushi; Tachibana, Masamitsu; Yagi, Takashi; Murakami, Mutsuaki

    2018-05-01

    Multilayer graphene sheets were prepared by heat treatment of polyimide films at temperatures of up to 3000 °C. The sheets consist of highly oriented graphite layers with excellent mechanical robustness and flexibility. Key features of these sheets include their high thermal conductivity in the in-plane direction, good mechanical properties, and high carbon purity. The results suggest that the multilayer graphene sheets have great potential for charge stripping foils that persist even under the highest ion beam intensities irradiation and can be used for accelerator applications.

  1. Enhanced photocatalytic activity and structural stability by hybridizing Ag3PO4 nanospheres with graphene oxide sheets.

    PubMed

    Liang, Qinghua; Shi, Yao; Ma, Wangjing; Li, Zhi; Yang, Xinmin

    2012-12-05

    Graphene oxide (GO)-Ag(3)PO(4) nanocomposites synthesized through a facile solution approach via electrostatic interaction were investigated as excellent photocatalysts for the degradation of rhodamine B (RhB) under visible light irradiation. SEM and TEM observations indicate that Ag(3)PO(4) nanospheres of ~120 nm in diameter were well dispersed and anchored onto the exfoliated GO sheets. The characterizations of FTIR and Raman demonstrated the existence of strong charge interactions between GO sheets and Ag(3)PO(4) nanospheres. As compared to Ag(3)PO(4) nanospheres alone, the attachments of GO sheets led to a band gap narrowing (2.10 eV) and a strong absorbance in the near infrared region (NIR). The photoluminescence (PL) analysis indicates a more efficient separation of electron-hole pairs in the GO-Ag(3)PO(4) nanocomposites. Notably, the incorporation of GO sheets not only significantly enhances the photocatalytic activity but also improves the structural stability of Ag(3)PO(4). The positive synergistic effects between Ag(3)PO(4) nanospheres and GO sheets are proposed to contribute to the improved photocatalytic properties. A possible photocatalytic mechanism of the GO-Ag(3)PO(4) nanocomposites was assumed as well. The integration of these advantages enables such GO-Ag(3)PO(4) hybrid material to be a nice photocatalyst for broad applications in a sewage treatment system.

  2. Cell delivery in regenerative medicine: the cell sheet engineering approach.

    PubMed

    Yang, Joseph; Yamato, Masayuki; Nishida, Kohji; Ohki, Takeshi; Kanzaki, Masato; Sekine, Hidekazu; Shimizu, Tatsuya; Okano, Teruo

    2006-11-28

    Recently, cell-based therapies have developed as a foundation for regenerative medicine. General approaches for cell delivery have thus far involved the use of direct injection of single cell suspensions into the target tissues. Additionally, tissue engineering with the general paradigm of seeding cells into biodegradable scaffolds has also evolved as a method for the reconstruction of various tissues and organs. With success in clinical trials, regenerative therapies using these approaches have therefore garnered significant interest and attention. As a novel alternative, we have developed cell sheet engineering using temperature-responsive culture dishes, which allows for the non-invasive harvest of cultured cells as intact sheets along with their deposited extracellular matrix. Using this approach, cell sheets can be directly transplanted to host tissues without the use of scaffolding or carrier materials, or used to create in vitro tissue constructs via the layering of individual cell sheets. In addition to simple transplantation, cell sheet engineered constructs have also been applied for alternative therapies such as endoscopic transplantation, combinatorial tissue reconstruction, and polysurgery to overcome limitations of regenerative therapies and cell delivery using conventional approaches.

  3. A statistical study of current-sheet formation above solar active regions based on selforganized criticality

    NASA Astrophysics Data System (ADS)

    Dimitropoulou, M.; Isliker, H.; Vlahos, L.; Georgoulis, M.; Anastasiadis, A.; Toutountzi, A.

    2013-09-01

    We treat flaring solar active regions as physical systems having reached the self-organized critical state. Their evolving magnetic configurations in the low corona may satisfy an instability criterion, related to the excession of a specific threshold in the curl of the magnetic field. This imposed instability criterion implies an almost zero resistivity everywhere in the solar corona, except in regions where magnetic-field discontinuities and. hence, local currents, reach the critical value. In these areas, current-driven instabilities enhance the resistivity by many orders of magnitude forming structures which efficiently accelerate charged particles. Simulating the formation of such structures (thought of as current sheets) via a refined SOC cellular-automaton model provides interesting information regarding their statistical properties. It is shown that the current density in such unstable regions follows power-law scaling. Furthermore, the size distribution of the produced current sheets is best fitted by power laws, whereas their formation probability is investigated against the photospheric magnetic configuration (e.g. Polarity Inversion Lines, Plage). The average fractal dimension of the produced current sheets is deduced depending on the selected critical threshold. The above-mentioned statistical description of intermittent electric field structures can be used by collisional relativistic test particle simulations, aiming to interpret particle acceleration in flaring active regions and in strongly turbulent media in astrophysical plasmas. The above work is supported by the Hellenic National Space Weather Research Network (HNSWRN) via the THALIS Programme.

  4. A Robust Method to Generate Mechanically Anisotropic Vascular Smooth Muscle Cell Sheets for Vascular Tissue Engineering.

    PubMed

    Backman, Daniel E; LeSavage, Bauer L; Shah, Shivem B; Wong, Joyce Y

    2017-06-01

    In arterial tissue engineering, mimicking native structure and mechanical properties is essential because compliance mismatch can lead to graft failure and further disease. With bottom-up tissue engineering approaches, designing tissue components with proper microscale mechanical properties is crucial to achieve the necessary macroscale properties in the final implant. This study develops a thermoresponsive cell culture platform for growing aligned vascular smooth muscle cell (VSMC) sheets by photografting N-isopropylacrylamide (NIPAAm) onto micropatterned poly(dimethysiloxane) (PDMS). The grafting process is experimentally and computationally optimized to produce PNIPAAm-PDMS substrates optimal for VSMC attachment. To allow long-term VSMC sheet culture and increase the rate of VSMC sheet formation, PNIPAAm-PDMS surfaces were further modified with 3-aminopropyltriethoxysilane yielding a robust, thermoresponsive cell culture platform for culturing VSMC sheets. VSMC cell sheets cultured on patterned thermoresponsive substrates exhibit cellular and collagen alignment in the direction of the micropattern. Mechanical characterization of patterned, single-layer VSMC sheets reveals increased stiffness in the aligned direction compared to the perpendicular direction whereas nonpatterned cell sheets exhibit no directional dependence. Structural and mechanical anisotropy of aligned, single-layer VSMC sheets makes this platform an attractive microstructural building block for engineering a vascular graft to match the in vivo mechanical properties of native arterial tissue. © 2017 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim.

  5. Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6

    PubMed Central

    Nowicki, Sophie M.J.; Payne, Tony; Larour, Eric; Seroussi, Helene; Goelzer, Heiko; Lipscomb, William; Gregory, Jonathan; Abe-Ouchi, Ayako; Shepherd, Andrew

    2018-01-01

    Reducing the uncertainty in the past, present and future contribution of ice sheets to sea-level change requires a coordinated effort between the climate and glaciology communities. The Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6) is the primary activity within the Coupled Model Intercomparison Project – phase 6 (CMIP6) focusing on the Greenland and Antarctic Ice Sheets. In this paper, we describe the framework for ISMIP6 and its relationship to other activities within CMIP6. The ISMIP6 experimental design relies on CMIP6 climate models and includes, for the first time within CMIP, coupled ice sheet – climate models as well as standalone ice sheet models. To facilitate analysis of the multi-model ensemble and to generate a set of standard climate inputs for standalone ice sheet models, ISMIP6 defines a protocol for all variables related to ice sheets. ISMIP6 will provide a basis for investigating the feedbacks, impacts, and sea-level changes associated with dynamic ice sheets and for quantifying the uncertainty in ice-sheet-sourced global sea-level change. PMID:29697697

  6. Ring current dynamics and plasma sheet sources. [magnetic storms

    NASA Technical Reports Server (NTRS)

    Lyons, L. R.

    1984-01-01

    The source of the energized plasma that forms in geomagnetic storm ring currents, and ring current decay are discussed. The dominant loss processes for ring current ions are identified as charge exchange and resonant interactions with ion-cyclotron waves. Ring current ions are not dominated by protons. At L4 and energies below a few tens of keV, O+ is the most abundant ion, He+ is second, and protons are third. The plasma sheet contributes directly or indirectly to the ring current particle population. An important source of plasma sheet ions is earthward streaming ions on the outer boundary of the plasma sheet. Ion interactions with the current across the geomagnetic tail can account for the formation of this boundary layer. Electron interactions with the current sheet are possibly an important source of plasma sheet electrons.

  7. β-Sheet Containment by Flanking Prolines: Molecular Dynamic Simulations of the Inhibition of β-Sheet Elongation by Proline Residues in Human Prion Protein

    PubMed Central

    Shamsir, Mohd S.; Dalby, Andrew R.

    2007-01-01

    Previous molecular dynamic simulations have reported elongation of the existing β-sheet in prion proteins. Detailed examination has shown that these elongations do not extend beyond the proline residues flanking these β-sheets. In addition, proline has also been suggested to possess a possible structural role in preserving protein interaction sites by preventing invasion of neighboring secondary structures. In this work, we have studied the possible structural role of the flanking proline residues by simulating mutant structures with alternate substitution of the proline residues with valine. Simulations showed a directional inhibition of elongation, with the elongation progressing in the direction of valine including evident inhibition of elongation by existing proline residues. This suggests that the flanking proline residues in prion proteins may have a containment role and would confine the β-sheet within a specific length. PMID:17172295

  8. Strain and mechanical properties of the VCM multilayer sheet and their composites using the digital speckle correlation method.

    PubMed

    Zhang, Dehai; Xie, Guizhong; Li, Yanqin; Liu, Jianxiu

    2015-09-01

    The digital speckle correlation method (DSCM) is introduced to solve the challenging problems in the related geometric measurement. Theoretical calculations of strain are deduced using the DSCM. Corresponding strains along x and y directions are obtained from uniaxial tension experiments and digital speckle measurements, using the VCM nondeep drawing multilayer sheet, the VCM deep-drawing multilayer sheet, clad films, nondeep drawing substrate, and deep-drawing substrate sheet as the targeted experimental objects. The results show that the maximum strains along the x direction of the VCM nondeep drawing multilayer sheet, the VCM deep-drawing multilayer sheet, clad film, nondeep drawing substrate, and deep-drawing substrate sheet are 68.473%, 48.632%, 91.632%, 50.784% and 40.068%, respectively, while the maximum strains along the y direction are -2.657%, -15.381%, 2.826%, -9.780% and -7.783%, respectively. The mechanical properties of the VCM multilayer sheet are between those of the substrate and clad film, while mechanical properties of the VCM deep-drawing multilayer sheet are superior to those of the VCM nondeep drawing multi-layer sheet.

  9. Direct Loan Overview Workshop. Participant's Guide.

    ERIC Educational Resources Information Center

    Department of Education, Washington, DC.

    This training guide for a one-day workshop provides an introduction to the William D. Ford Federal Direct Loan Program for administrative personnel at higher educations institutions. The seven sections of the guide, each corresponding to a single workshop session, include activity sheets, questions for participants to answer, and space for notes.…

  10. Silk Film Topography Directs Collective Epithelial Cell Migration

    PubMed Central

    Rosenblatt, Mark I.

    2012-01-01

    The following study provides new insight into how surface topography dictates directed collective epithelial cell sheet growth through the guidance of individual cell movement. Collective cell behavior of migrating human corneal limbal-epithelial cell sheets were studied on highly biocompatible flat and micro-patterned silk film surfaces. The silk film edge topography guided the migratory direction of individual cells making up the collective epithelial sheet, which resulted in a 75% increase in total culture elongation. This was due to a 3-fold decrease in cell sheet migration rate efficiency for movement perpendicular to the topography edge. Individual cell migration direction is preferred in the parallel approach to the edge topography where localization of cytoskeletal proteins to the topography’s edge region is reduced, which results in the directed growth of the collective epithelial sheet. Findings indicate customized biomaterial surfaces may be created to direct both the migration rate and direction of tissue epithelialization. PMID:23185573

  11. Direct measurements of meltwater runoff on the Greenland ice sheet surface.

    PubMed

    Smith, Laurence C; Yang, Kang; Pitcher, Lincoln H; Overstreet, Brandon T; Chu, Vena W; Rennermalm, Åsa K; Ryan, Jonathan C; Cooper, Matthew G; Gleason, Colin J; Tedesco, Marco; Jeyaratnam, Jeyavinoth; van As, Dirk; van den Broeke, Michiel R; van de Berg, Willem Jan; Noël, Brice; Langen, Peter L; Cullather, Richard I; Zhao, Bin; Willis, Michael J; Hubbard, Alun; Box, Jason E; Jenner, Brittany A; Behar, Alberto E

    2017-12-12

    Meltwater runoff from the Greenland ice sheet surface influences surface mass balance (SMB), ice dynamics, and global sea level rise, but is estimated with climate models and thus difficult to validate. We present a way to measure ice surface runoff directly, from hourly in situ supraglacial river discharge measurements and simultaneous high-resolution satellite/drone remote sensing of upstream fluvial catchment area. A first 72-h trial for a 63.1-km 2 moulin-terminating internally drained catchment (IDC) on Greenland's midelevation (1,207-1,381 m above sea level) ablation zone is compared with melt and runoff simulations from HIRHAM5, MAR3.6, RACMO2.3, MERRA-2, and SEB climate/SMB models. Current models cannot reproduce peak discharges or timing of runoff entering moulins but are improved using synthetic unit hydrograph (SUH) theory. Retroactive SUH applications to two older field studies reproduce their findings, signifying that remotely sensed IDC area, shape, and supraglacial river length are useful for predicting delays in peak runoff delivery to moulins. Applying SUH to HIRHAM5, MAR3.6, and RACMO2.3 gridded melt products for 799 surrounding IDCs suggests their terminal moulins receive lower peak discharges, less diurnal variability, and asynchronous runoff timing relative to climate/SMB model output alone. Conversely, large IDCs produce high moulin discharges, even at high elevations where melt rates are low. During this particular field experiment, models overestimated runoff by +21 to +58%, linked to overestimated surface ablation and possible meltwater retention in bare, porous, low-density ice. Direct measurements of ice surface runoff will improve climate/SMB models, and incorporating remotely sensed IDCs will aid coupling of SMB with ice dynamics and subglacial systems. Copyright © 2017 the Author(s). Published by PNAS.

  12. Direct measurements of meltwater runoff on the Greenland ice sheet surface

    PubMed Central

    Smith, Laurence C.; Yang, Kang; Pitcher, Lincoln H; Overstreet, Brandon T.; Chu, Vena W.; Rennermalm, Åsa K.; Ryan, Jonathan C.; Cooper, Matthew G.; Gleason, Colin J.; Tedesco, Marco; Jeyaratnam, Jeyavinoth; van As, Dirk; van den Broeke, Michiel R.; van de Berg, Willem Jan; Noël, Brice; Langen, Peter L.; Cullather, Richard I.; Zhao, Bin; Hubbard, Alun; Box, Jason E.; Jenner, Brittany A.; Behar, Alberto E.

    2017-01-01

    Meltwater runoff from the Greenland ice sheet surface influences surface mass balance (SMB), ice dynamics, and global sea level rise, but is estimated with climate models and thus difficult to validate. We present a way to measure ice surface runoff directly, from hourly in situ supraglacial river discharge measurements and simultaneous high-resolution satellite/drone remote sensing of upstream fluvial catchment area. A first 72-h trial for a 63.1-km2 moulin-terminating internally drained catchment (IDC) on Greenland’s midelevation (1,207–1,381 m above sea level) ablation zone is compared with melt and runoff simulations from HIRHAM5, MAR3.6, RACMO2.3, MERRA-2, and SEB climate/SMB models. Current models cannot reproduce peak discharges or timing of runoff entering moulins but are improved using synthetic unit hydrograph (SUH) theory. Retroactive SUH applications to two older field studies reproduce their findings, signifying that remotely sensed IDC area, shape, and supraglacial river length are useful for predicting delays in peak runoff delivery to moulins. Applying SUH to HIRHAM5, MAR3.6, and RACMO2.3 gridded melt products for 799 surrounding IDCs suggests their terminal moulins receive lower peak discharges, less diurnal variability, and asynchronous runoff timing relative to climate/SMB model output alone. Conversely, large IDCs produce high moulin discharges, even at high elevations where melt rates are low. During this particular field experiment, models overestimated runoff by +21 to +58%, linked to overestimated surface ablation and possible meltwater retention in bare, porous, low-density ice. Direct measurements of ice surface runoff will improve climate/SMB models, and incorporating remotely sensed IDCs will aid coupling of SMB with ice dynamics and subglacial systems. PMID:29208716

  13. Direct measurements of meltwater runoff on the Greenland ice sheet surface

    NASA Astrophysics Data System (ADS)

    Smith, Laurence C.; Yang, Kang; Pitcher, Lincoln H.; Overstreet, Brandon T.; Chu, Vena W.; Rennermalm, Åsa K.; Ryan, Jonathan C.; Cooper, Matthew G.; Gleason, Colin J.; Tedesco, Marco; Jeyaratnam, Jeyavinoth; van As, Dirk; van den Broeke, Michiel R.; van de Berg, Willem Jan; Noël, Brice; Langen, Peter L.; Cullather, Richard I.; Zhao, Bin; Willis, Michael J.; Hubbard, Alun; Box, Jason E.; Jenner, Brittany A.; Behar, Alberto E.

    2017-12-01

    Meltwater runoff from the Greenland ice sheet surface influences surface mass balance (SMB), ice dynamics, and global sea level rise, but is estimated with climate models and thus difficult to validate. We present a way to measure ice surface runoff directly, from hourly in situ supraglacial river discharge measurements and simultaneous high-resolution satellite/drone remote sensing of upstream fluvial catchment area. A first 72-h trial for a 63.1-km2 moulin-terminating internally drained catchment (IDC) on Greenland's midelevation (1,207–1,381 m above sea level) ablation zone is compared with melt and runoff simulations from HIRHAM5, MAR3.6, RACMO2.3, MERRA-2, and SEB climate/SMB models. Current models cannot reproduce peak discharges or timing of runoff entering moulins but are improved using synthetic unit hydrograph (SUH) theory. Retroactive SUH applications to two older field studies reproduce their findings, signifying that remotely sensed IDC area, shape, and supraglacial river length are useful for predicting delays in peak runoff delivery to moulins. Applying SUH to HIRHAM5, MAR3.6, and RACMO2.3 gridded melt products for 799 surrounding IDCs suggests their terminal moulins receive lower peak discharges, less diurnal variability, and asynchronous runoff timing relative to climate/SMB model output alone. Conversely, large IDCs produce high moulin discharges, even at high elevations where melt rates are low. During this particular field experiment, models overestimated runoff by +21 to +58%, linked to overestimated surface ablation and possible meltwater retention in bare, porous, low-density ice. Direct measurements of ice surface runoff will improve climate/SMB models, and incorporating remotely sensed IDCs will aid coupling of SMB with ice dynamics and subglacial systems.

  14. A growing Leaf as a Sheet of an Active Solid

    NASA Astrophysics Data System (ADS)

    Sharon, Eran

    A growing leaf is a thin sheet of active solid, which expands while obeying the laws of mechanics. The effective rheology of this active solid is nontrivial, allowing the leaf to increase its area by orders of magnitude, keeping its ''proper'' geometry. The questions of what the characteristics of the leaf growth field are and how it is regulated without any central ''headquarter'' are still open. I will present measurements of natural leaf growth with high time and space resolution. These show that the growth is a highly fluctuating process in both time and space. We suggest that the entire statistics of the growth field, not just its averages contain information important for the understanding of growth regulation. In another set of experiments we measure the effect of mechanical stress on deformation and growth. The measured effective rheology is viscoelastic with time varying parameters, indicating remodeling of the tissue in response to extended application of mechanical stress.

  15. Method and apparatus for determining weldability of thin sheet metal

    DOEpatents

    Goodwin, Gene M.; Hudson, Joseph D.

    1988-01-01

    A fixture is provided for testing thin sheet metal specimens to evaluate hot-cracking sensitivity for determining metal weldability on a heat-to-heat basis or through varying welding parameters. A test specimen is stressed in a first direction with a load selectively adjustable over a wide range and then a weldment is passed along over the specimen in a direction transverse to the direction of strain to evaluate the hot-cracking characteristics of the sheet metal which are indicative of the weldability of the metal. The fixture provides evaluations of hot-cracking sensitivity for determining metal weldability in a highly reproducible manner with minimum human error.

  16. Ice Sheet Model Intercomparison Project (ISMIP6) Contribution to CMIP6

    NASA Technical Reports Server (NTRS)

    Nowicki, Sophie M. J.; Payne, Tony; Larour, Eric; Seroussi, Helene; Goelzer, Heiko; Lipscomb, William; Gregory, Jonathan; Abe-Ouchi, Ayako; Shepherd, Andrew

    2016-01-01

    Reducing the uncertainty in the past, present, and future contribution of ice sheets to sea-level change requires a coordinated effort between the climate and glaciology communities. The Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6) is the primary activity within the Coupled Model Intercomparison Project phase 6 (CMIP6) focusing on the Greenland and Antarctic ice sheets. In this paper, we describe the framework for ISMIP6 and its relationship with other activities within CMIP6. The ISMIP6 experimental design relies on CMIP6 climate models and includes, for the first time within CMIP, coupled ice-sheetclimate models as well as standalone ice-sheet models. To facilitate analysis of the multi-model ensemble and to generate a set of standard climate inputs for standalone ice-sheet models, ISMIP6 defines a protocol for all variables related to ice sheets. ISMIP6 will provide a basis for investigating the feedbacks, impacts, and sea-level changes associated with dynamic ice sheets and for quantifying the uncertainty in ice-sheet-sourced global sea-level change.

  17. Dylan Pritchett, Storyteller. Cue Sheet for Students.

    ERIC Educational Resources Information Center

    Evans, Karen L. B.

    Designed to be used before and after attending a storytelling performance by Dylan Pritchett, this cue sheet presents information about the performance and suggests activities that can be done with classmates, friends, or family members. The cue sheet discusses where and why people tell stories, what makes a story good for telling, what makes a…

  18. Comparative evaluation of absorbable hemostats: advantages of fibrin-based sheets.

    PubMed

    Krishnan, Lissy K; Mohanty, Mira; Umashankar, P R; Lal, Arthur Vijayan

    2004-11-01

    Bioactive hemostats and wound dressings consist of either inherently active materials or act as delivery vehicles which contain such materials. Fibrin is a natural hemostat and scaffold, guiding the direction of wound contraction and closure. In order to improve the ease of application of liquid fibrin glue, we have made a freeze-dried form of polymerized fibrin that supports hemostasis and wound healing. The bleeding from the middle ear artery of rabbits was found to be arrested instantaneously on application of fibrin sheets, even when the animal was heparinized systemically. As the fibrin sheet was found to be fragile, gelatin was incorporated to the sheet and thus the mechanical stability was improved without compromising the hemostatic effect. The efficacy of the fabricated fibrin and fibrin-gelatin sheets to seal traumatized rat liver was compared with commercially available hemostats, Abgel (cross-linked gelatin) and Surgicel (cross-linked cellulose). Tissue compatibility of all the hemostats was studied by analyzing the liver tissue 15 days after application. While the hemostatic effect was best with fibrin and fibrin-gelatin sheets, both Surgicel and Abgel were not capable of arresting the bleeding quickly. Gross analysis of tissue on the 15th day of application, visibly, Abgel was not only degraded but resulted in severe adhesions of internal organs and histologically capsule formation around the implant was evident. Though Surgicel was also seen as cream soft material on the site of application that joined two pieces of liver, there was no adhesion of other internal organs and histologically, immune reaction and foreign-body-type giant cells were present in large amounts. Fibrin was not found grossly on application site whereas fibrin-gelatin was seen as a small white spot. Granulation tissue formation and cell migration into the fibrin-based sheets were evident, and therefore, fibrin-based sheets are not only efficient hemostats but showed optimum

  19. Reconstructing the last Irish Ice Sheet 2: a geomorphologically-driven model of ice sheet growth, retreat and dynamics

    NASA Astrophysics Data System (ADS)

    Greenwood, Sarah L.; Clark, Chris D.

    2009-12-01

    The ice sheet that once covered Ireland has a long history of investigation. Much prior work focussed on localised evidence-based reconstructions and ice-marginal dynamics and chronologies, with less attention paid to an ice sheet wide view of the first order properties of the ice sheet: centres of mass, ice divide structure, ice flow geometry and behaviour and changes thereof. In this paper we focus on the latter aspect and use our new, countrywide glacial geomorphological mapping of the Irish landscape (>39 000 landforms), and our analysis of the palaeo-glaciological significance of observed landform assemblages (article Part 1), to build an ice sheet reconstruction yielding these fundamental ice sheet properties. We present a seven stage model of ice sheet evolution, from initiation to demise, in the form of palaeo-geographic maps. An early incursion of ice from Scotland likely coalesced with local ice caps and spread in a south-westerly direction 200 km across Ireland. A semi-independent Irish Ice Sheet was then established during ice sheet growth, with a branching ice divide structure whose main axis migrated up to 140 km from the west coast towards the east. Ice stream systems converging on Donegal Bay in the west and funnelling through the North Channel and Irish Sea Basin in the east emerge as major flow components of the maximum stages of glaciation. Ice cover is reconstructed as extending to the continental shelf break. The Irish Ice Sheet became autonomous (i.e. separate from the British Ice Sheet) during deglaciation and fragmented into multiple ice masses, each decaying towards the west. Final sites of demise were likely over the mountains of Donegal, Leitrim and Connemara. Patterns of growth and decay of the ice sheet are shown to be radically different: asynchronous and asymmetric in both spatial and temporal domains. We implicate collapse of the ice stream system in the North Channel - Irish Sea Basin in driving such asymmetry, since rapid

  20. Using the glacial geomorphology of palaeo-ice streams to understand mechanisms of ice sheet collapse

    NASA Astrophysics Data System (ADS)

    Stokes, Chris R.; Margold, Martin; Clark, Chris; Tarasov, Lev

    2017-04-01

    progressively smaller percentage of the ice sheet perimeter, and their total discharge decreased. Underlying geology and topography clearly influenced ice stream activity, but - at the ice sheet scale - their drainage network adjusted and was strongly linked to changes in ice sheet volume. It is unclear whether these findings are directly translatable to modern ice sheets but, contrary to the view that sees ice streams as unstable entities that can draw-down large sectors of an ice sheet and accelerate its demise, we conclude that they reduced in effectiveness during deglaciation of the Laurentide Ice Sheet, with final deglaciation accomplished most effectively by surface melting. This raises some interesting questions about the source and nature of major meltwater pulses and iceberg discharge events in the sea-level record.

  1. Resistance Spot Welding of AA5052 Sheet Metal of Dissimilar Thickness

    NASA Astrophysics Data System (ADS)

    Mat Din, N. A.; Zuhailawati, H.; Anasyida, A. S.

    2016-02-01

    Resistance spot welding of dissimilar thickness of AA5052 aluminum alloy was performed in order to investigate the effect of metal thickness on the weldment strength. Resistance spot welding was done using a spot welder machine available in Coraza Systems Sdn Bhd using a hemispherical of chromium copper electrode tip with radius of 6.00 mm under 14 kA of current and 0.02 bar of pressure for all thickness combinations. Lap joint configuration was produced between 2.0 mm thick sheet and 1.2 - 3.2 mm thick sheet, respectively. Microstructure of joint showed asymmetrical nugget shape that was larger on the thicker side indicating larger molten metal volume. Joint 2.0 mm x 3.2 mm sheets has the lowest hardness in both transverse direction and through thickness direction because less heat left in the weld nugget. The microstructure shows that this joint has coarse grains of HAZ. As thickness of sheet metal increased, the failure load of the joints increased. However, there was no linear correlation established between joint strength and metal thickness due to different shape of fusion zone in dissimilar thickness sheet metal.

  2. Beating the Heat - Fast Scanning Melts Silk Beta Sheet Crystals

    NASA Astrophysics Data System (ADS)

    Cebe, Peggy; Hu, Xiao; Kaplan, David L.; Zhuravlev, Evgeny; Wurm, Andreas; Arbeiter, Daniela; Schick, Christoph

    2013-01-01

    Beta-pleated-sheet crystals are among the most stable of protein secondary structures, and are responsible for the remarkable physical properties of many fibrous proteins, such as silk, or proteins forming plaques as in Alzheimer's disease. Previous thinking, and the accepted paradigm, was that beta-pleated-sheet crystals in the dry solid state were so stable they would not melt upon input of heat energy alone. Here we overturn that assumption and demonstrate that beta-pleated-sheet crystals melt directly from the solid state to become random coils, helices, and turns. We use fast scanning chip calorimetry at 2,000 K/s and report the first reversible thermal melting of protein beta-pleated-sheet crystals, exemplified by silk fibroin. The similarity between thermal melting behavior of lamellar crystals of synthetic polymers and beta-pleated-sheet crystals is confirmed. Significance for controlling beta-pleated-sheet content during thermal processing of biomaterials, as well as towards disease therapies, is envisioned based on these new findings.

  3. Micro-Scale Mechanical Testing of Non-Woven Carbon Nanotube Sheets and Yarns

    NASA Technical Reports Server (NTRS)

    Magargee, J.; Morestin, F.; Cao, J.; Jones, J. S.

    2013-01-01

    Non-woven carbon nanotube (CNT) sheets and yarns were tested using a novel micro-scale mechanical testing system. CNT sheets were observed to delaminate during uniaxial testing using an adbesive gripping method, resulting from a higher proportion of load bearing in the outer sheets versus internal sheets and an apparently low interlaminar shear strength. In response to this, a new spool-grip method was used to alleviate non-uniform through-thickness stresses, circumvent premature delamination, and allow the sheet material to sustain a 72% increase in measured tensile strength. Furthermore, tension tests of CNT yarns showed that the yarn-structure was approximaiely 7 times stronger than the sheet structure, owing to a higher degree of CNT alignment in the test direction.

  4. Plasma sheet dynamics observed by the Polar spacecraft in association with substorm onsets

    NASA Astrophysics Data System (ADS)

    Toivanen, P. K.; Baker, D. N.; Peterson, W. K.; Li, X.; Donovan, E. F.; Viljanen, A.; Keiling, A.; Wygant, J. R.; Kletzing, C. A.

    2001-09-01

    We present observations of the Polar spacecraft of magnetospheric substorm signatures in the plasma sheet midway along auroral field lines between the ionosphere and the equatorial plasma sheet. On October 17, 1997, Polar was located in the onset meridian in conjunction with the Scandinavian magnetometer chain (International Monitor for Auroral Geomagnetic Effects; IMAGE). In addition, a geostationary spacecraft, LANL-97A, was located near the onset meridian. On August 29, 1997, Polar was magnetically conjugate to the Canadian magnetometer chain (Canadian Auroral Network for the OPEN Program Unified Study; CANOPUS) ~5 hours east of the onset meridian. In both cases, substorm activity was manifested as strong magnetic (20 nT) and electric (40 mVm-1) field variations with bursts of parallel Poynting flux (~1 ergcm-2s-1), predominantly directed toward the ionosphere. In the first event Polar was located in the plasma sheet near the plasma sheet boundary, and the field variations were initiated at the ground onset. In the second event, Polar crossed the plasma sheet boundary to the tail lobes a few minutes prior to a local plasma sheet expansion. As Polar was engulfed by the plasma sheet, the field variations occurred in the previously quiet plasma sheet boundary. This coincided with the auroral bulge reaching the CANOPUS stations. We compare these two events and argue that the field variations were most probably signatures of the reconnection of open field lines and the subsequent enhanced earthward flows. Furthermore, weak flow bursts were observed at Polar in both events ~9 min before the onset. In the first event, a gradual development toward a negative bay and a burst of Pi2 pulsations were associated with the flow bursts. We anticipate that these signatures, often described in terms of pseudobreakups, were a precursor of the substorm onset, the initiation of the reconnection of closed field lines.

  5. The Evolution of the Plasma Sheet Ion Composition: Storms and Recoveries: Plasma Sheet Ion Composition

    DOE PAGES

    Denton, M. H.; Thomsen, M. F.; Reeves, G. D.; ...

    2017-10-03

    The ion plasma sheet (~few hundred eV to ~few 10s keV) is usually dominated by H + ions. Here, changes in ion composition within the plasma sheet are explored both during individual events, and statistically during 54 calm-to-storm events and during 21 active-to-calm events. Ion composition data from the HOPE (Helium, Oxygen, Proton, Electron) instruments onboard Van Allen Probes satellites provide exceptional spatial and temporal resolution of the H +, O +, and He + ion fluxes in the plasma sheet. H+ shown to be the dominant ion in the plasma sheet in the calm-to-storm transition. However, the energy-flux ofmore » each ion changes in a quasi-linear manner during extended calm intervals. Heavy ions (O + and He +) become increasingly important during such periods as charge-exchange reactions result in faster loss for H + than for O + or He +. Results confirm previous investigations showing that the ion composition of the plasma sheet can be largely understood (and predicted) during calm intervals from knowledge of: (a) the composition of previously injected plasma at the onset of calm conditions, and (b) use of simple drift-physics models combined with calculations of charge-exchange losses.« less

  6. The Evolution of the Plasma Sheet Ion Composition: Storms and Recoveries: Plasma Sheet Ion Composition

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Denton, M. H.; Thomsen, M. F.; Reeves, G. D.

    The ion plasma sheet (~few hundred eV to ~few 10s keV) is usually dominated by H + ions. Here, changes in ion composition within the plasma sheet are explored both during individual events, and statistically during 54 calm-to-storm events and during 21 active-to-calm events. Ion composition data from the HOPE (Helium, Oxygen, Proton, Electron) instruments onboard Van Allen Probes satellites provide exceptional spatial and temporal resolution of the H +, O +, and He + ion fluxes in the plasma sheet. H+ shown to be the dominant ion in the plasma sheet in the calm-to-storm transition. However, the energy-flux ofmore » each ion changes in a quasi-linear manner during extended calm intervals. Heavy ions (O + and He +) become increasingly important during such periods as charge-exchange reactions result in faster loss for H + than for O + or He +. Results confirm previous investigations showing that the ion composition of the plasma sheet can be largely understood (and predicted) during calm intervals from knowledge of: (a) the composition of previously injected plasma at the onset of calm conditions, and (b) use of simple drift-physics models combined with calculations of charge-exchange losses.« less

  7. Modelling the Climate - Greenland Ice Sheet Interaction in the Coupled Ice-sheet/Climate Model EC-EARTH - PISM

    NASA Astrophysics Data System (ADS)

    Yang, S.; Madsen, M. S.; Rodehacke, C. B.; Svendsen, S. H.; Adalgeirsdottir, G.

    2014-12-01

    Recent observations show that the Greenland ice sheet (GrIS) has been losing mass with an increasing speed during the past decades. Predicting the GrIS changes and their climate consequences relies on the understanding of the interaction of the GrIS with the climate system on both global and local scales, and requires climate model systems with an explicit and physically consistent ice sheet module. A fully coupled global climate model with a dynamical ice sheet model for the GrIS has recently been developed. The model system, EC-EARTH - PISM, consists of the EC-EARTH, an atmosphere, ocean and sea ice model system, and the Parallel Ice Sheet Model (PISM). The coupling of PISM includes a modified surface physical parameterization in EC-EARTH adapted to the land ice surface over glaciated regions in Greenland. The PISM ice sheet model is forced with the surface mass balance (SMB) directly computed inside the EC-EARTH atmospheric module and accounting for the precipitation, the surface evaporation, and the melting of snow and ice over land ice. PISM returns the simulated basal melt, ice discharge and ice cover (extent and thickness) as boundary conditions to EC-EARTH. This coupled system is mass and energy conserving without being constrained by any anomaly correction or flux adjustment, and hence is suitable for investigation of ice sheet - climate feedbacks. Three multi-century experiments for warm climate scenarios under (1) the RCP85 climate forcing, (2) an abrupt 4xCO2 and (3) an idealized 1% per year CO2 increase are performed using the coupled model system. The experiments are compared with their counterparts of the standard CMIP5 simulations (without the interactive ice sheet) to evaluate the performance of the coupled system and to quantify the GrIS feedbacks. In particular, the evolution of the Greenland ice sheet under the warm climate and its impacts on the climate system are investigated. Freshwater fluxes from the Greenland ice sheet melt to the Arctic

  8. Method and apparatus for assessing material properties of sheet-like materials

    DOEpatents

    Telschow, Kenneth L.; Deason, Vance A.

    2002-01-01

    Apparatus for producing an indication of a material property of a sheet-like material according to the present invention may comprise an excitation source for vibrating the sheet-like material to produce at least one traveling wave therein. A light source configured to produce an object wavefront and a reference wavefront directs the object wavefront toward the sheet-like material to produce a modulated object wavefront. A modulator operatively associated with the reference wavefront modulates the reference wavefront in synchronization with the traveling wave on the sheet-like material to produce a modulated reference wavefront. A sensing medium positioned to receive the modulated object wavefront and the modulated reference wavefront produces an image of the traveling wave in the sheet-like material, the image of the anti-symmetric traveling wave being related to a displacement amplitude of the anti-symmetric traveling wave over a two-dimensional area of the vibrating sheet-like material. A detector detects the image of the traveling wave in the sheet-like material.

  9. SU-F-T-61: Treatment Planning Observations for the CivaSheet Directional Brachytherapy Device Using VariSeed 9.0

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Rivard, MJ; Rothley, DJ

    2016-06-15

    Purpose: The VariSeed 9.0 brachytherapy TPS is recently available and has new features such as ability to rotate a brachytherapy source away from normal to the imaging plane. Consequently, a dosimetric analysis was performed for a directional brachytherapy source (CivaSheet) with tests of this functionality and experiences from clinical treatment planning were documented. These observations contribute to safe, practical, and accurate use of such new software features. Methods: Several tests were established to evaluate the new rotational feature, specific to the CivaSheet for the first patients treated using this new brachytherapy device. These included suitability of imaging slice-thickness and in-planemore » resolution, window/level adjustments for brachytherapy source visualization, commissioning the source physical length for performing rotations, and using different planar and 3D window views to identify source orientation. Additional CivaSheet-specific tests were performed to determine the dosimetric influence on target coverage: changing the source tilt angle, source positioning in the treatment plan based on the CivaSheet rectangular array of CivaDots, and influence of prescription depth on the necessary treatment margin for adequate target coverage. Results: Higher imaging-resolution produced better accuracy for source orientation and positioning, with sub-millimeter CT slice-thickness and in-plane resolution preferred. Source rotation was possible only in sagittal or coronal views. The process for validating source orientation required iteratively altering rotations then checking them in the 3D view, which was cumbersome given the absence of quantitative plan documentation to indicate orientation. Given the small Pd-103 source size, influence of source tilt within 30° was negligible for <1.0 cm. Influence of source position was important when the source was positioned in/out of the adjacent source plane, causing changes of 15%, 7%, and 3% at depths of

  10. Modular control of endothelial sheet migration

    PubMed Central

    Vitorino, Philip; Meyer, Tobias

    2008-01-01

    Growth factor-induced migration of endothelial cell monolayers enables embryonic development, wound healing, and angiogenesis. Although collective migration is widespread and therapeutically relevant, the underlying mechanism by which cell monolayers respond to growth factor, sense directional signals, induce motility, and coordinate individual cell movements is only partially understood. Here we used RNAi to identify 100 regulatory proteins that enhance or suppress endothelial sheet migration into cell-free space. We measured multiple live-cell migration parameters for all siRNA perturbations and found that each targeted protein primarily regulates one of four functional outputs: cell motility, directed migration, cell–cell coordination, or cell density. We demonstrate that cell motility regulators drive random, growth factor-independent motility in the presence or absence of open space. In contrast, directed migration regulators selectively transduce growth factor signals to direct cells along the monolayer boundary toward open space. Lastly, we found that regulators of cell–cell coordination are growth factor-independent and reorient randomly migrating cells inside the sheet when boundary cells begin to migrate. Thus, cells transition from random to collective migration through a modular control system, whereby growth factor signals convert boundary cells into pioneers, while cells inside the monolayer reorient and follow pioneers through growth factor-independent migration and cell–cell coordination. PMID:19056882

  11. Deep drawability of Ti/resin/Ti laminated sheet

    NASA Astrophysics Data System (ADS)

    Hardada, Yasunroi; Hattori, Shuji

    2017-10-01

    Aiming to enhance functionality of titanium cup, the formability of titanium/resin/titanium laminated sheet by deep drawing was investigated. Although pure titanium has excellent corrosion resistance, the density of titanium is higher than that of light metals, such as aluminum and magnesium. Part of the titanium cup made of resin allows for weight reduction of the cup. Furthermore, the clad cup is more likely to have heat retention and protection against vibration characteristics. In the experiment, the materials were pure titanium and polycarbonate. The initial thickness of the sheet was 0.2 to 0.5 mm in thickness. A total plate thickness of the blank was 1.0 to 1.5 mm in thickness. The blank diameter is 70 mm. The laminated sheet was constituted by interposing resin between two titanium sheets. Each sheet in stacked condition was not joined each other. In the deep drawing process, the laminated sheet was employed and a flat sheet blank was formed into a circle by a punch. For the prevention of seizure in contact area between a drawing tool and titanium, titanium blank was treated by oxide coating. By this method, the fresh and clean titanium is not in direct contact with the die during the forming due to the existence of the oxide layer. The deep drawing was carried out to investigate the formability. The laminated sheet was successfully drawn without the cracks. The section of the drawn cup was observed to examine a formability of the resin sheet. The reduction rate of the thickness was less than 10%. It was found that the titanium/resin/titanium clad cup was successfully drawn.

  12. Effect of Cell Sheet Manipulation Techniques on the Expression of Collagen Type II and Stress Fiber Formation in Human Chondrocyte Sheets.

    PubMed

    Wongin, Sopita; Waikakul, Saranatra; Chotiyarnwong, Pojchong; Siriwatwechakul, Wanwipa; Viravaidya-Pasuwat, Kwanchanok

    2018-03-01

    Cell sheet technology is applied to human articular chondrocytes to construct a tissue-like structure as an alternative treatment for cartilage defect. The effect of a gelatin manipulator, as a cell sheet transfer system, on the quality of the chondrocyte sheets was investigated. The changes of important chondrogenic markers and stress fibers, resulting from the cell sheet manipulation, were also studied. The chondrocyte cell sheets were constructed with patient-derived chondrocytes using a temperature-responsive polymer and a gelatin manipulator as a transfer carrier. The properties of the cell sheets, including sizes, expression levels of collagen type II and I, and the localization of the stress fibers, were assessed and compared with those of the cell sheets harvested without the gelatin manipulator. Using the gelatin manipulator, the original size of the chondrocyte cell sheets was retained with abundant stress fibers, but with a decrease in the expression of collagen type II. Without the gelatin manipulator, although the cell shrinkage occurred, the cell sheet with suppressed stress fiber formation showed significantly higher levels of collagen type II. These results support our observations that stress fiber formation in chondrocyte cell sheets affected the production of chondrogenic markers. These densely packed tissue-like structures possessed a good chondrogenic activity, indicating their potential for use in autologous chondrocyte implantation to treat cartilage defects.

  13. Magnetic field dissipation in D-sheets

    NASA Technical Reports Server (NTRS)

    Burlaga, L. F.; Scudder, J. D.

    1973-01-01

    The effects of magnetic field annihilation at a tangential or rotational discontinuity in a resistive plasma are examined. The magnetic field intensity profile depends on (1) the field intensities far from the current sheet (+ and - infinity), (2) the angle between the two intensities, and (3) the electrical resistivity. For a tangential discontinuity, the theory predicts a depression in B, centered at the discontinuity, and it predicts a monotonic transition. The theory provides satisfactory fits to the magnetic field intensity and proton temperature profiles observed for two extremely broad D-sheets in the solar wind. Assuming a diffusion time 10 days, one obtains effective resistivities or approximately = 3 x 10 to the 12th power and 2 x 10 to the 13th power emu for the D-sheets. Either resistivity at directional discontinuities is much lower than 10 to the 12th power emu or annihilation does not always occur at discontinuities.

  14. Compact and efficient blue laser sheet for measurement

    NASA Astrophysics Data System (ADS)

    Qi, Yan; Wang, Yu; Wu, Bin; Wang, Yanwei; Yan, Boxia

    2017-10-01

    Compact and efficient blue laser sheet has important applications in the field of measurement, with laser diode end pumped Nd:YAG directly and LBO intracavity frequency doubling, a compact and efficient CW 473nm blue laser sheet composed of dual path liner blue laser is realized. At an incident pump power of 12.4W, up to 1.4W output power of the compound blue laser is achieved, the optical-to-optical conversion efficiency is as high as 11.3%.

  15. Indirect Versus Direct Heating of Sheet Materials: Superplastic Forming and Diffusion Bonding Using Lasers

    NASA Astrophysics Data System (ADS)

    Jocelyn, Alan; Kar, Aravinda; Fanourakis, Alexander; Flower, Terence; Ackerman, Mike; Keevil, Allen; Way, Jerome

    2010-06-01

    Many from within manufacturing industry consider superplastic forming (SPF) to be ‘high tech’, but it is often criticized as too complicated, expensive, slow and, in general, an unstable process when compared to other methods of manipulating sheet materials. Perhaps, the fundamental cause of this negative perception of SPF, and also of diffusion bonding (DB), is the fact that the current process of SPF/DB relies on indirect sources of heating to produce the conditions necessary for the material to be formed. Thus, heat is usually derived from the electrically heated platens of hydraulic presses, to a lesser extent from within furnaces and, sometimes, from heaters imbedded in ceramic moulds. Recent evaluations of these isothermal methods suggest they are slow, thermally inefficient and inappropriate for the process. In contrast, direct heating of only the material to be formed by modern, electrically efficient, lasers could transform SPF/DB into the first choice of designers in aerospace, automotive, marine, medical, architecture and leisure industries. Furthermore, ‘variable temperature’ direct heating which, in theory, is possible with a laser beam(s) may provide a means to control material thickness distribution, a goal of enormous importance as fuel efficient, lightweight structures for transportation systems are universally sought. This paper compares, and contrasts, the two systems and suggests how a change to laser heating might be achieved.

  16. Optimal swimming of a sheet.

    PubMed

    Montenegro-Johnson, Thomas D; Lauga, Eric

    2014-06-01

    Propulsion at microscopic scales is often achieved through propagating traveling waves along hairlike organelles called flagella. Taylor's two-dimensional swimming sheet model is frequently used to provide insight into problems of flagellar propulsion. We derive numerically the large-amplitude wave form of the two-dimensional swimming sheet that yields optimum hydrodynamic efficiency: the ratio of the squared swimming speed to the rate-of-working of the sheet against the fluid. Using the boundary element method, we show that the optimal wave form is a front-back symmetric regularized cusp that is 25% more efficient than the optimal sine wave. This optimal two-dimensional shape is smooth, qualitatively different from the kinked form of Lighthill's optimal three-dimensional flagellum, not predicted by small-amplitude theory, and different from the smooth circular-arc-like shape of active elastic filaments.

  17. Single-Molecule Light-Sheet Imaging of Suspended T Cells.

    PubMed

    Ponjavic, Aleks; McColl, James; Carr, Alexander R; Santos, Ana Mafalda; Kulenkampff, Klara; Lippert, Anna; Davis, Simon J; Klenerman, David; Lee, Steven F

    2018-05-08

    Adaptive immune responses are initiated by triggering of the T cell receptor. Single-molecule imaging based on total internal reflection fluorescence microscopy at coverslip/basal cell interfaces is commonly used to study this process. These experiments have suggested, unexpectedly, that the diffusional behavior and organization of signaling proteins and receptors may be constrained before activation. However, it is unclear to what extent the molecular behavior and cell state is affected by the imaging conditions, i.e., by the presence of a supporting surface. In this study, we implemented single-molecule light-sheet microscopy, which enables single receptors to be directly visualized at any plane in a cell to study protein dynamics and organization in live, resting T cells. The light sheet enabled the acquisition of high-quality single-molecule fluorescence images that were comparable to those of total internal reflection fluorescence microscopy. By comparing the apical and basal surfaces of surface-contacting T cells using single-molecule light-sheet microscopy, we found that most coated-glass surfaces and supported lipid bilayers profoundly affected the diffusion of membrane proteins (T cell receptor and CD45) and that all the surfaces induced calcium influx to various degrees. Our results suggest that, when studying resting T cells, surfaces are best avoided, which we achieve here by suspending cells in agarose. Copyright © 2018. Published by Elsevier Inc.

  18. Ice sheets play important role in climate change

    NASA Astrophysics Data System (ADS)

    Clark, Peter U.; MacAyeal, Douglas R.; Andrews, John T.; Bartlein, Patrick J.

    Ice sheets once were viewed as passive elements in the climate system enslaved to orbitally generated variations in solar radiation. Today, modeling results and new geologic records suggest that ice sheets actively participated in late-Pleistocene climate change, amplifying or driving significant variability at millennial as well as orbital timescales. Although large changes in global ice volume were ultimately caused by orbital variations (the Milankovitch hypothesis), once in existence, the former ice sheets behaved dynamically and strongly influenced regional and perhaps even global climate by altering atmospheric and oceanic circulation and temperature.Experiments with General Circulation Models (GCMs) yielded the first inklings of ice sheets' climatic significance. Manabe and Broccoli [1985], for example, found that the topographic and albedo effects of ice sheets alone explain much of the Northern Hemisphere cooling identified in paleoclimatic records of the last glacial maximum (˜21 ka).

  19. Structure of the Jovian Magnetodisk Current Sheet: Initial Galileo Observations

    NASA Technical Reports Server (NTRS)

    Russell, C. T.; Huddleston, D. E.; Khurana, K. K.; Kivelson, M. G.

    2001-01-01

    The ten-degree tilt of the Jovian magnetic dipole causes the magnetic equator to move back and forth across Jupiter's rotational equator and tile Galileo orbit that lies therein. Beyond about 24 Jovian radii, the equatorial current sheet thins and tile magnetic structure changes from quasi-dipolar into magnetodisk-like with two regions of nearly radial but antiparallel magnetic field separated by a strong current layer. The magnetic field at the center of the current sheet is very weak in this region. Herein we examine tile current sheet at radial distances from 24 55 Jovian radii. We find that the magnetic structure very much resembles tile structure seen at planetary magnetopause and tail current sheet crossings. Tile magnetic field variation is mainly linear with little rotation of the field direction, At times there is almost no small-scale structure present and the normal component of the magnetic field is almost constant through the current sheet. At other times there are strong small-scale structures present in both the southward and northward directions. This small-scale structure appears to grow with radial distance and may provide the seeds for tile explosive reconnection observed at even greater radial distances oil tile nightside. Beyond about 40 Jovian radii, the thin current sheet also appears to be almost constantly in oscillatory motion with periods of about 10 min. The amplitude of these oscillations also appears to grow with radial distance. The source of these fluctuations may be dynamical events in tile more distant magnetodisk.

  20. Selectable light-sheet uniformity using tuned axial scanning

    PubMed Central

    Duocastella, Martí; Arnold, Craig B.; Puchalla, Jason

    2016-01-01

    Light-sheet fluorescence microscopy (LSFM) is an optical sectioning technique capable of rapid three-dimensional (3D) imaging of a wide range of specimens with reduced phototoxicity and superior background rejection. However, traditional light-sheet generation approaches based on elliptical or circular Gaussian beams suffer an inherent trade-off between light-sheet thickness and area over which this thickness is preserved. Recently, an increase in light-sheet uniformity was demonstrated using rapid biaxial Gaussian beam scanning along the lateral and beam propagation directions. Here we apply a similar scanning concept to an elliptical beam generated by a cylindrical lens. In this case, only z-scanning of the elliptical beam is required and hence experimental implementation of the setup can be simplified. We introduce a simple dimensionless uniformity statistic to better characterize scanned light-sheets and experimentally demonstrate custom tailored uniformities up to a factor of 5 higher than those of un-scanned elliptical beams. This technique offers a straightforward way to generate and characterize a custom illumination profile that provides enhanced utilization of the detector dynamic range and field of view, opening the door to faster and more efficient 2D and 3D imaging. PMID:28132409

  1. Growth Factor-Reinforced ECM Fabricated from Chemically Hypoxic MSC Sheet with Improved In Vivo Wound Repair Activity.

    PubMed

    Du, Hui-Cong; Jiang, Lin; Geng, Wen-Xin; Li, Jing; Zhang, Rui; Dang, Jin-Ge; Shu, Mao-Guo; Li, Li-Wen

    2017-01-01

    MSC treatment can promote cutaneous wound repair through multiple mechanisms, and paracrine mediators secreted by MSC are responsible for most of its therapeutic benefits. Recently, MSC sheet composed of live MSCs and their secreted ECMs was reported to promote wound healing; however, whether its ECM alone could accelerate wound closure remained unknown. In this study, Nc-ECM and Cc-ECM were prepared from nonconditioned and CoCl 2 -conditioned MSC sheets, respectively, and their wound healing properties were evaluated in a mouse model of full-thickness skin defect. Our results showed that Nc-ECM can significantly promote wound repair through early adipocyte recruitment, rapid reepithelialization, enhanced granulation tissue growth, and augmented angiogenesis. Moreover, conditioning of MSC sheet with CoCl 2 dramatically enriched its ECM with collagen I, collagen III, TGF- β 1, VEGF, and bFGF via activation of HIF-1 α and hence remarkably improved its ECM's in vivo wound healing potency. All the Cc-ECM-treated wounds completely healed on day 7, while Nc-ECM-treated wounds healed about 85.0% ± 8.6%, and no-treatment wounds only healed 69.8% ± 9.6% ( p < 0.05). Therefore, we believe that such growth factor-reinforced ECM fabricated from chemically hypoxic MSC sheet has the potential for clinical translation and will lead to a MSC-derived, cost-effective, bankable biomaterial for wound management.

  2. AFRICAN MUSIC SPEAKS, NO. 6--PROJECT CUE, A TV UTILIZATION SHEET.

    ERIC Educational Resources Information Center

    BROWN, ROBERT M.

    FOURTEEN SETS OF EDUCATIONAL TV UTILIZATION GUIDE SHEETS WERE PREPARED AS TEACHER AIDS. THESE SHEETS COVER SUCH AREAS AS SYNOPSIS OF SUBJECT, SUGGESTED PREPARATION (PRETELECAST), KEY WORDS, WHAT PUPILS SHOULD LOOK AND LISTEN FOR, SUGGESTED FOLLOWUP ACTIVITIES, SUGGESTED RELATED ACTIVITIES, SUGGESTED EVALUATION, AND SUGGESTED RELATED MATERIALS.…

  3. Phthalocyanine based metal containing porous carbon sheet

    NASA Astrophysics Data System (ADS)

    Honda, Z.; Sakaguchi, Y.; Tashiro, M.; Hagiwara, M.; Kida, T.; Sakai, M.; Fukuda, T.; Kamata, N.

    2017-03-01

    Highly-ordered fused-ring poly copper phthalocyanine (PCuPc) was prepared using copper octacyanophthalocyanine as a building block, and two-dimensional (2D) square superlattices were directly observed by the transmission electron microscopy. Remarkably, we have found a formation of polymer network that consists of a 2D porous PCuPc sheet in which the centers of phthalocyanine units are alternately occupied by Cu atom and vacancy. Using this "half-filling" PCuPc, it must be possible to create alternating arrangements for transition metal centers, and therefore control the magnetic properties of the 2D carbon sheets.

  4. Influence of silicone sheets on microvascular anastomosis.

    PubMed

    Hoang Nguyen, The; Kloeppel, Marcus; Hoehnke, Christoph; Staudenmaier, Rainer

    2008-12-01

    The use of silicone products combined with free flap transfer is well established in reconstructive surgery. We determined the risk of thrombosis as a result of direct contact between the silicone sheet and the point of microanastomosis. We performed microvascular surgery in 24 female Chinchilla Bastard rabbits weighing 3500 to 4000 g using two groups: Group 1 (n = 12), microanastomosis directly in contact with silicone sheets; and Group 2 (n = 12), microanastomosis protected by a 2 x 3 x 1-cm muscle cuff before being placed in contact with the silicone. We assessed flow-through of the microanastomosis by selective microangiography and histology at 1 and 3 weeks. All microanastomoses in Group 1 were occluded by postoperative thromboses, whereas all microanastomoses in Group 2 had adequate flow-through. Histologic analysis revealed thromboses in Group 1 formed from collagenous bundles of fiber securely attached to the intraluminal wall of the vessel. Three weeks after the procedure, these thromboses were canalized by varying small vessels. In Group 2, a slight luminal stenosis with evidence of infiltration of inflammatory cells at the microanastomosis line was observed histologically in all cases. Prefabricated flaps using silicone sheets and muscular cuffs placed around the anastomoses appear to reduce the risk of thrombosis and enhance neovascularization.

  5. 3D tissue formation by stacking detachable cell sheets formed on nanofiber mesh.

    PubMed

    Kim, Min Sung; Lee, Byungjun; Kim, Hong Nam; Bang, Seokyoung; Yang, Hee Seok; Kang, Seong Min; Suh, Kahp-Yang; Park, Suk-Hee; Jeon, Noo Li

    2017-03-23

    We present a novel approach for assembling 3D tissue by layer-by-layer stacking of cell sheets formed on aligned nanofiber mesh. A rigid frame was used to repeatedly collect aligned electrospun PCL (polycaprolactone) nanofiber to form a mesh structure with average distance between fibers 6.4 µm. When human umbilical vein endothelial cells (HUVECs), human foreskin dermal fibroblasts, and skeletal muscle cells (C2C12) were cultured on the nanofiber mesh, they formed confluent monolayers and could be handled as continuous cell sheets with areas 3 × 3 cm 2 or larger. Thicker 3D tissues have been formed by stacking multiple cell sheets collected on frames that can be nested (i.e. Matryoshka dolls) without any special tools. When cultured on the nanofiber mesh, skeletal muscle, C2C12 cells oriented along the direction of the nanofibers and differentiated into uniaxially aligned multinucleated myotube. Myotube cell sheets were stacked (upto 3 layers) in alternating or aligned directions to form thicker tissue with ∼50 µm thickness. Sandwiching HUVEC cell sheets with two dermal fibroblast cell sheets resulted in vascularized 3D tissue. HUVECs formed extensive networks and expressed CD31, a marker of endothelial cells. Cell sheets formed on nanofiber mesh have a number of advantages, including manipulation and stacking of multiple cell sheets for constructing 3D tissue and may find applications in a variety of tissue engineering applications.

  6. Unsteady aerodynamics and vortex-sheet formation of a two-dimensional airfoil

    NASA Astrophysics Data System (ADS)

    Xia, X.; Mohseni, K.

    2017-11-01

    Unsteady inviscid flow models of wings and airfoils have been developed to study the aerodynamics of natural and man-made flyers. Vortex methods have been extensively applied to reduce the dimensionality of these aerodynamic models, based on the proper estimation of the strength and distribution of the vortices in the wake. In such modeling approaches, one of the most fundamental questions is how the vortex sheets are generated and released from sharp edges. To determine the formation of the trailing-edge vortex sheet, the classical Kutta condition can be extended to unsteady situations by realizing that a flow cannot turn abruptly around a sharp edge. This condition can be readily applied to a flat plate or an airfoil with cusped trailing edge since the direction of the forming vortex sheet is known to be tangential to the trailing edge. However, for a finite-angle trailing edge, or in the case of flow separation away from a sharp corner, the direction of the forming vortex sheet is ambiguous. To remove any ad-hoc implementation, the unsteady Kutta condition, the conservation of circulation, as well as the conservation laws of mass and momentum are coupled to analytically solve for the angle, strength, and relative velocity of the trailing-edge vortex sheet. The two-dimensional aerodynamic model together with the proposed vortex-sheet formation condition is verified by comparing flow structures and force calculations with experimental results for airfoils in steady and unsteady background flows.

  7. A coronal magnetic field model with horizontal volume and sheet currents

    NASA Technical Reports Server (NTRS)

    Zhao, Xuepu; Hoeksema, J. Todd

    1994-01-01

    When globally mapping the observed photospheric magnetic field into the corona, the interaction of the solar wind and magnetic field has been treated either by imposing source surface boundary conditions that tacitly require volume currents outside the source surface or by limiting the interaction to thin current sheets between oppositely directed field regions. Yet observations and numerical Magnetohydrodynamic (MHD) calculations suggest the presence of non-force-free volume currents throughout the corona as well as thin current sheets in the neighborhoods of the interfaces between closed and open field lines or between oppositely directed open field lines surrounding coronal helmet-streamer structures. This work presents a model including both horizontal volume currents and streamer sheet currents. The present model builds on the magnetostatic equilibria developed by Bogdan and Low and the current-sheet modeling technique developed by Schatten. The calculation uses synoptic charts of the line-of-sight component of the photospheric magnetic field measured at the Wilcox Solar Observatory. Comparison of an MHD model with the calculated model results for the case of a dipole field and comparison of eclipse observations with calculations for CR 1647 (near solar minimum) show that this horizontal current-current-sheet model reproduces polar plumes and axes of corona streamers better than the source-surface model and reproduces polar plumes and axes of corona streamers better than the source-surface model and reproduces coro nal helmet structures better than the current-sheet model.

  8. Sequentially bridged graphene sheets with high strength, toughness, and electrical conductivity

    PubMed Central

    Wan, Sijie; Li, Yuchen; Mu, Jiuke; Aliev, Ali E.; Fang, Shaoli; Kotov, Nicholas A.; Jiang, Lei; Cheng, Qunfeng; Baughman, Ray H.

    2018-01-01

    We here show that infiltrated bridging agents can convert inexpensively fabricated graphene platelet sheets into high-performance materials, thereby avoiding the need for a polymer matrix. Two types of bridging agents were investigated for interconnecting graphene sheets, which attach to sheets by either π–π bonding or covalent bonding. When applied alone, the π–π bonding agent is most effective. However, successive application of the optimized ratio of π–π bonding and covalent bonding agents provides graphene sheets with the highest strength, toughness, fatigue resistance, electrical conductivity, electromagnetic interference shielding efficiency, and resistance to ultrasonic dissolution. Raman spectroscopy measurements of stress transfer to graphene platelets allow us to decipher the mechanisms of property improvement. In addition, the degree of orientation of graphene platelets increases with increasing effectiveness of the bonding agents, and the interlayer spacing increases. Compared with other materials that are strong in all directions within a sheet, the realized tensile strength (945 MPa) of the resin-free graphene platelet sheets was higher than for carbon nanotube or graphene platelet composites, and comparable to that of commercially available carbon fiber composites. The toughness of these composites, containing the combination of π–π bonding and covalent bonding, was much higher than for these other materials having high strengths for all in-plane directions, thereby opening the path to materials design of layered nanocomposites using multiple types of quantitatively engineered chemical bonds between nanoscale building blocks. PMID:29735659

  9. Strain induced chemical potential difference between monolayer graphene sheets.

    PubMed

    Zhang, Yupeng; Luo, Chengzhi; Li, Weiping; Pan, Chunxu

    2013-04-07

    Monolayer graphene sheets were deposited on a transparent and flexible polydimethylsiloxane (PDMS) substrate, and a tensile strain was loaded by stretching the substrate in one direction. It was found that an electric potential difference between stretched and static monolayer graphene sheets reached 8 mV when the strain was 5%. Theoretical calculations for the band structure and total energy revealed an alternative way to experimentally tune the band gap of monolayer graphene, and induce the generation of electricity.

  10. Distribution of energetic oxygen and hydrogen in the near-Earth plasma sheet

    NASA Astrophysics Data System (ADS)

    Kronberg, E. A.; Grigorenko, E. E.; Haaland, S. E.; Daly, P. W.; Delcourt, D. C.; Luo, H.; Kistler, L. M.; Dandouras, I.

    2015-05-01

    The spatial distributions of different ion species are useful indicators for plasma sheet dynamics. In this statistical study based on 7 years of Cluster observations, we establish the spatial distributions of oxygen ions and protons at energies from 274 to 955 keV, depending on geomagnetic and solar wind (SW) conditions. Compared with protons, the distribution of energetic oxygen has stronger dawn-dusk asymmetry in response to changes in the geomagnetic activity. When the interplanetary magnetic field (IMF) is directed southward, the oxygen ions show significant acceleration in the tail plasma sheet. Changes in the SW dynamic pressure (Pdyn) affect the oxygen and proton intensities in the same way. The energetic protons show significant intensity increases at the near-Earth duskside during disturbed geomagnetic conditions, enhanced SW Pdyn, and southward IMF, implying there location of effective inductive acceleration mechanisms and a strong duskward drift due to the increase of the magnetic field gradient in the near-Earth tail. Higher losses of energetic ions are observed in the dayside plasma sheet under disturbed geomagnetic conditions and enhanced SW Pdyn. These observations are in agreement with theoretical models.

  11. Ionospheric control of the dawn-dusk asymmetry of the Mars magnetotail current sheet

    NASA Astrophysics Data System (ADS)

    Liemohn, Michael W.; Xu, Shaosui; Dong, Chuanfei; Bougher, Stephen W.; Johnson, Blake C.; Ilie, Raluca; De Zeeuw, Darren L.

    2017-06-01

    This study investigates the role of solar EUV intensity at controlling the location of the Mars magnetotail current sheet and the structure of the lobes. Four simulation results are examined from a multifluid magnetohydrodynamic model. The solar wind and interplanetary magnetic field (IMF) conditions are held constant, and the Mars crustal field sources are omitted from the simulation configuration. This isolates the influence of solar EUV. It is found that solar maximum conditions, regardless of season, result in a Venus-like tail configuration with the current sheet shifted to the -Y (dawnside) direction. Solar minimum conditions result in a flipped tail configuration with the current sheet shifted to the +Y (duskside) direction. The lobes follow this pattern, with the current sheet shifting away from the larger lobe with the higher magnetic field magnitude. The physical process responsible for this solar EUV control of the magnetotail is the magnetization of the dayside ionosphere. During solar maximum, the ionosphere is relatively strong and the draped IMF field lines quickly slip past Mars. At solar minimum, the weaker ionosphere allows the draped IMF to move closer to the planet. These lower altitudes of the closest approach of the field line to Mars greatly hinder the day-to-night flow of magnetic flux. This results in a buildup of magnetic flux in the dawnside lobe as the S-shaped topology on that side of the magnetosheath extends farther downtail. The study demonstrates that the Mars dayside ionosphere exerts significant control over the nightside induced magnetosphere of that planet.Plain Language SummaryMars, which does not have a strong magnetic field, has an induced magnetic environment from the draping of the interplanetary magnetic field from the Sun. It folds around Mars, forming two "lobes" of magnetic field behind the planet with a current <span class="hlt">sheet</span> of electrified gas (plasma) behind it. The current <span class="hlt">sheet</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/39852-new-high-strength-high-conductivity-cu-ag-alloy-sheets','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/39852-new-high-strength-high-conductivity-cu-ag-alloy-sheets"><span>New high-strength, high-conductivity Cu-Ag alloy <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Sakai, Y.; Inoue, K.; Maeda, H.</p> <p>1995-04-01</p> <p>A <span class="hlt">sheet</span>-conductor fabrication method has been developed for Cu-Ag alloys containing 6--24 wt% Ag in which high-strength and high-conductivity are obtained by coldworking combined with intermediate heat treatments. The intermediate heat treatments were repeated three times at 400--450 C for 1--2 h at appropriate stages of cold-rolling. The optimized Cu-24 wt% Ag alloy <span class="hlt">sheet</span> with a 96% reduction ratio shows an ultimate tensile strength of 1,050 MPa and an electrical conductivity of 75% IACS at room temperature. Anisotropy in the strength with respect to the rolling <span class="hlt">direction</span> is less than 10%, and no anisotropy in the electrical conductivity occurs. Themore » authors demonstrated the ability to manufacture the Cu-Ag <span class="hlt">sheets</span> for Bitter magnet on a commercial basis. The <span class="hlt">sheets</span> fabricated by this method are promising as conductors for high-field Bitter magnet coils.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5509018','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5509018"><span>Neurovascular Cell <span class="hlt">Sheet</span> Transplantation in a Canine Model of Intracranial Hemorrhage</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Lee, Woo-Jin; Lee, Jong Young; Jung, Keun-Hwa; Lee, Soon-Tae; Kim, Hyo Yeol; Park, Dong-Kyu; Yu, Jung-Suk; Kim, So-Yun; Jeon, Daejong; Kim, Manho; Lee, Sang Kun; Roh, Jae-Kyu; Chu, Kon</p> <p>2017-01-01</p> <p>Cell-based therapy for intracerebral hemorrhage (ICH) has a great therapeutic potential. However, methods to effectively induce <span class="hlt">direct</span> regeneration of the damaged neural tissue after cell transplantation have not been established, which, if done, would improve the efficacy of cell-based therapy. In this study, we aimed to develop a cell <span class="hlt">sheet</span> with neurovasculogenic potential and evaluate its usefulness in a canine ICH model. We designed a composite cell <span class="hlt">sheet</span> made of neural progenitors derived from human olfactory neuroepithelium and vascular progenitors from human adipose tissue-derived stromal cells. We also generated a physiologic canine ICH model by manually injecting and then infusing autologous blood under arterial pressure. We transplanted the <span class="hlt">sheet</span> cells (cell <span class="hlt">sheet</span> group) or saline (control group) at the cortex over the hematoma at subacute stages (2 weeks from ICH induction). At 4 weeks from the cell transplantation, cell survival, migration, and differentiation were evaluated. Hemispheric atrophy and neurobehavioral recovery were also compared between the groups. As a result, the cell <span class="hlt">sheet</span> was rich in extracellular matrices and expressed neurotrophic factors as well as the markers for neuronal development. After transplantation, the cells successfully survived for 4 weeks, and a large portion of those migrated to the perihematomal site and differentiated into neurons and pericytes (20% and 30% of migrated stem cells, respectively). Transplantation of cell <span class="hlt">sheets</span> alleviated hemorrhage-related hemispheric atrophy (p = 0.042) and showed tendency for improving functional recovery (p = 0.062). Therefore, we concluded that the cell <span class="hlt">sheet</span> transplantation technique might induce <span class="hlt">direct</span> regeneration of neural tissue and might improve outcomes of intracerebral hemorrhage. PMID:28713638</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016MS%26E..124a2168S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016MS%26E..124a2168S"><span>Stampless fabrication of <span class="hlt">sheet</span> bars using disposable templates</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smolentsev, V. P.; Safonov, S. V.; Smolentsev, E. V.; Fedonin, O. N.</p> <p>2016-04-01</p> <p>The article is devoted to the new method of small-scale fabrication of <span class="hlt">sheet</span> bars. The procedure is performed by using disposable overlay templates, or those associated with a <span class="hlt">sheet</span>, which parameters are obtained <span class="hlt">directly</span> from the drawing. The proposed method used as a substitution of die cutting enables to intensify the preparatory technological process, which is particularly effective when launching the market-oriented items into production. It significantly increases the competitiveness of mechanical engineering and creates the conditions for technical support of present-day flexible production systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29920963','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29920963"><span>Diffuse light-<span class="hlt">sheet</span> microscopy for stripe-free calcium imaging of neural populations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Taylor, Michael A; Vanwalleghem, Gilles C; Favre-Bulle, Itia A; Scott, Ethan K</p> <p>2018-06-19</p> <p>Light-<span class="hlt">sheet</span> microscopy is used extensively in developmental biology and neuroscience. One limitation of this approach is that absorption and scattering produces shadows in the illuminating light <span class="hlt">sheet</span>, resulting in stripe artifacts. Here, we introduce diffuse light-<span class="hlt">sheet</span> microscopes that use a line diffuser to randomize the light propagation within the image plane, allowing the light <span class="hlt">sheets</span> to reform after obstacles. We incorporate diffuse light <span class="hlt">sheets</span> in two existing configurations: selective plane illumination microscopy (SPIM) in which the sample is illuminated with a static <span class="hlt">sheet</span> of light, and digitally scanned light <span class="hlt">sheet</span> (DSLS) in which a thin Gaussian beam is scanned across the image plane during each acquisition. We compare diffuse light-<span class="hlt">sheet</span> microscopes to their conventional counterparts for calcium imaging of neural <span class="hlt">activity</span> in larval zebrafish. We show that stripe artifacts can cast deep shadows that conceal some neurons, and that the stripes can flicker, producing spurious signals that could be interpreted as biological <span class="hlt">activity</span>. Diffuse light <span class="hlt">sheets</span> mitigate these problems, illuminating the blind spots produced by stripes and removing artifacts produced by the stripes' movements. The upgrade to diffuse light <span class="hlt">sheets</span> is simple and inexpensive, especially in the case of DSLS, where it requires the addition of one optical element. This article is protected by copyright. All rights reserved. This article is protected by copyright. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23197526','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23197526"><span>Ice-<span class="hlt">sheet</span> response to oceanic forcing.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Joughin, Ian; Alley, Richard B; Holland, David M</p> <p>2012-11-30</p> <p>The ice <span class="hlt">sheets</span> of Greenland and Antarctica are losing ice at accelerating rates, much of which is a response to oceanic forcing, especially of the floating ice shelves. Recent observations establish a clear correspondence between the increased delivery of oceanic heat to the ice-<span class="hlt">sheet</span> margin and increased ice loss. In Antarctica, most of these processes are reasonably well understood but have not been rigorously quantified. In Greenland, an understanding of the processes by which warmer ocean temperatures drive the observed retreat remains elusive. Experiments designed to identify the relevant processes are confounded by the logistical difficulties of instrumenting ice-choked fjords with <span class="hlt">actively</span> calving glaciers. For both ice <span class="hlt">sheets</span>, multiple challenges remain before the fully coupled ice-ocean-atmosphere models needed for rigorous sea-level projection are available.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3243706','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3243706"><span>Mechanochemical Modeling of Dynamic Microtubule Growth Involving <span class="hlt">Sheet</span>-to-Tube Transition</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ji, Xiang-Ying; Feng, Xi-Qiao</p> <p>2011-01-01</p> <p>Microtubule dynamics is largely influenced by nucleotide hydrolysis and the resultant tubulin configuration changes. The GTP cap model has been proposed to interpret the stabilizing mechanisms of microtubule growth from the view of hydrolysis effects. Besides, the growth of a microtubule involves the closure of a curved <span class="hlt">sheet</span> at its growing end. The curvature conversion from the longitudinal <span class="hlt">direction</span> to the circumferential <span class="hlt">direction</span> also helps to stabilize the successive growth, and the curved <span class="hlt">sheet</span> is referred to as the conformational cap. However, there still lacks theoretical investigation on the mechanical–chemical coupling growth process of microtubules. In this paper, we study the growth mechanisms of microtubules by using a coarse-grained molecular method. First, the closure process involving a <span class="hlt">sheet</span>-to-tube transition is simulated. The results verify the stabilizing effect of the <span class="hlt">sheet</span> structure and predict that the minimum conformational cap length that can stabilize the growth is two dimers. Then, we show that the conformational cap and the GTP cap can function independently and harmoniously, signifying the pivotal role of mechanical factors. Furthermore, based on our theoretical results, we describe a Tetris-like growth style of microtubules: the stochastic tubulin assembly is regulated by energy and harmonized with the seam zipping such that the <span class="hlt">sheet</span> keeps a practically constant length during growth. PMID:22205994</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/4203901','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/4203901"><span>PRODUCTION OF <span class="hlt">SHEET</span> FROM PARTICULATE MATERIAL</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Blainey, A.</p> <p>1959-05-12</p> <p>A process is presented for forming coherent <span class="hlt">sheet</span> material from particulate material such as granular or powdered metal, granular or powdered oxide, slurries, pastes, and plastic mixes which cohere under pressure. The primary object is to avoid the use of expensive and/ or short lived pressing tools, that is, dies and specially profiled rolls, and so to reduce the cost of the product and to prcvide in a simple manner for the making of the product in a variety of shapes or sizes. The <span class="hlt">sheet</span> material is formed when the particulate material is laterally confined in a boundary material deformable in all lateral <span class="hlt">directions</span> under axial pressure and then axially compressing the layer of particulate material together with the boundary material.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2628249','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2628249"><span>Influence of Silicone <span class="hlt">Sheets</span> on Microvascular Anastomosis</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kloeppel, Marcus; Hoehnke, Christoph; Staudenmaier, Rainer</p> <p>2008-01-01</p> <p>The use of silicone products combined with free flap transfer is well established in reconstructive surgery. We determined the risk of thrombosis as a result of <span class="hlt">direct</span> contact between the silicone <span class="hlt">sheet</span> and the point of microanastomosis. We performed microvascular surgery in 24 female Chinchilla Bastard rabbits weighing 3500 to 4000 g using two groups: Group 1 (n = 12), microanastomosis <span class="hlt">directly</span> in contact with silicone <span class="hlt">sheets</span>; and Group 2 (n = 12), microanastomosis protected by a 2 × 3 × 1-cm muscle cuff before being placed in contact with the silicone. We assessed flow-through of the microanastomosis by selective microangiography and histology at 1 and 3 weeks. All microanastomoses in Group 1 were occluded by postoperative thromboses, whereas all microanastomoses in Group 2 had adequate flow-through. Histologic analysis revealed thromboses in Group 1 formed from collagenous bundles of fiber securely attached to the intraluminal wall of the vessel. Three weeks after the procedure, these thromboses were canalized by varying small vessels. In Group 2, a slight luminal stenosis with evidence of infiltration of inflammatory cells at the microanastomosis line was observed histologically in all cases. Prefabricated flaps using silicone <span class="hlt">sheets</span> and muscular cuffs placed around the anastomoses appear to reduce the risk of thrombosis and enhance neovascularization. PMID:18636304</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AnGeo..26.3525S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AnGeo..26.3525S"><span>Magnetic configurations of the tilted current <span class="hlt">sheets</span> in magnetotail</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shen, C.; Rong, Z. J.; Li, X.; Dunlop, M.; Liu, Z. X.; Malova, H. V.; Lucek, E.; Carr, C.</p> <p>2008-11-01</p> <p>In this research, the geometrical structures of tilted current <span class="hlt">sheet</span> and tail flapping waves have been analysed based on multiple spacecraft measurements and some features of the tilted current <span class="hlt">sheets</span> have been made clear for the first time. The geometrical features of the tilted current <span class="hlt">sheet</span> revealed in this investigation are as follows: (1) The magnetic field lines (MFLs) in the tilted current <span class="hlt">sheet</span> are generally plane curves and the osculating planes in which the MFLs lie are about vertical to the equatorial plane, while the normal of the tilted current <span class="hlt">sheet</span> leans severely to the dawn or dusk side. (2) The tilted current <span class="hlt">sheet</span> may become very thin, the half thickness of its neutral <span class="hlt">sheet</span> is generally much less than the minimum radius of the curvature of the MFLs. (3) In the neutral <span class="hlt">sheet</span>, the field-aligned current density becomes very large and has a maximum value at the center of the current <span class="hlt">sheet</span>. (4) In some cases, the current density is a bifurcated one, and the two humps of the current density often superpose two peaks in the gradient of magnetic strength, indicating that the magnetic gradient drift current is possibly responsible for the formation of the two humps of the current density in some tilted current <span class="hlt">sheets</span>. Tilted current <span class="hlt">sheets</span> often appear along with tail current <span class="hlt">sheet</span> flapping waves. It is found that, in the tail flapping current <span class="hlt">sheets</span>, the minimum curvature radius of the MFLs in the current <span class="hlt">sheet</span> is rather large with values around 1 RE, while the neutral <span class="hlt">sheet</span> may be very thin, with its half thickness being several tenths of RE. During the flapping waves, the current <span class="hlt">sheet</span> is tilted substantially, and the maximum tilt angle is generally larger than 45°. The phase velocities of these flapping waves are several tens km/s, while their periods and wavelengths are several tens of minutes, and several earth radii, respectively. These tail flapping events generally last several hours and occur during quiet periods or periods of weak</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_8 --> <div id="page_9" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="161"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014APS..MARY11001C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014APS..MARY11001C"><span>Beating the Heat: Fast Scanning Melts Beta <span class="hlt">Sheet</span> Crystals</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cebe, Peggy; Hu, Xiao; Kaplan, David; Zhuravlev, Evgeny; Wurm, Andreas; Arbeiter, Daniella; Schick, Christoph</p> <p>2014-03-01</p> <p>Beta-pleated-<span class="hlt">sheet</span> crystals are among the most stable of protein secondary structures, and are responsible for the remarkable physical properties of many fibrous proteins, such as silk. Previous thinking was that beta-pleated-<span class="hlt">sheet</span> crystals in the dry solid state would not melt upon input of heat energy alone. Indeed, at conventional heating rates (~1-50 °C/min), silk exhibits its glass transition (~175 °C), followed by cold crystallization, and then by immediate thermal degradation beginning at about 225 °C. Here we demonstrate that beta-pleated-<span class="hlt">sheet</span> crystals can melt <span class="hlt">directly</span> from the solid state to become random coils, helices, and turns. We use fast scanning chip calorimetry at 2,000 K/s to avoid thermal degradation, and report the first reversible thermal melting of protein beta-pleated-<span class="hlt">sheet</span> crystals, exemplified by silk fibroin. The similarity between thermal melting behavior of lamellar crystals of synthetic polymers and beta-pleated-<span class="hlt">sheet</span> crystals is confirmed. The authors acknowledge support from the National Science Foundation and German Academic Exchange Service DAAD; EZ acknowledges a European Union funded Marie Curie EST fellowship (ADVATEC); XH and DK acknowledge NIH P41 Tissue Engineering Resource Center.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25055727','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25055727"><span>Self-enhanced catalytic <span class="hlt">activities</span> of functionalized graphene <span class="hlt">sheets</span> in the combustion of nitromethane: molecular dynamic simulations by molecular reactive force field.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhang, Chaoyang; Wen, Yushi; Xue, Xianggui</p> <p>2014-08-13</p> <p>Functionalized graphene <span class="hlt">sheet</span> (FGS) is a promising additive that enhances fuel/propellant combustion, and the determination of its mechanism has attracted much interest. In the present study, a series of molecular dynamic simulations based on a reactive force field (ReaxFF) are performed to explore the catalytic <span class="hlt">activity</span> (CA) of FGS in the thermal decay of nitromethane (NM, CH3NO2). FGSs and pristine graphene <span class="hlt">sheets</span> (GSs) are oxidized in hot NM liquid to increase their functionalities and subsequently show self-enhanced CAs during the decay. The CAs result from the interatomic exchanges between the functional groups on the <span class="hlt">sheets</span> and the NM liquid, i.e., mainly between H and O atoms. CA is dependent on the density of NM, functionalities of <span class="hlt">sheets</span>, and temperature. The GSs and FGSs that originally exhibit different functionalities tend to possess similar functionalities and consequently similar CAs as temperature increases. Other carbon materials and their oxides can accelerate combustion of other fuels/propellants similar to NM, provided that they can be dispersed and their key reaction steps in combustion are similar to NM.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1410841-room-temperature-mechanical-properties-electron-beam-welded-zircaloy-sheet','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1410841-room-temperature-mechanical-properties-electron-beam-welded-zircaloy-sheet"><span>Room temperature mechanical properties of electron beam welded zircaloy-4 <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Parga, C. J.; Rooyen, I. J.; Coryell, B. D.</p> <p></p> <p>Room temperature mechanical properties of electron beam welded and plain Zircaloy-4 <span class="hlt">sheet</span> (1.6mm thick) have been measured and compared. Various welding parameters were utilized to join <span class="hlt">sheet</span> material. Electron beam welded specimens and as-received <span class="hlt">sheet</span> specimens show comparable mechanical properties. Zr-4 <span class="hlt">sheet</span> displays anisotropy; tensile properties measured for transverse display higher elastic modulus, yield strength, reduction of area and slightly lower ductility than for the longitudinal (rolling <span class="hlt">direction</span>). Higher welding power increases the alloy’s hardness, elastic modulus and yield strength, with a corresponding decrease in tensile strength and ductility. The hardness measured at weld is comparable to the parent metalmore » hardness. Hardness at heat-affected-zone is slightly higher. Electron microscopic examination shows distinct microstructure morphology and grain size at the weld zone, HAZ and parent metal. A correlation between welding parameters, mechanical properties and microstructural features was established for electron beam welded Zircaloy-4 <span class="hlt">sheet</span> material.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1410841-room-temperature-mechanical-properties-electron-beam-welded-zircaloy-sheet','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1410841-room-temperature-mechanical-properties-electron-beam-welded-zircaloy-sheet"><span>Room temperature mechanical properties of electron beam welded zircaloy-4 <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Parga, C. J.; Rooyen, I. J.; Coryell, B. D.; ...</p> <p>2017-11-04</p> <p>Room temperature mechanical properties of electron beam welded and plain Zircaloy-4 <span class="hlt">sheet</span> (1.6mm thick) have been measured and compared. Various welding parameters were utilized to join <span class="hlt">sheet</span> material. Electron beam welded specimens and as-received <span class="hlt">sheet</span> specimens show comparable mechanical properties. Zr-4 <span class="hlt">sheet</span> displays anisotropy; tensile properties measured for transverse display higher elastic modulus, yield strength, reduction of area and slightly lower ductility than for the longitudinal (rolling <span class="hlt">direction</span>). Higher welding power increases the alloy’s hardness, elastic modulus and yield strength, with a corresponding decrease in tensile strength and ductility. The hardness measured at weld is comparable to the parent metalmore » hardness. Hardness at heat-affected-zone is slightly higher. Electron microscopic examination shows distinct microstructure morphology and grain size at the weld zone, HAZ and parent metal. A correlation between welding parameters, mechanical properties and microstructural features was established for electron beam welded Zircaloy-4 <span class="hlt">sheet</span> material.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28649411','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28649411"><span>The microbiome of glaciers and ice <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Anesio, Alexandre M; Lutz, Stefanie; Chrismas, Nathan A M; Benning, Liane G</p> <p>2017-01-01</p> <p>Glaciers and ice <span class="hlt">sheets</span>, like other biomes, occupy a significant area of the planet and harbour biological communities with distinct interactions and feedbacks with their physical and chemical environment. In the case of the glacial biome, the biological processes are dominated almost exclusively by microbial communities. Habitats on glaciers and ice <span class="hlt">sheets</span> with enough liquid water to sustain microbial <span class="hlt">activity</span> include snow, surface ice, cryoconite holes, englacial systems and the interface between ice and overridden rock/soil. There is a remarkable similarity between the different specific glacial habitats across glaciers and ice <span class="hlt">sheets</span> worldwide, particularly regarding their main primary producers and ecosystem engineers. At the surface, cyanobacteria dominate the carbon production in aquatic/sediment systems such as cryoconite holes, while eukaryotic Zygnematales and Chlamydomonadales dominate ice surfaces and snow dynamics, respectively. Microbially driven chemolithotrophic processes associated with sulphur and iron cycle and C transformations in subglacial ecosystems provide the basis for chemical transformations at the rock interface under the ice that underpin an important mechanism for the delivery of nutrients to downstream ecosystems. In this review, we focus on the main ecosystem engineers of glaciers and ice <span class="hlt">sheets</span> and how they interact with their chemical and physical environment. We then discuss the implications of this microbial <span class="hlt">activity</span> on the icy microbiome to the biogeochemistry of downstream ecosystems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017PhRvE..95b3209K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017PhRvE..95b3209K"><span>Criticality and turbulence in a resistive magnetohydrodynamic current <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Klimas, Alexander J.; Uritsky, Vadim M.</p> <p>2017-02-01</p> <p>Scaling properties of a two-dimensional (2d) plasma physical current-<span class="hlt">sheet</span> simulation model involving a full set of magnetohydrodynamic (MHD) equations with current-dependent resistivity are investigated. The current <span class="hlt">sheet</span> supports a spatial magnetic field reversal that is forced through loading of magnetic flux containing plasma at boundaries of the simulation domain. A balance is reached between loading and annihilation of the magnetic flux through reconnection at the current <span class="hlt">sheet</span>; the transport of magnetic flux from boundaries to current <span class="hlt">sheet</span> is realized in the form of spatiotemporal avalanches exhibiting power-law statistics of lifetimes and sizes. We identify this dynamics as self-organized criticality (SOC) by verifying an extended set of scaling laws related to both global and local properties of the current <span class="hlt">sheet</span> (critical susceptibility, finite-size scaling of probability distributions, geometric exponents). The critical exponents obtained from this analysis suggest that the model operates in a slowly driven SOC state similar to the mean-field state of the <span class="hlt">directed</span> stochastic sandpile model. We also investigate multiscale correlations in the velocity field and find them numerically indistinguishable from certain intermittent turbulence (IT) theories. The results provide clues on physical conditions for SOC behavior in a broad class of plasma systems with propagating instabilities, and suggest that SOC and IT may coexist in driven current <span class="hlt">sheets</span> which occur ubiquitously in astrophysical and space plasmas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28297949','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28297949"><span>Criticality and turbulence in a resistive magnetohydrodynamic current <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Klimas, Alexander J; Uritsky, Vadim M</p> <p>2017-02-01</p> <p>Scaling properties of a two-dimensional (2d) plasma physical current-<span class="hlt">sheet</span> simulation model involving a full set of magnetohydrodynamic (MHD) equations with current-dependent resistivity are investigated. The current <span class="hlt">sheet</span> supports a spatial magnetic field reversal that is forced through loading of magnetic flux containing plasma at boundaries of the simulation domain. A balance is reached between loading and annihilation of the magnetic flux through reconnection at the current <span class="hlt">sheet</span>; the transport of magnetic flux from boundaries to current <span class="hlt">sheet</span> is realized in the form of spatiotemporal avalanches exhibiting power-law statistics of lifetimes and sizes. We identify this dynamics as self-organized criticality (SOC) by verifying an extended set of scaling laws related to both global and local properties of the current <span class="hlt">sheet</span> (critical susceptibility, finite-size scaling of probability distributions, geometric exponents). The critical exponents obtained from this analysis suggest that the model operates in a slowly driven SOC state similar to the mean-field state of the <span class="hlt">directed</span> stochastic sandpile model. We also investigate multiscale correlations in the velocity field and find them numerically indistinguishable from certain intermittent turbulence (IT) theories. The results provide clues on physical conditions for SOC behavior in a broad class of plasma systems with propagating instabilities, and suggest that SOC and IT may coexist in driven current <span class="hlt">sheets</span> which occur ubiquitously in astrophysical and space plasmas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSM13B2380L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSM13B2380L"><span>Intrinsic Dawn-Dusk Asymmetry of Magnetotail Thin Current <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lu, S.; Pritchett, P. L.; Angelopoulos, V.; Artemyev, A.</p> <p>2017-12-01</p> <p>Magnetic reconnection and its related phenomena (flux ropes, dipolarization fronts, bursty bulk flows, particle injections, etc.) occur more frequently on the duskside in the Earth's magnetotail. Magnetohydrodynamic simulations attributed the asymmetry to the nonuniform ionospheric conductance through global scale magnetosphere-ionosphere interaction. Hybrid simulations, on the other hand, found an alternative responsible mechanism: the Hall effect in the magnetotail thin current <span class="hlt">sheet</span>, but left an open question: What is the physical origin of the asymmetric Hall effect? The answer could be the temperature difference on the two sides and/or the dawn-dusk transportation of magnetic flux and plasmas. In this work, we use 3-D particle-in-cell simulations to further explore the magnetotail dawn-dusk asymmetry. The magnetotail equilibrium contains a dipole magnetic field and a current <span class="hlt">sheet</span> region. The simulation is driven by a symmetric and localized (in the y <span class="hlt">direction</span>) high-latitude electric field, under which the current <span class="hlt">sheet</span> thins with a decrease of Bz. During the same time, a dawn-dusk asymmetry is formed intrinsically in the thin current <span class="hlt">sheet</span>, with a smaller Bz, a stronger Hall effect (indicated by the Hall electric field Ez), and a stronger cross-tail current jy on the duskside. The deep origin of the asymmetry is also shown to be dominated by the dawnward E×B drift of magnetic flux and plasmas. A <span class="hlt">direct</span> consequence of this intrinsic dawn-dusk asymmetry is that it favors magnetotail reconnection and related phenomena to preferentially occur on the duskside.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/29771','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/29771"><span>Tests for Z-<span class="hlt">direction</span> fiber orientation</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>David W. Vahey; John M. Considine</p> <p>2007-01-01</p> <p>Fibers that acquire a Z-<span class="hlt">direction</span> tilt in the forming process help bond adjacent strata of the paper <span class="hlt">sheet</span>, increasing Z-<span class="hlt">direction</span> shear and other properties. For certain tests, this manifests itself as a test difference upon 180° in-plane rotation of the <span class="hlt">sheet</span>. Seven of eight different paper grades ranging in grammage from 73 to 268 g/m2 were found to show this...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014PhFl...26a2103K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014PhFl...26a2103K"><span>Electric field induced <span class="hlt">sheeting</span> and breakup of dielectric liquid jets</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Khoshnevis, Ahmad; Tsai, Scott S. H.; Esmaeilzadeh, Esmaeil</p> <p>2014-01-01</p> <p>We report experimental observations of the controlled deformation of a dielectric liquid jet subjected to a local high-voltage electrostatic field in the <span class="hlt">direction</span> normal to the jet. The jet deforms to the shape of an elliptic cylinder upon application of a normal electrostatic field. As the applied electric field strength is increased, the elliptic cylindrical jet deforms permanently into a flat <span class="hlt">sheet</span>, and eventually breaks-up into droplets. We interpret this observation—the stretch of the jet is in the normal <span class="hlt">direction</span> to the applied electric field—qualitatively using the Taylor-Melcher leaky dielectric theory, and develop a simple scaling model that predicts the critical electric field strength for the jet-to-<span class="hlt">sheet</span> transition. Our model shows a good agreement with experimental results, and has a form that is consistent with the classical drop deformation criterion in the Taylor-Melcher theory. Finally, we statistically analyze the resultant droplets from <span class="hlt">sheet</span> breakup, and find that increasing the applied electric field strength improves droplet uniformity and reduces droplet size.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19770003212','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19770003212"><span>A thrust-<span class="hlt">sheet</span> propulsion concept using fissionable elements</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Moeckel, W. E.</p> <p>1976-01-01</p> <p>A space propulsion concept is proposed and analyzed which consists of a thin <span class="hlt">sheet</span> coated on one side with fissionable material, so that nuclear power is converted <span class="hlt">directly</span> into propulsive power. Thrust is available both from ejected fission fragments and from thermal radiation. Optimum thicknesses are determined for the <span class="hlt">active</span> and substrate layers. This concept is shown to have potential mission capability (in terms of velocity increments) superior to that of all other advanced propulsion concepts for which performance estimates are available. A suitable spontaneously fissioning material such as Cf254 could provide an extremely high-performance first stage beyond earth orbit. In contrast with some other advanced nuclear propulsion concepts, there is no minimum size below which this concept is infeasible.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19770030165&hterms=1042&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2526%25231042','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19770030165&hterms=1042&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2526%25231042"><span>A thrust-<span class="hlt">sheet</span> propulsion concept using fissionable elements</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Moeckel, W. E.</p> <p>1976-01-01</p> <p>A space propulsion concept is proposed and analyzed which consists of a thin <span class="hlt">sheet</span> coated on one side with fissionable material, so that nuclear power is converted <span class="hlt">directly</span> into propulsive power. Thrust is available both from ejected fission fragments and from thermal radiation. Optimum thicknesses are determined for the <span class="hlt">active</span> and substrate layers. This concept is shown to have potential mission capability (in terms of velocity increments) superior to that of all other advanced propulsion concepts for which performance estimates are available. A suitable spontaneously fissioning material such as Cf-254 could provide an extremely high-performance first stage beyond earth orbit. In contrast with some other advanced nuclear propulsion concepts, there is no minimum size below which this concept is infeasible.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1813272G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1813272G"><span>ISMIP6 - initMIP: Greenland ice <span class="hlt">sheet</span> model initialisation experiments</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Goelzer, Heiko; Nowicki, Sophie; Payne, Tony; Larour, Eric; Abe Ouchi, Ayako; Gregory, Jonathan; Lipscomb, William; Seroussi, Helene; Shepherd, Andrew; Edwards, Tamsin</p> <p>2016-04-01</p> <p>Earlier large-scale Greenland ice <span class="hlt">sheet</span> sea-level projections e.g. those run during ice2sea and SeaRISE initiatives have shown that ice <span class="hlt">sheet</span> initialisation can have a large effect on the projections and gives rise to important uncertainties. This intercomparison exercise (initMIP) aims at comparing, evaluating and improving the initialization techniques used in the ice <span class="hlt">sheet</span> modeling community and to estimate the associated uncertainties. It is the first in a series of ice <span class="hlt">sheet</span> model intercomparison <span class="hlt">activities</span> within ISMIP6 (Ice <span class="hlt">Sheet</span> Model Intercomparison Project for CMIP6). The experiments are conceived for the large-scale Greenland ice <span class="hlt">sheet</span> and are designed to allow intercomparison between participating models of 1) the initial present-day state of the ice <span class="hlt">sheet</span> and 2) the response in two schematic forward experiments. The latter experiments serve to evaluate the initialisation in terms of model drift (forward run without any forcing) and response to a large perturbation (prescribed surface mass balance anomaly). We present and discuss first results of the intercomparison and highlight important uncertainties with respect to projections of the Greenland ice <span class="hlt">sheet</span> sea-level contribution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23708437','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23708437"><span>Synthesis of N-doped microporous carbon via chemical <span class="hlt">activation</span> of polyindole-modified graphene oxide <span class="hlt">sheets</span> for selective carbon dioxide adsorption.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Saleh, Muhammad; Chandra, Vimlesh; Kemp, K Christian; Kim, Kwang S</p> <p>2013-06-28</p> <p>A polyindole-reduced graphene oxide (PIG) hybrid was synthesized by reducing graphene oxide <span class="hlt">sheets</span> in the presence of polyindole. We have shown PIG as a material for capturing carbon dioxide (CO2). The PIG hybrid was chemically <span class="hlt">activated</span> at temperatures of 400-800 °C, which resulted in nitrogen (N)-doped graphene <span class="hlt">sheets</span>. The N-doped graphene <span class="hlt">sheets</span> are microporous with an adsorption pore size of 0.6 nm for CO2 and show a maximum (Brunauer, Emmet and Teller) surface area of 936 m(2) g(-1). The hybrid <span class="hlt">activated</span> at 600 °C (PIG6) possesses a surface area of 534 m(2) g(-1) and a micropore volume of 0.29 cm(3) g(-1). PIG6 shows a maximum CO2 adsorption capacity of 3.0 mmol g(-1) at 25 °C and 1 atm. This high CO2 uptake is due to the highly microporous character of the material and its N content. The material retains its original adsorption capacity on recycling even after 10 cycles (within experimental error). PIG6 also shows high adsorption selectivity ratios for CO2 over N2, CH4 and H2 of 23, 4 and 85 at 25 °C, respectively.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24586898','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24586898"><span>The <span class="hlt">direction</span> of stretch-induced cell and stress fiber orientation depends on collagen matrix stress.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tondon, Abhishek; Kaunas, Roland</p> <p>2014-01-01</p> <p>Cell structure depends on both matrix strain and stiffness, but their interactive effects are poorly understood. We investigated the interactive roles of matrix properties and stretching patterns on cell structure by uniaxially stretching U2OS cells expressing GFP-actin on silicone rubber <span class="hlt">sheets</span> supporting either a surface-adsorbed coating or thick hydrogel of type-I collagen. Cells and their actin stress fibers oriented perpendicular to the <span class="hlt">direction</span> of cyclic stretch on collagen-coated <span class="hlt">sheets</span>, but oriented parallel to the stretch <span class="hlt">direction</span> on collagen gels. There was significant alignment parallel to the <span class="hlt">direction</span> of a steady increase in stretch for cells on collagen gels, while cells on collagen-coated <span class="hlt">sheets</span> did not align in any <span class="hlt">direction</span>. The extent of alignment was dependent on both strain rate and duration. Stretch-induced alignment on collagen gels was blocked by the myosin light-chain kinase inhibitor ML7, but not by the Rho-kinase inhibitor Y27632. We propose that <span class="hlt">active</span> orientation of the actin cytoskeleton perpendicular and parallel to <span class="hlt">direction</span> of stretch on stiff and soft substrates, respectively, are responses that tend to maintain intracellular tension at an optimal level. Further, our results indicate that cells can align along <span class="hlt">directions</span> of matrix stress without collagen fibril alignment, indicating that matrix stress can <span class="hlt">directly</span> regulate cell morphology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMSM51B2468S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMSM51B2468S"><span>Triggering of explosive reconnection in a thick current <span class="hlt">sheet</span> via current <span class="hlt">sheet</span> compression: Less current <span class="hlt">sheet</span> thinning, more temperature anisotropy</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shimizu, K.; Shinohara, I.; Fujimoto, M.</p> <p>2016-12-01</p> <p>Two-dimensional kinetic simulations of compression of thick current <span class="hlt">sheets</span> are performed to see how it can lead to triggering of explosive magnetic reconnection. The current <span class="hlt">sheet</span> under study is simply in a Harris-like anti-paralell and symmetric geometry. A one-dimensional pre-study shows that the compression is more effective to make the plasma anisotropy than to thin the current <span class="hlt">sheet</span> width. When the lobe magnetic field is amplified by a factor of 2, the plasma temperature anisotropy inside the current <span class="hlt">sheet</span> reaches 2 but the current <span class="hlt">sheet</span> thickness is reduced only by 1/sqrt(2). If a current <span class="hlt">sheet</span> thickness needs to be comparable to the ion inertial scale for reconnection triggering take place, as is widely and frequently mentioned in the research community, the initial thickness cannot be more than a few ion scale for reconnection to set-in. On the other hand, the temperature anisotropy of 2 can be significant for the triggering problem. Two-dimensional simulations show explosive magnetic reconnection to take place even when the initial current <span class="hlt">sheet</span> thickness more than an order of magnitude thicker than the ion scale, indicating the resilient triggering drive supplied by the temperature anisotropy. We also discuss how the reconnection triggering capability of the temperature anisotropy boosted tearing mode for thick current <span class="hlt">sheets</span> compares with the instabilities in the plane orthogonal to the reconnecting field.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PMag...98.1068L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PMag...98.1068L"><span>Effect of temperature on the anisotropy of AZ31 magnesium alloy rolling <span class="hlt">sheet</span> under high strain rate deformation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, Yanyu; Mao, Pingli; Zhang, Feng; Liu, Zheng; Wang, Zhi</p> <p>2018-04-01</p> <p>In order to investigate the effect of temperature on the anisotropic behaviour of AZ31 magnesium alloy rolling <span class="hlt">sheet</span> under high strain rate deformation, the Split Hopkinson Pressure Bar was used to analyse the dynamic mechanical properties of AZ31 magnesium alloy rolling <span class="hlt">sheet</span> in three <span class="hlt">directions</span>, rolling <span class="hlt">direction</span>(RD), transverse <span class="hlt">direction</span> (TD) and normal <span class="hlt">direction</span> (ND). The texture of the rolling <span class="hlt">sheet</span> was characterised by X-ray analysis and the microstructure prior and after high strain rate deformation was observed by optical microscope (OM). The results demonstrated that AZ31magnesium alloy rolling <span class="hlt">sheet</span> has strong initial {0 0 0 2} texture, which resulted at the obvious anisotropy in high strain rate deformation at 20 °C. The anisotropy reflected in stress-strain curve, yield stress, peak stress and microstructure. The anisotropy became much weaker when the deformation temperature increased up to 250 °C. Continuing to increase the deformation temperature to 350 °C the anisotropy of AZ31 rolling <span class="hlt">sheet</span> essentially disappeared. The decreasing tendency of anisotropy with increasing temperature was due to the fact that when the deformation temperature increased, the critical resolved shear stress (CRSS) for pyramidal 〈c + a〉 slip, which was the predominant slip mechanism for ND, decreased close to that of twinning, which was the predominant deformation mechanism for RD and TD. The deformation mechanism at different <span class="hlt">directions</span> and temperatures and the Schmid factor (SF) at different <span class="hlt">directions</span> were discussed in the present paper.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AIPC.1896t0010R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AIPC.1896t0010R"><span>Development of a low energy micro <span class="hlt">sheet</span> forming machine</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Razali, A. R.; Ann, C. T.; Shariff, H. M.; Kasim, N. I.; Musa, M. A.; Ahmad, A. F.</p> <p>2017-10-01</p> <p>It is expected that with the miniaturization of materials being processed, energy consumption is also being `miniaturized' proportionally. The focus of this study was to design a low energy micro-<span class="hlt">sheet</span>-forming machine for thin <span class="hlt">sheet</span> metal application and fabricate a low <span class="hlt">direct</span> current powered micro-<span class="hlt">sheet</span>-forming machine. A prototype of low energy system for a micro-<span class="hlt">sheet</span>-forming machine which includes mechanical and electronic elements was developed. The machine was tested for its performance in terms of natural frequency, punching forces, punching speed and capability, energy consumption (single punch and frequency-time based). Based on the experiments, the machine can do 600 stroke per minute and the process is unaffected by the machine's natural frequency. It was also found that sub-Joule of power was required for a single stroke of punching/blanking process. Up to 100micron thick carbon steel shim was successfully tested and punched. It concludes that low power forming machine is feasible to be developed and be used to replace high powered machineries to form micro-products/parts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29264722','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29264722"><span>One-pot exfoliation, functionalization, and size manipulation of graphene <span class="hlt">sheets</span>: efficient system for biomedical applications.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bani, Farhad; Bodaghi, Ali; Dadkhah, Abbas; Movahedi, Soodabeh; Bodaghabadi, Narges; Sadeghizadeh, Majid; Adeli, Mohsen</p> <p>2018-05-01</p> <p>In this work, we reported a facile method to produce stable aqueous graphene dispersion through <span class="hlt">direct</span> exfoliation of graphite by modified hyperbranched polyglycerol. Size of graphene <span class="hlt">sheets</span> was manipulated by simultaneous exfoliation and sonication of graphite, and functionalized graphene <span class="hlt">sheets</span> with narrow size distribution were obtained. The polyglycerol-functionalized graphene <span class="hlt">sheets</span> exhibited highly efficient cellular uptake and photothermal conversion, enabling it to serve as a photothermal agent for cancer therapy.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011JGRA..116.9218R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011JGRA..116.9218R"><span>Statistical survey on the magnetic structure in magnetotail current <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rong, Z. J.; Wan, W. X.; Shen, C.; Li, X.; Dunlop, M. W.; Petrukovich, A. A.; Zhang, T. L.; Lucek, E.</p> <p>2011-09-01</p> <p>On the basis of the multipoint magnetic observations of Cluster in the region 15-19 RE downtail, the magnetic field structure in magnetotail current <span class="hlt">sheet</span> (CS) center is statistically surveyed. It is found that the By component (in GSM coordinates) is distributed mainly within ∣By∣ < 5nT, while the Bz component is mostly positive and distributes mainly within 1˜10 nT. The plane of the magnetic field lines (MFLs) is mostly vertical to the equatorial plane, with the radius of curvature (Rc) of the MFLs being <span class="hlt">directed</span> earthward and the binormal (perpendicular to the curvature and magnetic field <span class="hlt">direction</span>) being <span class="hlt">directed</span> azimuthally westward. The curvature radius of MFLs reaches a minimum, Rc,min, at the CS center and is larger than the corresponding local half thickness of the neutral <span class="hlt">sheet</span>, h. Statistically, it is found that the overall surface of the CS, with the normal pointing basically along the south-north <span class="hlt">direction</span>, can be approximated to be a plane parallel to equatorial plane, although the local CS may be flapping and is frequently tilted to the equatorial plane. The tilted CS (normal inclined to the equatorial plane) is apt to be observed near both flanks and is mainly associated with the slippage of magnetic flux tubes. It is statistically verified that the minimum curvature radius, Rc,min, half thickness of neutral <span class="hlt">sheet</span>, h, and the slipping angle of MFLs, δ, in the CS satisfies h = Rc,min cosδ. The current density, with a mean strength of 4-8 nA/m2, basically flows azimuthally and tangentially to the surface of the CS, from dawn side to the dusk side. There is an obvious dawn-dusk asymmetry of CS, however. For magnetic local times (MLT) ˜21:00-˜01:00, the CS is relatively thinner; the minimum curvature radius of MFLs, Rc,min (0.6-1 RE) and the half-thickness of neutral <span class="hlt">sheet</span>, h (0.2-0.4 RE), are relatively smaller, and Bz (3-5 nT) and the minimum magnetic field, Bmin (5-7 nT), are weaker. It is also found that negative Bz has a higher probability</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_9 --> <div id="page_10" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="181"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900024452&hterms=population+characteristic&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dpopulation%2Bcharacteristic*','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900024452&hterms=population+characteristic&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dpopulation%2Bcharacteristic*"><span>Spectral characteristics of plasma <span class="hlt">sheet</span> ion and electron populations during undisturbed geomagnetic conditions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Christon, S. P.; Williams, D. J.; Mitchell, D. G.; Frank, L. A.; Huang, C. Y.</p> <p>1989-01-01</p> <p>The spectral characteristics of plasma-<span class="hlt">sheet</span> ion and electron populations during periods of low geomagnetic <span class="hlt">activity</span> were determined from the analysis of 127 one-hour average samples of central plasma <span class="hlt">sheet</span> ions and electrons. Particle data from the ISEE-1 low-energy proton and electron differential energy analyzer and medium-energy particle instrument were combined to obtain differential energy spectra in the plasma <span class="hlt">sheet</span> at geocentric radial distances above 12 earth radii. The relationships between the ion and electron spectral shapes and between the spectral shapes and the geomagnetic <span class="hlt">activity</span> index were statistically investigated. It was found that the presence of interplanetary particle fluxes does not affect the plasma <span class="hlt">sheet</span> particle spectral shape.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.loc.gov/pictures/collection/hh/item/ca1230.photos.011800p/','SCIGOV-HHH'); return false;" href="https://www.loc.gov/pictures/collection/hh/item/ca1230.photos.011800p/"><span>71. PALMDALE WATER COMPANY, EASTWOOD MULTIPLEARCHED DAM: STRESS <span class="hlt">SHEET</span>, <span class="hlt">SHEET</span> ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>71. PALMDALE WATER COMPANY, EASTWOOD MULTIPLE-ARCHED DAM: STRESS <span class="hlt">SHEET</span>, <span class="hlt">SHEET</span> 3; DECEMBER 20, 1918. Littlerock Water District files. - Little Rock Creek Dam, Little Rock Creek, Littlerock, Los Angeles County, CA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110009938','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110009938"><span>Formation and Reconnection of Three-Dimensional Current <span class="hlt">Sheets</span> in the Solar Corona</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Edmondson, J. K.; Antiochos, S. K.; DeVore, C. R.; Zurbuchen, T. H.</p> <p>2010-01-01</p> <p>Current-<span class="hlt">sheet</span> formation and magnetic reconnection are believed to be the basic physical processes responsible for much of the <span class="hlt">activity</span> observed in astrophysical plasmas, such as the Sun s corona. We investigate these processes for a magnetic configuration consisting of a uniform background field and an embedded line dipole, a topology that is expected to be ubiquitous in the corona. This magnetic system is driven by a uniform horizontal flow applied at the line-tied photosphere. Although both the initial field and the driver are translationally symmetric, the resulting evolution is calculated using a fully three-dimensional magnetohydrodynamic (3D MHD) simulation with adaptive mesh refinement that resolves the current <span class="hlt">sheet</span> and reconnection dynamics in detail. The advantage of our approach is that it allows us to apply <span class="hlt">directly</span> the vast body of knowledge gained from the many studies of 2D reconnection to the fully 3D case. We find that a current <span class="hlt">sheet</span> forms in close analogy to the classic Syrovatskii 2D mechanism, but the resulting evolution is different than expected. The current <span class="hlt">sheet</span> is globally stable, showing no evidence for a disruption or a secondary instability even for aspect ratios as high as 80:1. The global evolution generally follows the standard Sweet- Parker 2D reconnection model except for an accelerated reconnection rate at a very thin current <span class="hlt">sheet</span>, due to the tearing instability and the formation of magnetic islands. An interesting conclusion is that despite the formation of fully 3D structures at small scales, the system remains close to 2D at global scales. We discuss the implications of our results for observations of the solar corona. Subject Headings: Sun: corona Sun: magnetic fields Sun: reconnection</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C23A1194T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C23A1194T"><span>The Sensitivity of the Greenland Ice <span class="hlt">Sheet</span> to Glacial-Interglacial Oceanic Forcing</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tabone, I.; Blasco Navarro, J.; Robinson, A.; Alvarez-Solas, J.; Montoya, M.</p> <p>2017-12-01</p> <p>Up to now, the scientific community has mainly focused on the sensitivity of the Greenland Ice <span class="hlt">Sheet</span> (GrIS) to atmospheric variations. However, several studies suggest that the enhanced ice mass loss experienced by the GrIS in the past decades is <span class="hlt">directly</span> connected to the increasing North Atlantic temperatures. Melting of GrIS outlet glaciers triggers grounding-line retreat increasing ice discharge into the ocean. This new evidence leads to consider the ocean as a relevant driver to be taken into account when modeling the evolution of the GrIS. The ice-ocean interaction is a primary factor controling not only the likely future retreat of GrIS outlet glaciers, or the huge ice loss in past warming climates, but also, and more strongly, the past GrIS glacial expansion. The latter assumption is supported by reconstructions which propose the GrIS to be fully marine-based during glacials, and thus more exposed to the influence of the ocean. Here, for the first time, we investigate the response of the GrIS to past oceanic changes using a three-dimensional hybrid ice-<span class="hlt">sheet</span>/ice-shelf model, which combines the Shallow Ice Approximation (SIA) for slow grounded ice <span class="hlt">sheets</span> and the Shallow Shelf Approximation (SSA) in ice shelves and ice streams. The model accounts for a time-dependent parametrisation of the marine basal melting rate, which is used to reproduce past oceanic variations. In this work simulations of the last two glacial cycles are performed. Our results show that the GrIS is very sensitive to the ocean-triggered submarine melting (freezing). Mild oceanic temperature variations lead to a rapid retreat (expansion) of the GrIS margins, which, inducing a dynamic adjustment of the grounded ice <span class="hlt">sheet</span>, drive the evolution of the whole ice <span class="hlt">sheet</span>. Our results strongly suggest the need to consider the ocean as an <span class="hlt">active</span> forcing in paleo ice <span class="hlt">sheet</span> models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3504962','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3504962"><span>Photophysiology and albedo-changing potential of the ice algal community on the surface of the Greenland ice <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Yallop, Marian L; Anesio, Alexandre M; Perkins, Rupert G; Cook, Joseph; Telling, Jon; Fagan, Daniel; MacFarlane, James; Stibal, Marek; Barker, Gary; Bellas, Chris; Hodson, Andy; Tranter, Martyn; Wadham, Jemma; Roberts, Nicholas W</p> <p>2012-01-01</p> <p>Darkening of parts of the Greenland ice <span class="hlt">sheet</span> surface during the summer months leads to reduced albedo and increased melting. Here we show that heavily pigmented, <span class="hlt">actively</span> photosynthesising microalgae and cyanobacteria are present on the bare ice. We demonstrate the widespread abundance of green algae in the Zygnematophyceae on the ice <span class="hlt">sheet</span> surface in Southwest Greenland. Photophysiological measurements (variable chlorophyll fluorescence) indicate that the ice algae likely use screening mechanisms to downregulate photosynthesis when exposed to high intensities of visible and ultraviolet radiation, rather than non-photochemical quenching or cell movement. Using imaging microspectrophotometry, we demonstrate that intact cells and filaments absorb light with characteristic spectral profiles across ultraviolet and visible wavelengths, whereas inorganic dust particles typical for these areas display little absorption. Our results indicate that the phototrophic community growing <span class="hlt">directly</span> on the bare ice, through their photophysiology, most likely have an important role in changing albedo, and subsequently may impact melt rates on the ice <span class="hlt">sheet</span>. PMID:23018772</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23018772','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23018772"><span>Photophysiology and albedo-changing potential of the ice algal community on the surface of the Greenland ice <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yallop, Marian L; Anesio, Alexandre M; Perkins, Rupert G; Cook, Joseph; Telling, Jon; Fagan, Daniel; MacFarlane, James; Stibal, Marek; Barker, Gary; Bellas, Chris; Hodson, Andy; Tranter, Martyn; Wadham, Jemma; Roberts, Nicholas W</p> <p>2012-12-01</p> <p>Darkening of parts of the Greenland ice <span class="hlt">sheet</span> surface during the summer months leads to reduced albedo and increased melting. Here we show that heavily pigmented, <span class="hlt">actively</span> photosynthesising microalgae and cyanobacteria are present on the bare ice. We demonstrate the widespread abundance of green algae in the Zygnematophyceae on the ice <span class="hlt">sheet</span> surface in Southwest Greenland. Photophysiological measurements (variable chlorophyll fluorescence) indicate that the ice algae likely use screening mechanisms to downregulate photosynthesis when exposed to high intensities of visible and ultraviolet radiation, rather than non-photochemical quenching or cell movement. Using imaging microspectrophotometry, we demonstrate that intact cells and filaments absorb light with characteristic spectral profiles across ultraviolet and visible wavelengths, whereas inorganic dust particles typical for these areas display little absorption. Our results indicate that the phototrophic community growing <span class="hlt">directly</span> on the bare ice, through their photophysiology, most likely have an important role in changing albedo, and subsequently may impact melt rates on the ice <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19810023062','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19810023062"><span>Ice <span class="hlt">sheet</span> altimetry</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Brooks, R. L.</p> <p>1981-01-01</p> <p>Generalized surface slopes were computed for the Antarctic and Greenland ice <span class="hlt">sheets</span> by differencing plotted contour levels and dividing them by the distance between the contours. It was observed that more than 90% of the ice <span class="hlt">sheets</span> have surface slopes less than 1%. Seasat test mode-1 Seasat altimeter measurements over Greenland were analyzed by comparisons with collinear and intersecting normal mode Seasat altimeter passes. Over the ice <span class="hlt">sheet</span>, the computed surface elevations from test mode-1 measurements were consistently lower by about 45 m and the AGC levels were down by approximately 6 dB. No test mode-1 data were acquired over Antarctica. It is concluded that analysis of the existing altimeter data base over the two ice <span class="hlt">sheets</span> is crucial in designing a future improved altimeter tracking capability. It is recommended that additional waveform retracking be performed to characterize ice <span class="hlt">sheet</span> topography as a function of geographic area and elevation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27364369','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27364369"><span>Guided bone regeneration using individualized ceramic <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Malmström, J; Anderud, J; Abrahamsson, P; Wälivaara, D-Å; Isaksson, S G; Adolfsson, E</p> <p>2016-10-01</p> <p>Guided bone regeneration (GBR) describes the use of membranes to regenerate bony defects. A membrane for GBR needs to be biocompatible, cell-occlusive, non-toxic, and mouldable, and possess space-maintaining properties including stability. The purpose of this pilot study was to describe a new method of GBR using individualized ceramic <span class="hlt">sheets</span> to perfect bone regeneration prior to implant placement; bone regeneration was assessed using traditional histology and three-dimensional (3D) volumetric changes in the bone and soft tissue. Three patients were included. After full-thickness flap reflection, the individualized ceramic <span class="hlt">sheets</span> were fixed. The sites were left to heal for 7 months. All patients were evaluated preoperatively and at 7 months postoperative using cone beam computed tomography and 3D optical equipment. Samples of the regenerated bone and soft tissue were collected and analyzed. The bone regenerated in the entire interior volume of all <span class="hlt">sheets</span>. Bone biopsies revealed newly formed trabecular bone with a lamellar structure. Soft tissue biopsies showed connective tissue with no signs of an inflammatory response. This was considered to be newly formed periosteum. Thus ceramic individualized <span class="hlt">sheets</span> can be used to regenerate large volumes of bone in both vertical and horizontal <span class="hlt">directions</span> independent of the bone defect and with good biological acceptance of the material. Copyright © 2016 International Association of Oral and Maxillofacial Surgeons. Published by Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25319318','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25319318"><span>Cell <span class="hlt">sheet</span>-based tissue engineering for fabricating 3-dimensional heart tissues.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shimizu, Tatsuya</p> <p>2014-01-01</p> <p>In addition to stem cell biology, tissue engineering is an essential research field for regenerative medicine. In contrast to cell injection, bioengineered tissue transplantation minimizes cell loss and has the potential to repair tissue defects. A popular approach is scaffold-based tissue engineering, which utilizes a biodegradable polymer scaffold for seeding cells; however, new techniques of cell <span class="hlt">sheet</span>-based tissue engineering have been developed. Cell <span class="hlt">sheets</span> are harvested from temperature-responsive culture dishes by simply lowering the temperature. Monolayer or stacked cell <span class="hlt">sheets</span> are transplantable <span class="hlt">directly</span> onto damaged tissues and cell <span class="hlt">sheet</span> transplantation has already been clinically applied. Cardiac cell <span class="hlt">sheet</span> stacking produces pulsatile heart tissue; however, lack of vasculature limits the viable tissue thickness to 3 layers. Multistep transplantation of triple-layer cardiac cell <span class="hlt">sheets</span> cocultured with endothelial cells has been used to form thick vascularized cardiac tissue in vivo. Furthermore, in vitro functional blood vessel formation within 3-dimensional (3D) tissues has been realized by successfully imitating in vivo conditions. Triple-layer cardiac cell <span class="hlt">sheets</span> containing endothelial cells were layered on vascular beds and the constructs were media-perfused using novel bioreactor systems. Interestingly, cocultured endothelial cells migrate into the vascular beds and form perfusable blood vessels. An in vitro multistep procedure has also enabled the fabrication of thick, vascularized heart tissues. Cell <span class="hlt">sheet</span>-based tissue engineering has revealed great potential to fabricate 3D cardiac tissues and should contribute to future treatment of severe heart diseases and human tissue model production.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900054857&hterms=magnetic+cooling&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dmagnetic%2Bcooling','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900054857&hterms=magnetic+cooling&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dmagnetic%2Bcooling"><span>Heating and cooling of the earth's plasma <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Goertz, C. K.</p> <p>1990-01-01</p> <p>Magnetic-field models based on pressure equilibrium in the quiet magnetotail require nonadiabatic cooling of the plasma as it convects inward or a decrease of the flux tube content. Recent in situ observations of plasma density and temperature indicate that, during quiet convection, the flux tube content may actually increase. Thus the plasma must be cooled during quiet times. The earth plasma <span class="hlt">sheet</span> is generally significantly hotter after the expansion phase of a substorm than before the plasma <span class="hlt">sheet</span> thinning begins and cools during the recovery phase. Heating mechanisms such as reconnection, current <span class="hlt">sheet</span> acceleration, plasma expansion, and resonant absorption of surface waves are discussed. It seems that all mechanisms are <span class="hlt">active</span>, albeit in different regions of the plasma <span class="hlt">sheet</span>. Near-earth tail signatures of substorms require local heating as well as a decrease of the flux tube content. It is shown that the resonant absorption of surface waves can provide both.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.loc.gov/pictures/collection/hh/item/nj0254.photos.110293p/','SCIGOV-HHH'); return false;" href="https://www.loc.gov/pictures/collection/hh/item/nj0254.photos.110293p/"><span>5. Historic American Buildings Survey Taken from drawing <span class="hlt">sheet</span>, <span class="hlt">SHEET</span> ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>5. Historic American Buildings Survey Taken from drawing <span class="hlt">sheet</span>, <span class="hlt">SHEET</span> #21, Showing the house as restored since Survey. (Dormer windows omitted as not authentic) - Samuel des Marest House, River Road, New Milford, Bergen County, NJ</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20050207500&hterms=EIT&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DEIT','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20050207500&hterms=EIT&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DEIT"><span>Coronal Current <span class="hlt">Sheet</span> Evolution in the Aftermath of a CME</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bemporad, A.; Poletto, G.; Suess, S. T.; Ko, Y.-K.; Schwadron, N. A.; Elliott, H. A.; Raymond, J. C.</p> <p>2005-01-01</p> <p>We report on SOHO-UVCS observations of coronal restructuring following a Coronal Mass Ejection (CME) on November 26, 2002, at the time of a SOHO-Ulysses quadrature campaign. Starting about 3 hours after the CME, which was <span class="hlt">directed</span> towards Ulysses, UVCS began taking spectra at 1.7 solar radii, covering emission from both cool and hot plasma. Observations continued, with occasional gaps, for more than 2 days. Emission in the 974.8 Angstrom line of [Fe XVIII], indicating temperatures above 6x10(6) K, was observed throughout the campaign in a spatially limited location. Comparison with EIT images shows the [Fe XVIII] emission to overlie a growing post-flare loop system formed in the aftermath of the CME. The emission most likely originates in a current <span class="hlt">sheet</span> overlying the arcade. Analysis of the [Fe XVIII] emission allows us to infer the evolution of physical parameters in the current <span class="hlt">sheet</span> over the entire span of our observations: in particular, we give the temperature vs. time in the current <span class="hlt">sheet</span> and estimate the density. Ulysses was <span class="hlt">directly</span> above the location of the CME and intercepted the ejecta. High ionization state Fe was detected by SWICS throughout the magnetic cloud associated with the CME, although the rapid temporal variation suggests bursty, rather than smooth, reconnection in the coronal current <span class="hlt">sheet</span>. Both the remote and in situ observations are compared with predictions of theoretical CME models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JGRA..120.1022L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JGRA..120.1022L"><span>Acceleration of O+ from the cusp to the plasma <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liao, J.; Kistler, L. M.; Mouikis, C. G.; Klecker, B.; Dandouras, I.</p> <p>2015-02-01</p> <p>Heavy ions from the ionosphere that are accelerated in the cusp/cleft have been identified as a <span class="hlt">direct</span> source for the hot plasma in the plasma <span class="hlt">sheet</span>. However, the details of the acceleration and transport that transforms the originally cold ions into the hot plasma <span class="hlt">sheet</span> population are not fully understood. The polar orbit of the Cluster satellites covers the main transport path of the O+ from the cusp to the plasma <span class="hlt">sheet</span>, so Cluster is ideal for tracking its velocity changes. However, because the cusp outflow is dispersed according to its velocity as it is transported to the tail, due to the velocity filter effect, the observed changes in beam velocity over the Cluster orbit may simply be the result of the spacecraft accessing different spatial regions and not necessarily evidence of acceleration. Using the Cluster Ion Spectrometry/Composition Distribution Function instrument onboard Cluster, we compare the distribution function of streaming O+ in the tail lobes with the initial distribution function observed over the cusp and reveal that the observations of energetic streaming O+ in the lobes around -20 RE are predominantly due to the velocity filter effect during nonstorm times. During storm times, the cusp distribution is further accelerated. In the plasma <span class="hlt">sheet</span> boundary layer, however, the average O+ distribution function is above the upper range of the outflow distributions at the same velocity during both storm and nonstorm times, indicating that acceleration has taken place. Some of the velocity increase is in the <span class="hlt">direction</span> perpendicular to the magnetic field, indicating that the E × B velocity is enhanced. However, there is also an increase in the parallel <span class="hlt">direction</span>, which could be due to nonadiabatic acceleration at the boundary or wave heating.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21430323','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21430323"><span>Utilizing boron nitride <span class="hlt">sheets</span> as thin supports for high resolution imaging of nanocrystals.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wu, Yimin A; Kirkland, Angus I; Schäffel, Franziska; Porfyrakis, Kyriakos; Young, Neil P; Briggs, G Andrew D; Warner, Jamie H</p> <p>2011-05-13</p> <p>We demonstrate the use of thin BN <span class="hlt">sheets</span> as supports for imaging nanocrystals using low voltage (80 kV) aberration-corrected high resolution transmission electron microscopy. This provides an alternative to the previously utilized 2D crystal supports of graphene and graphene oxide. A simple chemical exfoliation method is applied to get few layer boron nitride (BN) <span class="hlt">sheets</span> with micrometer-sized dimensions. This generic approach of using BN <span class="hlt">sheets</span> as supports is shown by depositing Mn doped ZnSe nanocrystals <span class="hlt">directly</span> onto the BN <span class="hlt">sheets</span> and resolving the atomic structure from both the ZnSe nanocrystals and the BN support. Phase contrast images reveal moiré patterns of interference between the beams diffracted by the nanocrystals and the BN substrate that are used to determine the relative orientation of the nanocrystals with respect to the BN <span class="hlt">sheets</span> and interference lattice planes. Double diffraction is observed and has been analyzed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25143114','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25143114"><span>A microbial ecosystem beneath the West Antarctic ice <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Christner, Brent C; Priscu, John C; Achberger, Amanda M; Barbante, Carlo; Carter, Sasha P; Christianson, Knut; Michaud, Alexander B; Mikucki, Jill A; Mitchell, Andrew C; Skidmore, Mark L; Vick-Majors, Trista J</p> <p>2014-08-21</p> <p>Liquid water has been known to occur beneath the Antarctic ice <span class="hlt">sheet</span> for more than 40 years, but only recently have these subglacial aqueous environments been recognized as microbial ecosystems that may influence biogeochemical transformations on a global scale. Here we present the first geomicrobiological description of water and surficial sediments obtained from <span class="hlt">direct</span> sampling of a subglacial Antarctic lake. Subglacial Lake Whillans (SLW) lies beneath approximately 800 m of ice on the lower portion of the Whillans Ice Stream (WIS) in West Antarctica and is part of an extensive and evolving subglacial drainage network. The water column of SLW contained metabolically <span class="hlt">active</span> microorganisms and was derived primarily from glacial ice melt with solute sources from lithogenic weathering and a minor seawater component. Heterotrophic and autotrophic production data together with small subunit ribosomal RNA gene sequencing and biogeochemical data indicate that SLW is a chemosynthetically driven ecosystem inhabited by a diverse assemblage of bacteria and archaea. Our results confirm that aquatic environments beneath the Antarctic ice <span class="hlt">sheet</span> support viable microbial ecosystems, corroborating previous reports suggesting that they contain globally relevant pools of carbon and microbes that can mobilize elements from the lithosphere and influence Southern Ocean geochemical and biological systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29719765','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29719765"><span>Electrostatic force spectroscopy revealing the degree of reduction of individual graphene oxide <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shen, Yue; Wang, Ying; Zhou, Yuan; Hai, Chunxi; Hu, Jun; Zhang, Yi</p> <p>2018-01-01</p> <p>Electrostatic force spectroscopy (EFS) is a method for monitoring the electrostatic force microscopy (EFM) phase with high resolution as a function of the electrical <span class="hlt">direct</span> current bias applied either to the probe or sample. Based on the dielectric constant difference of graphene oxide (GO) <span class="hlt">sheets</span> (reduced using various methods), EFS can be used to characterize the degree of reduction of uniformly reduced one-atom-thick GO <span class="hlt">sheets</span> at the nanoscale. In this paper, using thermally or chemically reduced individual GO <span class="hlt">sheets</span> on mica substrates as examples, we characterize their degree of reduction at the nanoscale using EFS. For the reduced graphene oxide (rGO) <span class="hlt">sheets</span> with a given degree of reduction (sample n), the EFS curve is very close to a parabola within a restricted area. We found that the change in parabola opening <span class="hlt">direction</span> (or sign the parabola opening value) indicates the onset of reduction on GO <span class="hlt">sheets</span>. Moreover, the parabola opening value, the peak bias value (tip bias leads to the peak or valley EFM phases) and the EFM phase contrast at a certain tip bias less than the peak value can all indicate the degree of reduction of rGO samples, which is positively correlated with the dielectric constant. In addition, we gave the ranking of degree for reduction on thermally or chemically reduced GO <span class="hlt">sheets</span> and evaluated the effects of the reducing conditions. The identification of the degree of reduction of GO <span class="hlt">sheets</span> using EFS is important for reduction strategy optimization and mass application of GO, which is highly desired owing to its mechanical, thermal, optical and electronic applications. Furthermore, as a general and quantitative technique for evaluating the small differences in the dielectric properties of nanomaterials, the EFS technique will extend and facilitate its nanoscale electronic devices applications in the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMEP54A..05V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMEP54A..05V"><span>Modeling the transition between upper plane bed regime and <span class="hlt">sheet</span> flow without an <span class="hlt">active</span> layer formulation. Preliminary results.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Viparelli, E.; Hernandez Moreira, R. R.; Blom, A.</p> <p>2015-12-01</p> <p>A perusal of the literature on bedload transport revealed that, notwithstanding the large number of studies on bedform morphology performed in the past decades, the upper plane bed regime has not been thoroughly investigated and the distinction between the upper plane bed and <span class="hlt">sheet</span> flow transport regimes is still poorly defined. Previous experimental work demonstrated that the upper plane bed regime is characterized by long wavelength and small amplitude bedforms that migrate downstream. These bedforms, however, were not observed in experiments on <span class="hlt">sheet</span> flow transport suggesting that the upper plane bed and the <span class="hlt">sheet</span> flow are two different regimes. We thus designed and performed experiments in a sediment feed flume in the hydraulic laboratory of the Department of Civil and Environmental Engineering at the University of South Carolina at Columbia to study the transition from upper plane bed to <span class="hlt">sheet</span> flow regime. Periodic measurements of water surface and bed elevation, bedform geometry and thicknesses of the bedload layer were performed by eyes, and with cameras, movies and a system of six ultrasonic probes that record the variations of bed elevation at a point over time. We used the time series of bed elevations to determine the probability functions of bed elevation. These probability functions are implemented in a continuous model of river morphodynamics, i.e. a model that does not use the <span class="hlt">active</span> layer approximation to describe the sediment fluxes between the bedload and the deposit and that should thus be able to capture the details of the vertical and streamwise variation of the deposit grain size distribution. This model is validated against the experimental results for the case of uniform material. We then use the validated model in the attempt to study if and how the spatial distribution of grain sizes in the deposit changes from upper plane bed regime to <span class="hlt">sheet</span> flow and if these results are influenced by the imposed rates of base level rise.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20179339','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20179339"><span>Rapid model building of beta-<span class="hlt">sheets</span> in electron-density maps.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Terwilliger, Thomas C</p> <p>2010-03-01</p> <p>A method for rapidly building beta-<span class="hlt">sheets</span> into electron-density maps is presented. beta-Strands are identified as tubes of high density adjacent to and nearly parallel to other tubes of density. The alignment and <span class="hlt">direction</span> of each strand are identified from the pattern of high density corresponding to carbonyl and C(beta) atoms along the strand averaged over all repeats present in the strand. The beta-strands obtained are then assembled into a single atomic model of the beta-<span class="hlt">sheet</span> regions. The method was tested on a set of 42 experimental electron-density maps at resolutions ranging from 1.5 to 3.8 A. The beta-<span class="hlt">sheet</span> regions were nearly completely built in all but two cases, the exceptions being one structure at 2.5 A resolution in which a third of the residues in beta-<span class="hlt">sheets</span> were built and a structure at 3.8 A in which under 10% were built. The overall average r.m.s.d. of main-chain atoms in the residues built using this method compared with refined models of the structures was 1.5 A.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19295607','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19295607"><span>Obliquity-paced Pliocene West Antarctic ice <span class="hlt">sheet</span> oscillations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Naish, T; Powell, R; Levy, R; Wilson, G; Scherer, R; Talarico, F; Krissek, L; Niessen, F; Pompilio, M; Wilson, T; Carter, L; DeConto, R; Huybers, P; McKay, R; Pollard, D; Ross, J; Winter, D; Barrett, P; Browne, G; Cody, R; Cowan, E; Crampton, J; Dunbar, G; Dunbar, N; Florindo, F; Gebhardt, C; Graham, I; Hannah, M; Hansaraj, D; Harwood, D; Helling, D; Henrys, S; Hinnov, L; Kuhn, G; Kyle, P; Läufer, A; Maffioli, P; Magens, D; Mandernack, K; McIntosh, W; Millan, C; Morin, R; Ohneiser, C; Paulsen, T; Persico, D; Raine, I; Reed, J; Riesselman, C; Sagnotti, L; Schmitt, D; Sjunneskog, C; Strong, P; Taviani, M; Vogel, S; Wilch, T; Williams, T</p> <p>2009-03-19</p> <p>Thirty years after oxygen isotope records from microfossils deposited in ocean sediments confirmed the hypothesis that variations in the Earth's orbital geometry control the ice ages, fundamental questions remain over the response of the Antarctic ice <span class="hlt">sheets</span> to orbital cycles. Furthermore, an understanding of the behaviour of the marine-based West Antarctic ice <span class="hlt">sheet</span> (WAIS) during the 'warmer-than-present' early-Pliocene epoch ( approximately 5-3 Myr ago) is needed to better constrain the possible range of ice-<span class="hlt">sheet</span> behaviour in the context of future global warming. Here we present a marine glacial record from the upper 600 m of the AND-1B sediment core recovered from beneath the northwest part of the Ross ice shelf by the ANDRILL programme and demonstrate well-dated, approximately 40-kyr cyclic variations in ice-<span class="hlt">sheet</span> extent linked to cycles in insolation influenced by changes in the Earth's axial tilt (obliquity) during the Pliocene. Our data provide <span class="hlt">direct</span> evidence for orbitally induced oscillations in the WAIS, which periodically collapsed, resulting in a switch from grounded ice, or ice shelves, to open waters in the Ross embayment when planetary temperatures were up to approximately 3 degrees C warmer than today and atmospheric CO(2) concentration was as high as approximately 400 p.p.m.v. (refs 5, 6). The evidence is consistent with a new ice-<span class="hlt">sheet</span>/ice-shelf model that simulates fluctuations in Antarctic ice volume of up to +7 m in equivalent sea level associated with the loss of the WAIS and up to +3 m in equivalent sea level from the East Antarctic ice <span class="hlt">sheet</span>, in response to ocean-induced melting paced by obliquity. During interglacial times, diatomaceous sediments indicate high surface-water productivity, minimal summer sea ice and air temperatures above freezing, suggesting an additional influence of surface melt under conditions of elevated CO(2).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19830000204&hterms=tapping&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dtapping','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19830000204&hterms=tapping&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dtapping"><span>Transporter for Treated <span class="hlt">Sheet</span> Materials</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Pollack, M., H.</p> <p>1983-01-01</p> <p>Plastic spacers keep parts separated during transport or storage. Cart with rods and spacers holds <span class="hlt">sheets</span> with delicate finishes for storage or transport. <span class="hlt">Sheets</span> supported vertically by rods, or horizontally. Spacers keep <span class="hlt">sheets</span> separated. Designed to eliminate time and expense of tapping, wrapping, and sometimes refinishing aluminum <span class="hlt">sheets</span> with delicate anodized finished.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_10 --> <div id="page_11" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="201"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19850000125&hterms=baking&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dbaking','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19850000125&hterms=baking&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dbaking"><span>Perforating Thin Metal <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Davidson, M. E.</p> <p>1985-01-01</p> <p><span class="hlt">Sheets</span> only few mils thick bonded together, punched, then debonded. Three-step process yields perforated <span class="hlt">sheets</span> of metal. (1): Individual <span class="hlt">sheets</span> bonded together to form laminate. (2): laminate perforated in desired geometric pattern. (3): After baking, laminate separates into individual <span class="hlt">sheets</span>. Developed for fabricating conductive layer on blankets that collect and remove ions; however, perforated foils have other applications - as conductive surfaces on insulating materials; stiffeners and conductors in plastic laminates; reflectors in antenna dishes; supports for thermal blankets; lightweight grille cover materials; and material for mockup of components.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016SPIE.9690E..12S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016SPIE.9690E..12S"><span>Mapping whole-brain <span class="hlt">activity</span> with cellular resolution by light-<span class="hlt">sheet</span> microscopy and high-throughput image analysis (Conference Presentation)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Silvestri, Ludovico; Rudinskiy, Nikita; Paciscopi, Marco; Müllenbroich, Marie Caroline; Costantini, Irene; Sacconi, Leonardo; Frasconi, Paolo; Hyman, Bradley T.; Pavone, Francesco S.</p> <p>2016-03-01</p> <p>Mapping neuronal <span class="hlt">activity</span> patterns across the whole brain with cellular resolution is a challenging task for state-of-the-art imaging methods. Indeed, despite a number of technological efforts, quantitative cellular-resolution <span class="hlt">activation</span> maps of the whole brain have not yet been obtained. Many techniques are limited by coarse resolution or by a narrow field of view. High-throughput imaging methods, such as light <span class="hlt">sheet</span> microscopy, can be used to image large specimens with high resolution and in reasonable times. However, the bottleneck is then moved from image acquisition to image analysis, since many TeraBytes of data have to be processed to extract meaningful information. Here, we present a full experimental pipeline to quantify neuronal <span class="hlt">activity</span> in the entire mouse brain with cellular resolution, based on a combination of genetics, optics and computer science. We used a transgenic mouse strain (Arc-dVenus mouse) in which neurons which have been <span class="hlt">active</span> in the last hours before brain fixation are fluorescently labelled. Samples were cleared with CLARITY and imaged with a custom-made confocal light <span class="hlt">sheet</span> microscope. To perform an automatic localization of fluorescent cells on the large images produced, we used a novel computational approach called semantic deconvolution. The combined approach presented here allows quantifying the amount of Arc-expressing neurons throughout the whole mouse brain. When applied to cohorts of mice subject to different stimuli and/or environmental conditions, this method helps finding correlations in <span class="hlt">activity</span> between different neuronal populations, opening the possibility to infer a sort of brain-wide 'functional connectivity' with cellular resolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1409590-principles-designing-proteins-cavities-formed-curved-sheets','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1409590-principles-designing-proteins-cavities-formed-curved-sheets"><span>Principles for designing proteins with cavities formed by curved β <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Marcos, Enrique; Basanta, Benjamin; Chidyausiku, Tamuka M.</p> <p></p> <p><span class="hlt">Active</span> sites and ligand-binding cavities in native proteins are often formed by curved β <span class="hlt">sheets</span>, and the ability to control β-<span class="hlt">sheet</span> curvature would allow design of binding proteins with cavities customized to specific ligands. Toward this end, we investigated the mechanisms controlling β-<span class="hlt">sheet</span> curvature by studying the geometry of β <span class="hlt">sheets</span> in naturally occurring protein structures and folding simulations. The principles emerging from this analysis were used to design, de novo, a series of proteins with curved β <span class="hlt">sheets</span> topped with α helices. Nuclear magnetic resonance and crystal structures of the designs closely match the computational models, showing that β-sheetmore » curvature can be controlled with atomic-level accuracy. Our approach enables the design of proteins with cavities and provides a route to custom design ligand-binding and catalytic sites.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018CliPa..14..455T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018CliPa..14..455T"><span>The sensitivity of the Greenland Ice <span class="hlt">Sheet</span> to glacial-interglacial oceanic forcing</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tabone, Ilaria; Blasco, Javier; Robinson, Alexander; Alvarez-Solas, Jorge; Montoya, Marisa</p> <p>2018-04-01</p> <p>Observations suggest that during the last decades the Greenland Ice <span class="hlt">Sheet</span> (GrIS) has experienced a gradually accelerating mass loss, in part due to the observed speed-up of several of Greenland's marine-terminating glaciers. Recent studies <span class="hlt">directly</span> attribute this to warming North Atlantic temperatures, which have triggered melting of the outlet glaciers of the GrIS, grounding-line retreat and enhanced ice discharge into the ocean, contributing to an acceleration of sea-level rise. Reconstructions suggest that the influence of the ocean has been of primary importance in the past as well. This was the case not only in interglacial periods, when warmer climates led to a rapid retreat of the GrIS to land above sea level, but also in glacial periods, when the GrIS expanded as far as the continental shelf break and was thus more <span class="hlt">directly</span> exposed to oceanic changes. However, the GrIS response to palaeo-oceanic variations has yet to be investigated in detail from a mechanistic modelling perspective. In this work, the evolution of the GrIS over the past two glacial cycles is studied using a three-dimensional hybrid ice-<span class="hlt">sheet</span>-shelf model. We assess the effect of the variation of oceanic temperatures on the GrIS evolution on glacial-interglacial timescales through changes in submarine melting. The results show a very high sensitivity of the GrIS to changing oceanic conditions. Oceanic forcing is found to be a primary driver of GrIS expansion in glacial times and of retreat in interglacial periods. If switched off, palaeo-atmospheric variations alone are not able to yield a reliable glacial configuration of the GrIS. This work therefore suggests that considering the ocean as an <span class="hlt">active</span> forcing should become standard practice in palaeo-ice-<span class="hlt">sheet</span> modelling.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSM33B2642A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSM33B2642A"><span>The Topology and Properties of Mercury's Tail Current <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Al Asad, M.; Johnson, C.; Philpott, L. C.</p> <p>2017-12-01</p> <p>The MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft orbited Mercury from March 2011 until April 2015, measuring the vector magnetic field inside and outside the magnetosphere. MESSENGER repeatedly encountered the tail current <span class="hlt">sheet</span> (TCS) on the nightside of the planet. We examined 1s magnetic field data within 20 minutes of the magnetic equator position on 2435 orbit to characterize the shape and properties of Mercury's TCS and investigate its response to solar wind conditions. Identification of the TCS from vector magnetic field data used the following criteria: (1) a rapid rotation in the field <span class="hlt">direction</span> from anti-sunward in the southern tail lobe to sunward in the northern lobe, accompanied by (2) a decrease in the field magnitude and (3) an increase in field variability. The current <span class="hlt">sheet</span> was encountered on 606 orbits allowing the probability of encountering the tail current <span class="hlt">sheet</span> in the equatorial plane to be mapped. Orbits on which the TCS was identified were binned spatially and superposed epoch analysis used to determine the field magnitude at the edge of the TCS, from which its time-averaged 3D shape was extracted. The TCS has an inner edge at 1.5 RM downtail in the midnight plane with a thickness of 0.34 RM, extends to the observation limit of 2.8 RM, decreasing in thickness to 0.28 RM. The thickness of the TCS increases in the dawn/dusk <span class="hlt">directions</span> to 0.7 RM at 1.8 RM downtail and ± 1.5 RM from the noon-midnight plane and it warps towards the planet in the dawn/dusk <span class="hlt">directions</span>. No strong correlations were found between the time-averaged shape and position of the TCS and solar wind conditions such as the solar wind ram pressure and the magnetic disturbance index, nor with parameters that control these conditions such as heliocentric distance. However, it is likely that the TCS does respond to these conditions on time scales too short to be characterized with MESSENGER data. In addition to mapping the shape of the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GMD....10..255P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GMD....10..255P"><span>An ice <span class="hlt">sheet</span> model validation framework for the Greenland ice <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Price, Stephen F.; Hoffman, Matthew J.; Bonin, Jennifer A.; Howat, Ian M.; Neumann, Thomas; Saba, Jack; Tezaur, Irina; Guerber, Jeffrey; Chambers, Don P.; Evans, Katherine J.; Kennedy, Joseph H.; Lenaerts, Jan; Lipscomb, William H.; Perego, Mauro; Salinger, Andrew G.; Tuminaro, Raymond S.; van den Broeke, Michiel R.; Nowicki, Sophie M. J.</p> <p>2017-01-01</p> <p>We propose a new ice <span class="hlt">sheet</span> model validation framework - the Cryospheric Model Comparison Tool (CmCt) - that takes advantage of ice <span class="hlt">sheet</span> altimetry and gravimetry observations collected over the past several decades and is applied here to modeling of the Greenland ice <span class="hlt">sheet</span>. We use realistic simulations performed with the Community Ice <span class="hlt">Sheet</span> Model (CISM) along with two idealized, non-dynamic models to demonstrate the framework and its use. Dynamic simulations with CISM are forced from 1991 to 2013, using combinations of reanalysis-based surface mass balance and observations of outlet glacier flux change. We propose and demonstrate qualitative and quantitative metrics for use in evaluating the different model simulations against the observations. We find that the altimetry observations used here are largely ambiguous in terms of their ability to distinguish one simulation from another. Based on basin-scale and whole-ice-<span class="hlt">sheet</span>-scale metrics, we find that simulations using both idealized conceptual models and dynamic, numerical models provide an equally reasonable representation of the ice <span class="hlt">sheet</span> surface (mean elevation differences of < 1 m). This is likely due to their short period of record, biases inherent to digital elevation models used for model initial conditions, and biases resulting from firn dynamics, which are not explicitly accounted for in the models or observations. On the other hand, we find that the gravimetry observations used here are able to unambiguously distinguish between simulations of varying complexity, and along with the CmCt, can provide a quantitative score for assessing a particular model and/or simulation. The new framework demonstrates that our proposed metrics can distinguish relatively better from relatively worse simulations and that dynamic ice <span class="hlt">sheet</span> models, when appropriately initialized and forced with the right boundary conditions, demonstrate a predictive skill with respect to observed dynamic changes that have occurred on</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1340442','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1340442"><span>An ice <span class="hlt">sheet</span> model validation framework for the Greenland ice <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Price, Stephen F.; Hoffman, Matthew J.; Bonin, Jennifer A.</p> <p></p> <p>We propose a new ice <span class="hlt">sheet</span> model validation framework the Cryospheric Model Comparison Tool (CMCT) that takes advantage of ice <span class="hlt">sheet</span> altimetry and gravimetry observations collected over the past several decades and is applied here to modeling of the Greenland ice <span class="hlt">sheet</span>. We use realistic simulations performed with the Community Ice <span class="hlt">Sheet</span> Model (CISM) along with two idealized, non-dynamic models to demonstrate the framework and its use. Dynamic simulations with CISM are forced from 1991 to 2013 using combinations of reanalysis-based surface mass balance and observations of outlet glacier flux change. We propose and demonstrate qualitative and quanti- tative metricsmore » for use in evaluating the different model simulations against the observations. We find 10 that the altimetry observations used here are largely ambiguous in terms of their ability to distinguish one simulation from another. Based on basin- and whole-ice-<span class="hlt">sheet</span> scale metrics, the model initial condition as well as output from idealized and dynamic models all provide an equally reasonable representation of the ice <span class="hlt">sheet</span> surface (mean elevation differences of <1 m). This is likely due to their short period of record, biases inherent to digital elevation models used for model initial conditions, and biases resulting from firn dynamics, which are not explicitly accounted for in the models or observations. On the other hand, we find that the gravimetry observations used here are able to unambiguously distinguish between simulations of varying complexity, and along with the CMCT, can provide a quantitative score for assessing a particular model and/or simulation. The new framework demonstrates that our proposed metrics can distinguish relatively better from relatively worse simulations and that dynamic ice <span class="hlt">sheet</span> models, when appropriately initialized and forced with the right boundary conditions, demonstrate predictive skill with respect to observed dynamic changes occurring on Greenland over the past few</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5911937','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5911937"><span>An ice <span class="hlt">sheet</span> model validation framework for the Greenland ice <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Price, Stephen F.; Hoffman, Matthew J.; Bonin, Jennifer A.; Howat, Ian M.; Neumann, Thomas; Saba, Jack; Tezaur, Irina; Guerber, Jeffrey; Chambers, Don P.; Evans, Katherine J.; Kennedy, Joseph H.; Lenaerts, Jan; Lipscomb, William H.; Perego, Mauro; Salinger, Andrew G.; Tuminaro, Raymond S.; van den Broeke, Michiel R.; Nowicki, Sophie M. J.</p> <p>2018-01-01</p> <p>We propose a new ice <span class="hlt">sheet</span> model validation framework – the Cryospheric Model Comparison Tool (CmCt) – that takes advantage of ice <span class="hlt">sheet</span> altimetry and gravimetry observations collected over the past several decades and is applied here to modeling of the Greenland ice <span class="hlt">sheet</span>. We use realistic simulations performed with the Community Ice <span class="hlt">Sheet</span> Model (CISM) along with two idealized, non-dynamic models to demonstrate the framework and its use. Dynamic simulations with CISM are forced from 1991 to 2013 using combinations of reanalysis-based surface mass balance and observations of outlet glacier flux change. We propose and demonstrate qualitative and quantitative metrics for use in evaluating the different model simulations against the observations. We find that the altimetry observations used here are largely ambiguous in terms of their ability to distinguish one simulation from another. Based on basin- and whole-ice-<span class="hlt">sheet</span> scale metrics, we find that simulations using both idealized conceptual models and dynamic, numerical models provide an equally reasonable representation of the ice <span class="hlt">sheet</span> surface (mean elevation differences of <1 m). This is likely due to their short period of record, biases inherent to digital elevation models used for model initial conditions, and biases resulting from firn dynamics, which are not explicitly accounted for in the models or observations. On the other hand, we find that the gravimetry observations used here are able to unambiguously distinguish between simulations of varying complexity, and along with the CmCt, can provide a quantitative score for assessing a particular model and/or simulation. The new framework demonstrates that our proposed metrics can distinguish relatively better from relatively worse simulations and that dynamic ice <span class="hlt">sheet</span> models, when appropriately initialized and forced with the right boundary conditions, demonstrate predictive skill with respect to observed dynamic changes occurring on Greenland over the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29697704','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29697704"><span>An ice <span class="hlt">sheet</span> model validation framework for the Greenland ice <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Price, Stephen F; Hoffman, Matthew J; Bonin, Jennifer A; Howat, Ian M; Neumann, Thomas; Saba, Jack; Tezaur, Irina; Guerber, Jeffrey; Chambers, Don P; Evans, Katherine J; Kennedy, Joseph H; Lenaerts, Jan; Lipscomb, William H; Perego, Mauro; Salinger, Andrew G; Tuminaro, Raymond S; van den Broeke, Michiel R; Nowicki, Sophie M J</p> <p>2017-01-01</p> <p>We propose a new ice <span class="hlt">sheet</span> model validation framework - the Cryospheric Model Comparison Tool (CmCt) - that takes advantage of ice <span class="hlt">sheet</span> altimetry and gravimetry observations collected over the past several decades and is applied here to modeling of the Greenland ice <span class="hlt">sheet</span>. We use realistic simulations performed with the Community Ice <span class="hlt">Sheet</span> Model (CISM) along with two idealized, non-dynamic models to demonstrate the framework and its use. Dynamic simulations with CISM are forced from 1991 to 2013 using combinations of reanalysis-based surface mass balance and observations of outlet glacier flux change. We propose and demonstrate qualitative and quantitative metrics for use in evaluating the different model simulations against the observations. We find that the altimetry observations used here are largely ambiguous in terms of their ability to distinguish one simulation from another. Based on basin- and whole-ice-<span class="hlt">sheet</span> scale metrics, we find that simulations using both idealized conceptual models and dynamic, numerical models provide an equally reasonable representation of the ice <span class="hlt">sheet</span> surface (mean elevation differences of <1 m). This is likely due to their short period of record, biases inherent to digital elevation models used for model initial conditions, and biases resulting from firn dynamics, which are not explicitly accounted for in the models or observations. On the other hand, we find that the gravimetry observations used here are able to unambiguously distinguish between simulations of varying complexity, and along with the CmCt, can provide a quantitative score for assessing a particular model and/or simulation. The new framework demonstrates that our proposed metrics can distinguish relatively better from relatively worse simulations and that dynamic ice <span class="hlt">sheet</span> models, when appropriately initialized and forced with the right boundary conditions, demonstrate predictive skill with respect to observed dynamic changes occurring on Greenland over the past</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1340442-ice-sheet-model-validation-framework-greenland-ice-sheet','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1340442-ice-sheet-model-validation-framework-greenland-ice-sheet"><span>An ice <span class="hlt">sheet</span> model validation framework for the Greenland ice <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Price, Stephen F.; Hoffman, Matthew J.; Bonin, Jennifer A.; ...</p> <p>2017-01-17</p> <p>We propose a new ice <span class="hlt">sheet</span> model validation framework the Cryospheric Model Comparison Tool (CMCT) that takes advantage of ice <span class="hlt">sheet</span> altimetry and gravimetry observations collected over the past several decades and is applied here to modeling of the Greenland ice <span class="hlt">sheet</span>. We use realistic simulations performed with the Community Ice <span class="hlt">Sheet</span> Model (CISM) along with two idealized, non-dynamic models to demonstrate the framework and its use. Dynamic simulations with CISM are forced from 1991 to 2013 using combinations of reanalysis-based surface mass balance and observations of outlet glacier flux change. We propose and demonstrate qualitative and quanti- tative metricsmore » for use in evaluating the different model simulations against the observations. We find 10 that the altimetry observations used here are largely ambiguous in terms of their ability to distinguish one simulation from another. Based on basin- and whole-ice-<span class="hlt">sheet</span> scale metrics, the model initial condition as well as output from idealized and dynamic models all provide an equally reasonable representation of the ice <span class="hlt">sheet</span> surface (mean elevation differences of <1 m). This is likely due to their short period of record, biases inherent to digital elevation models used for model initial conditions, and biases resulting from firn dynamics, which are not explicitly accounted for in the models or observations. On the other hand, we find that the gravimetry observations used here are able to unambiguously distinguish between simulations of varying complexity, and along with the CMCT, can provide a quantitative score for assessing a particular model and/or simulation. The new framework demonstrates that our proposed metrics can distinguish relatively better from relatively worse simulations and that dynamic ice <span class="hlt">sheet</span> models, when appropriately initialized and forced with the right boundary conditions, demonstrate predictive skill with respect to observed dynamic changes occurring on Greenland over the past few</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170003152','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170003152"><span>An Ice <span class="hlt">Sheet</span> Model Validation Framework for the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Price, Stephen F.; Hoffman, Matthew J.; Bonin, Jennifer A.; Howat, Ian M.; Neumann, Thomas A.; Saba, Jack; Tezaur, Irina; Guerber, Jeffrey R.; Chambers, Don P.; Evans, Katherine J.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20170003152'); toggleEditAbsImage('author_20170003152_show'); toggleEditAbsImage('author_20170003152_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20170003152_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20170003152_hide"></p> <p>2017-01-01</p> <p>We propose a new ice <span class="hlt">sheet</span> model validation framework - the Cryospheric Model Comparison Tool (CmCt) - that takes advantage of ice <span class="hlt">sheet</span> altimetry and gravimetry observations collected over the past several decades and is applied here to modeling of the Greenland ice <span class="hlt">sheet</span>. We use realistic simulations performed with the Community Ice <span class="hlt">Sheet</span> Model (CISM) along with two idealized, non-dynamic models to demonstrate the framework and its use. Dynamic simulations with CISM are forced from 1991 to 2013, using combinations of reanalysis-based surface mass balance and observations of outlet glacier flux change. We propose and demonstrate qualitative and quantitative metrics for use in evaluating the different model simulations against the observations. We find that the altimetry observations used here are largely ambiguous in terms of their ability to distinguish one simulation from another. Based on basin-scale and whole-ice-<span class="hlt">sheet</span>-scale metrics, we find that simulations using both idealized conceptual models and dynamic, numerical models provide an equally reasonable representation of the ice <span class="hlt">sheet</span> surface (mean elevation differences of less than 1 meter). This is likely due to their short period of record, biases inherent to digital elevation models used for model initial conditions, and biases resulting from firn dynamics, which are not explicitly accounted for in the models or observations. On the other hand, we find that the gravimetry observations used here are able to unambiguously distinguish between simulations of varying complexity, and along with the CmCt, can provide a quantitative score for assessing a particular model and/or simulation. The new framework demonstrates that our proposed metrics can distinguish relatively better from relatively worse simulations and that dynamic ice <span class="hlt">sheet</span> models, when appropriately initialized and forced with the right boundary conditions, demonstrate a predictive skill with respect to observed dynamic changes that have occurred</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.loc.gov/pictures/collection/hh/item/ca3307.photos.197671p/','SCIGOV-HHH'); return false;" href="https://www.loc.gov/pictures/collection/hh/item/ca3307.photos.197671p/"><span>17. INTAKE PIER, BRIDGE STRESS <span class="hlt">SHEET</span>, <span class="hlt">SHEET</span> 8 OF 117, ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>17. INTAKE PIER, BRIDGE STRESS <span class="hlt">SHEET</span>, <span class="hlt">SHEET</span> 8 OF 117, 1920. - Sacramento River Water Treatment Plant Intake Pier & Access Bridge, Spanning Sacramento River approximately 175 feet west of eastern levee on river; roughly .5 mile downstream from confluence of Sacramento & American Rivers, Sacramento, Sacramento County, CA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002EGSGA..27.5116M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002EGSGA..27.5116M"><span>Cluster Observations of Currents In The Plasma <span class="hlt">Sheet</span> During Substorm Expansions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McPherron, R. L.; Kivelson, M. G.; Khurana, K.; Balogh, A.; Conners, M.; Creutzberg, F.; Moldwin, M.; Rostoker, G.; Russell, C. T.</p> <p></p> <p>From 00 to 12 UT on August 15, 2001 the Cluster spacecraft passed through the plasma <span class="hlt">sheet</span> at 0100 lt and distance 18 Re. During this passage three substorms with multiple onsets were observed in the magnetic field and plasma. The North American ground sector was well located to provide the context and timing of these substorms. We find that each substorm was initially associated with strong Earthward <span class="hlt">directed</span> field-aligned current. The first substorm occurred when the Cluster array was at the boundary of the plasma <span class="hlt">sheet</span>. The effects of the substorm appear at Cluster in associ- ation with an intensification of the expansion into the morning sector and are initiated by a wave of plasma <span class="hlt">sheet</span> thickening followed by vertical oscillations of the plasma <span class="hlt">sheet</span> boundary. The third substorm occurred with Cluster at the neutral <span class="hlt">sheet</span>. It began with a transient pulse of southward Bz followed by a burst of tailward flow. Subse- quently a sequence of bursts of Earthward flow cause stepwise dipolarization of the local magnetic field. Our goal is to present a coherent three-dimensional representa- tion of the Cluster observations for each of these various substorms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920015552','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920015552"><span>FDTD modeling of thin impedance <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Luebbers, Raymond; Kunz, Karl</p> <p>1991-01-01</p> <p>Thin <span class="hlt">sheets</span> of resistive or dielectric material are commonly encountered in radar cross section calculations. Analysis of such <span class="hlt">sheets</span> is simplified by using <span class="hlt">sheet</span> impedances. It is shown that <span class="hlt">sheet</span> impedances can be modeled easily and accurately using Finite Difference Time Domain (FDTD) methods. These <span class="hlt">sheets</span> are characterized by a discontinuity in the tangential magnetic field on either side of the <span class="hlt">sheet</span> but no discontinuity in tangential electric field. This continuity, or single valued behavior of the electric field, allows the <span class="hlt">sheet</span> current to be expressed in terms of an impedance multiplying this electric field.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017PhyE...90...42R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017PhyE...90...42R"><span>Comparative study on predicting Young's modulus of graphene <span class="hlt">sheets</span> using nano-scale continuum mechanics approach</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rafiee, Roham; Eskandariyun, Amirali</p> <p>2017-06-01</p> <p>In this research, nano-scale continuum modeling is employed to predict Young's modulus of graphene <span class="hlt">sheet</span>. The lattice nano-structure of a graphene <span class="hlt">sheet</span> is replaced with a discrete space-frame structure simulating carbon-carbon bonds with either beam or spring elements. A comparative study is carried out to check the influence of employed elements on estimated Young's moduli of graphene <span class="hlt">sheets</span> in both horizontal and vertical <span class="hlt">directions</span>. A detailed analysis is also conducted to investigate the influence of graphene <span class="hlt">sheet</span> sizes on its Young's modulus and corresponding aspect ratios that unwelcomed end effects disappear on the results are extracted. At the final stage, defected graphene <span class="hlt">sheets</span> suffering from vacancy defects are investigated through a stochastic analysis taking into account both number of defects and their locations as random parameters. The reduction level in the Young's moduli of defected graphene <span class="hlt">sheets</span> compared with non-defected ones is analyzed and reported.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018CPL...693...23K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018CPL...693...23K"><span>Silver nanoparticles anchored reduced graphene oxide for enhanced electrocatalytic <span class="hlt">activity</span> towards methanol oxidation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kumar, Sanjeev; Mahajan, Mani; Singh, Rajinder; Mahajan, Aman</p> <p>2018-02-01</p> <p>In this report, silver nanoparticles (Ag NPs) anchored reduced graphene oxide (rGO) <span class="hlt">sheets</span> (rGO/Ag) nanohybrid has been explored as anode material in <span class="hlt">direct</span> methanol fuel cells (DMFCs). The synthesized rGO/Ag nanohybrid is characterized by XRD, XPS, FTIR spectroscopy and HRTEM techniques. Cyclic voltammograms demonstrate that the rGO/Ag nanohybrid exhibits higher electrocatalytic <span class="hlt">activity</span> in comparison to rGO <span class="hlt">sheets</span> for methanol oxidation reaction (MOR). This enhancement is attributed to the synergetic effect produced by the presence of more <span class="hlt">active</span> sites provided by Ag NPs anchored on a conducting network of large surface area rGO <span class="hlt">sheets</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/871716','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/871716"><span>Method for heating a glass <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Boaz, Premakaran Tucker</p> <p>1998-01-01</p> <p>A method for heating a glass <span class="hlt">sheet</span> includes the steps of heating a glass <span class="hlt">sheet</span> to a first predetermined temperature and applying microwave energy to the glass <span class="hlt">sheet</span> to heat the glass <span class="hlt">sheet</span> to at least a second predetermined temperature to allow the glass <span class="hlt">sheet</span> to be formed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5468947','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5468947"><span>Clinching for <span class="hlt">sheet</span> materials</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>He, Xiaocong</p> <p>2017-01-01</p> <p>Abstract Latest developments in the clinching of <span class="hlt">sheet</span> materials are reviewed in this article. Important issues are discussed, such as tool design, process parameters and joinability of some new lightweight <span class="hlt">sheet</span> materials. Hybrid and modified clinching processes are introduced to a general reader. Several unaddressed issues in the clinching of <span class="hlt">sheet</span> materials are identified. PMID:28656065</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23215495','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23215495"><span>Observations of ionospheric electron beams in the plasma <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zheng, H; Fu, S Y; Zong, Q G; Pu, Z Y; Wang, Y F; Parks, G K</p> <p>2012-11-16</p> <p>Electrons streaming along the magnetic field <span class="hlt">direction</span> are frequently observed in the plasma <span class="hlt">sheet</span> of Earth's geomagnetic tail. The impact of these field-aligned electrons on the dynamics of the geomagnetic tail is however not well understood. Here we report the first detection of field-aligned electrons with fluxes increasing at ~1 keV forming a "cool" beam just prior to the dissipation of energy in the current <span class="hlt">sheet</span>. These field-aligned beams at ~15 R(E) in the plasma <span class="hlt">sheet</span> are nearly identical to those commonly observed at auroral altitudes, suggesting the beams are auroral electrons accelerated upward by electric fields parallel (E([parallel])) to the geomagnetic field. The density of the beams relative to the ambient electron density is δn(b)/n(e)~5-13% and the current carried by the beams is ~10(-8)-10(-7) A m(-2). These beams in high β plasmas with large density and temperature gradients appear to satisfy the Bohm criteria to initiate current driven instabilities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19870009353','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19870009353"><span>Liquid <span class="hlt">sheet</span> radiator</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chubb, Donald L.; White, K. Alan, III</p> <p>1987-01-01</p> <p>A new external flow radiator concept, the liquid <span class="hlt">sheet</span> radiator (LSR), is introduced. The LSR <span class="hlt">sheet</span> flow is described and an expression for the length/width (l/w), ratio is presented. A linear dependence of l/w on velocity is predicted that agrees with experimental results. Specific power for the LSR is calculated and is found to be nearly the same as the specific power of a liquid droplet radiator, (LDR). Several <span class="hlt">sheet</span> thicknesses and widths were experimentally investigated. In no case was the flow found to be unstable.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_11 --> <div id="page_12" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="221"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/672583','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/672583"><span>Method for heating a glass <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Boaz, P.T.</p> <p>1998-07-21</p> <p>A method for heating a glass <span class="hlt">sheet</span> includes the steps of heating a glass <span class="hlt">sheet</span> to a first predetermined temperature and applying microwave energy to the glass <span class="hlt">sheet</span> to heat the glass <span class="hlt">sheet</span> to at least a second predetermined temperature to allow the glass <span class="hlt">sheet</span> to be formed. 5 figs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AnGeo..34..303X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AnGeo..34..303X"><span>A statistical study on the shape and position of the magnetotail neutral <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xiao, Sudong; Zhang, Tielong; Ge, Yasong; Wang, Guoqiang; Baumjohann, Wolfgang; Nakamura, Rumi</p> <p>2016-02-01</p> <p>We study the average shape and position of the magnetotail neutral <span class="hlt">sheet</span> based on magnetic field data obtained by Cluster, Geotail, TC-1, and THEMIS from the years 1995 to 2013. All data in the aberrated GSM (geocentric solar magnetospheric) coordinate system are normalized to the same solar wind pressure 2 nPa and downtail distance X ˜ -20RE. Our results show characteristics of the neutral <span class="hlt">sheet</span>, as follows. (1) The neutral <span class="hlt">sheet</span> assumes a greater degree of curve in the YZ cross section when the dipole tilt increases, the Earth dipole tilt angle affects the neutral <span class="hlt">sheet</span> configuration not only in the YZ cross section but also in the XY cross section, and the neutral <span class="hlt">sheet</span> assumes a more significant degree of tilt in the XY cross section when the dipole tilt increases. (2) Counterclockwise twisting of the neutral <span class="hlt">sheet</span> with 3.10° is observed, looking along the downtail <span class="hlt">direction</span>, for the positive interplanetary magnetic field (IMF) BY with a value of 3 to 8 nT, and clockwise twisting of the neutral <span class="hlt">sheet</span> with 3.37° for the negative IMF BY with a value of -8 to -3 nT, and a northward IMF can result in a greater twisting of the near-tail neutral <span class="hlt">sheet</span> than southward. The above results can be a reference to the neutral <span class="hlt">sheet</span> model. Our large database also shows that the displaced ellipse model is effective to study the average shape of the neutral <span class="hlt">sheet</span> with proper parameters when the dipole tilt angle is larger (less) than 10° (-10° ).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016GeoRL..4311295S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016GeoRL..4311295S"><span>Greenland Ice <span class="hlt">Sheet</span> flow response to runoff variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stevens, Laura A.; Behn, Mark D.; Das, Sarah B.; Joughin, Ian; Noël, Brice P. Y.; Broeke, Michiel R.; Herring, Thomas</p> <p>2016-11-01</p> <p>We use observations of ice <span class="hlt">sheet</span> surface motion from a Global Positioning System network operating from 2006 to 2014 around North Lake in west Greenland to investigate the dynamical response of the Greenland Ice <span class="hlt">Sheet</span>'s ablation area to interannual variability in surface melting. We find no statistically significant relationship between runoff season characteristics and ice flow velocities within a given year or season. Over the 7 year time series, annual velocities at North Lake decrease at an average rate of -0.9 ± 1.1 m yr-2, consistent with the negative trend in annual velocities observed in neighboring regions over recent decades. We find that net runoff integrated over several preceding years has a negative correlation with annual velocities, similar to findings from the two other available decadal records of ice velocity in western Greenland. However, we argue that this correlation is not necessarily evidence for a <span class="hlt">direct</span> hydrologic mechanism acting on the timescale of multiple years but could be a statistical construct. Finally, we stress that neither the decadal slowdown trend nor the negative correlation between velocity and integrated runoff is predicted by current ice-<span class="hlt">sheet</span> models, underscoring that these models do not yet capture all the relevant feedbacks between runoff and ice dynamics needed to predict long-term trends in ice <span class="hlt">sheet</span> flow.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950056510&hterms=disintegration&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Ddisintegration','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950056510&hterms=disintegration&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Ddisintegration"><span>Geometry of thin liquid <span class="hlt">sheet</span> flows</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chubb, Donald L.; Calfo, Frederick D.; Mcconley, Marc W.; Mcmaster, Matthew S.; Afjeh, Abdollah A.</p> <p>1994-01-01</p> <p>Incompresible, thin <span class="hlt">sheet</span> flows have been of research interest for many years. Those studies were mainly concerned with the stability of the flow in a surrounding gas. Squire was the first to carry out a linear, invicid stability analysis of <span class="hlt">sheet</span> flow in air and compare the results with experiment. Dombrowski and Fraser did an experimental study of the disintegration of <span class="hlt">sheet</span> flows using several viscous liquids. They also detected the formulation of holes in their <span class="hlt">sheet</span> flows. Hagerty and Shea carried out an inviscid stability analysis and calculated growth rates with experimental values. They compared their calculated growth rates with experimental values. Taylor studied extensively the stability of thin liquid <span class="hlt">sheets</span> both theoretically and experimentally. He showed that thin <span class="hlt">sheets</span> in a vacuum are stable. Brown experimentally investigated thin liquid <span class="hlt">sheet</span> flows as a method of application of thin films. Clark and Dumbrowski carried out second-order stability analysis for invicid <span class="hlt">sheet</span> flows. Lin introduced viscosity into the linear stability analysis of thin <span class="hlt">sheet</span> flows in a vacuum. Mansour and Chigier conducted an experimental study of the breakup of a <span class="hlt">sheet</span> flow surrounded by high-speed air. Lin et al. did a linear stability analysis that included viscosity and a surrounding gas. Rangel and Sirignano carried out both a linear and nonlinear invisid stability analysis that applies for any density ratio between the <span class="hlt">sheet</span> liquid and the surrounding gas. Now there is renewed interest in <span class="hlt">sheet</span> flows because of their possible application as low mass radiating surfaces. The objective of this study is to investigate the fluid dynamics of <span class="hlt">sheet</span> flows that are of interest for a space radiator system. Analytical expressions that govern the <span class="hlt">sheet</span> geometry are compared with experimental results. Since a space radiator will operate in a vacuum, the analysis does not include any drag force on the <span class="hlt">sheet</span> flow.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title37-vol1/pdf/CFR-2012-title37-vol1-sec1-76.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title37-vol1/pdf/CFR-2012-title37-vol1-sec1-76.pdf"><span>37 CFR 1.76 - Application data <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 37 Patents, Trademarks, and Copyrights 1 2012-07-01 2012-07-01 false Application data <span class="hlt">sheet</span>. 1.76... Application data <span class="hlt">sheet</span>. (a) Application data <span class="hlt">sheet</span>. An application data <span class="hlt">sheet</span> is a <span class="hlt">sheet</span> or <span class="hlt">sheets</span>, that may... bibliographic data, arranged in a format specified by the Office. An application data <span class="hlt">sheet</span> must be titled...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JSG....69..351W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JSG....69..351W"><span>Structural analysis of the Lombard thrust <span class="hlt">sheet</span> and adjacent areas in the Helena salient, southwest Montana, USA</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Whisner, Stephen C.; Schmidt, Christopher J.; Whisner, Jennifer B.</p> <p>2014-12-01</p> <p>The Helena salient is a prominent craton-convex curve in the Cordillera thrust belt of Montana, USA. The Lombard thrust <span class="hlt">sheet</span> is the primary <span class="hlt">sheet</span> in the salient. Structural analysis of fold trends, cleavage attitudes, and movement on minor faults is used to better understand both the geometry of the Lombard thrust and the kinematic development of the salient. Early W-E to WNW-ENE shortening <span class="hlt">directions</span> in the Lombard <span class="hlt">sheet</span> are indicated by fold trends in the center of the thrust <span class="hlt">sheet</span>. The same narrow range of shortening <span class="hlt">directions</span> is inferred from kinematic analysis of movement on minor faults and the orientations of unrotated cleavage planes along the southern lateral ramp boundary of the salient. As the salient developed, the amount and <span class="hlt">direction</span> of shortening were locally modified as listric detachment faults rotated some tight folds to the NW, and as right-lateral simple shear, caused by lock-up and folding of the Jefferson Canyon fault above the lateral ramp, rotated other folds northeastward. Where the lateral ramp and frontal-oblique ramp intersect, folds were rotated back to the NW. Our interpretation of dominant W-E to WNW-ESE shortening in the Lombard <span class="hlt">sheet</span>, later altered by local rotations, supports a model of salient formation by primary parallel transport modified by interactions with a lateral ramp.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018InPhT..89...77L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018InPhT..89...77L"><span>Pore-level determination of spectral reflection behaviors of high-porosity metal foam <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Yang; Xia, Xin-Lin; Ai, Qing; Sun, Chuang; Tan, He-Ping</p> <p>2018-03-01</p> <p>Open cell metal foams are currently attracting attention and their radiative behaviors are of primary importance in high temperature applications. The spectral reflection behaviors of high-porosity metal foam <span class="hlt">sheets</span>, bidirectional reflectance distribution function (BRDF) and <span class="hlt">directional</span>-hemispherical reflectivity were numerically investigated. A set of realistic nickel foams with porosity from 0.87 to 0.97 and pore density from 10 to 40 pores per inch were tomographied to obtain their 3-D digital cell network. A Monte Carlo ray-tracing method was employed in order to compute the pore-level radiative transfer inside the network within the limit of geometrical optics. The apparent reflection behaviors and their dependency on the textural parameters and strut optical properties were comprehensively computed and analysed. The results show a backward scattering of the reflected energy at the foam <span class="hlt">sheet</span> surface. Except in the cases of large incident angles, an energy peak is located almost along the incident <span class="hlt">direction</span> and increases with increasing incident angles. Through an analytical relation established, the <span class="hlt">directional</span>-hemispherical reflectivity can be related <span class="hlt">directly</span> to the porosity of the foam <span class="hlt">sheet</span> and to the complex refractive index of the solid phase as well as the specularity parameter which characterizes the local reflection model. The computations show that a linear decrease in normal-hemispherical reflectivity occurs with increasing porosity. The rate of this decrease is <span class="hlt">directly</span> proportional to the strut normal reflectivity. In addition, the hemispherical reflectivity increases as a power function of the incident angle cosine.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED363017.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED363017.pdf"><span>Communication Fact <span class="hlt">Sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>American Speech-Language-Hearing Association, Rockville, MD.</p> <p></p> <p>This brief fact <span class="hlt">sheet</span> examines key aspects of communication, communication disabilities, and intervention. The fact <span class="hlt">sheet</span> addresses the following questions: the nature of communication; communication disabilities (definitions of hearing impairments and speech and language impairments are given); effects of communication disabilities (factors…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018APLM....6c6107Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018APLM....6c6107Y"><span>Single crystalline electronic structure and growth mechanism of aligned square graphene <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yang, H. F.; Chen, C.; Wang, H.; Liu, Z. K.; Zhang, T.; Peng, H.; Schröter, N. B. M.; Ekahana, S. A.; Jiang, J.; Yang, L. X.; Kandyba, V.; Barinov, A.; Chen, C. Y.; Avila, J.; Asensio, M. C.; Peng, H. L.; Liu, Z. F.; Chen, Y. L.</p> <p>2018-03-01</p> <p>Recently, commercially available copper foil has become an efficient and inexpensive catalytic substrate for scalable growth of large-area graphene films for fundamental research and applications. Interestingly, despite its hexagonal honeycomb lattice, graphene can be grown into large aligned square-shaped <span class="hlt">sheets</span> on copper foils. Here, by applying angle-resolved photoemission spectroscopy with submicron spatial resolution (micro-ARPES) to study the three-dimensional electronic structures of square graphene <span class="hlt">sheets</span> grown on copper foils, we verified the high quality of individual square graphene <span class="hlt">sheets</span> as well as their merged regions (with aligned orientation). Furthermore, by simultaneously measuring the graphene <span class="hlt">sheets</span> and their substrate copper foil, we not only established the (001) copper surface structure but also discovered that the square graphene <span class="hlt">sheets</span>' sides align with the ⟨110⟩ copper <span class="hlt">direction</span>, suggesting an important role of copper substrate in the growth of square graphene sheets—which will help the development of effective methods to synthesize high-quality large-size regularly shaped graphene <span class="hlt">sheets</span> for future applications. This work also demonstrates the effectiveness of micro-ARPES in exploring low-dimensional materials down to atomic thickness and sub-micron lateral size (e.g., besides graphene, it can also be applied to transition metal dichalcogenides and various van der Waals heterostructures)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3334875','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3334875"><span>The Decisional Balance <span class="hlt">Sheet</span> to Promote Healthy Behavior Among Ethnically Diverse Older Adults</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Geller, Karly S.; Mendoza, Ilora D.; Timbobolan, Jasah; Montjoy, Holly L.; Nigg, Claudio R.</p> <p>2012-01-01</p> <p>Objective The rising health care costs and increasing older adult population in the United States make preventive medicine for this age group especially crucial. Regular physical <span class="hlt">activity</span> and fruit and vegetable consumption may prevent or delay the onset of many chronic conditions that are common among older adults. The decisional balance <span class="hlt">sheet</span> is a promotional tool targeting the perceived pros and cons of behavior adoption. The current study tested the efficiency and effectiveness of a single-day decisional balance <span class="hlt">sheet</span> program, targeting increased physical <span class="hlt">activity</span> and fruit and vegetable intake among older adults. Design and Sample Participating adults (N = 21, age = 72.2) who represented a diverse population in Hawaii (Japanese = 5, Filipino = 4, Caucasian = 4, Native American = 1, Native Hawaiian = 1, Hispanic = 1, and Others = 5) were recruited from housing communities and randomized to a decisional balance <span class="hlt">sheet</span> program adapted for physical <span class="hlt">activity</span> or fruit and vegetable consumption. Measures Physical <span class="hlt">activity</span> was assessed using the International Physical <span class="hlt">Activity</span> Questionnaire (IPAQ) short form, and daily fruit and vegetable intake with the National Health and Nutrition Examination Survey single item instrument. Baseline and follow-up data were collected. Results Both programs were implemented efficiently, and participants in both groups improved their daily physical <span class="hlt">activity</span>. The decisional balance <span class="hlt">sheet</span> for fruit and vegetable consumption appeared less effective. Conclusions Specific suggestions for similar programs are reported. PMID:22512425</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018QSRv..179...24P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018QSRv..179...24P"><span>Large-scale glacitectonic deformation in response to <span class="hlt">active</span> ice <span class="hlt">sheet</span> retreat across Dogger Bank (southern central North Sea) during the Last Glacial Maximum</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Phillips, Emrys; Cotterill, Carol; Johnson, Kirstin; Crombie, Kirstin; James, Leo; Carr, Simon; Ruiter, Astrid</p> <p>2018-01-01</p> <p>High resolution seismic data from the Dogger Bank in the central southern North Sea has revealed that the Dogger Bank Formation records a complex history of sedimentation and penecontemporaneous, large-scale, ice-marginal to proglacial glacitectonic deformation. These processes led to the development of a large thrust-block moraine complex which is buried beneath a thin sequence of Holocene sediments. This buried glacitectonic landsystem comprises a series of elongate, arcuate moraine ridges (200 m up to > 15 km across; over 40-50 km long) separated by low-lying ice marginal to proglacial sedimentary basins and/or meltwater channels, preserving the shape of the margin of this former ice <span class="hlt">sheet</span>. The moraines are composed of highly deformed (folded and thrust) Dogger Bank Formation with the lower boundary of the deformed sequence (up to 40-50 m thick) being marked by a laterally extensive décollement. The ice-distal parts of the thrust moraine complex are interpreted as a "forward" propagating imbricate thrust stack developed in response to S/SE-<span class="hlt">directed</span> ice-push. The more complex folding and thrusting within the more ice-proximal parts of the thrust-block moraines record the accretion of thrust slices of highly deformed sediment as the ice repeatedly reoccupied this ice marginal position. Consequently, the internal structure of the Dogger Bank thrust-moraine complexes can be <span class="hlt">directly</span> related to ice <span class="hlt">sheet</span> dynamics, recording the former positions of a highly dynamic, oscillating Weichselian ice <span class="hlt">sheet</span> margin as it retreated northwards at the end of the Last Glacial Maximum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.5232H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.5232H"><span>Sensitivities of Greenland ice <span class="hlt">sheet</span> volume inferred from an ice <span class="hlt">sheet</span> adjoint model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Heimbach, P.; Bugnion, V.</p> <p>2009-04-01</p> <p>We present a new and original approach to understanding the sensitivity of the Greenland ice <span class="hlt">sheet</span> to key model parameters and environmental conditions. At the heart of this approach is the use of an adjoint ice <span class="hlt">sheet</span> model. Since its introduction by MacAyeal (1992), the adjoint method has become widespread to fit ice stream models to the increasing number and diversity of satellite observations, and to estimate uncertain model parameters such as basal conditions. However, no attempt has been made to extend this method to comprehensive ice <span class="hlt">sheet</span> models. As a first step toward the use of adjoints of comprehensive three-dimensional ice <span class="hlt">sheet</span> models we have generated an adjoint of the ice <span class="hlt">sheet</span> model SICOPOLIS of Greve (1997). The adjoint was generated by means of the automatic differentiation (AD) tool TAF. The AD tool generates exact source code representing the tangent linear and adjoint model of the nonlinear parent model provided. Model sensitivities are given by the partial derivatives of a scalar-valued model diagnostic with respect to the controls, and can be efficiently calculated via the adjoint. By way of example, we determine the sensitivity of the total Greenland ice volume to various control variables, such as spatial fields of basal flow parameters, surface and basal forcings, and initial conditions. Reliability of the adjoint was tested through finite-difference perturbation calculations for various control variables and perturbation regions. Besides confirming qualitative aspects of ice <span class="hlt">sheet</span> sensitivities, such as expected regional variations, we detect regions where model sensitivities are seemingly unexpected or counter-intuitive, albeit ``real'' in the sense of actual model behavior. An example is inferred regions where sensitivities of ice <span class="hlt">sheet</span> volume to basal sliding coefficient are positive, i.e. where a local increase in basal sliding parameter increases the ice <span class="hlt">sheet</span> volume. Similarly, positive ice temperature sensitivities in certain parts</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/458589','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/458589"><span>Microcomponent <span class="hlt">sheet</span> architecture</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Wegeng, R.S.; Drost, M.K..; McDonald, C.E.</p> <p>1997-03-18</p> <p>The invention is a microcomponent <span class="hlt">sheet</span> architecture wherein macroscale unit processes are performed by microscale components. The <span class="hlt">sheet</span> architecture may be a single laminate with a plurality of separate microcomponent sections or the <span class="hlt">sheet</span> architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation. 14 figs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/870866','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/870866"><span>Microcomponent <span class="hlt">sheet</span> architecture</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Wegeng, Robert S.; Drost, M. Kevin; McDonald, Carolyn E.</p> <p>1997-01-01</p> <p>The invention is a microcomponent <span class="hlt">sheet</span> architecture wherein macroscale unit processes are performed by microscale components. The <span class="hlt">sheet</span> architecture may be a single laminate with a plurality of separate microcomponent sections or the <span class="hlt">sheet</span> architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED097519.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED097519.pdf"><span>Aircraft <span class="hlt">Sheet</span> Metal Practices; <span class="hlt">Sheet</span> Metal Work 2: 9855.01.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Dade County Public Schools, Miami, FL.</p> <p></p> <p>The course outline will serve as a guide to the 11th grade student interested in <span class="hlt">sheet</span> metal occupations. Requiring 135 clock hours, the basic course covers orientation and techniques in aircraft <span class="hlt">sheet</span> metal. Emphasis will be placed on the proper use of tools and machines, safety, fabrication methods, aircraft materials, basic layout, and special…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012MMI....18..295J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012MMI....18..295J"><span>Texture and mechanical properties of Al-0.5Mg-1.0Si-0.5Cu alloy <span class="hlt">sheets</span> manufactured via a cross rolling method</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jeon, Jae-Yeol; Son, Hyeon-Taek; Woo, Kee-Do; Lee, Kwang-Jin</p> <p>2012-04-01</p> <p>The relationship between the texture and mechanical properties of 6xxx aluminum alloy <span class="hlt">sheets</span> processed via cross rolling was investigated. The microstructures of the conventional rolled and cross rolled <span class="hlt">sheets</span> after annealing were analyzed using optical micrographs (OM). The texture distribution across the thickness in the Al-Mg-Si-Cu alloy, conventional rolled <span class="hlt">sheets</span>, and cross rolled <span class="hlt">sheets</span> both before and after annealing was investigated via X-ray texture measurements. The texture was analyzed in three layers from the surface to the center of the <span class="hlt">sheet</span>. The β-fiber texture of the conventional rolled <span class="hlt">sheet</span> was typical of the texture obtained using aluminumoll ring. After annealing, the typical β-fiber orientations were changed to recrystallization textures: cube{001}<100> and normal <span class="hlt">direction</span> (ND)-rotated cubes. However, the texture of the cross rolled <span class="hlt">sheet</span> was composed of an asymmetrical, rolling <span class="hlt">direction</span> (RD)-rotated cubes. After annealing, the asymmetrical orientations in the cross rolled <span class="hlt">sheet</span> were changed to a randomized texture. The average R-value of the annealed cross rolled <span class="hlt">sheets</span> was higher than that of the conventional rolled <span class="hlt">sheets</span>. The limit dome height (LDH) test results demonstrated that cross rolling is effective in improving the formability of the Al-Mg-Si-Cu alloy <span class="hlt">sheets</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008cosp...37.3554Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008cosp...37.3554Y"><span>Temporal evolution of a Current <span class="hlt">Sheet</span> with Initial Finite Perturbations by Three-dimensional MHD Simulations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yokoyama, Takaaki</p> <p></p> <p>Temporal evolution of a current <span class="hlt">sheet</span> with initial perturbations is studied by using the threedimensional resistive magnetohydrodynamic (MHD) simulations. The magnetic reconnection is considered to be the main engine of the energy rele ase in solar flares. The structure of the diffusion region is, however, not stil l understood under the circumstances with enormously large magnetic Reynolds num ber as the solar corona. In particular, the relationship between the flare's macroscopic physics and the microscopic ones are unclear. It is generally believed that the MHD turbulence s hould play a role in the intermediate scale. The initial current <span class="hlt">sheet</span> is in an approximately hydromagnetic equilibrium with anti-parallel magnetic field in the y-<span class="hlt">direction</span>. We imposed a finite-amplitude perturbations (=50ee what happens. Special attention is paid upon the evolution of a three-dimens ional structure in the <span class="hlt">direction</span> along the initial electric current (z-<span class="hlt">direction</span> ). Our preliminary results are as follows: (1) In the early phase of the evolut ion, high wavenumber modes in the z-<span class="hlt">direction</span> are excited and grow. (2) Many "X "-type neutral points (lines) are generated along the magnetic neutral line (pla ne) in the current <span class="hlt">sheet</span>. When they evolve into the non-linear phase, three-dime nsional structures in the z-<span class="hlt">direction</span> also evolve. The spatial scale in the z-di rection seems to be almost comparable with that in the xy-plane. (3) The energy release rate is reduced in case of 3D simulations compared with 2D ones probably because of the reduction of the inflow cross sections by the formation of pattc hy structures in the current <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.C54A..02P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.C54A..02P"><span>A Historical Forcing Ice <span class="hlt">Sheet</span> Model Validation Framework for Greenland</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Price, S. F.; Hoffman, M. J.; Howat, I. M.; Bonin, J. A.; Chambers, D. P.; Kalashnikova, I.; Neumann, T.; Nowicki, S.; Perego, M.; Salinger, A.</p> <p>2014-12-01</p> <p>We propose an ice <span class="hlt">sheet</span> model testing and validation framework for Greenland for the years 2000 to the present. Following Perego et al. (2014), we start with a realistic ice <span class="hlt">sheet</span> initial condition that is in quasi-equilibrium with climate forcing from the late 1990's. This initial condition is integrated forward in time while simultaneously applying (1) surface mass balance forcing (van Angelen et al., 2013) and (2) outlet glacier flux anomalies, defined using a new dataset of Greenland outlet glacier flux for the past decade (Enderlin et al., 2014). Modeled rates of mass and elevation change are compared <span class="hlt">directly</span> to remote sensing observations obtained from GRACE and ICESat. Here, we present a detailed description of the proposed validation framework including the ice <span class="hlt">sheet</span> model and model forcing approach, the model-to-observation comparison process, and initial results comparing model output and observations for the time period 2000-2013.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017MS%26E..225a2004A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017MS%26E..225a2004A"><span>Effect of Punch Stroke on Deformation During <span class="hlt">Sheet</span> Forming Through Finite Element</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Akinlabi, Stephen; Akinlabi, Esther</p> <p>2017-08-01</p> <p>Forming is one of the traditional methods of making shapes, bends and curvature in metallic components during a fabrication process. Mechanical forming, in particular, employs the use of a punch, which is pressed against the <span class="hlt">sheet</span> material to be deformed into a die by the application of an external force. This study reports on the finite element analysis of the effects of punch stroke on the resulting <span class="hlt">sheet</span> deformation, which is <span class="hlt">directly</span> a function of the structural integrity of the formed components for possible application in the automotive industry. The results show that punch stroke is <span class="hlt">directly</span> proportional to the resulting bend angle of the formed components. It was further revealed that the developed plastic strain increases as the punch stroke increases.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011JGRA..116.6215J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011JGRA..116.6215J"><span>A statistical study of the inner edge of the electron plasma <span class="hlt">sheet</span> and the net convection potential as a function of geomagnetic <span class="hlt">activity</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jiang, F.; Kivelson, M. G.; Walker, R. J.; Khurana, K. K.; Angelopoulos, V.; Hsu, T.</p> <p>2011-06-01</p> <p>A widely accepted explanation of the location of the inner edge of the electron plasma <span class="hlt">sheet</span> and its dependence on electron energy is based on drift motions of individual particles. The boundary is identified as the separatrix between drift trajectories linking the tail to the dayside magnetopause (open paths) and trajectories closed around the Earth. A statistical study of the inner edge of the electron plasma <span class="hlt">sheet</span> using THEMIS Electrostatic Analyzer plasma data from November 2007 to April 2009 enabled us to examine this model. Using a dipole magnetic field and a Volland-Stern electric field with shielding, we find that a steady state drift boundary model represents the average location of the electron plasma <span class="hlt">sheet</span> boundary and reflects its variation with the solar wind electric field in the local time region between 21:00 and 06:00, except at high <span class="hlt">activity</span> levels. However, the model does not reproduce the observed energy dispersion of the boundaries. We have also used the location of the inner edge of the electron plasma <span class="hlt">sheet</span> to parameterize the potential drop of the tail convection electric field as a function of solar wind electric field (Esw) and geomagnetic <span class="hlt">activity</span>. The range of Esw examined is small because the data were acquired near solar minimum. For the range of values tested (meaningful statistics only for Esw < 2 mV/m), reasonably good agreement is found between the potential drop of the tail convection electric field inferred from the location of the inner edge and the polar cap potential drop calculated from the model of Boyle et al. (1997).</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_12 --> <div id="page_13" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="241"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SPIE10137E..0MO','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SPIE10137E..0MO"><span>Extracellular matrix <span class="hlt">directions</span> estimation of the heart on micro-focus x-ray CT volumes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Oda, Hirohisa; Oda, Masahiro; Kitasaka, Takayuki; Akita, Toshiaki; Mori, Kensaku</p> <p>2017-03-01</p> <p>In this paper we propose an estimation method of extracellular matrix <span class="hlt">directions</span> of the heart. Myofiber are surrounded by the myocardial cell <span class="hlt">sheets</span> whose <span class="hlt">directions</span> have strong correspondence between heart failure. Estimation of the myocardial cell <span class="hlt">sheet</span> <span class="hlt">directions</span> is difficult since they are very thin. Therefore, we estimate the extracellular matrices which are touching to the <span class="hlt">sheets</span> as if piled up. First, we perform a segmentation of the extracellular matrices by using the Hessian analysis. Each extracellular matrix region has <span class="hlt">sheet</span>-like shape. We estimate the <span class="hlt">direction</span> of each extracellular matrix region by the principal component analysis (PCA). In our experiments, mean inclination angles of two normal canine hearts were 50.6 and 46.2 degrees, while the angle of a failing canine heart was 57.4 degrees. This results well fit the anatomical knowledge that failing hearts tend to have vertical myocardical cell <span class="hlt">sheets</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1257882','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1257882"><span>Photovoltaics Fact <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>None</p> <p>2016-02-01</p> <p>This fact <span class="hlt">sheet</span> is an overview of the Photovoltaics (PV) subprogram at the U.S. Department of Energy SunShot Initiative. The U.S. Department of Energy (DOE)’s Solar Energy Technologies Office works with industry, academia, national laboratories, and other government agencies to advance solar PV, which is the <span class="hlt">direct</span> conversion of sunlight into electricity by a semiconductor, in support of the goals of the SunShot Initiative. SunShot supports research and development to aggressively advance PV technology by improving efficiency and reliability and lowering manufacturing costs. SunShot’s PV portfolio spans work from early-stage solar cell research through technology commercialization, including work on materials,more » processes, and device structure and characterization techniques.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.loc.gov/pictures/collection/hh/item/in0331.photos.374795p/','SCIGOV-HHH'); return false;" href="https://www.loc.gov/pictures/collection/hh/item/in0331.photos.374795p/"><span>13. Photograph of <span class="hlt">sheet</span> 1 (index and title <span class="hlt">sheet</span>) of ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>13. Photograph of <span class="hlt">sheet</span> 1 (index and title <span class="hlt">sheet</span>) of the Indiana State Highway Commission repair plans of 1969 for the Cicott Street Bridge. Photograph of a 24' by 36' print made from microfilm in the archives of the Indiana Department of Transportation in Indianapolis. - Cicott Street Bridge, Spanning Wabash River at State Road 25, Logansport, Cass County, IN</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27538109','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27538109"><span>The Efficacy of a Silicone <span class="hlt">Sheet</span> in Postoperative Scar Management.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kim, Jin Sam; Hong, Joon Pio; Choi, Jong Woo; Seo, Dong Kyo; Lee, Eun Sook; Lee, Ho Seong</p> <p>2016-09-01</p> <p>Silicone gel <span class="hlt">sheeting</span> has been introduced to prevent scarring, but objective evidence for its usefulness in scar healing is limited. Therefore, the authors' objective was to examine the effectiveness of silicone gel <span class="hlt">sheeting</span> by randomly applying it to only unilateral scars from a bilateral hallux valgus surgery with symmetrical closure. In a prospective randomized, blinded, intraindividual comparison study, the silicone gel <span class="hlt">sheeting</span> was applied to 1 foot of a hallux valgus incision scar (an experiment group) for 12 weeks upon removal of the stitches, whereas the symmetrical scar from the other foot was left untreated (a control group). The scars were evaluated at 4 and 12 weeks after the silicon <span class="hlt">sheet</span> application. The Vancouver Scar Scale was used to measure the vascularity, pigmentation, pliability, height, and length of the scars. Adverse effects were also evaluated, and they included pain, itchiness, rash, erythema, and skin softening. At weeks 4 and 12, the experiment group scored significantly better on the Vancouver Scar Scale in all items, except length (P < .05 for all except the length of scar), compared with the control group. In all items, adverse effects of the experiment group were significantly lower than those of the control group at week 12, suggesting that <span class="hlt">direct</span> attachment of the silicone <span class="hlt">sheet</span> does not cause adverse effects (P < .05). To the authors' knowledge, this is one of the first models to minimize bias related to scar evaluation by using symmetrical scars. The early silicone <span class="hlt">sheet</span> application did show a significant improvement in prevention of postoperative scarring.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1999PhDT.......166M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1999PhDT.......166M"><span>Nonlinear distortion of thin liquid <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mehring, Carsten Ralf</p> <p></p> <p>Thin planar, annular and conical liquid <span class="hlt">sheets</span> or films are analyzed, in a unified manner, by means of a reduced- dimension approach providing governing equations for the nonlinear motion of planar and swirling annular thin inviscid and incompressible liquid <span class="hlt">sheets</span> in zero gravity and with axial disturbances only. Temporal analyses of periodically disturbed infinite <span class="hlt">sheets</span> are considered, as well as spatial analyses of semi-infinite <span class="hlt">sheets</span> modulated at the nozzle exit. Results on planar and swirling annular or conical <span class="hlt">sheets</span> are presented for a zero density ambient gas. Here, conical <span class="hlt">sheets</span> are obtained in the nearfield of the nozzle exit by considering <span class="hlt">sheets</span> or films with swirl in excess of that needed to stabilize the discharging stream in its annular configuration. For nonswirling annular <span class="hlt">sheets</span> a spatially and/or temporally constant gas-core pressure is assumed. A model extension considering the influence of aerodynamic effects on planar <span class="hlt">sheets</span> is proposed. For planar and annular <span class="hlt">sheets</span>, linear analyses of the pure initial- and pure boundary-value problem provide insight into the propagation characteristics of dilational and sinuous waves, the (linear) coupling between both wave modes, the stability limits for the annular configuration, as well as the appearance of particular waves on semi-infinite modulated <span class="hlt">sheets</span> downstream from the nozzle exit. Nonlinear steady-state solutions for the conical configuration (without modulation) are illustrated. Comparison between nonlinear and linear numerical and linear analytical solutions for temporally or spatially developing <span class="hlt">sheets</span> provides detailed information on the nonlinear distortion characteristics including nonlinear wave propagation and mode-coupling for all the considered geometric configurations and for a variety of parameter configurations. Sensitivity studies on the influence of Weber number, modulation frequency, annular radius, forcing amplitude and <span class="hlt">sheet</span> divergence on breakup or collapse length and times</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19920041911&hterms=balance+sheet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dbalance%2Bsheet','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19920041911&hterms=balance+sheet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dbalance%2Bsheet"><span>Nonadiabatic heating of the central plasma <span class="hlt">sheet</span> at substorm onset</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Huang, C. Y.; Frank, L. A.; Rostoker, G.; Fennell, J.; Mitchell, D. G.</p> <p>1992-01-01</p> <p>Heating events in the plasma <span class="hlt">sheet</span> boundary layer and central plasma <span class="hlt">sheet</span> are found to occur at the onset of expansive phase <span class="hlt">activity</span>. The main effect is a dramatic increase in plasma temperature, coincident with a partial dipolarization of the magnetic field. Fluxes of energetic particles increase without dispersion during these events which occur at all radial distances up to 23 RE, the apogee of the ISEE spacecraft. A major difference between these heating events and those observed at geosynchronous distances lies in the heating mechanism which is nonadiabatic beyond 10 RE but may be adiabatic closer to earth. The energy required to account for the increase in plasma thermal energy is comparable with that required for Joule heating of the ionosphere. The plasma <span class="hlt">sheet</span> must be considered as a major sink in the energy balance of a substorm. Lobe magnetic pressures during these events are estimated. Change in lobe pressure are generally not correlated with onsets or intensifications of expansive phase <span class="hlt">activity</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21898102','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21898102"><span>Environmental controls on microbial abundance and <span class="hlt">activity</span> on the greenland ice <span class="hlt">sheet</span>: a multivariate analysis approach.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stibal, Marek; Telling, Jon; Cook, Joe; Mak, Ka Man; Hodson, Andy; Anesio, Alexandre M</p> <p>2012-01-01</p> <p>Microbes in supraglacial ecosystems have been proposed to be significant contributors to regional and possibly global carbon cycling, and quantifying the biogeochemical cycling of carbon in glacial ecosystems is of great significance for global carbon flow estimations. Here we present data on microbial abundance and productivity, collected along a transect across the ablation zone of the Greenland ice <span class="hlt">sheet</span> (GrIS) in summer 2010. We analyse the relationships between the physical, chemical and biological variables using multivariate statistical analysis. Concentrations of debris-bound nutrients increased with distance from the ice <span class="hlt">sheet</span> margin, as did both cell numbers and <span class="hlt">activity</span> rates before reaching a peak (photosynthesis) or a plateau (respiration, abundance) between 10 and 20 km from the margin. The results of productivity measurements suggest an overall net autotrophy on the GrIS and support the proposed role of ice <span class="hlt">sheet</span> ecosystems in carbon cycling as regional sinks of CO(2) and places of production of organic matter that can be a potential source of nutrients for downstream ecosystems. Principal component analysis based on chemical and biological data revealed three clusters of sites, corresponding to three 'glacier ecological zones', confirmed by a redundancy analysis (RDA) using physical data as predictors. RDA using data from the largest 'bare ice zone' showed that glacier surface slope, a proxy for melt water flow, accounted for most of the variation in the data. Variation in the chemical data was fully explainable by the determined physical variables. Abundance of phototrophic microbes and their proportion in the community were identified as significant controls of the carbon cycling-related microbial processes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27139861','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27139861"><span>Light manipulation with flat and conformal inhomogeneous dispersive impedance <span class="hlt">sheets</span>: an efficient FDTD modeling.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jafar-Zanjani, Samad; Cheng, Jierong; Mosallaei, Hossein</p> <p>2016-04-10</p> <p>An efficient auxiliary differential equation method for incorporating 2D inhomogeneous dispersive impedance <span class="hlt">sheets</span> in the finite-difference time-domain solver is presented. This unique proposed method can successfully solve optical problems of current interest involving 2D <span class="hlt">sheets</span>. It eliminates the need for ultrafine meshing in the thickness <span class="hlt">direction</span>, resulting in a significant reduction of computation time and memory requirements. We apply the method to characterize a novel broad-beam leaky-wave antenna created by cascading three sinusoidally modulated reactance surfaces and also to study the effect of curvature on the radiation characteristic of a conformal impedance <span class="hlt">sheet</span> holographic antenna. Considerable improvement in the simulation time based on our technique in comparison with the traditional volumetric model is reported. Both applications are of great interest in the field of antennas and 2D <span class="hlt">sheets</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110008252','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110008252"><span>Recent Changes in the Greenland Ice <span class="hlt">Sheet</span> as Seen from Space</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hall, Dorothy K.</p> <p>2011-01-01</p> <p>Many changes in the Greenland Ice <span class="hlt">Sheet</span> have been reported in the recent scientific literature and have been attributed to various responses of the ice <span class="hlt">sheet</span> due to regional (and global) warming. Because melting of the ice <span class="hlt">sheet</span> would contribute approximately 7 m to sea-level rise, the lives and habitat of hundreds of millions of people worldwide would be <span class="hlt">directly</span> and indirectly affected if continued ice-<span class="hlt">sheet</span> melting occurs. As mean-annual global temperatures have increased, there has been an increasing focus on studying the Greenland Ice <span class="hlt">Sheet</span> using available satellite data, and numerous expeditions have been undertaken. Regional "clear-sky" surface temperature increases since the early 1980s in the Arctic, measured using Advanced Very High Resolution Radiometer (AVHRR) infrared data, range from 0.57+/-0.02 C to 0.72+/-0.10 C per decade. Arctic warming has important implications for ice-<span class="hlt">sheet</span> mass balance because much of the periphery of the Greenland Ice <span class="hlt">Sheet</span> is already near O C during the melt season, and is thus vulnerable to more extensive melting if temperatures continue to increase. An increase in melting of the ice <span class="hlt">sheet</span> would accelerate sea-level rise, an issue of increasing concern to billions of people worldwide. The surface temperature of the ice <span class="hlt">sheet</span> has been studied in even greater detail using Moderate-Resolution Imaging Spectroradiometer (MODIS) data in the six individual drainage basins as well as for the ice <span class="hlt">sheet</span> as a whole. Surface temperature trends in the decade of the 2000s have not been strong, according to the MODIS measurements. In addition to surface-temperature increases over the last few decades as measured by AVHRR, other changes have been observed such as accelerated movement of many of Greenland's outlet glaciers and sudden draining of supraglacial lakes. Decreasing mass of the ice <span class="hlt">sheet</span> since (at least) 2002 has been measured using Gravity Recovery and Climate Experiment (GRACE) data, along with an build-up of ice at the higher</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED498906.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED498906.pdf"><span>College Experience and Volunteering. Fact <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Marcelo, Karlo Barrios</p> <p>2007-01-01</p> <p>College experience and volunteering are positively correlated. Measurable differences in civic <span class="hlt">activity</span> exist between young people who attend college and young people who do not. This fact <span class="hlt">sheet</span> explores volunteering as civic engagement among youth with college experience, ages 19-25, which was down for the second year in a row in 2006. The…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4508962','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4508962"><span>Radiostratigraphy and age structure of the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>MacGregor, Joseph A; Fahnestock, Mark A; Catania, Ginny A; Paden, John D; Prasad Gogineni, S; Young, S Keith; Rybarski, Susan C; Mabrey, Alexandria N; Wagman, Benjamin M; Morlighem, Mathieu</p> <p>2015-01-01</p> <p>Several decades of ice-penetrating radar surveys of the Greenland and Antarctic ice <span class="hlt">sheets</span> have observed numerous widespread internal reflections. Analysis of this radiostratigraphy has produced valuable insights into ice <span class="hlt">sheet</span> dynamics and motivates additional mapping of these reflections. Here we present a comprehensive deep radiostratigraphy of the Greenland Ice <span class="hlt">Sheet</span> from airborne deep ice-penetrating radar data collected over Greenland by The University of Kansas between 1993 and 2013. To map this radiostratigraphy efficiently, we developed new techniques for predicting reflection slope from the phase recorded by coherent radars. When integrated along track, these slope fields predict the radiostratigraphy and simplify semiautomatic reflection tracing. Core-intersecting reflections were dated using synchronized depth-age relationships for six deep ice cores. Additional reflections were dated by matching reflections between transects and by extending reflection-inferred depth-age relationships using the local effective vertical strain rate. The oldest reflections, dating to the Eemian period, are found mostly in the northern part of the ice <span class="hlt">sheet</span>. Within the onset regions of several fast-flowing outlet glaciers and ice streams, reflections typically do not conform to the bed topography. Disrupted radiostratigraphy is also observed in a region north of the Northeast Greenland Ice Stream that is not presently flowing rapidly. Dated reflections are used to generate a gridded age volume for most of the ice <span class="hlt">sheet</span> and also to determine the depths of key climate transitions that were not observed <span class="hlt">directly</span>. This radiostratigraphy provides a new constraint on the dynamics and history of the Greenland Ice <span class="hlt">Sheet</span>. Key Points Phase information predicts reflection slope and simplifies reflection tracing Reflections can be dated away from ice cores using a simple ice flow model Radiostratigraphy is often disrupted near the onset of fast ice flow PMID:26213664</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.loc.gov/pictures/collection/hh/item/in0331.photos.374791p/','SCIGOV-HHH'); return false;" href="https://www.loc.gov/pictures/collection/hh/item/in0331.photos.374791p/"><span>9. Photograph of <span class="hlt">sheet</span> 1 (index and title <span class="hlt">sheet</span>) of ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>9. Photograph of <span class="hlt">sheet</span> 1 (index and title <span class="hlt">sheet</span>) of the State Highway Department of Indiana repair plans of 1957 for the Cicott Street Bridge. Photograph of a 24' by 36' print made from microfilm in the archives of the Indiana Department of Transportation in Indianapolis. - Cicott Street Bridge, Spanning Wabash River at State Road 25, Logansport, Cass County, IN</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920010505','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920010505"><span>FDTD modeling of thin impedance <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Luebbers, Raymond J.; Kunz, Karl S.</p> <p>1991-01-01</p> <p>Thin <span class="hlt">sheets</span> of resistive or dielectric material are commonly encountered in radar cross section calculations. Analysis of such <span class="hlt">sheets</span> is simplified by using <span class="hlt">sheet</span> impedances. In this paper it is shown that <span class="hlt">sheet</span> impedances can be modeled easily and accurately using Finite Difference Time Domain (FDTD) methods.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70034736','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70034736"><span>Obliquity-paced Pliocene West Antarctic ice <span class="hlt">sheet</span> oscillations</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Naish, T.; Powell, R.; Levy, R.; Wilson, G.; Scherer, R.; Talarico, F.; Krissek, L.; Niessen, F.; Pompilio, M.; Wilson, T.; Carter, L.; DeConto, R.; Huybers, P.; McKay, R.; Pollard, D.; Ross, J.; Winter, D.; Barrett, P.; Browne, G.; Cody, R.; Cowan, E.; Crampton, J.; Dunbar, G.; Dunbar, N.; Florindo, F.; Gebhardt, C.; Graham, I.; Hannah, M.; Hansaraj, D.; Harwood, D.; Helling, D.; Henrys, S.; Hinnov, L.; Kuhn, G.; Kyle, P.; Laufer, A.; Maffioli, P.; Magens, D.; Mandernack, K.; McIntosh, W.; Millan, C.; Morin, R.; Ohneiser, C.; Paulsen, T.; Persico, D.; Raine, I.; Reed, J.; Riesselman, C.; Sagnotti, L.; Schmitt, D.; Sjunneskog, C.; Strong, P.; Taviani, M.; Vogel, S.; Wilch, T.; Williams, T.</p> <p>2009-01-01</p> <p>Thirty years after oxygen isotope records from microfossils deposited in ocean sediments confirmed the hypothesis that variations in the Earth's orbital geometry control the ice ages1, fundamental questions remain over the response of the Antarctic ice <span class="hlt">sheets</span> to orbital cycles2. Furthermore, an understanding of the behaviour of the marine-based West Antarctic ice <span class="hlt">sheet</span> (WAIS) during the 'warmer-than-present' early-Pliocene epoch (5–3 Myr ago) is needed to better constrain the possible range of ice-<span class="hlt">sheet</span> behaviour in the context of future global warming3. Here we present a marine glacial record from the upper 600 m of the AND-1B sediment core recovered from beneath the northwest part of the Ross ice shelf by the ANDRILL programme and demonstrate well-dated, 40-kyr cyclic variations in ice-<span class="hlt">sheet</span> extent linked to cycles in insolation influenced by changes in the Earth's axial tilt (obliquity) during the Pliocene. Our data provide <span class="hlt">direct</span> evidence for orbitally induced oscillations in the WAIS, which periodically collapsed, resulting in a switch from grounded ice, or ice shelves, to open waters in the Ross embayment when planetary temperatures were up to 3 °C warmer than today4 and atmospheric CO2 concentration was as high as 400 p.p.m.v. (refs 5, 6). The evidence is consistent with a new ice-<span class="hlt">sheet</span>/ice-shelf model7 that simulates fluctuations in Antarctic ice volume of up to +7 m in equivalent sea level associated with the loss of the WAIS and up to +3 m in equivalent sea level from the East Antarctic ice <span class="hlt">sheet</span>, in response to ocean-induced melting paced by obliquity. During interglacial times, diatomaceous sediments indicate high surface-water productivity, minimal summer sea ice and air temperatures above freezing, suggesting an additional influence of surface melt8 under conditions of elevated CO2.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JGRA..119.1827C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JGRA..119.1827C"><span>The quiet evening auroral arc and the structure of the growth phase near-Earth plasma <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Coroniti, F. V.; Pritchett, P. L.</p> <p>2014-03-01</p> <p>The plasma pressure and current configuration of the near-Earth plasma <span class="hlt">sheet</span> that creates and sustains the quiet evening auroral arc during the growth phase of magnetospheric substorms is investigated. We propose that the quiet evening arc (QEA) connects to the thin near-Earth current <span class="hlt">sheet</span>, which forms during the development of the growth phase enhancement of convection. The current <span class="hlt">sheet</span>'s large polarization electric fields are shielded from the ionosphere by an Inverted-V parallel potential drop, thereby producing the electron precipitation responsible for the arc's luminosity. The QEA is located in the plasma <span class="hlt">sheet</span> region of maximal radial pressure gradient and, in the east-west <span class="hlt">direction</span>, follows the vanishing of the approximately dawn-dusk-<span class="hlt">directed</span> gradient or fold in the plasma pressure. In the evening sector, the boundary between the Region1 and Region 2 current systems occurs where the pressure maximizes (approximately radial gradient of the pressure vanishes) and where the approximately radial gradient of the magnetic flux tube volume also vanishes in an inflection region. The proposed intricate balance of plasma <span class="hlt">sheet</span> pressure and currents may well be very sensitive to disruption by the arrival of equatorward traveling auroral streamers and their associated earthward traveling dipolarization fronts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018CPL...698...85S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018CPL...698...85S"><span>Structural, electronic structure and antibacterial properties of graphene-oxide nano-<span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sharma, Aditya; Varshney, Mayora; Nanda, Sitansu Sekhar; Shin, Hyun Joon; Kim, Namdong; Yi, Dong Kee; Chae, Keun-Hwa; Ok Won, Sung</p> <p>2018-04-01</p> <p>Correlation between the structural/electronic structure properties and bio-<span class="hlt">activity</span> of graphene-based materials need to be thoroughly evaluated before their commercial implementation in the health and environment precincts. To better investigate the local hybridization of sp2/sp3 orbitals of the functional groups of graphene-oxide (GO) and their execution in the antimicrobial mechanism, we exemplify the antibacterial <span class="hlt">activity</span> of GO <span class="hlt">sheets</span> towards the Escherichia coli bacteria (E. coli) by applying the field-emission scanning electron microscopy (FESEM), near edge X-ray absorption fine structure (NEXAFS) and scanning transmission X-ray microscope (STXM) techniques. C K-edge and O K-edge NEXAFS spectra have revealed lesser sp2 carbon atoms in the aromatic ring and attachment of functional oxygen groups at GO <span class="hlt">sheets</span>. Entrapment of E. coli bacteria by GO <span class="hlt">sheets</span> is evidenced by FESEM investigations and has also been corroborated by nano-scale imaging of bacteria using the STXM. Spectroscopy evidence of functional oxygen moieties with GO <span class="hlt">sheets</span> and physiochemical entrapment of E. coli bacteria have assisted us to elaborate the mechanism of cellular oxidative stress-induced disruption of bacterial membrane.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3601593','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3601593"><span>Three dimensional HiLo-based structured illumination for a digital scanned laser <span class="hlt">sheet</span> microscopy (DSLM) in thick tissue imaging</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Bhattacharya, Dipanjan; Singh, Vijay Raj; Zhi, Chen; So, Peter T. C.; Matsudaira, Paul; Barbastathis, George</p> <p>2012-01-01</p> <p>Laser <span class="hlt">sheet</span> based microscopy has become widely accepted as an effective <span class="hlt">active</span> illumination method for real time three-dimensional (3D) imaging of biological tissue samples. The light <span class="hlt">sheet</span> geometry, where the camera is oriented perpendicular to the <span class="hlt">sheet</span> itself, provides an effective method of eliminating some of the scattered light and minimizing the sample exposure to radiation. However, residual background noise still remains, limiting the contrast and visibility of potentially interesting features in the samples. In this article, we investigate additional structuring of the illumination for improved background rejection, and propose a new technique, “3D HiLo” where we combine two HiLo images processed from orthogonal <span class="hlt">directions</span> to improve the condition of the 3D reconstruction. We present a comparative study of conventional structured illumination based demodulation methods, namely 3Phase and HiLo with a newly implemented 3D HiLo approach and demonstrate that the latter yields superior signal-to-background ratio in both lateral and axial dimensions, while simultaneously suppressing image processing artifacts. PMID:23262684</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23262684','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23262684"><span>Three dimensional HiLo-based structured illumination for a digital scanned laser <span class="hlt">sheet</span> microscopy (DSLM) in thick tissue imaging.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bhattacharya, Dipanjan; Singh, Vijay Raj; Zhi, Chen; So, Peter T C; Matsudaira, Paul; Barbastathis, George</p> <p>2012-12-03</p> <p>Laser <span class="hlt">sheet</span> based microscopy has become widely accepted as an effective <span class="hlt">active</span> illumination method for real time three-dimensional (3D) imaging of biological tissue samples. The light <span class="hlt">sheet</span> geometry, where the camera is oriented perpendicular to the <span class="hlt">sheet</span> itself, provides an effective method of eliminating some of the scattered light and minimizing the sample exposure to radiation. However, residual background noise still remains, limiting the contrast and visibility of potentially interesting features in the samples. In this article, we investigate additional structuring of the illumination for improved background rejection, and propose a new technique, "3D HiLo" where we combine two HiLo images processed from orthogonal <span class="hlt">directions</span> to improve the condition of the 3D reconstruction. We present a comparative study of conventional structured illumination based demodulation methods, namely 3Phase and HiLo with a newly implemented 3D HiLo approach and demonstrate that the latter yields superior signal-to-background ratio in both lateral and axial dimensions, while simultaneously suppressing image processing artifacts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=US+AND+fertility+AND+rates&pg=4&id=ED305283','ERIC'); return false;" href="https://eric.ed.gov/?q=US+AND+fertility+AND+rates&pg=4&id=ED305283"><span>World Population: Facts in Focus. World Population Data <span class="hlt">Sheet</span> Workbook. Population Learning Series.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Crews, Kimberly A.</p> <p></p> <p>This workbook teaches population analysis using world population statistics. To complete the four student <span class="hlt">activity</span> <span class="hlt">sheets</span>, the students refer to the included "1988 World Population Data <span class="hlt">Sheet</span>" which lists nations' statistical data that includes population totals, projected population, birth and death rates, fertility levels, and the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22512425','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22512425"><span>The decisional balance <span class="hlt">sheet</span> to promote healthy behavior among ethnically diverse older adults.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Geller, Karly S; Mendoza, Ilora D; Timbobolan, Jasah; Montjoy, Holly L; Nigg, Claudio R</p> <p>2012-01-01</p> <p>The rising health care costs and increasing older adult population in the United States make preventive medicine for this age group especially crucial. Regular physical <span class="hlt">activity</span> and fruit and vegetable consumption may prevent or delay the onset of many chronic conditions that are common among older adults. The decisional balance <span class="hlt">sheet</span> is a promotional tool targeting the perceived pros and cons of behavior adoption. The current study tested the efficiency and effectiveness of a single-day decisional balance <span class="hlt">sheet</span> program, targeting increased physical <span class="hlt">activity</span> and fruit and vegetable intake among older adults. Participating adults (N = 21, age = 72.2) who represented a diverse population in Hawaii (Japanese = 5, Filipino = 4, Caucasian = 4, Native American = 1, Native Hawaiian = 1, Hispanic = 1, and Others = 5) were recruited from housing communities and randomized to a decisional balance <span class="hlt">sheet</span> program adapted for physical <span class="hlt">activity</span> or fruit and vegetable consumption. Physical <span class="hlt">activity</span> was assessed using the International Physical <span class="hlt">Activity</span> Questionnaire (IPAQ) short form, and daily fruit and vegetable intake with the National Health and Nutrition Examination Survey single item instrument. Baseline and follow-up data were collected. Both programs were implemented efficiently, and participants in both groups improved their daily physical <span class="hlt">activity</span>. The decisional balance <span class="hlt">sheet</span> for fruit and vegetable consumption appeared less effective. Specific suggestions for similar programs are reported. © 2011 Wiley Periodicals, Inc.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_13 --> <div id="page_14" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="261"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AnGeo..35.1015X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AnGeo..35.1015X"><span>Occurrence rate of dipolarization fronts in the plasma <span class="hlt">sheet</span>: Cluster observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xiao, Sudong; Zhang, Tielong; Wang, Guoqiang; Volwerk, Martin; Ge, Yasong; Schmid, Daniel; Nakamura, Rumi; Baumjohann, Wolfgang; Plaschke, Ferdinand</p> <p>2017-08-01</p> <p>We investigate the occurrence rate of dipolarization fronts (DFs) in the plasma <span class="hlt">sheet</span> by taking full advantage of all four Cluster satellites (C1-4) from years 2001 to 2009. In total, we select 466 joint-observation DF events, in which 318, 282, 254, and 236 DFs are observed by C1, C2, C3, and C4, respectively. Our findings are as follows: (1) the maximum occurrence rate is ˜ 15.3 events per day at X ˜ 15 RE in the XY plane, and the average occurrence rate is ˜ 5.4 events per day over the whole observation period; (2) the occurrence rate on the dusk side of the plasma <span class="hlt">sheet</span> is larger and decreases with increasing BXY/BLobe; (3) the occurrence rate within |Y| < 6 RE increases gradually from X ≈ -19 to -15 RE and then decreases from X ≈ -15 to -10 RE; (4) the occurrence rate when AE > 200 nT is much larger than that when AE < 200 nT, indicating that DFs preferentially occur during high geomagnetic <span class="hlt">activity</span>. The magnetic pileup and earthward and duskward ion flows could contribute to the increases in the occurrence rate from X ≈ -19 to -15 RE. We suggest that both geomagnetic <span class="hlt">activity</span> and multiple DFs contribute to the high occurrence rate of the DFs. In addition, the finite length of the DF in the dawn-dusk <span class="hlt">direction</span> can affect the chance that a satellite observes the DF.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23633029','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23633029"><span>Dissecting the structural determinants for the difference in mechanical stability of silk and amyloid beta-<span class="hlt">sheet</span> stacks.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Xiao, Senbo; Xiao, Shijun; Gräter, Frauke</p> <p>2013-06-14</p> <p>Stacking of β-<span class="hlt">sheets</span> results in a protein super secondary structure with remarkable mechanical properties. β-Stacks are the determinants of a silk fiber's resilience and are also the building blocks of amyloid fibrils. While both silk and amyloid-type crystals are known to feature a high resistance against rupture, their structural and mechanical similarities and particularities are yet to be fully understood. Here, we systematically compare the rupture force and stiffness of amyloid and spider silk poly-alanine β-stacks of comparable sizes using Molecular Dynamics simulations. We identify the <span class="hlt">direction</span> of force application as the primary determinant of the rupture strength; β-<span class="hlt">sheets</span> in silk are orientated along the fiber axis, i.e. the pulling <span class="hlt">direction</span>, and consequently require high forces in the several nanoNewton range for shearing β-strands apart, while β-<span class="hlt">sheets</span> in amyloid are oriented vertically to the fiber, allowing a zipper-like rupture at sub-nanoNewton forces. A secondary factor rendering amyloid β-stacks softer and weaker than their spider silk counterparts is the sub-optimal side-chain packing between β-<span class="hlt">sheets</span> due to the sequence variations of amyloid-forming proteins as opposed to the perfectly packed poly-alanine β-<span class="hlt">sheets</span> of silk. Taken together, amyloid fibers can reach the stiffness of silk fibers in spite of their softer and weaker β-<span class="hlt">sheet</span> arrangement as they are missing a softening amorphous matrix.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/866298','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/866298"><span>Horizontal electromagnetic casting of thin metal <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Hull, John R.; Lari, Robert J.; Praeg, Walter F.; Turner, Larry R.</p> <p>1987-01-01</p> <p>Thin metal <span class="hlt">sheets</span> are cast by magnetically suspending molten metal deposited within a ferromagnetic yoke and between AC conducting coils and linearly displacing the magnetically levitated liquid metal while it is being cooled to form a solid metal <span class="hlt">sheet</span>. Magnetic flux increases as the molten metal <span class="hlt">sheet</span> moves downward and decreases as the molten metal <span class="hlt">sheet</span> moves upward to stabilize the <span class="hlt">sheet</span> and maintain it in equilibrium as it is linearly displaced and solidified by cooling gases. A conducting shield is electrically coupled to the molten metal <span class="hlt">sheet</span> by means of either metal <span class="hlt">sheet</span> engaging rollers or brushes on the solidified metal, and by means of an electrode in the vessel containing the molten metal thereby providing a return path for the eddy currents induced in the metal <span class="hlt">sheet</span> by the AC coil generated magnetic flux. Variation in the geometry of the conducting shield allows the magnetic flux between the metal <span class="hlt">sheet</span> and the conducting shield to be varied and the thickness in surface quality of the metal <span class="hlt">sheet</span> to be controlled. Side guards provide lateral containment for the molten metal <span class="hlt">sheet</span> and stabilize and shape the magnetic field while a leader <span class="hlt">sheet</span> having electromagnetic characteristics similar to those of the metal <span class="hlt">sheet</span> is used to start the casting process and precedes the molten metal <span class="hlt">sheet</span> through the magnet and forms a continuous <span class="hlt">sheet</span> therewith. The magnet may be either U-shaped with a single racetrack coil or may be rectangular with a pair of facing bedstead coils.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/866574','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/866574"><span>Horizontal electromagnetic casting of thin metal <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Hull, John R.; Lari, Robert J.; Praeg, Walter F.; Turner, Larry R.</p> <p>1988-01-01</p> <p>Thin metal <span class="hlt">sheets</span> are cast by magnetically suspending molten metal deposited within a ferromagnetic yoke and between AC conducting coils and linearly displacing the magnetically levitated liquid metal while it is being cooled to form a solid metal <span class="hlt">sheet</span>. Magnetic flux increases as the molten metal <span class="hlt">sheet</span> moves downward and decreases as the molten metal <span class="hlt">sheet</span> moves upward to stabilize the <span class="hlt">sheet</span> and maintain it in equilibrium as it is linearly displaced and solidified by cooling gases. A conducting shield is electrically coupled to the molten metal <span class="hlt">sheet</span> by means of either metal <span class="hlt">sheet</span> engaging rollers or brushes on the solidified metal, and by means of an electrode in the vessel containing the molten metal thereby providing a return path for the eddy currents induced in the metal <span class="hlt">sheet</span> by the AC coil generated magnetic flux. Variation in the geometry of the conducting shield allows the magnetic flux between the metal <span class="hlt">sheet</span> and the conducting shield to be varied and the thickness in surface quality of the metal <span class="hlt">sheet</span> to be controlled. Side guards provide lateral containment for the molten metal <span class="hlt">sheet</span> and stabilize and shape the magnetic field while a leader <span class="hlt">sheet</span> having electromagnetic characteristics similar to those of the metal <span class="hlt">sheet</span> is used to start the casting process and precedes the molten metal <span class="hlt">sheet</span> through the magnet and forms a continuous <span class="hlt">sheet</span> therewith. The magnet may be either U-shaped with a single racetrack coil or may be rectangular with a pair of facing bedstead coils.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27136124','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27136124"><span>Formation of Highly Aligned Collagen Nanofibers by Continuous Cyclic Stretch of a Collagen Hydrogel <span class="hlt">Sheet</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Nam, Eunryel; Lee, Won Chul; Takeuchi, Shoji</p> <p>2016-07-01</p> <p>A collagen <span class="hlt">sheet</span> with highly aligned collagen fibers is fabricated by continuous cyclic stretch. The rearrangement of the collagen fibers depends on the different process parameters of the cyclic stretch, including magnitude, frequency, and period of stretch. The collagen fibers are aligned perpendicularly to the <span class="hlt">direction</span> of the stretch. Corneal stromal cells and smooth muscle cells cultivated on the highly aligned collagen <span class="hlt">sheet</span> show alignment along the collagen fibers without the stretch during culture. Thus, the <span class="hlt">sheet</span> can be a suitable scaffold for use in regenerative medicine. © 2016 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/16095612','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/16095612"><span>Folding cooperativity in a three-stranded beta-<span class="hlt">sheet</span> model.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Roe, Daniel R; Hornak, Viktor; Simmerling, Carlos</p> <p>2005-09-16</p> <p>The thermodynamic behavior of a previously designed three-stranded beta-<span class="hlt">sheet</span> was studied via several microseconds of standard and replica exchange molecular dynamics simulations. The system is shown to populate at least four thermodynamic minima, including two partially folded states in which only a single hairpin is formed. Simulated melting curves show different profiles for the C and N-terminal hairpins, consistent with differences in secondary structure content in published NMR and CD/FTIR measurements, which probed different regions of the chain. Individual beta-hairpins that comprise the three-stranded beta-<span class="hlt">sheet</span> are observed to form cooperatively. Partial folding cooperativity between the component hairpins is observed, and good agreement between calculated and experimental values quantifying this cooperativity is obtained when similar analysis techniques are used. However, the structural detail in the ensemble of conformations sampled in the simulations permits a more <span class="hlt">direct</span> analysis of this cooperativity than has been performed on the basis of experimental data. The results indicate the actual folding cooperativity perpendicular to strand <span class="hlt">direction</span> is significantly larger than the lower bound obtained previously.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4805115','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4805115"><span>Folding cooperativity in a 3-stranded β-<span class="hlt">sheet</span> model</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Roe, Daniel R.; Hornak, Viktor</p> <p>2015-01-01</p> <p>Summary The thermodynamic behavior of a previously designed three-stranded β-<span class="hlt">sheet</span> was studied via several µs of standard and replica exchange molecular dynamics simulations. The system is shown to populate at least four thermodynamic minima, including 2 partially folded states in which only a single hairpin is formed. Simulated melting curves show different profiles for the C and N-terminal hairpins, consistent with differences in secondary structure content in published NMR and CD/FTIR measurements, which probed different regions of the chain. Individual β-hairpins that comprise the 3-stranded β-<span class="hlt">sheet</span> are observed to form cooperatively. Partial folding cooperativity between the component hairpins is observed, and good agreement between calculated and experimental values quantifying this cooperativity is obtained when similar analysis techniques are used. However, the structural detail in the ensemble of conformations sampled in the simulations permits a more <span class="hlt">direct</span> analysis of this cooperatively than has been performed based on experimental data. The results indicate the actual folding cooperativity perpendicular to strand <span class="hlt">direction</span> is significantly larger than the lower bound obtained previously. PMID:16095612</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1918710V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1918710V"><span>A Transient Initialization Routine of the Community Ice <span class="hlt">Sheet</span> Model for the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>van der Laan, Larissa; van den Broeke, Michiel; Noël, Brice; van de Wal, Roderik</p> <p>2017-04-01</p> <p>The Community Ice <span class="hlt">Sheet</span> Model (CISM) is to be applied in future simulations of the Greenland Ice <span class="hlt">Sheet</span> under a range of climate change scenarios, determining the sensitivity of the ice <span class="hlt">sheet</span> to individual climatic forcings. In order to achieve reliable results regarding ice <span class="hlt">sheet</span> stability and assess the probability of future occurrence of tipping points, a realistic initial ice <span class="hlt">sheet</span> geometry is essential. The current work describes and evaluates the development of a transient initialization routine, using NGRIP 18O isotope data to create a temperature anomaly field. Based on the latter, surface mass balance components runoff and precipitation are perturbed for the past 125k years. The precipitation and runoff fields originate from a downscaled 1 km resolution version of the regional climate model RACMO2.3 for the period 1961-1990. The result of the initialization routine is a present-day ice <span class="hlt">sheet</span> with a transient memory of the last glacial-interglacial cycle, which will serve as the future runs' initial condition.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005GApFD..99..433C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005GApFD..99..433C"><span>Wave-induced drift of large floating <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Christensen, K. H.; Weber, J. E.</p> <p></p> <p>In this article we study the wave-induced drift of large, flexible shallow floating objects, referred to as <span class="hlt">sheets</span>. When surface waves propagate through a <span class="hlt">sheet</span>, they provide a mean stress on the <span class="hlt">sheet</span>, resulting in a mean drift. In response, the <span class="hlt">sheet</span> generates an Ekman current. The drift velocity of the <span class="hlt">sheet</span> is determined by (i) the wave-induced stress, (ii) the viscous stress due to the Ekman current, and (iii) the Coriolis force. The <span class="hlt">sheet</span> velocity and the current beneath the <span class="hlt">sheet</span> are determined for constant and depth-varying eddy viscosities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1179035','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1179035"><span>Electrically driven rapidly vaporizing foils, wires and strips used for collision welding and <span class="hlt">sheet</span> metal forming</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Vivek, Anupam; Daehn, Glenn S; Taber, Geoffrey A</p> <p>2015-05-05</p> <p>A method for forming a piece of a <span class="hlt">sheet</span> metal is performed by positioning a consumable body, made of metal, proximate to the piece of the <span class="hlt">sheet</span> metal. The consumable body is rapidly vaporized, and the gas pressure generated thereby is <span class="hlt">directed</span> into the piece of the <span class="hlt">sheet</span> metal. This results in acceleration of the piece of <span class="hlt">sheet</span> metal, and it is collided into a stationary body at a velocity, generally in excess of 200 m/s. Depending upon the type of stationary body, the piece of <span class="hlt">sheet</span> metal is deformed into a predetermined shape or is welded onto the stationarymore » body. The vaporization is accomplished by passing a high current of electricity into the consumable body. The effect of the vaporized metal may be augmented by additional components in the consumable body.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED099653.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED099653.pdf"><span>Skill <span class="hlt">Sheets</span> for Agricultural Mechanics.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Iowa State Univ. of Science and Technology, Ames. Dept. of Agricultural Education.</p> <p></p> <p>This set of 33 skill <span class="hlt">sheets</span> for agricultural mechanics was developed for use in high school and vocational school agricultural mechanics programs. Some <span class="hlt">sheets</span> teach operational procedures while others are for simple projects. Each skill <span class="hlt">sheet</span> covers a single topic and includes: (1) a diagram, (2) a step-by-step construction or operational…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19870011449','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19870011449"><span>Static current-<span class="hlt">sheet</span> models of quiescent prominences</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wu, F.; Low, B. C.</p> <p>1986-01-01</p> <p>A particular class of theoretical models idealize the prominence to be a discrete flat electric-current <span class="hlt">sheet</span> suspended vertically in a potential magnetic field. The weight of the prominence is supported by the Lorentz force in the current <span class="hlt">sheet</span>. These models can be extended to have curved electric-current <span class="hlt">sheets</span> and to vary three-dimensionally. The equation for force balance is 1 over 4 pi (del times B) times Bdel p- p9 z=zero. Using Cartesian coordinates we take, for simplicity, a uniform gravity with constant acceleration g in the <span class="hlt">direction</span> -z. If we are interested not in the detailed internal structure of the prominence, but in the global magnetic configuration around the prominence, we may take prominence plasma to be cold. Consideration is given to how such equilibrium states can be constructed. To simplify the mathematical problem, suppose there is no electric current in the atmosphere except for the discrete currents in the cold prominence <span class="hlt">sheet</span>. Let us take the plane z =0 to be the base of the atmosphere and restrict our attention to the domain z greater than 0. The task we have is to solve for a magnetic field which is everywhere potential except on some free surface S, subject to suit able to boundary conditions. The surface S is determined by requiring that it possesses a discrete electric current density such that the Lorentz force on it is everywhere vertically upward to balance the weight of the material m(S). Since the magnetic field is potential in the external atmosphere, the latter is decoupled from the magnetic field and its plane parallel hydrostatic pressure and density can be prescribed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1986NASCP2442...69W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1986NASCP2442...69W"><span>Static current-<span class="hlt">sheet</span> models of quiescent prominences</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wu, F.; Low, B. C.</p> <p>1986-12-01</p> <p>A particular class of theoretical models idealize the prominence to be a discrete flat electric-current <span class="hlt">sheet</span> suspended vertically in a potential magnetic field. The weight of the prominence is supported by the Lorentz force in the current <span class="hlt">sheet</span>. These models can be extended to have curved electric-current <span class="hlt">sheets</span> and to vary three-dimensionally. The equation for force balance is 1 over 4 pi (del times B) times Bdel p- p9 z=zero. Using Cartesian coordinates we take, for simplicity, a uniform gravity with constant acceleration g in the <span class="hlt">direction</span> -z. If we are interested not in the detailed internal structure of the prominence, but in the global magnetic configuration around the prominence, we may take prominence plasma to be cold. Consideration is given to how such equilibrium states can be constructed. To simplify the mathematical problem, suppose there is no electric current in the atmosphere except for the discrete currents in the cold prominence <span class="hlt">sheet</span>. Let us take the plane z =0 to be the base of the atmosphere and restrict our attention to the domain z greater than 0. The task we have is to solve for a magnetic field which is everywhere potential except on some free surface S, subject to suit able to boundary conditions. The surface S is determined by requiring that it possesses a discrete electric current density such that the Lorentz force on it is everywhere vertically upward to balance the weight of the material m(S). Since the magnetic field is potential in the external atmosphere, the latter is decoupled from the magnetic field and its plane parallel hydrostatic pressure and density can be prescribed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.T13D3045C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.T13D3045C"><span>Cryosphere Science Outreach using the Ice <span class="hlt">Sheet</span> System Model and a Virtual Ice <span class="hlt">Sheet</span> Laboratory</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cheng, D. L. C.; Halkides, D. J.; Larour, E. Y.</p> <p>2015-12-01</p> <p>Understanding the role of Cryosphere Science within the larger context of Sea Level Rise is both a technical and educational challenge that needs to be addressed if the public at large is to trulyunderstand the implications and consequences of Climate Change. Within this context, we propose a new approach in which scientific tools are used <span class="hlt">directly</span> inside a mobile/website platform geared towards Education/Outreach. Here, we apply this approach by using the Ice <span class="hlt">Sheet</span> System Model, a state of the art Cryosphere model developed at NASA, and integrated within a Virtual Ice <span class="hlt">Sheet</span> Laboratory, with the goal is to outreach Cryospherescience to K-12 and College level students. The approach mixes laboratory experiments, interactive classes/lessons on a website, and a simplified interface to a full-fledged instance of ISSM to validate the classes/lessons. This novel approach leverages new insights from the Outreach/Educational community and the interest of new generations in web based technologies and simulation tools, all of it delivered in a seamlessly integrated web platform. This work was performed at the California Institute of Technology's Jet Propulsion Laboratory undera contract with the National Aeronautics and Space Administration's Cryosphere Science Program.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29916810','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29916810"><span>High-fidelity Characterization on Anisotropic Thermal Conductivity of Carbon Nanotube <span class="hlt">Sheets</span> and on their effects of Thermal Enhancement of Nanocomposites.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhang, Xiao; Tan, Wei; Smail, Fiona; De Volder, Michael; Fleck, Norman; Boies, Adam</p> <p>2018-06-19</p> <p>Some assemblies of nanomaterials, like carbon nanotube (CNT) <span class="hlt">sheet</span> or film, always show outstanding and anisotropic thermal properties. However, there is still a lack of comprehensive thermal conductivity (κ) characterizations on CNT <span class="hlt">sheets</span>, as well as lack of estimations of their true contributions on thermal enhancement of polymer composites when used as additives. Always, these characterizations were hindered by the low heat capacity, anisotropic thermal properties or low electrical conductivity of assemblies and their nanocomposites. And the transient κ measurement and calculations were also hampered by accurate determination of parameters, like specific heat capacity, density and cross-section, which could be difficult and controversial for nanomaterials, like CNT <span class="hlt">sheets</span>. Here, to measure anisotropic κ of CNT <span class="hlt">sheets</span> <span class="hlt">directly</span> with high fidelity, we modified the conventional steady-state method by measuring under vacuum and by infrared camera, and then comparing temperature profiles on both reference standard material and a CNT <span class="hlt">sheet</span> sample. The highly anisotropic thermal conductivities of CNT <span class="hlt">sheets</span> were characterized comprehensively, with κ/ρ in alignment <span class="hlt">direction</span> as ~95 mW·m^2/(K·kg). Furthermore, by comparing the measured thermal properties of different CNT-epoxy resin composites, the heat conduction pathway created by the CNT hierarchical network was demonstrated to remain intact after the in-situ polymerization and curing process. The reliable and <span class="hlt">direct</span> κ measurement rituals used here, dedicated to nanomaterials, will be also essential to assist in assemblies' application to heat dissipation and composite thermal enhancement. © 2018 IOP Publishing Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=importance+AND+leisure+AND+time&pg=6&id=ED252007','ERIC'); return false;" href="https://eric.ed.gov/?q=importance+AND+leisure+AND+time&pg=6&id=ED252007"><span>Someday I May Want to Know about...Leisure and Recreational <span class="hlt">Activities</span> for Children and Adults with Mental Retardation. A MCARC Information <span class="hlt">Sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Montgomery County Association for Retarded Citizens, Rockville, MD.</p> <p></p> <p>The fact <span class="hlt">sheet</span> considers the importance of recreation and leisure time <span class="hlt">activities</span> for people with mental retardation. A case is made for mainstreamed services, and suggestions are offered for families seeking to procure successful mainstreamed experiences in community recreational programs. Among suggestions are adapting family games to the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23907770','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23907770"><span>Aligned carbon nanotube-silicon <span class="hlt">sheets</span>: a novel nano-architecture for flexible lithium ion battery electrodes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Fu, Kun; Yildiz, Ozkan; Bhanushali, Hardik; Wang, Yongxin; Stano, Kelly; Xue, Leigang; Zhang, Xiangwu; Bradford, Philip D</p> <p>2013-09-25</p> <p>Aligned carbon nanotube <span class="hlt">sheets</span> provide an engineered scaffold for the deposition of a silicon <span class="hlt">active</span> material for lithium ion battery anodes. The <span class="hlt">sheets</span> are low-density, allowing uniform deposition of silicon thin films while the alignment allows unconstrained volumetric expansion of the silicon, facilitating stable cycling performance. The flat <span class="hlt">sheet</span> morphology is desirable for battery construction. © 2013 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29932425','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29932425"><span>Fabrication of multiwall carbon nanotube <span class="hlt">sheet</span> based hydrogen sensor on a stacking multi-layer structure.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yan, Keyi; Toku, Yuhki; Morita, Yasuyuki; Ju, Yang</p> <p>2018-06-22</p> <p>In this research, we propose a new simple method to fabricate hydrogen gas sensor by stacking the multiwall carbon nanotube (MWCNT) <span class="hlt">sheets</span>. MWCNT <span class="hlt">sheet</span> offers a larger surface area and more CNT contacts, which are key factors for gas sensing, because of its super-high alignment and end-to-end structure comparing to the traditional CNT film. Besides, MWCNT <span class="hlt">sheet</span> can be <span class="hlt">directly</span> drawn from the spinnable CNT array in large scales. Therefore, this method is a potential answer for the mass production and commercialization of CNT based sensor with high response. By stacking different layers of <span class="hlt">sheet</span>, microstructure and CNT interactions in the layers were changed and their influences towards gas sensing were investigated. It was observed that the sample with 3 layers of <span class="hlt">sheet</span> and functionalized with 3 nm-thick Pd showed the best gas sensing performance with a response of 12.31% at 4% H2 and response time below 200 s. © 2018 IOP Publishing Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4451805','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4451805"><span>Theoretical predictions on the electronic structure and charge carrier mobility in 2D Phosphorus <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Xiao, Jin; Long, Mengqiu; Zhang, Xiaojiao; Ouyang, Jun; Xu, Hui; Gao, Yongli</p> <p>2015-01-01</p> <p>We have investigated the electronic structure and carrier mobility of four types of phosphorous monolayer <span class="hlt">sheet</span> (α-P, β-P,γ-P and δ-P) using density functional theory combined with Boltzmann transport method and relaxation time approximation. It is shown that α-P, β-P and γ-P are indirect gap semiconductors, while δ-P is a <span class="hlt">direct</span> one. All four <span class="hlt">sheets</span> have ultrahigh carrier mobility and show anisotropy in-plane. The highest mobility value is ~3 × 105 cm2V−1s−1, which is comparable to that of graphene. Because of the huge difference between the hole and electron mobilities, α-P, γ-P and δ-P <span class="hlt">sheets</span> can be considered as n-type semiconductors, and β-P <span class="hlt">sheet</span> can be considered as a p-type semiconductor. Our results suggest that phosphorous monolayer <span class="hlt">sheets</span> can be considered as a new type of two dimensional materials for applications in optoelectronics and nanoelectronic devices. PMID:26035176</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19930068913&hterms=powder+metallurgy&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dpowder%2Bmetallurgy','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19930068913&hterms=powder+metallurgy&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3Dpowder%2Bmetallurgy"><span>A laboratory means to produce tough aluminum <span class="hlt">sheet</span> from powder</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Singleton, O. R.; Royster, D. M.; Thomas, J. R.</p> <p>1990-01-01</p> <p>The rapid solidification of aluminum alloys as powder and the subsequent fabrication processes can be used to develop and tailor alloys to satisfy specific aerospace design requirements, including high strength and toughness. Laboratory procedures to produce aluminum powder-metallurgy (PM) materials are efficient but require evidence that the laboratory methods used can produce a product with superior properties. This paper describes laboratory equipment and procedures which can be used to produce tough aluminum PM <span class="hlt">sheet</span>. The processing of a 2124 + 0.9 percent Zr aluminum alloy powder is used as an example. The fully hardened <span class="hlt">sheet</span> product is evaluated in terms of properties and microstructure. The key features of the vacuum hot press pressing operation used to consolidate the powder are described. The 2124 + 0.9 percent Zr - T8 temper aluminum <span class="hlt">sheet</span> produced was both strong (460-490 MPa yield strength) and tough (Kahn Tear unit-propagation- energy values over three times those typical for ingot metallurgy 2024-T81). Both the longitudinal and longitudinal-transverse <span class="hlt">directions</span> of the <span class="hlt">sheet</span> were tested. The microstructure was well refined with subgrains of one or two micrometers. Fine dispersoids of Al3Zr in the precipitate free regions adjacent to boundaries are believed to contribute to the improved toughness.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_14 --> <div id="page_15" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="281"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.U53C..03T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.U53C..03T"><span>Whillans Ice Stream Subglacial Access Research Drilling (WISSARD): Integrative Study of Marine Ice <span class="hlt">Sheet</span> Stability and Subglacial Life Habitats (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tulaczyk, S. M.; Anandakrishnan, S.; Behar, A. E.; Christner, B. C.; Fisher, A. T.; Fricker, H. A.; Holland, D. M.; Jacobel, R. W.; Mikucki, J.; Mitchell, A. C.; Powell, R. D.; Priscu, J. C.; Scherer, R. P.; Severinghaus, J. P.</p> <p>2009-12-01</p> <p>The WISSARD project is a large, NSF-funded, interdisciplinary initiative focused on scientific drilling, exploration, and investigation of Antarctic subglacial aquatic environments. The project consists of three interrelated components: (1) LISSARD - Lake and Ice Stream Subglacial Access Research Drilling, (2) RAGES - Robotic Access to Grounding-zones for Exploration and Science, and (3) GBASE - GeomicroBiology of Antarctic Subglacial Environments). A number of previous studies in West Antarctica highlighted the importance of understanding ice <span class="hlt">sheet</span> interactions with water, either at the basal boundary where ice streams come in contact with <span class="hlt">active</span> subglacial hydrologic and geological systems or at the marine margin where the ice <span class="hlt">sheet</span> is exposed to forcing from the global ocean and sedimentation. Recent biological investigations of Antarctic subglacial environments show that they provide a significant habitat for life and source of bacterial carbon in a setting that was previously thought to be inhospitable. Subglacial microbial ecosystems also enhance biogeochemical weathering, mobilizing elements from long term geological storage. The overarching scientific objective of WISSARD is to examine the subglacial hydrological system of West Antarctica in glaciological, geological, microbiological, geochemical, and oceanographic contexts. <span class="hlt">Direct</span> sampling will yield seminal information on these systems and test the overarching hypothesis that <span class="hlt">active</span> hydrological systems connect various subglacial environments and exert major control on ice <span class="hlt">sheet</span> dynamics, subglacial sediment transfer, geochemistry, metabolic and phylogenetic diversity, and biogeochemical transformations and geological records of ice <span class="hlt">sheet</span> history. Technological advances during WISSARD will provide the US-science community with a capability to access and study sub-ice <span class="hlt">sheet</span> environments. Developing this technological infrastructure will benefit the broader science community and it will be available for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=Global+AND+Warming+OR+Climate+AND+Change+OR+Warning&pg=6&id=EJ802493','ERIC'); return false;" href="https://eric.ed.gov/?q=Global+AND+Warming+OR+Climate+AND+Change+OR+Warning&pg=6&id=EJ802493"><span>The Physics of Ice <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Bassis, J. N.</p> <p>2008-01-01</p> <p>The great ice <span class="hlt">sheets</span> in Antarctica and Greenland are vast deposits of frozen freshwater that contain enough to raise sea level by approximately 70 m if they were to completely melt. Because of the potentially catastrophic impact that ice <span class="hlt">sheets</span> can have, it is important that we understand how ice <span class="hlt">sheets</span> have responded to past climate changes and…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19970024843','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19970024843"><span>Stability of Thin Liquid <span class="hlt">Sheet</span> Flows</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>McConley, Marc W.; Chubb, Donald L.; McMaster, Matthew S.; Afjeh, Abdollah A.</p> <p>1997-01-01</p> <p>A two-dimensional, linear stability analysis of a thin nonplanar liquid <span class="hlt">sheet</span> flow in vacuum is carried out. A <span class="hlt">sheet</span> flow created by a narrow slit of W and tau attains a nonplanar cross section as a consequence of cylinders forming on the <span class="hlt">sheet</span> edge under the influence of surface tension forces. The region where these edge cylinders join the <span class="hlt">sheet</span> is one of high curvature, and this is found to be the location where instability is most likely to occur. The <span class="hlt">sheet</span> flow is found to be unstable, but with low growth rates for symmetric wave disturbances and high growth rates for antisymmetric disturbances. By combining the symmetric and antisymmetric disturbance modes, a wide range of stability characteristics is obtained. The product of unstable growth rate and flow time is proportional to the width-to-thickness ratio of the sift generating the <span class="hlt">sheet</span> Three-dimensional effects can alter these results, particularly when the <span class="hlt">sheet</span> length-to-width ratio is not much greater than unity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003AGUFMED21B1217B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003AGUFMED21B1217B"><span>Web-based Tools for Educators: Outreach <span class="hlt">Activities</span> of the Polar Radar for Ice <span class="hlt">Sheet</span> Measurements (PRISM) Project</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Braaten, D. A.; Holvoet, J. F.; Gogineni, S.</p> <p>2003-12-01</p> <p>The Radar Systems and Remote Sensing Laboratory at the University of Kansas (KU) has implemented extensive outreach <span class="hlt">activities</span> focusing on Polar Regions as part of the Polar Radar for Ice <span class="hlt">Sheet</span> Measurements (PRISM) project. The PRISM project is developing advanced intelligent remote sensing technology that involves radar systems, an autonomous rover, and communications systems to measure detailed ice <span class="hlt">sheet</span> characteristics, and to determine bed conditions (frozen or wet) below <span class="hlt">active</span> ice <span class="hlt">sheets</span> in both Greenland and Antarctica. These measurements will provide a better understanding of the response of polar ice <span class="hlt">sheets</span> to global climate change and the resulting impact the ice <span class="hlt">sheets</span> will have on sea level rise. Many of the research and technological development aspects of the PRISM project, such as robotics, radar systems, climate change and exploration of harsh environments, can kindle an excitement and interest in students about science and technology. These topics form the core of our K-12 education and training outreach initiatives, which are designed to capture the imagination of young students, and prompt them to consider an educational path that will lead them to scientific or engineering careers. The K-12 PRISM outreach initiatives are being developed and implemented in a collaboration with the Advanced Learning Technology Program (ALTec) of the High Plains Regional Technology in Education Consortium (HPR*TEC). ALTec is associated with the KU School of Education, and is a well-established educational research center that develops and hosts web tools to enable teachers nationwide to network, collaborate, and share resources with other teachers. An example of an innovative and successful web interface developed by ALTec is called TrackStar. Teachers can use TrackStar over the Web to develop interactive, resource-based lessons (called tracks) on-line for their students. Once developed, tracks are added to the TrackStar database and can be accessed and modified</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900050982&hterms=silicone+sheet&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dsilicone%2Bsheet','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900050982&hterms=silicone+sheet&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dsilicone%2Bsheet"><span>Scaling results for the liquid <span class="hlt">sheet</span> radiator</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chubb, Donald L.; Calfo, Frederick D.</p> <p>1989-01-01</p> <p>Surface tension forces at the edges of a thin liquid (approx 100 micrometers) <span class="hlt">sheet</span> flow result in a triangularly shaped <span class="hlt">sheet</span>. Such a geometry is ideal for an external flow radiator. The experimental investigation of such <span class="hlt">sheet</span> flows was extended to large <span class="hlt">sheets</span> (width = 23.5 cm, length = 3.5 m). Experimental L/W results are greater than the calculated results. However, more experimental results are necessary for a complete comparison. The calculated emissivity of a <span class="hlt">sheet</span> of Dow-Corning 705 silicone oil, which is low temperature (300-400 K) candidate for a liquid <span class="hlt">sheet</span> radiator (LSR), is greater than 0.8 for <span class="hlt">sheet</span> thicknesses greater than 100 micrometers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21469697','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21469697"><span>Factors controlling the size of graphene oxide <span class="hlt">sheets</span> produced via the graphite oxide route.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pan, Shuyang; Aksay, Ilhan A</p> <p>2011-05-24</p> <p>We have studied the effect of the oxidation path and the mechanical energy input on the size of graphene oxide <span class="hlt">sheets</span> derived from graphite oxide. The cross-planar oxidation of graphite from the (0002) plane results in periodic cracking of the uppermost graphene oxide layer, limiting its lateral dimension to less than 30 μm. We use an energy balance between the elastic strain energy associated with the undulation of graphene oxide <span class="hlt">sheets</span> at the hydroxyl and epoxy sites, the crack formation energy, and the interaction energy between graphene layers to determine the cell size of the cracks. As the effective crack propagation rate in the cross-planar <span class="hlt">direction</span> is an order of magnitude smaller than the edge-to-center oxidation rate, graphene oxide single <span class="hlt">sheets</span> larger than those defined by the periodic cracking cell size are produced depending on the aspect ratio of the graphite particles. We also demonstrate that external energy input from hydrodynamic drag created by fluid motion or sonication, further reduces the size of the graphene oxide <span class="hlt">sheets</span> through tensile stress buildup in the <span class="hlt">sheets</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1993JCli....6.1253B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1993JCli....6.1253B"><span>Modeled Variations of Precipitation over the Greenland Ice <span class="hlt">Sheet</span>.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bromwich, David H.; Robasky, Frank M.; Keen, Richard A.; Bolzan, John F.</p> <p>1993-07-01</p> <p>A parameterization of the synoptic <span class="hlt">activity</span> at 500 hPa and a simple orographic scheme are used to model the spatial and temporal variations of precipitation over the Greenland Ice <span class="hlt">Sheet</span> for 1963-88 from analyzed geopotential height fields produced by the National Meteorological Center (NMC). Model coefficients are fitted to observed accumulation data, primarily from the summit area of the ice <span class="hlt">sheet</span>. All major spatial characteristics of the observed accumulation distribution are reproduced apart from the orographic accumulation maximum over the northwestern coastal slopes. The modeled time-averaged total precipitation amount over Greenland is within the range of values determined by other investigators from surface-based observations. A realistic degree of interannual variability in precipitation is also simulated.A downward trend in simulated ice <span class="hlt">sheet</span> precipitation over the 26 years is found. This is supported by a number of lines of evidence. It matches the accumulation trends during this period from ice cores drilled in south-central Greenland. The lower tropospheric specific humidifies at two south coastal radiosonde stations also decrease over this interval. A systematic shift away from Greenland and a decrease in <span class="hlt">activity</span> of the dominant storm track are found for relatively low precipitation periods as compared to relatively high precipitation periods. This negative precipitation trend would mean that the Greenland Ice <span class="hlt">Sheet</span>, depending on its 1963 mass balance state, has over the 1963-88 period either decreased its negative, or increased its positive, contribution to recently observed global sea level rise.Superimposed on the declining simulated precipitation rate for the entire ice <span class="hlt">sheet</span> is a pronounced 3-5-yr periodicity. This is prominent in the observed and modeled precipitation time series from Summit, Greenland. This cycle shows some aspects in common with the Southern Oscillation.Some deficiencies in the NMC analysts were highlighted by this work. A</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20504035','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20504035"><span>Orientation determination of interfacial beta-<span class="hlt">sheet</span> structures in situ.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Nguyen, Khoi Tan; King, John Thomas; Chen, Zhan</p> <p>2010-07-01</p> <p>Structural information such as orientations of interfacial proteins and peptides is important for understanding properties and functions of such biological molecules, which play crucial roles in biological applications and processes such as antimicrobial selectivity, membrane protein <span class="hlt">activity</span>, biocompatibility, and biosensing performance. The alpha-helical and beta-<span class="hlt">sheet</span> structures are the most widely encountered secondary structures in peptides and proteins. In this paper, for the first time, a method to quantify the orientation of the interfacial beta-<span class="hlt">sheet</span> structure using a combined attenuated total reflectance Fourier transformation infrared spectroscopic (ATR-FTIR) and sum frequency generation (SFG) vibrational spectroscopic study was developed. As an illustration of the methodology, the orientation of tachyplesin I, a 17 amino acid peptide with an antiparallel beta-<span class="hlt">sheet</span>, adsorbed to polymer surfaces as well as associated with a lipid bilayer was determined using the regular and chiral SFG spectra, together with polarized ATR-FTIR amide I signals. Both the tilt angle (theta) and the twist angle (psi) of the beta-<span class="hlt">sheet</span> at interfaces are determined. The developed method in this paper can be used to obtain in situ structural information of beta-<span class="hlt">sheet</span> components in complex molecules. The combination of this method and the existing methodology that is currently used to investigate alpha-helical structures will greatly broaden the application of optical spectroscopy in physical chemistry, biochemistry, biophysics, and structural biology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20080048203','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080048203"><span>Flexible Structural-Health-Monitoring <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Qing, Xinlin; Kuo, Fuo</p> <p>2008-01-01</p> <p>A generic design for a type of flexible structural-health-monitoring <span class="hlt">sheet</span> with multiple sensor/actuator types and a method of manufacturing such <span class="hlt">sheets</span> has been developed. A <span class="hlt">sheet</span> of this type contains an array of sensing and/or actuation elements, associated wires, and any other associated circuit elements incorporated into various flexible layers on a thin, flexible substrate. The <span class="hlt">sheet</span> can be affixed to a structure so that the array of sensing and/or actuation elements can be used to analyze the structure in accordance with structural-health-monitoring techniques. Alternatively, the <span class="hlt">sheet</span> can be designed to be incorporated into the body of the structure, especially if the structure is made of a composite material. Customarily, structural-health monitoring is accomplished by use of sensors and actuators arrayed at various locations on a structure. In contrast, a <span class="hlt">sheet</span> of the present type can contain an entire sensor/actuator array, making it unnecessary to install each sensor and actuator individually on or in a structure. Sensors of different types such as piezoelectric and fiber-optic can be embedded in the <span class="hlt">sheet</span> to form a hybrid sensor network. Similarly, the traces for electric communication can be deposited on one or two layers as required, and an entirely separate layer can be employed to shield the sensor elements and traces.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRA..12211389L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRA..12211389L"><span>Electron Cooling and Isotropization during Magnetotail Current <span class="hlt">Sheet</span> Thinning: Implications for Parallel Electric Fields</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lu, San; Artemyev, A. V.; Angelopoulos, V.</p> <p>2017-11-01</p> <p>Magnetotail current <span class="hlt">sheet</span> thinning is a distinctive feature of substorm growth phase, during which magnetic energy is stored in the magnetospheric lobes. Investigation of charged particle dynamics in such thinning current <span class="hlt">sheets</span> is believed to be important for understanding the substorm energy storage and the current <span class="hlt">sheet</span> destabilization responsible for substorm expansion phase onset. We use Time History of Events and Macroscale Interactions during Substorms (THEMIS) B and C observations in 2008 and 2009 at 18 - 25 RE to show that during magnetotail current <span class="hlt">sheet</span> thinning, the electron temperature decreases (cooling), and the parallel temperature decreases faster than the perpendicular temperature, leading to a decrease of the initially strong electron temperature anisotropy (isotropization). This isotropization cannot be explained by pure adiabatic cooling or by pitch angle scattering. We use test particle simulations to explore the mechanism responsible for the cooling and isotropization. We find that during the thinning, a fast decrease of a parallel electric field (<span class="hlt">directed</span> toward the Earth) can speed up the electron parallel cooling, causing it to exceed the rate of perpendicular cooling, and thus lead to isotropization, consistent with observation. If the parallel electric field is too small or does not change fast enough, the electron parallel cooling is slower than the perpendicular cooling, so the parallel electron anisotropy grows, contrary to observation. The same isotropization can also be accomplished by an increasing parallel electric field <span class="hlt">directed</span> toward the equatorial plane. Our study reveals the existence of a large-scale parallel electric field, which plays an important role in magnetotail particle dynamics during the current <span class="hlt">sheet</span> thinning process.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/11689941','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/11689941"><span>Thinning of the ice <span class="hlt">sheet</span> in northwest Greenland over the past forty years.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Paterson, W S; Reeh, N</p> <p>2001-11-01</p> <p>Thermal expansion of the oceans, as well as melting of glaciers, ice <span class="hlt">sheets</span> and ice caps have been the main contributors to global sea level rise over the past century. The greatest uncertainty in predicting future sea level changes lies with our estimates of the mass balance of the ice <span class="hlt">sheets</span> in Greenland and Antarctica. Satellite measurements have been used to determine changes in these ice <span class="hlt">sheets</span> on short timescales, demonstrating that surface-elevation changes on timescales of decades or less result mainly from variations in snow accumulation. Here we present <span class="hlt">direct</span> measurements of the changes in surface elevation between 1954 and 1995 on a traverse across the north Greenland ice <span class="hlt">sheet</span>. Measurements over a time interval of this length should reflect changes in ice flow-the important quantity for predicting changes in sea level-relatively unperturbed by short-term fluctuations in snow accumulation. We find only small changes in the eastern part of the transect, except for some thickening of the north ice stream. On the west side, however, the thinning rates of the ice <span class="hlt">sheet</span> are significantly higher and thinning extends to higher elevations than had been anticipated from previous studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.C41B0663K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.C41B0663K"><span>Using paleoclimate data to improve models of the Antarctic Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>King, M. A.; Phipps, S. J.; Roberts, J. L.; White, D.</p> <p>2016-12-01</p> <p>Ice <span class="hlt">sheet</span> models are the most descriptive tools available to simulate the future evolution of the Antarctic Ice <span class="hlt">Sheet</span> (AIS), including its contribution towards changes in global sea level. However, our knowledge of the dynamics of the coupled ice-ocean-lithosphere system is inevitably limited, in part due to a lack of observations. Furthemore, to build computationally efficient models that can be run for multiple millennia, it is necessary to use simplified descriptions of ice dynamics. Ice <span class="hlt">sheet</span> modeling is therefore an inherently uncertain exercise. The past evolution of the AIS provides an opportunity to constrain the description of physical processes within ice <span class="hlt">sheet</span> models and, therefore, to constrain our understanding of the role of the AIS in driving changes in global sea level. We use the Parallel Ice <span class="hlt">Sheet</span> Model (PISM) to demonstrate how paleoclimate data can improve our ability to predict the future evolution of the AIS. A large, perturbed-physics ensemble is generated, spanning uncertainty in the parameterizations of four key physical processes within ice <span class="hlt">sheet</span> models: ice rheology, ice shelf calving, and the stress balances within ice <span class="hlt">sheets</span> and ice shelves. A Latin hypercube approach is used to optimally sample the range of uncertainty in parameter values. This perturbed-physics ensemble is used to simulate the evolution of the AIS from the Last Glacial Maximum ( 21,000 years ago) to present. Paleoclimate records are then used to determine which ensemble members are the most realistic. This allows us to use data on past climates to <span class="hlt">directly</span> constrain our understanding of the past contribution of the AIS towards changes in global sea level. Critically, it also allows us to determine which ensemble members are likely to generate the most realistic projections of the future evolution of the AIS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19850023782','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19850023782"><span>A panel method study of vortex <span class="hlt">sheets</span> with special emphasis on <span class="hlt">sheets</span> of axisymmetric geometry. M.S. Thesis</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Sugioka, I.; Widnall, S. E.</p> <p>1985-01-01</p> <p>The self induced evolution of a vortex <span class="hlt">sheet</span> was simulated by modeling the <span class="hlt">sheet</span> using an integration of discrete elements of vorticity. Replacing small sections of a vortex <span class="hlt">sheet</span> by flat panels of constant vorticity is found to reproduce more accurately the initial conditions for the Lagrangian simulation technique than replacement by point vortices. The flat panel method for the vortex <span class="hlt">sheet</span> was then extended to model axisymmetric vortex <span class="hlt">sheets</span>. The local and far field velocities induced by the axisymmetric panels were obtained using matched asymptotic analysis, and some of the uncertainties involved in other models of the axisymmetric vortex <span class="hlt">sheet</span> have been eliminated. One important result of this analysis is the determination of the proper choice of core size for a circular vortex filament which may replace a section of an axisymmetric vortex <span class="hlt">sheet</span>. Roll-up of both two dimensional and axisymmetric vortex <span class="hlt">sheets</span> was computed using the panel methods developed in the report.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PhRvL.120p4501M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PhRvL.120p4501M"><span>Dynamics of Radially Expanding Liquid <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Majumdar, Nayanika; Tirumkudulu, Mahesh S.</p> <p>2018-04-01</p> <p>The process of atomization often involves ejecting thin liquid <span class="hlt">sheets</span> at high speeds from a nozzle that causes the <span class="hlt">sheet</span> to flap violently and break up into fine droplets. The flapping of the liquid <span class="hlt">sheet</span> has long been attributed to the <span class="hlt">sheet</span>'s interaction with the surrounding gas phase. Here, we present experimental evidence to the contrary and show that the flapping is caused by the thinning of the liquid <span class="hlt">sheet</span> as it spreads out from the nozzle exit. The measured growth rates of the waves agree remarkably well with the predictions of a recent theory that accounts for the <span class="hlt">sheet</span>'s thinning but ignores aerodynamic interactions. We anticipate these results to not only lead to more accurate predictions of the final drop-size distribution but also enable more efficient designs of atomizers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012ApSS..258.5405G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012ApSS..258.5405G"><span>Ultraviolet photodetectors based on ZnO <span class="hlt">sheets</span>: The effect of <span class="hlt">sheet</span> size on photoresponse properties</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ghasempour Ardakani, Abbas; Pazoki, Meysam; Mahdavi, Seyed Mohammad; Bahrampour, Ali Reza; Taghavinia, Nima</p> <p>2012-05-01</p> <p>In this work, ultraviolet photodetectors based on electrodeposited ZnO <span class="hlt">sheet</span> thin films were fabricated on a glass substrate. Before electrodeposition, a thin buffer layer of ZnO was deposited on the glass by pulsed laser deposition method. This layer not only acted as a nucleation site for ZnO <span class="hlt">sheet</span> growth, but also made it possible to use cheap glass substrate instead of conventional fluorine-doped tin oxide (FTO) substrate. Our results showed that photoresponse properties of the photodetectors strongly depend on the <span class="hlt">sheet</span> sizes. The smaller <span class="hlt">sheets</span> exhibited enhanced photosensitivity, shortened fall times and decreased gain compared to larger ones. We showed that photodetectors based on ZnO <span class="hlt">sheets</span> have a faster response than ones based on polycrystalline films. It was also shown that even less response time could be obtained by using comb-like electrodes instead of two-electrode.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016erl3.book.1085R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016erl3.book.1085R"><span>Cause and Prevention of Explosions Involving DC Casting of Aluminum <span class="hlt">Sheet</span> Ingot</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Richter, Ray T.; Ekenes, J. Martin</p> <p></p> <p>The casting of aluminum alloy <span class="hlt">sheet</span> ingot and T-bar presents the potential for some of the most volatile situations that can occur in DC (<span class="hlt">direct</span> chill) and EMC (Electromagnetic) casting processes. Aluminum Association explosion incident data from over 300 explosions spanning a twenty-year period were reviewed and analyzed looking for common factors and repetitive reasons for explosions. Analysis of explosions occurring during the three stages of <span class="hlt">sheet</span> ingot casting, `start of cast', `steady state' and `end of cast', were examined and prioritized. Case studies illustrate the need for understanding both technical and non-technical factors contributing to explosions involving molten metal. This paper identifies the major causes of explosions involving DC casting of aluminum alloy <span class="hlt">sheet</span> ingot and makes recommendations for how to prevent the recurrence of such events and minimize the risk of injury.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3725507','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3725507"><span>Surface Structure Dependent Electrocatalytic <span class="hlt">Activity</span> of Co3O4 Anchored on Graphene <span class="hlt">Sheets</span> toward Oxygen Reduction Reaction</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Xiao, Junwu; Kuang, Qin; Yang, Shihe; Xiao, Fei; Wang, Shuai; Guo, Lin</p> <p>2013-01-01</p> <p>Catalytic <span class="hlt">activity</span> is primarily a surface phenomenon, however, little is known about Co3O4 nanocrystals in terms of the relationship between the oxygen reduction reaction (ORR) catalytic <span class="hlt">activity</span> and surface structure, especially when dispersed on a highly conducting support to improve the electrical conductivity and so to enhance the catalytic <span class="hlt">activity</span>. Herein, we report a controllable synthesis of Co3O4 nanorods (NR), nanocubes (NC) and nano-octahedrons (OC) with the different exposed nanocrystalline surfaces ({110}, {100}, and {111}), uniformly anchored on graphene <span class="hlt">sheets</span>, which has allowed us to investigate the effects of the surface structure on the ORR <span class="hlt">activity</span>. Results show that the catalytically <span class="hlt">active</span> sites for ORR should be the surface Co2+ ions, whereas the surface Co3+ ions catalyze CO oxidation, and the catalytic ability is closely related to the density of the catalytically <span class="hlt">active</span> sites. These results underscore the importance of morphological control in the design of highly efficient ORR catalysts. PMID:23892418</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20000057300','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20000057300"><span>Glacio-Seismotectonics: Ice <span class="hlt">Sheets</span>, Crustal Deformation and Seismicity</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Sauber, Jeanne; Stewart, Iain S.; Rose, James</p> <p>2000-01-01</p> <p>The last decade has witnessed a significant growth in our understanding of the past and continuing effects of ice <span class="hlt">sheets</span> and glaciers on contemporary crustal deformation and seismicity. This growth has been driven largely by the emergence of postglacial rebound models (PGM) constrained by new field observations that incorporate increasingly realistic rheological, mechanical, and glacial parameters. In this paper, we highlight some of these recent field-based investigations and new PGMs, and examine their implications for understanding crustal deformation and seismicity during glaciation and following deglaciation. The emerging glacial rebound models outlined in the paper support the view that both tectonic stresses and glacial rebound stresses are needed to explain the distribution and style of contemporary earthquake <span class="hlt">activity</span> in former glaciated shields of eastern Canada and Fennoscandia. However, many of these models neglect important parameters, such as topography, lateral variations in lithospheric strength and tectonic strain built up during glaciation. In glaciated mountainous terrains, glacial erosion may <span class="hlt">directly</span> modulate tectonic deformation by resetting the orogenic topography and thereby providing an additional compensatory uplift mechanism. Such effects are likely to be important both in tectonically <span class="hlt">active</span> orogens and in the mountainous regions of glaciated shields.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatCo...712697L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatCo...712697L"><span>Metallic tin quantum <span class="hlt">sheets</span> confined in graphene toward high-efficiency carbon dioxide electroreduction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lei, Fengcai; Liu, Wei; Sun, Yongfu; Xu, Jiaqi; Liu, Katong; Liang, Liang; Yao, Tao; Pan, Bicai; Wei, Shiqiang; Xie, Yi</p> <p>2016-09-01</p> <p>Ultrathin metal layers can be highly <span class="hlt">active</span> carbon dioxide electroreduction catalysts, but may also be prone to oxidation. Here we construct a model of graphene confined ultrathin layers of highly reactive metals, taking the synthetic highly reactive tin quantum <span class="hlt">sheets</span> confined in graphene as an example. The higher electrochemical <span class="hlt">active</span> area ensures 9 times larger carbon dioxide adsorption capacity relative to bulk tin, while the highly-conductive graphene favours rate-determining electron transfer from carbon dioxide to its radical anion. The lowered tin-tin coordination numbers, revealed by X-ray absorption fine structure spectroscopy, enable tin quantum <span class="hlt">sheets</span> confined in graphene to efficiently stabilize the carbon dioxide radical anion, verified by 0.13 volts lowered potential of hydroxyl ion adsorption compared with bulk tin. Hence, the tin quantum <span class="hlt">sheets</span> confined in graphene show enhanced electrocatalytic <span class="hlt">activity</span> and stability. This work may provide a promising lead for designing efficient and robust catalysts for electrolytic fuel synthesis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-GSFC_20171208_Archive_e000258.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-GSFC_20171208_Archive_e000258.html"><span>NASA: First Map Of Thawed Areas Under Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2017-12-08</p> <p>NASA researchers have helped produce the first map showing what parts of the bottom of the massive Greenland Ice <span class="hlt">Sheet</span> are thawed – key information in better predicting how the ice <span class="hlt">sheet</span> will react to a warming climate. Greenland’s thick ice <span class="hlt">sheet</span> insulates the bedrock below from the cold temperatures at the surface, so the bottom of the ice is often tens of degrees warmer than at the top, because the ice bottom is slowly warmed by heat coming from the Earth’s depths. Knowing whether Greenland’s ice lies on wet, slippery ground or is anchored to dry, frozen bedrock is essential for predicting how this ice will flow in the future, But scientists have very few <span class="hlt">direct</span> observations of the thermal conditions beneath the ice <span class="hlt">sheet</span>, obtained through fewer than two dozen boreholes that have reached the bottom. Now, a new study synthesizes several methods to infer the Greenland Ice Sheet’s basal thermal state –whether the bottom of the ice is melted or not– leading to the first map that identifies frozen and thawed areas across the whole ice <span class="hlt">sheet</span>. Map caption: This first-of-a-kind map, showing which parts of the bottom of the Greenland Ice <span class="hlt">Sheet</span> are likely thawed (red), frozen (blue) or still uncertain (gray), will help scientists better predict how the ice will flow in a warming climate. Credit: NASA Earth Observatory/Jesse Allen Read more: go.nasa.gov/2avKgl2 NASA image use policy. NASA Goddard Space Flight Center enables NASA’s mission through four scientific endeavors: Earth Science, Heliophysics, Solar System Exploration, and Astrophysics. Goddard plays a leading role in NASA’s accomplishments by contributing compelling scientific knowledge to advance the Agency’s mission. Follow us on Twitter Like us on Facebook Find us on Instagram</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_15 --> <div id="page_16" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="301"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.C31C..05G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.C31C..05G"><span>Results of the Greenland Ice <span class="hlt">Sheet</span> Model Initialisation Experiments ISMIP6 - initMIP-Greenland</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Goelzer, H.; Nowicki, S.; Edwards, T.; Beckley, M.; Abe-Ouchi, A.; Aschwanden, A.; Calov, R.; Gagliardini, O.; Gillet-chaulet, F.; Golledge, N. R.; Gregory, J. M.; Greve, R.; Humbert, A.; Huybrechts, P.; Larour, E. Y.; Lipscomb, W. H.; Le ´h, S.; Lee, V.; Kennedy, J. H.; Pattyn, F.; Payne, A. J.; Rodehacke, C. B.; Rückamp, M.; Saito, F.; Schlegel, N.; Seroussi, H. L.; Shepherd, A.; Sun, S.; Vandewal, R.; Ziemen, F. A.</p> <p>2016-12-01</p> <p>Earlier large-scale Greenland ice <span class="hlt">sheet</span> sea-level projections e.g. those run during ice2sea and SeaRISE initiatives have shown that ice <span class="hlt">sheet</span> initialisation can have a large effect on the projections and gives rise to important uncertainties. The goal of this intercomparison exercise (initMIP-Greenland) is to compare, evaluate and improve the initialization techniques used in the ice <span class="hlt">sheet</span> modeling community and to estimate the associated uncertainties. It is the first in a series of ice <span class="hlt">sheet</span> model intercomparison <span class="hlt">activities</span> within ISMIP6 (Ice <span class="hlt">Sheet</span> Model Intercomparison Project for CMIP6). Two experiments for the large-scale Greenland ice <span class="hlt">sheet</span> have been designed to allow intercomparison between participating models of 1) the initial present-day state of the ice <span class="hlt">sheet</span> and 2) the response in two schematic forward experiments. The forward experiments serve to evaluate the initialisation in terms of model drift (forward run without any forcing) and response to a large perturbation (prescribed surface mass balance anomaly). We present and discuss final results of the intercomparison and highlight important uncertainties with respect to projections of the Greenland ice <span class="hlt">sheet</span> sea-level contribution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20040129600','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20040129600"><span>Computer-Aided Light <span class="hlt">Sheet</span> Flow Visualization</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stacy, Kathryn; Severance, Kurt; Childers, Brooks A.</p> <p>1993-01-01</p> <p>A computer-aided flow visualization process has been developed to analyze video images acquired from rotating and translating light <span class="hlt">sheet</span> visualization systems. The computer process integrates a mathematical model for image reconstruction, advanced computer graphics concepts, and digital image processing to provide a quantitative and visual analysis capability. The image reconstruction model, based on photogrammetry, uses knowledge of the camera and light <span class="hlt">sheet</span> locations and orientations to project two-dimensional light <span class="hlt">sheet</span> video images into three-dimensional space. A sophisticated computer visualization package, commonly used to analyze computational fluid dynamics (CFD) data sets, was chosen to interactively display the reconstructed light <span class="hlt">sheet</span> images, along with the numerical surface geometry for the model or aircraft under study. A description is provided of the photogrammetric reconstruction technique, and the image processing and computer graphics techniques and equipment. Results of the computer aided process applied to both a wind tunnel translating light <span class="hlt">sheet</span> experiment and an in-flight rotating light <span class="hlt">sheet</span> experiment are presented. The capability to compare reconstructed experimental light <span class="hlt">sheet</span> images and CFD solutions in the same graphics environment is also demonstrated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19850042373&hterms=glacier+melt&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dglacier%2Bmelt','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19850042373&hterms=glacier+melt&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dglacier%2Bmelt"><span>Ice <span class="hlt">sheet</span> margins and ice shelves</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Thomas, R. H.</p> <p>1984-01-01</p> <p>The effect of climate warming on the size of ice <span class="hlt">sheet</span> margins in polar regions is considered. Particular attention is given to the possibility of a rapid response to warming on the order of tens to hundreds of years. It is found that the early response of the polar regions to climate warming would be an increase in the area of summer melt on the ice <span class="hlt">sheets</span> and ice shelves. For sufficiently large warming (5-10C) the delayed effects would include the breakup of the ice shelves by an increase in ice drainage rates, particularly from the ice <span class="hlt">sheets</span>. On the basis of published data for periodic changes in the thickness and melting rates of the marine ice <span class="hlt">sheets</span> and fjord glaciers in Greenland and Antarctica, it is shown that the rate of retreat (or advance) of an ice <span class="hlt">sheet</span> is primarily determined by: bedrock topography; the basal conditions of the grounded ice <span class="hlt">sheet</span>; and the ice shelf condition downstream of the grounding line. A program of satellite and ground measurements to monitor the state of ice <span class="hlt">sheet</span> equilibrium is recommended.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19930064120&hterms=computer+tomography&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dcomputer%2Btomography','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19930064120&hterms=computer+tomography&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dcomputer%2Btomography"><span>Computer-aided light <span class="hlt">sheet</span> flow visualization</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stacy, Kathryn; Severance, Kurt; Childers, Brooks A.</p> <p>1993-01-01</p> <p>A computer-aided flow visualization process has been developed to analyze video images acquired from rotating and translating light <span class="hlt">sheet</span> visualization systems. The computer process integrates a mathematical model for image reconstruction, advanced computer graphics concepts, and digital image processing to provide a quantitative and visual analysis capability. The image reconstruction model, based on photogrammetry, uses knowledge of the camera and light <span class="hlt">sheet</span> locations and orientations to project two-dimensional light <span class="hlt">sheet</span> video images into three-dimensional space. A sophisticated computer visualization package, commonly used to analyze computational fluid dynamics (CFD) data sets, was chosen to interactively display the reconstructed light <span class="hlt">sheet</span> images, along with the numerical surface geometry for the model or aircraft under study. A description is provided of the photogrammetric reconstruction technique, and the image processing and computer graphics techniques and equipment. Results of the computer aided process applied to both a wind tunnel translating light <span class="hlt">sheet</span> experiment and an in-flight rotating light <span class="hlt">sheet</span> experiment are presented. The capability to compare reconstructed experimental light <span class="hlt">sheet</span> images and CFD solutions in the same graphics environment is also demonstrated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.4409G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.4409G"><span>Results of the Greenland ice <span class="hlt">sheet</span> model initialisation experiments: ISMIP6 - initMIP-Greenland</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Goelzer, Heiko; Nowicki, Sophie; Edwards, Tamsin; Beckley, Matthew</p> <p>2017-04-01</p> <p>Ice <span class="hlt">sheet</span> model initialisation has a large effect on projected future sea-level contributions and gives rise to important uncertainties. The goal of this intercomparison exercise for the continental-scale Greenland ice <span class="hlt">sheet</span> is therefore to compare, evaluate and improve the initialisation techniques used in the ice <span class="hlt">sheet</span> modelling community. The initMIP-Greenland project is the first in a series of ice <span class="hlt">sheet</span> model intercomparison <span class="hlt">activities</span> within ISMIP6 (Ice <span class="hlt">Sheet</span> Model Intercomparison Project for CMIP6). The experimental set-up has been designed to allow comparison of the initial present-day state of the Greenland ice <span class="hlt">sheet</span> between participating models and against observations. Furthermore, the initial states are tested with two schematic forward experiments to evaluate the initialisation in terms of model drift (forward run without any forcing) and response to a large perturbation (prescribed surface mass balance anomaly). We present and discuss results that highlight the wide diversity of data sets, boundary conditions and initialisation techniques used in the community to generate initial states of the Greenland ice <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JAP...120j4901M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JAP...120j4901M"><span>Airy acoustical-<span class="hlt">sheet</span> spinner tweezers</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mitri, F. G.</p> <p>2016-09-01</p> <p>The Airy acoustical beam exhibits parabolic propagation and spatial acceleration, meaning that the propagation bending angle continuously increases before the beam trajectory reaches a critical angle where it decays after a propagation distance, without applying any external bending force. As such, it is of particular importance to investigate its properties from the standpoint of acoustical radiation force, spin torque, and particle dynamics theories, in the development of novel particle sorting techniques and acoustically mediated clearing systems. This work investigates these effects on a two-dimensional (2D) circular absorptive structure placed in the field of a nonparaxial Airy "acoustical-<span class="hlt">sheet</span>" (i.e., finite beam in 2D), for potential applications in surface acoustic waves and acousto-fluidics. Based on the characteristics of the acoustic field, the beam is capable of manipulating the circular cylindrical fluid cross-section and guides it along a transverse or parabolic trajectory. This feature of Airy acoustical beams could lead to a unique characteristic in single-beam acoustical tweezers related to acoustical sieving, filtering, and removal of particles and cells from a section of a small channel. The analysis developed here is based on the description of the nonparaxial Airy beam using the angular spectrum decomposition of plane waves in close association with the partial-wave series expansion method in cylindrical coordinates. The numerical results demonstrate the ability of the nonparaxial Airy acoustical-<span class="hlt">sheet</span> beam to pull, propel, or accelerate a particle along a parabolic trajectory, in addition to particle confinement in the transverse <span class="hlt">direction</span> of wave propagation. Negative or positive radiation force and spin torque causing rotation in the clockwise or the anticlockwise <span class="hlt">direction</span> can occur depending on the nondimensional parameter ka (where k is the wavenumber and a is the radius) and the location of the cylinder in the beam. Applications in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.C13A0732Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.C13A0732Y"><span>Monitoring Antarctic ice <span class="hlt">sheet</span> surface melting with TIMESAT algorithm</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ye, Y.; Cheng, X.; Li, X.; Liang, L.</p> <p>2011-12-01</p> <p>Antarctic ice <span class="hlt">sheet</span> contributes significantly to the global heat budget by controlling the exchange of heat, moisture, and momentum at the surface-atmosphere interface, which <span class="hlt">directly</span> influence the global atmospheric circulation and climate change. Ice <span class="hlt">sheet</span> melting will cause snow humidity increase, which will accelerate the disintegration and movement of ice <span class="hlt">sheet</span>. As a result, detecting Antarctic ice <span class="hlt">sheet</span> melting is essential for global climate change research. In the past decades, various methods have been proposed for extracting snowmelt information from multi-channel satellite passive microwave data. Some methods are based on brightness temperature values or a composite index of them, and others are based on edge detection. TIMESAT (Time-series of Satellite sensor data) is an algorithm for extracting seasonality information from time-series of satellite sensor data. With TIMESAT long-time series brightness temperature (SSM/I 19H) is simulated by Double Logistic function. Snow is classified to wet and dry snow with generalized Gaussian model. The results were compared with those from a wavelet algorithm. On this basis, Antarctic automatic weather station data were used for ground verification. It shows that this algorithm is effective in ice <span class="hlt">sheet</span> melting detection. The spatial distribution of melting areas(Fig.1) shows that, the majority of melting areas are located on the edge of Antarctic ice shelf region. It is affected by land cover type, surface elevation and geographic location (latitude). In addition, the Antarctic ice <span class="hlt">sheet</span> melting varies with seasons. It is particularly acute in summer, peaking at December and January, staying low in March. In summary, from 1988 to 2008, Ross Ice Shelf and Ronnie Ice Shelf have the greatest interannual variability in amount of melting, which largely determines the overall interannual variability in Antarctica. Other regions, especially Larsen Ice Shelf and Wilkins Ice Shelf, which is in the Antarctic Peninsula</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSM43C2737M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSM43C2737M"><span>Impact of the storm-time plasma <span class="hlt">sheet</span> ion composition on the ring current energy density</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mouikis, C.; Kistler, L. M.; Petrinec, S. M.; Fuselier, S. A.; Cohen, I.</p> <p>2017-12-01</p> <p>The adiabatic inward transport of the night-side near-earth ( 6 Re) hot plasma <span class="hlt">sheet</span> is the dominant contributor to the ring current pressure during storm times. During storm times, the plasma <span class="hlt">sheet</span> composition in the 6 - 12 Re tail region changes due to O+ entry from the lobes (from the cusp) and the <span class="hlt">direct</span> feeding from the night side auroral region. In addition, at substorm onset the plasma <span class="hlt">sheet</span> O+ ions can be preferentially accelerated. We use MMS and observations during two magnetic storms, 5/8/2016 and 7/16/2017, to monitor the composition changes and energization in the 6 - 12 Re plasma <span class="hlt">sheet</span> region. For both storms the MMS apogee was in the tail. In addition, we use subsequent Van Allen Probe observations (with apogee in the dawn and dusk respectively) to test if the 6-12 Re plasma <span class="hlt">sheet</span>, observed by MMS, is a sufficient source of the O+ in the ring current. For this we will compare the phase space density (PSD) of the plasma <span class="hlt">sheet</span> source population and the PSD of the inner magnetosphere at constant magnetic moment values as used in Kistler et al., [2016].</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29094005','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29094005"><span>Bone regeneration with osteogenic matrix cell <span class="hlt">sheet</span> and tricalcium phosphate: An experimental study in sheep.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kira, Tsutomu; Akahane, Manabu; Omokawa, Shohei; Shimizu, Takamasa; Kawate, Kenji; Onishi, Tadanobu; Tanaka, Yasuhito</p> <p>2017-10-18</p> <p>To determine the effects of a cell <span class="hlt">sheet</span> created from sheep bone marrow and tricalcium phosphate (TCP) on osteogenesis. Bone marrow cells were harvested from a sheep and cultured in a minimal essential medium (MEM) containing ascorbic acid phosphate (AscP) and dexamethasone (Dex). After 2 wk, the formed osteogenic matrix cell <span class="hlt">sheet</span> was lifted from the culture dish using a scraper. Additionally, harvested bone marrow cells were cultured in MEM only as a negative control group, and in MEM with AscP, Dex, and β-glycerophosphate as a positive control group. For in vitro evaluation, we measured the alkaline phosphatase (ALP) <span class="hlt">activity</span> and osteocalcin (OC) content in the media of the cultured cells from each group. For in vivo analysis, a porous TCP ceramic was used as a scaffold. We prepared an experimental group comprising TCP scaffolds wrapped with the osteogenic matrix cell <span class="hlt">sheets</span> and a control group consisting of the TCP scaffold only. The constructs were implanted subcutaneously into athymic rats and the cell donor sheep, and bone formation was confirmed by histology after 4 wk. In the in vitro part, the mean ALP <span class="hlt">activity</span> was 0.39 ± 0.03 mg/well in the negative control group, 0.67 ± 0.04 mg/well in the <span class="hlt">sheet</span> group, and 0.65 ± 0.07 mg/well in the positive control group. The mean OC levels were 1.46 ± 0.33 ng/well in the negative control group, 3.92 ± 0.16 ng/well in the <span class="hlt">sheet</span> group, and 4.4 ± 0.47 ng/well in the positive control group, respectively. The ALP <span class="hlt">activity</span> and OC levels were significantly higher in the cell <span class="hlt">sheet</span> and positive control groups than in the negative control group ( P < 0.05). There was no significant difference in ALP <span class="hlt">activity</span> or OC levels between the cell <span class="hlt">sheet</span> group and the positive control group ( P > 0.05). TCP constructs wrapped with cell <span class="hlt">sheets</span> prior to implantation showed bone formation, in contrast to TCP scaffolds alone, which exhibited poor bone formation when implanted, in the subcutaneous layer both in athymic rats and in the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70027092','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70027092"><span>Effects of wave shape on <span class="hlt">sheet</span> flow sediment transport</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hsu, T.-J.; Hanes, D.M.</p> <p>2004-01-01</p> <p>A two-phase model is implemented to study the effects of wave shape on the transport of coarse-grained sediment in the <span class="hlt">sheet</span> flow regime. The model is based on balance equations for the average mass, momentum, and fluctuation energy for both the fluid and sediment phases. Model simulations indicate that the responses of the <span class="hlt">sheet</span> flow, such as the velocity profiles, the instantaneous bed shear stress, the sediment flux, and the total amount of the mobilized sediment, cannot be fully parameterized by quasi-steady free-stream velocity and may be correlated with the magnitude of local horizontal pressure gradient (or free-stream acceleration). A net sediment flux in the <span class="hlt">direction</span> of wave advance is obtained for both skewed and saw-tooth wave shapes typical of shoaled and breaking waves. The model further suggests that at critical values of the horizontal pressure gradient, there is a failure event within the bed that mobilizes more sediment into the mobile <span class="hlt">sheet</span> and enhances the sediment flux. Preliminary attempts to parameterize the total bed shear stress and the total sediment flux appear promising. Copyright 2004 by the American Geophysical Union.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/7252579','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/7252579"><span>Dual circuit embossed <span class="hlt">sheet</span> heat transfer panel</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Morgan, G.D.</p> <p>1984-02-21</p> <p>A heat transfer panel provides redundant cooling for fusion reactors or the like environment requiring low-mass construction. Redundant cooling is provided by two independent cooling circuits, each circuit consisting of a series of channels joined to inlet and outlet headers. The panel comprises a welded joinder of two full-size and two much smaller partial-size <span class="hlt">sheets</span>. The first full-size <span class="hlt">sheet</span> is embossed to form first portions of channels for the first and second circuits, as well as a header for the first circuit. The second full-sized <span class="hlt">sheet</span> is then laid over and welded to the first full-size <span class="hlt">sheet</span>. The first and second partial-size <span class="hlt">sheets</span> are then overlaid on separate portions of the second full-sized <span class="hlt">sheet</span>, and are welded thereto. The first and second partial-sized <span class="hlt">sheets</span> are embossed to form inlet and outlet headers, which communicate with channels of the second circuit through apertures formed in the second full-sized <span class="hlt">sheet</span>. 6 figs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/5955851','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/5955851"><span>Dual-circuit embossed-<span class="hlt">sheet</span> heat-transfer panel</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Morgan, G.D.</p> <p>1982-08-23</p> <p>A heat transfer panel provides redundant cooling for fusion reactors or the like environment requiring low-mass construction. Redundant cooling is provided by two independent cooling circuits, each circuit consisting of a series of channels joined to inlet and outlet headers. The panel comprises a welded joinder of two full-size and two much smaller partial-size <span class="hlt">sheets</span>. The first full-size <span class="hlt">sheet</span> is embossed for form first portions of channels for the first and second circuits, as well as a header for the first circuit. The second full-sized <span class="hlt">sheet</span> is then laid over and welded to the first full-size <span class="hlt">sheet</span>. The first and second partial-size <span class="hlt">sheets</span> are then overlaid on separate portions of the second full-sized <span class="hlt">sheet</span>, and are welded thereto. The first and second partial-sized <span class="hlt">sheets</span> are embossed to form inlet and outlet headers, which communicate with channels of the second circuit through apertures formed in the second full-sized <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/864892','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/864892"><span>Dual circuit embossed <span class="hlt">sheet</span> heat transfer panel</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Morgan, Grover D.</p> <p>1984-01-01</p> <p>A heat transfer panel provides redundant cooling for fusion reactors or the like environment requiring low-mass construction. Redundant cooling is provided by two independent cooling circuits, each circuit consisting of a series of channels joined to inlet and outlet headers. The panel comprises a welded joinder of two full-size and two much smaller partial-size <span class="hlt">sheets</span>. The first full-size <span class="hlt">sheet</span> is embossed to form first portions of channels for the first and second circuits, as well as a header for the first circuit. The second full-sized <span class="hlt">sheet</span> is then laid over and welded to the first full-size <span class="hlt">sheet</span>. The first and second partial-size <span class="hlt">sheets</span> are then overlaid on separate portions of the second full-sized <span class="hlt">sheet</span>, and are welded thereto. The first and second partial-sized <span class="hlt">sheets</span> are embossed to form inlet and outlet headers, which communicate with channels of the second circuit through apertures formed in the second full-sized <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19860020298','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19860020298"><span>Vortex <span class="hlt">sheet</span> modeling with higher order curved panels. Ph.D Thesis Final Technical Report</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Nagati, M. G.</p> <p>1985-01-01</p> <p>A numerical technique is presented for modeling the vortex <span class="hlt">sheet</span> with a deformable surface definition, along which a continuous vortex strength distribution in the spanwise <span class="hlt">direction</span> is applied, so that by repeatedly modifying its shape, its true configuration is approached, in the proximity of its generating wing. Design problems requiring the inclusion of a realistic configuration of the vortex <span class="hlt">sheet</span> are numerous. Examples discussed include: control effectiveness and stability derivatives, longitudinal stability, lateral stability, canards, propellers and helicopter rotors, and trailing vortex hazards.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27828359','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27828359"><span>kW-class <span class="hlt">direct</span> diode laser for <span class="hlt">sheet</span> metal cutting based on DWDM of pump modules by use of ultra-steep dielectric filters.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Witte, U; Schneider, F; Traub, M; Hoffmann, D; Drovs, S; Brand, T; Unger, A</p> <p>2016-10-03</p> <p>A <span class="hlt">direct</span> diode laser was built with > 800 W output power at 940 nm to 980 nm. The radiation is coupled into a 100 µm fiber and the NA ex fiber is 0.17. The laser system is based on pump modules that are wavelength stabilized by VBGs. Dense and coarse wavelength multiplexing are realized with commercially available ultra-steep dielectric filters. The electro-optical efficiency is above 30%. Based on a detailed analysis of losses, an improved e-o-efficiency in the range of 40% to 45% is expected in the near future. System performance and reliability were demonstrated with <span class="hlt">sheet</span> metal cutting tests on stainless steel with a thickness of 4.2 mm.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMED12A..06H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMED12A..06H"><span>Improving Climate Literacy Using The Ice <span class="hlt">Sheet</span> System Model (ISSM): A Prototype Virtual Ice <span class="hlt">Sheet</span> Laboratory For Use In K-12 Classrooms</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Halkides, D. J.; Larour, E. Y.; Perez, G.; Petrie, K.; Nguyen, L.</p> <p>2013-12-01</p> <p>Statistics indicate that most Americans learn what they will know about science within the confines of our public K-12 education system and the media. Next Generation Science Standards (NGSS) aim to remedy science illiteracy and provide guidelines to exceed the Common Core State Standards that most U.S. state governments have adopted, by integrating disciplinary cores with crosscutting ideas and real life practices. In this vein, we present a prototype ';Virtual Ice <span class="hlt">Sheet</span> Laboratory' (I-Lab), geared to K-12 students, educators and interested members of the general public. I-Lab will allow users to perform experiments using a state-of-the-art dynamical ice <span class="hlt">sheet</span> model and provide detailed downloadable lesson plans, which incorporate this model and are consistent with NGSS Physical Science criteria for different grade bands (K-2, 3-5, 6-8, and 9-12). The ultimate goal of this website is to improve public climate science literacy, especially in regards to the crucial role of the polar ice <span class="hlt">sheets</span> in Earth's climate and sea level. The model used will be the Ice <span class="hlt">Sheet</span> System Model (ISSM), an ice flow model developed at NASA's Jet Propulsion Laboratory and UC Irvine, that simulates the near-term evolution of polar ice <span class="hlt">sheets</span> (Greenland and Antarctica) and includes high spatial resolution capabilities and data assimilation to produce realistic simulations of ice <span class="hlt">sheet</span> dynamics at the continental scale. Open sourced since 2011, ISSM is used in cutting edge cryosphere research around the globe. Thru I-Lab, students will be able to access ISSM using a simple, online graphical interface that can be launched from a web browser on a computer, tablet or smart phone. The interface will allow users to select different climate conditions and watch how the polar ice <span class="hlt">sheets</span> evolve in time under those conditions. Lesson contents will include links to background material and <span class="hlt">activities</span> that teach observation recording, concept articulation, hypothesis formulation and testing, and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMED31B0283S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMED31B0283S"><span>Interactive Ice <span class="hlt">Sheet</span> Flowline Model for High School and College Students</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stearns, L. A.; Rezvanbehbahani, S.; Shankar, S.</p> <p>2017-12-01</p> <p>Teaching about climate and climate change is conceptually challenging. While teaching tools and lesson plans are rapidly evolving to help teachers and students improve their understanding of climate processes, there are very few tools targeting ice <span class="hlt">sheet</span> and glacier dynamics. We have built an interactive ice <span class="hlt">sheet</span> model that allows students to explore how Antarctic glaciers respond to different climate perturbations. Interactive models offer advantages that are hard to obtain in traditional classroom settings; users can systematically investigate hypothetical situations, explore the effects of modifying systems, and repeatedly observe how systems interrelate. As a result, this project provides a much-needed bridge between the data and models used by the scientific community and students in high school and college. We target our instructional and assessment <span class="hlt">activities</span> to three high school and college students with the overall aim of increasing understanding of ice <span class="hlt">sheet</span> dynamics and the different ways that ice <span class="hlt">sheets</span> are impacted by climate change, while also improving their fundamental math skills.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA21757.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA21757.html"><span>Monitoring Sand <span class="hlt">Sheets</span> and Dunes</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2017-06-12</p> <p>NASA's Mars Reconnaissance Orbiter (MRO) captured this crater featuring sand dunes and sand <span class="hlt">sheets</span> on its floor. What are sand <span class="hlt">sheets</span>? Snow fall on Earth is a good example of sand <span class="hlt">sheets</span>: when it snows, the ground gets blanketed with up to a few meters of snow. The snow mantles the ground and "mimics" the underlying topography. Sand <span class="hlt">sheets</span> likewise mantle the ground as a relatively thin deposit. This kind of environment has been monitored by HiRISE since 2007 to look for movement in the ripples covering the dunes and <span class="hlt">sheets</span>. This is how scientists who study wind-blown sand can track the amount of sand moving through the area and possibly where the sand came from. Using the present environment is crucial to understanding the past: sand dunes, <span class="hlt">sheets</span>, and ripples sometimes become preserved as sandstone and contain clues as to how they were deposited The map is projected here at a scale of 25 centimeters (9.8 inches) per pixel. [The original image scale is 25 centimeters (9.8 inches) per pixel (with 1 x 1 binning); objects on the order of 75 centimeters (29.5 inches) across are resolved.] North is up. https://photojournal.jpl.nasa.gov/catalog/PIA21757</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19910000195&hterms=Artistic&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DArtistic','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19910000195&hterms=Artistic&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DArtistic"><span>Twin-Mirrored-Galvanometer Laser-Light-<span class="hlt">Sheet</span> Generator</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Rhodes, David B.; Franke, John M.; Jones, Stephen B.; Leighty, Bradley D.</p> <p>1991-01-01</p> <p>Multiple, rotating laser-light <span class="hlt">sheets</span> generated to illuminate flows in wind tunnels. Designed and developed to provide flexibility and adaptability to wide range of applications. Design includes capability to control size and location of laser-light <span class="hlt">sheet</span> in real time, to generate horizontal or vertical <span class="hlt">sheets</span>, to sweep <span class="hlt">sheet</span> repeatedly through volume, to generate multiple <span class="hlt">sheets</span> with controllable separation, and to rotate single or multiple laser-light <span class="hlt">sheets</span>. Includes electronic equipment and laser mounted on adjustable-height platform. Twin-mirrored galvanometer unit supported by tripod to reduce vibration. Other possible applications include use in construction industry to align beams of building. Artistic or display applications also possible.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3599259','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3599259"><span>Keratinocyte cytoskeletal roles in cell <span class="hlt">sheet</span> engineering</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2013-01-01</p> <p>Background There is an increasing need to understand cell-cell interactions for cell and tissue engineering purposes, such as optimizing cell <span class="hlt">sheet</span> constructs, as well as for examining adhesion defect diseases. For cell-<span class="hlt">sheet</span> engineering, one major obstacle to <span class="hlt">sheet</span> function is that cell <span class="hlt">sheets</span> in suspension are fragile and, over time, will contract. While the role of the cytoskeleton in maintaining the structure and adhesion of cells cultured on a rigid substrate is well-characterized, a systematic examination of the role played by different components of the cytoskeleton in regulating cell <span class="hlt">sheet</span> contraction and cohesion in the absence of a substrate has been lacking. Results In this study, keratinocytes were cultured until confluent and cell <span class="hlt">sheets</span> were generated using dispase to remove the influence of the substrate. The effects of disrupting actin, microtubules or intermediate filaments on cell-cell interactions were assessed by measuring cell <span class="hlt">sheet</span> cohesion and contraction. Keratin intermediate filament disruption caused comparable effects on cell <span class="hlt">sheet</span> cohesion and contraction, when compared to actin or microtubule disruption. Interfering with actomyosin contraction demonstrated that interfering with cell contraction can also diminish cell cohesion. Conclusions All components of the cytoskeleton are involved in maintaining cell <span class="hlt">sheet</span> cohesion and contraction, although not to the same extent. These findings demonstrate that substrate-free cell <span class="hlt">sheet</span> biomechanical properties are dependent on the integrity of the cytoskeleton network. PMID:23442760</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_16 --> <div id="page_17" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="321"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatSR...626109J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatSR...626109J"><span>Infused polymers for cell <span class="hlt">sheet</span> release</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Juthani, Nidhi; Howell, Caitlin; Ledoux, Haylea; Sotiri, Irini; Kelso, Susan; Kovalenko, Yevgen; Tajik, Amanda; Vu, Thy L.; Lin, Jennifer J.; Sutton, Amy; Aizenberg, Joanna</p> <p>2016-05-01</p> <p>Tissue engineering using whole, intact cell <span class="hlt">sheets</span> has shown promise in many cell-based therapies. However, current systems for the growth and release of these <span class="hlt">sheets</span> can be expensive to purchase or difficult to fabricate, hindering their widespread use. Here, we describe a new approach to cell <span class="hlt">sheet</span> release surfaces based on silicone oil-infused polydimethylsiloxane. By coating the surfaces with a layer of fibronectin (FN), we were able to grow mesenchymal stem cells to densities comparable to those of tissue culture polystyrene controls (TCPS). Simple introduction of oil underneath an edge of the <span class="hlt">sheet</span> caused it to separate from the substrate. Characterization of <span class="hlt">sheets</span> post-transfer showed that they retain their FN layer and morphology, remain highly viable, and are able to grow and proliferate normally after transfer. We expect that this method of cell <span class="hlt">sheet</span> growth and detachment may be useful for low-cost, flexible, and customizable production of cellular layers for tissue engineering.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4870626','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4870626"><span>Infused polymers for cell <span class="hlt">sheet</span> release</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Juthani, Nidhi; Howell, Caitlin; Ledoux, Haylea; Sotiri, Irini; Kelso, Susan; Kovalenko, Yevgen; Tajik, Amanda; Vu, Thy L.; Lin, Jennifer J.; Sutton, Amy; Aizenberg, Joanna</p> <p>2016-01-01</p> <p>Tissue engineering using whole, intact cell <span class="hlt">sheets</span> has shown promise in many cell-based therapies. However, current systems for the growth and release of these <span class="hlt">sheets</span> can be expensive to purchase or difficult to fabricate, hindering their widespread use. Here, we describe a new approach to cell <span class="hlt">sheet</span> release surfaces based on silicone oil-infused polydimethylsiloxane. By coating the surfaces with a layer of fibronectin (FN), we were able to grow mesenchymal stem cells to densities comparable to those of tissue culture polystyrene controls (TCPS). Simple introduction of oil underneath an edge of the <span class="hlt">sheet</span> caused it to separate from the substrate. Characterization of <span class="hlt">sheets</span> post-transfer showed that they retain their FN layer and morphology, remain highly viable, and are able to grow and proliferate normally after transfer. We expect that this method of cell <span class="hlt">sheet</span> growth and detachment may be useful for low-cost, flexible, and customizable production of cellular layers for tissue engineering. PMID:27189419</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27189419','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27189419"><span>Infused polymers for cell <span class="hlt">sheet</span> release.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Juthani, Nidhi; Howell, Caitlin; Ledoux, Haylea; Sotiri, Irini; Kelso, Susan; Kovalenko, Yevgen; Tajik, Amanda; Vu, Thy L; Lin, Jennifer J; Sutton, Amy; Aizenberg, Joanna</p> <p>2016-05-18</p> <p>Tissue engineering using whole, intact cell <span class="hlt">sheets</span> has shown promise in many cell-based therapies. However, current systems for the growth and release of these <span class="hlt">sheets</span> can be expensive to purchase or difficult to fabricate, hindering their widespread use. Here, we describe a new approach to cell <span class="hlt">sheet</span> release surfaces based on silicone oil-infused polydimethylsiloxane. By coating the surfaces with a layer of fibronectin (FN), we were able to grow mesenchymal stem cells to densities comparable to those of tissue culture polystyrene controls (TCPS). Simple introduction of oil underneath an edge of the <span class="hlt">sheet</span> caused it to separate from the substrate. Characterization of <span class="hlt">sheets</span> post-transfer showed that they retain their FN layer and morphology, remain highly viable, and are able to grow and proliferate normally after transfer. We expect that this method of cell <span class="hlt">sheet</span> growth and detachment may be useful for low-cost, flexible, and customizable production of cellular layers for tissue engineering.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.1573J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.1573J"><span>Coupled ice <span class="hlt">sheet</span>-ocean modelling to investigate ocean driven melting of marine ice <span class="hlt">sheets</span> in Antarctica</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jong, Lenneke; Gladstone, Rupert; Galton-Fenzi, Ben</p> <p>2017-04-01</p> <p>Ocean induced melting below the ice shelves of marine ice <span class="hlt">sheets</span> is a major source of uncertainty for predictions of ice mass loss and Antarctica's resultant contribution to future sea level rise. The floating ice shelves provide a buttressing force against the flow of ice across the grounding line into the ocean. Thinning of these ice shelves due to an increase in melting reduces this force and can lead to an increase in the discharge of grounded ice. Fully coupled modelling of ice <span class="hlt">sheet</span>-ocean interactions is key to improving understanding the influence of the Southern ocean on the evolution of the Antarctic ice <span class="hlt">sheet</span>, and to predicting its future behaviour under changing climate conditions. Coupling of ocean and ice <span class="hlt">sheet</span> models is needed to provide more realistic melt rates at the base of ice shelves and hence make better predictions of the behaviour of the grounding line and the shape of the ice-shelf cavity as the ice <span class="hlt">sheet</span> evolves. The Framework for Ice <span class="hlt">Sheet</span> - Ocean Coupling (FISOC) has been developed to provide a flexible platform for performing coupled ice <span class="hlt">sheet</span> - ocean modelling experiments. We present preliminary results using FISOC to couple the Regional Ocean Modelling System (ROMS) with Elmer/Ice in idealised experiments Marine Ice <span class="hlt">Sheet</span>-Ocean Model Intercomparison Project (MISOMIP). These experiments use an idealised geometry motivated by that of Pine Island glacier and the adjacent Amundsen Sea in West Antarctica, a region which has shown shown signs of thinning ice and grounding line retreat.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.C22C..03R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.C22C..03R"><span>Isostasy as a Driver of Paleo Retreat of the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Robinson, A.; Tabone, I.; Alvarez-Solas, J.; Montoya, M.</p> <p>2016-12-01</p> <p>During glacial times, the Greenland ice <span class="hlt">sheet</span> (GrIS) extended onto the continental shelf, and thus was much more <span class="hlt">directly</span> affected by changing ocean temperatures through basal melt of the marine ice margins than it is today. The larger glacial ice <span class="hlt">sheet</span> also induced lithospheric depression of several hundred meters in regions that are near sea level today. As the ice <span class="hlt">sheet</span> retreated inland under interglacial climatic forcing, the regions significantly affected by local isostatic changes in elevation were exposed to much higher basal melt rates than they would have been given the present-day topography. Here we explore this effect using a hybrid ice <span class="hlt">sheet</span> model that represents both grounded and floating ice, as well as local isostatic effects, and is driven by both atmospheric and oceanic temperature anomalies. We find that when transient oceanic forcing is included in the model, isostasy plays an important role in allowing oceanic melting to drive GrIS retreat in some regions. During the last interglacial, for example, this effect can account for a significant additional sea-level contribution, as well as an increase in the rate of sea-level rise. Our results highlight the importance of accounting for ice-ocean-lithosphere interactions in the past, in order to be able to properly reconstruct the evolution of the ice <span class="hlt">sheet</span>, and for estimating its sensitivity to potential changes in climate in the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/871091','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/871091"><span>Method for heating and forming a glass <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Boaz, Premakaran Tucker</p> <p>1997-01-01</p> <p>A method for heating and forming a glass <span class="hlt">sheet</span> includes the steps of heating a glass <span class="hlt">sheet</span> to at least a first predetermined temperature, applying microwave energy to the glass <span class="hlt">sheet</span> to heat the glass <span class="hlt">sheet</span> to at least a second predetermined temperature, cooling an outer surface of the glass <span class="hlt">sheet</span> to at least a third predetermined temperature and forming the glass <span class="hlt">sheet</span> using forming rollers to a predetermined configuration.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003EAEJA....13008H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003EAEJA....13008H"><span>Glaciological constraints on current ice mass changes from modelling the ice <span class="hlt">sheets</span> over the glacial cycles</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Huybrechts, P.</p> <p>2003-04-01</p> <p>The evolution of continental ice <span class="hlt">sheets</span> introduces a long time scale in the climate system. Large ice <span class="hlt">sheets</span> have a memory of millenia, hence the present-day ice <span class="hlt">sheets</span> of Greenland and Antarctica are still adjusting to climatic variations extending back to the last glacial period. This trend is separate from the <span class="hlt">direct</span> response to mass-balance changes on decadal time scales and needs to be correctly accounted for when assessing current and future contributions to sea level. One way to obtain estimates of current ice mass changes is to model the past history of the ice <span class="hlt">sheets</span> and their underlying beds over the glacial cycles. Such calculations assist to distinguish between the longer-term ice-dynamic evolution and short-term mass-balance changes when interpreting altimetry data, and are helpful to isolate the effects of postglacial rebound from gravity and altimetry trends. The presentation will discuss results obtained from 3-D thermomechanical ice-<span class="hlt">sheet</span>/lithosphere/bedrock models applied to the Antarctic and Greenland ice <span class="hlt">sheets</span>. The simulations are forced by time-dependent boundary conditions derived from sediment and ice core records and are constrained by geomorphological and glacial-geological data of past ice <span class="hlt">sheet</span> and sea-level stands. Current simulations suggest that the Greenland ice <span class="hlt">sheet</span> is close to balance, while the Antarctic ice <span class="hlt">sheet</span> is still losing mass, mainly due to incomplete grounding-line retreat of the West Antarctic ice <span class="hlt">sheet</span> since the LGM. The results indicate that altimetry trends are likely dominated by ice thickness changes but that the gravitational signal mainly reflects postglacial rebound.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21431481','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21431481"><span>Use of silicone gel <span class="hlt">sheets</span> for prevention of keloid scars after median sternotomy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sakuraba, Motoki; Takahashi, Nobumasa; Akahoshi, Taku; Miyasaka, Yoshikazu; Suzuki, Kenji</p> <p>2011-04-01</p> <p>A keloid scar often appears at the incision site of patients after median sternotomy. Use of silicone gel to treat hypertrophic burn scars and fresh incisions has yielded encouraging results. In this study, we report our experience with the preventive use of silicone gel <span class="hlt">sheets</span> for keloid scars after median sternotomy. Nine patients who underwent a median sternotomy were studied. A silicone gel <span class="hlt">sheet</span> was kept <span class="hlt">directly</span> on the surgical incision for 24 h starting 2 weeks after surgery. The treatment was repeated with a new <span class="hlt">sheet</span> every 4 weeks for 24 weeks, at which times the subjective symptoms and the changes in keloid scars were determined. None of the patients experienced an aggravation of any subjective symptoms during the 24-week study. After 24 weeks, all patients were free of a keloid scar that showed a rise and contraction of skin and causes discomfort. No adverse events were reported by any of the patients. A silicone gel <span class="hlt">sheet</span> is safe and effective for the preventing the formation of keloid scars after median sternotomy.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016MMTA...47.4425B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016MMTA...47.4425B"><span>Effect of Temperature and <span class="hlt">Sheet</span> Temper on Isothermal Solidification Kinetics in Clad Aluminum Brazing <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Benoit, Michael J.; Whitney, Mark A.; Wells, Mary A.; Winkler, Sooky</p> <p>2016-09-01</p> <p>Isothermal solidification (IS) is a phenomenon observed in clad aluminum brazing <span class="hlt">sheets</span>, wherein the amount of liquid clad metal is reduced by penetration of the liquid clad into the core. The objective of the current investigation is to quantify the rate of IS through the use of a previously derived parameter, the Interface Rate Constant (IRC). The effect of peak temperature and initial <span class="hlt">sheet</span> temper on IS kinetics were investigated. The results demonstrated that IS is due to the diffusion of silicon (Si) from the liquid clad layer into the solid core. Reduced amounts of liquid clad at long liquid duration times, a roughened <span class="hlt">sheet</span> surface, and differences in resolidified clad layer morphology between <span class="hlt">sheet</span> tempers were observed. Increased IS kinetics were predicted at higher temperatures by an IRC model as well as by experimentally determined IRC values; however, the magnitudes of these values are not in good agreement due to deficiencies in the model when applied to alloys. IS kinetics were found to be higher for <span class="hlt">sheets</span> in the fully annealed condition when compared with work-hardened <span class="hlt">sheets</span>, due to the influence of core grain boundaries providing high diffusivity pathways for Si diffusion, resulting in more rapid liquid clad penetration.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140011561','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140011561"><span>Extensive Liquid Meltwater Storage in Firn Within the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Forster, Richard R.; Box, Jason E.; vandenBroeke, Michael R.; Miege, Clement; Burgess, Evan W.; vanAngelen, Jan H.; Lenaerts, Jan T. M.; Koenig, Lora S.; Paden, John; Lewis, Cameron; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20140011561'); toggleEditAbsImage('author_20140011561_show'); toggleEditAbsImage('author_20140011561_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20140011561_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20140011561_hide"></p> <p>2013-01-01</p> <p>The accelerating loss of mass from the Greenland ice <span class="hlt">sheet</span> is a major contribution to current sea level rise. Increased melt water runoff is responsible for half of Greenlands mass loss increase. Surface melt has been increasing in extent and intensity, setting a record for surface area melt and runoff in 2012. The mechanisms and timescales involved in allowing surface melt water to reach the ocean where it can contribute to sea level rise are poorly understood. The potential capacity to store this water in liquid or frozen form in the firn (multi-year snow layer) is significant, and could delay its sea-level contribution. Here we describe <span class="hlt">direct</span> observation of water within a perennial firn aquifer persisting throughout the winter in the southern ice <span class="hlt">sheet</span>,where snow accumulation and melt rates are high. This represents a previously unknown storagemode for water within the ice <span class="hlt">sheet</span>. Ice cores, groundairborne radar and a regional climatemodel are used to estimate aquifer area (70 plue or minus 10 x 10(exp 3) square kilometers ) and water table depth (5-50 m). The perennial firn aquifer represents a new glacier facies to be considered 29 in future ice <span class="hlt">sheet</span> mass 30 and energy budget calculations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.G31C0929H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.G31C0929H"><span>Long term ice <span class="hlt">sheet</span> mass change rates and inter-annual variability from GRACE gravimetry.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harig, C.</p> <p>2017-12-01</p> <p>The GRACE time series of gravimetry now stretches 15 years since its launch in 2002. Here we use Slepian functions to estimate the long term ice mass trends of Greenland, Antarctica, and several glaciated regions. The spatial representation shows multi-year to decadal regional shifts in accelerations, in agreement with increases in radar derived ice velocity. Interannual variations in ice mass are of particular interest since they can <span class="hlt">directly</span> link changes in ice <span class="hlt">sheets</span> to the drivers of change in the polar ocean and atmosphere. The spatial information retained in Slepian functions provides a tool to determine how this link varies in different regions within an ice <span class="hlt">sheet</span>. We present GRACE observations of the 2013-2014 slowdown in mass loss of the Greenland ice <span class="hlt">sheet</span>, which was concentrated in specific parts of the ice <span class="hlt">sheet</span> and in certain months of the year. We also discuss estimating the relative importance of climate factors that control ice mass balance, as a function of location of the glacier/ice cap as well as the spatial variation within an ice <span class="hlt">sheet</span> by comparing gravimetry with observations of surface air temperature, ocean temperature, etc. as well as model data from climate reanalysis products.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4999180','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4999180"><span>eduSPIM: Light <span class="hlt">Sheet</span> Microscopy in the Museum</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Schmid, Benjamin; Weber, Michael; Huisken, Jan</p> <p>2016-01-01</p> <p>Light <span class="hlt">Sheet</span> Microscopy in the Museum Light <span class="hlt">sheet</span> microscopy (or selective plane illumination microscopy) is an important imaging technique in the life sciences. At the same time, this technique is also ideally suited for community outreach projects, because it produces visually appealing, highly dynamic images of living organisms and its working principle can be understood with basic optics knowledge. Still, the underlying concepts are widely unknown to the non-scientific public. On the occasion of the UNESCO International Year of Light, a technical museum in Dresden, Germany, launched a special, interactive exhibition. We built a fully functional, educational selective plane illumination microscope (eduSPIM) to demonstrate how developments in microscopy promote discoveries in biology. Design Principles of an Educational Light <span class="hlt">Sheet</span> Microscope To maximize educational impact, we radically reduced a standard light <span class="hlt">sheet</span> microscope to its essential components without compromising functionality and incorporated stringent safety concepts beyond those needed in the lab. Our eduSPIM system features one illumination and one detection path and a sealed sample chamber. We image fixed zebrafish embryos with fluorescent vasculature, because the structure is meaningful to laymen and visualises the optical principles of light <span class="hlt">sheet</span> microscopy. Via a simplified interface, visitors acquire fluorescence and transmission data simultaneously. The eduSPIM Design Is Tailored Easily to Fit Numerous Applications The universal concepts presented here may also apply to other scientific approaches that are communicated to laymen in interactive settings. The specific eduSPIM design is adapted easily for various outreach and teaching <span class="hlt">activities</span>. eduSPIM may even prove useful for labs needing a simple SPIM. A detailed parts list and schematics to rebuild eduSPIM are provided. PMID:27560188</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22305947-adsorbing-hs-onto-single-graphene-sheet-possible-gas-sensor','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22305947-adsorbing-hs-onto-single-graphene-sheet-possible-gas-sensor"><span>Adsorbing H₂S onto a single graphene <span class="hlt">sheet</span>: A possible gas sensor</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Reshak, A. H., E-mail: maalidph@yahoo.co.uk; Center of Excellence Geopolymer and Green Technology, School of Material Engineering, University Malaysia Perlis, 01007 Kangar, Perlis; Auluck, S.</p> <p>2014-09-14</p> <p>The electronic structure of pristine graphene <span class="hlt">sheet</span> and the resulting structure of adsorbing a single molecule of H₂S on pristine graphene in three different sites (bridge, top, and hollow) are studied using the full potential linearized augmented plane wave method. Our calculations show that the adsorption of H₂S molecule on the bridge site opens up a small <span class="hlt">direct</span> energy gap of about 0.1 eV at symmetry point M, while adsorption of H₂S on top site opens a gap of 0.3 eV around the symmetry point K. We find that adsorbed H₂S onto the hollow site of pristine graphene <span class="hlt">sheet</span> causesmore » to push the conduction band minimum and the valence band maximum towards Fermi level resulting in a metallic behavior. Comparing the angular momentum decomposition of the atoms projected electronic density of states of pristine graphene <span class="hlt">sheet</span> with that of H₂S–graphene for three different cases, we find a significant influence of the location of the H₂S molecule on the electronic properties especially the strong hybridization between H₂S molecule and graphene <span class="hlt">sheet</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22587118-analysis-formability-ca-added-magnesium-alloy-sheets-low-temperatures','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22587118-analysis-formability-ca-added-magnesium-alloy-sheets-low-temperatures"><span>Analysis of formability of Ca-added magnesium alloy <span class="hlt">sheets</span> at low temperatures</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Kim, Se-Jong; Lee, Young-Seon; Kim, Daeyong, E-mail: daeyong@kims.re.kr</p> <p></p> <p>The formability of <span class="hlt">sheets</span> of the Ca-added magnesium alloy AZX311 was analyzed. The parameters affecting the <span class="hlt">sheet</span> formability, such as the strain-hardening rate and the strain-rate sensitivity, did not seem to be higher in the alloy AZX311 at temperatures of room temperature (RT) and 200 °C. In addition, the critical stress for fracture at RT was lower in AZX311 than in AZ31. However, AZX311 exhibited higher stretchability and formability at low temperatures than AZ31. Electron back-scattered diffraction microscopy revealed that AZX311 had a weaker basal texture as well as broadened basal poles along the transverse <span class="hlt">direction</span>. Polycrystal plasticity simulations confirmedmore » that this weaker basal texture increases the <span class="hlt">activity</span> of basal slip over thickness strain, resulting in the higher formability of AZX311. - Highlights: • A weak basal texture with broadening basal poles along the TD in AZX311 • Lower critical stress for fracture at RT in AZX311 than in AZ31 • Lower strain-hardening rates at low temperatures in the AZX311 than in the AZ31 • Higher formability at low temperatures in AZX311 because of the weak basal texture.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/527755','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/527755"><span>Method for heating and forming a glass <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Boaz, P.T.</p> <p>1997-08-12</p> <p>A method for heating and forming a glass <span class="hlt">sheet</span> includes the steps of heating a glass <span class="hlt">sheet</span> to at least a first predetermined temperature, applying microwave energy to the glass <span class="hlt">sheet</span> to heat the glass <span class="hlt">sheet</span> to at least a second predetermined temperature, cooling an outer surface of the glass <span class="hlt">sheet</span> to at least a third predetermined temperature and forming the glass <span class="hlt">sheet</span> using forming rollers to a predetermined configuration. 5 figs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MNRAS.478..983S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MNRAS.478..983S"><span>Predicting pulsar scintillation from refractive plasma <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Simard, Dana; Pen, Ue-Li</p> <p>2018-07-01</p> <p>The dynamic and secondary spectra of many pulsars show evidence for long-lived, aligned images of the pulsar that are stationary on a thin scattering <span class="hlt">sheet</span>. One explanation for this phenomenon considers the effects of wave crests along <span class="hlt">sheets</span> in the ionized interstellar medium, such as those due to Alfvén waves propagating along current <span class="hlt">sheets</span>. If these <span class="hlt">sheets</span> are closely aligned to our line of sight to the pulsar, high bending angles arise at the wave crests and a selection effect causes alignment of images produced at different crests, similar to grazing reflection off of a lake. Using geometric optics, we develop a simple parametrized model of these corrugated <span class="hlt">sheets</span> that can be constrained with a single observation and that makes observable predictions for variations in the scintillation of the pulsar over time and frequency. This model reveals qualitative differences between lensing from overdense and underdense corrugated <span class="hlt">sheets</span>: only if the <span class="hlt">sheet</span> is overdense compared to the surrounding interstellar medium can the lensed images be brighter than the line-of-sight image to the pulsar, and the faint lensed images are closer to the pulsar at higher frequencies if the <span class="hlt">sheet</span> is underdense, but at lower frequencies if the <span class="hlt">sheet</span> is overdense.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018MNRAS.tmp.1079S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018MNRAS.tmp.1079S"><span>Predicting Pulsar Scintillation from Refractive Plasma <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Simard, Dana; Pen, Ue-Li</p> <p>2018-05-01</p> <p>The dynamic and secondary spectra of many pulsars show evidence for long-lived, aligned images of the pulsar that are stationary on a thin scattering <span class="hlt">sheet</span>. One explanation for this phenomenon considers the effects of wave crests along <span class="hlt">sheets</span> in the ionized interstellar medium, such as those due to Alfvén waves propagating along current <span class="hlt">sheets</span>. If these <span class="hlt">sheets</span> are closely aligned to our line-of-sight to the pulsar, high bending angles arise at the wave crests and a selection effect causes alignment of images produced at different crests, similar to grazing reflection off of a lake. Using geometric optics, we develop a simple parameterized model of these corrugated <span class="hlt">sheets</span> that can be constrained with a single observation and that makes observable predictions for variations in the scintillation of the pulsar over time and frequency. This model reveals qualitative differences between lensing from overdense and underdense corrugated <span class="hlt">sheets</span>: Only if the <span class="hlt">sheet</span> is overdense compared to the surrounding interstellar medium can the lensed images be brighter than the line-of-sight image to the pulsar, and the faint lensed images are closer to the pulsar at higher frequencies if the <span class="hlt">sheet</span> is underdense, but at lower frequencies if the <span class="hlt">sheet</span> is overdense.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018TCry...12.1433G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018TCry...12.1433G"><span>Design and results of the ice <span class="hlt">sheet</span> model initialisation experiments initMIP-Greenland: an ISMIP6 intercomparison</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Goelzer, Heiko; Nowicki, Sophie; Edwards, Tamsin; Beckley, Matthew; Abe-Ouchi, Ayako; Aschwanden, Andy; Calov, Reinhard; Gagliardini, Olivier; Gillet-Chaulet, Fabien; Golledge, Nicholas R.; Gregory, Jonathan; Greve, Ralf; Humbert, Angelika; Huybrechts, Philippe; Kennedy, Joseph H.; Larour, Eric; Lipscomb, William H.; Le clec'h, Sébastien; Lee, Victoria; Morlighem, Mathieu; Pattyn, Frank; Payne, Antony J.; Rodehacke, Christian; Rückamp, Martin; Saito, Fuyuki; Schlegel, Nicole; Seroussi, Helene; Shepherd, Andrew; Sun, Sainan; van de Wal, Roderik; Ziemen, Florian A.</p> <p>2018-04-01</p> <p>Earlier large-scale Greenland ice <span class="hlt">sheet</span> sea-level projections (e.g. those run during the ice2sea and SeaRISE initiatives) have shown that ice <span class="hlt">sheet</span> initial conditions have a large effect on the projections and give rise to important uncertainties. The goal of this initMIP-Greenland intercomparison exercise is to compare, evaluate, and improve the initialisation techniques used in the ice <span class="hlt">sheet</span> modelling community and to estimate the associated uncertainties in modelled mass changes. initMIP-Greenland is the first in a series of ice <span class="hlt">sheet</span> model intercomparison <span class="hlt">activities</span> within ISMIP6 (the Ice <span class="hlt">Sheet</span> Model Intercomparison Project for CMIP6), which is the primary <span class="hlt">activity</span> within the Coupled Model Intercomparison Project Phase 6 (CMIP6) focusing on the ice <span class="hlt">sheets</span>. Two experiments for the large-scale Greenland ice <span class="hlt">sheet</span> have been designed to allow intercomparison between participating models of (1) the initial present-day state of the ice <span class="hlt">sheet</span> and (2) the response in two idealised forward experiments. The forward experiments serve to evaluate the initialisation in terms of model drift (forward run without additional forcing) and in response to a large perturbation (prescribed surface mass balance anomaly); they should not be interpreted as sea-level projections. We present and discuss results that highlight the diversity of data sets, boundary conditions, and initialisation techniques used in the community to generate initial states of the Greenland ice <span class="hlt">sheet</span>. We find good agreement across the ensemble for the dynamic response to surface mass balance changes in areas where the simulated ice <span class="hlt">sheets</span> overlap but differences arising from the initial size of the ice <span class="hlt">sheet</span>. The model drift in the control experiment is reduced for models that participated in earlier intercomparison exercises.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1436954-design-results-ice-sheet-model-initialisation-experiments-initmip-greenland-ismip6-intercomparison','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1436954-design-results-ice-sheet-model-initialisation-experiments-initmip-greenland-ismip6-intercomparison"><span>Design and results of the ice <span class="hlt">sheet</span> model initialisation experiments initMIP-Greenland: an ISMIP6 intercomparison</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Goelzer, Heiko; Nowicki, Sophie; Edwards, Tamsin; ...</p> <p>2018-04-19</p> <p>Earlier large-scale Greenland ice <span class="hlt">sheet</span> sea-level projections (e.g. those run during the ice2sea and SeaRISE initiatives) have shown that ice <span class="hlt">sheet</span> initial conditions have a large effect on the projections and give rise to important uncertainties. Here, the goal of this initMIP-Greenland intercomparison exercise is to compare, evaluate, and improve the initialisation techniques used in the ice <span class="hlt">sheet</span> modelling community and to estimate the associated uncertainties in modelled mass changes. initMIP-Greenland is the first in a series of ice <span class="hlt">sheet</span> model intercomparison <span class="hlt">activities</span> within ISMIP6 (the Ice <span class="hlt">Sheet</span> Model Intercomparison Project for CMIP6), which is the primary <span class="hlt">activity</span> within themore » Coupled Model Intercomparison Project Phase 6 (CMIP6) focusing on the ice <span class="hlt">sheets</span>. Two experiments for the large-scale Greenland ice <span class="hlt">sheet</span> have been designed to allow intercomparison between participating models of (1) the initial present-day state of the ice <span class="hlt">sheet</span> and (2) the response in two idealised forward experiments. The forward experiments serve to evaluate the initialisation in terms of model drift (forward run without additional forcing) and in response to a large perturbation (prescribed surface mass balance anomaly); they should not be interpreted as sea-level projections. We present and discuss results that highlight the diversity of data sets, boundary conditions, and initialisation techniques used in the community to generate initial states of the Greenland ice <span class="hlt">sheet</span>. We find good agreement across the ensemble for the dynamic response to surface mass balance changes in areas where the simulated ice <span class="hlt">sheets</span> overlap but differences arising from the initial size of the ice <span class="hlt">sheet</span>. The model drift in the control experiment is reduced for models that participated in earlier intercomparison exercises.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1436954','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1436954"><span>Design and results of the ice <span class="hlt">sheet</span> model initialisation experiments initMIP-Greenland: an ISMIP6 intercomparison</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Goelzer, Heiko; Nowicki, Sophie; Edwards, Tamsin</p> <p></p> <p>Earlier large-scale Greenland ice <span class="hlt">sheet</span> sea-level projections (e.g. those run during the ice2sea and SeaRISE initiatives) have shown that ice <span class="hlt">sheet</span> initial conditions have a large effect on the projections and give rise to important uncertainties. Here, the goal of this initMIP-Greenland intercomparison exercise is to compare, evaluate, and improve the initialisation techniques used in the ice <span class="hlt">sheet</span> modelling community and to estimate the associated uncertainties in modelled mass changes. initMIP-Greenland is the first in a series of ice <span class="hlt">sheet</span> model intercomparison <span class="hlt">activities</span> within ISMIP6 (the Ice <span class="hlt">Sheet</span> Model Intercomparison Project for CMIP6), which is the primary <span class="hlt">activity</span> within themore » Coupled Model Intercomparison Project Phase 6 (CMIP6) focusing on the ice <span class="hlt">sheets</span>. Two experiments for the large-scale Greenland ice <span class="hlt">sheet</span> have been designed to allow intercomparison between participating models of (1) the initial present-day state of the ice <span class="hlt">sheet</span> and (2) the response in two idealised forward experiments. The forward experiments serve to evaluate the initialisation in terms of model drift (forward run without additional forcing) and in response to a large perturbation (prescribed surface mass balance anomaly); they should not be interpreted as sea-level projections. We present and discuss results that highlight the diversity of data sets, boundary conditions, and initialisation techniques used in the community to generate initial states of the Greenland ice <span class="hlt">sheet</span>. We find good agreement across the ensemble for the dynamic response to surface mass balance changes in areas where the simulated ice <span class="hlt">sheets</span> overlap but differences arising from the initial size of the ice <span class="hlt">sheet</span>. The model drift in the control experiment is reduced for models that participated in earlier intercomparison exercises.« less</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_17 --> <div id="page_18" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="341"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMSM21B..06G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMSM21B..06G"><span>Energized Oxygen : Speiser Current <span class="hlt">Sheet</span> Bifurcation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>George, D. E.; Jahn, J. M.</p> <p>2017-12-01</p> <p>A single population of energized Oxygen (O+) is shown to produce a cross-tail bifurcated current <span class="hlt">sheet</span> in 2.5D PIC simulations of the magnetotail without the influence of magnetic reconnection. Treatment of oxygen in simulations of space plasmas, specifically a magnetotail current <span class="hlt">sheet</span>, has been limited to thermal energies despite observations of and mechanisms which explain energized ions. We performed simulations of a homogeneous oxygen background, that has been energized in a physically appropriate manner, to study the behavior of current <span class="hlt">sheets</span> and magnetic reconnection, specifically their bifurcation. This work uses a 2.5D explicit Particle-In-a-Cell (PIC) code to investigate the dynamics of energized heavy ions as they stream Dawn-to-Dusk in the magnetotail current <span class="hlt">sheet</span>. We present a simulation study dealing with the response of a current <span class="hlt">sheet</span> system to energized oxygen ions. We establish a, well known and studied, 2-species GEM Challenge Harris current <span class="hlt">sheet</span> as a starting point. This system is known to eventually evolve and produce magnetic reconnection upon thinning of the current <span class="hlt">sheet</span>. We added a uniform distribution of thermal O+ to the background. This 3-species system is also known to eventually evolve and produce magnetic reconnection. We add one additional variable to the system by providing an initial duskward velocity to energize the O+. We also traced individual particle motion within the PIC simulation. Three main results are shown. First, energized dawn- dusk streaming ions are clearly seen to exhibit sustained Speiser motion. Second, a single population of heavy ions clearly produces a stable bifurcated current <span class="hlt">sheet</span>. Third, magnetic reconnection is not required to produce the bifurcated current <span class="hlt">sheet</span>. Finally a bifurcated current <span class="hlt">sheet</span> is compatible with the Harris current <span class="hlt">sheet</span> model. This work is the first step in a series of investigations aimed at studying the effects of energized heavy ions on magnetic reconnection. This work differs</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4822606','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4822606"><span>Breaking the diffraction limit of light-<span class="hlt">sheet</span> fluorescence microscopy by RESOLFT</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Hoyer, Patrick; de Medeiros, Gustavo; Balázs, Bálint; Norlin, Nils; Besir, Christina; Hanne, Janina; Kräusslich, Hans-Georg; Engelhardt, Johann; Sahl, Steffen J.; Hell, Stefan W.; Hufnagel, Lars</p> <p>2016-01-01</p> <p>We present a plane-scanning RESOLFT [reversible saturable/switchable optical (fluorescence) transitions] light-<span class="hlt">sheet</span> (LS) nanoscope, which fundamentally overcomes the diffraction barrier in the axial <span class="hlt">direction</span> via confinement of the fluorescent molecular state to a <span class="hlt">sheet</span> of subdiffraction thickness around the focal plane. To this end, reversibly switchable fluorophores located right above and below the focal plane are transferred to a nonfluorescent state at each scanning step. LS-RESOLFT nanoscopy offers wide-field 3D imaging of living biological specimens with low light dose and axial resolution far beyond the diffraction barrier. We demonstrate optical sections that are thinner by 5–12-fold compared with their conventional diffraction-limited LS analogs. PMID:26984498</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19830051105&hterms=Critical+Technology&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DCritical%2BTechnology','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19830051105&hterms=Critical+Technology&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DCritical%2BTechnology"><span>Critical technology limits to silicon material and <span class="hlt">sheet</span> production</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Leipold, M. H.</p> <p>1982-01-01</p> <p>Earlier studies have indicated that expenditures related to the preparation of high-purity silicon and its conversion to silicon <span class="hlt">sheet</span> represent from 40 to 52 percent of the cost of the entire panel. The present investigation is concerned with the elements which were selected for study in connection with the Flat-Plate Solar Array (FSA) Project. The first of two technologies which are being developed within the FSA Project involves the conversion of metallurgical-grade silicon through a silane purification process to silicon particles. The second is concerned with the conversion of trichlorosilane to dichlorosilane, and the subsequent production of silicon using modified rod reactors of the Siemens type. With respect to silicon <span class="hlt">sheet</span> preparation, efforts have been focused both on the preparation of ingots, followed by wafering, and the <span class="hlt">direct</span> crystallization of molten silicon into a ribbon or film.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AIPC.1960o0005K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AIPC.1960o0005K"><span>Experimental formability analysis of bondal sandwich <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kami, Abdolvahed; Banabic, Dorel</p> <p>2018-05-01</p> <p>Metal/polymer/metal sandwich <span class="hlt">sheets</span> have recently attracted the interests of industries like automotive industry. These sandwich <span class="hlt">sheets</span> have superior properties over single-layer metallic <span class="hlt">sheets</span> including good sound and vibration damping and light weight. However, the formability of these sandwich <span class="hlt">sheets</span> should be enhanced which requires more research. In this paper, the formability of Bondal <span class="hlt">sheet</span> (DC06/viscoelastic polymer/DC06 sandwich <span class="hlt">sheet</span>) was studied through different types of experiments. The mechanical properties of Bondal were determined by uniaxial tensile tests. Hemispherical punch stretching and hydraulic bulge tests were carried out to determine the forming limit diagram (FLD) of Bondal. Furthermore, cylindrical and square cup drawing tests were performed in dry and oil lubricated conditions. These tests were conducted at different blank holding forces (BHFs). An interesting observation about Bondal <span class="hlt">sheet</span> deep drawing was obtaining of higher drawing depths at dry condition in comparison with oil-lubricated condition.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27392366','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27392366"><span><span class="hlt">Active</span> Manual Movement Improves <span class="hlt">Directional</span> Perception of Illusory Force.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Amemiya, Tomohiro; Gomi, Hiroaki</p> <p>2016-01-01</p> <p><span class="hlt">Active</span> touch sensing is known to facilitate the discrimination or recognition of the spatial properties of an object from the movement of tactile sensors on the skin and by integrating proprioceptive feedback about hand positions or motor commands related to ongoing hand movements. On the other hand, several studies have reported that tactile processing is suppressed by hand movement. Thus, it is unclear whether or not the <span class="hlt">active</span> exploration of force <span class="hlt">direction</span> by using hand or arm movement improves the perception of the force <span class="hlt">direction</span>. Here, we show that <span class="hlt">active</span> manual movement in both the rotational and translational <span class="hlt">directions</span> enhances the precise perception of the force <span class="hlt">direction</span>. To make it possible to move a hand in space without any physical constraints, we have adopted a method of inducing the sensation of illusory force by asymmetric vibration. We found that the precision of the perceived force <span class="hlt">direction</span> was significantly better when the shoulder is rotated medially and laterally. We also found that <span class="hlt">directional</span> errors supplied by the motor response of the perceived force were smaller than those resulting from perceptual judgments between visual and haptic <span class="hlt">directional</span> stimuli. These results demonstrate that <span class="hlt">active</span> manual movement boosts the precision of the perceived <span class="hlt">direction</span> of an illusory force.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMED13A0927P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMED13A0927P"><span>Hand-Drawn 'Weekly Information <span class="hlt">Sheets</span>' Focus Teaching, Engage Students, and Improve Communication</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pound, K. S.</p> <p>2016-12-01</p> <p>Hand-drawn and lettered `Weekly Information <span class="hlt">Sheets</span>' (WIS) were created on a weekly basis for an upper-level Sedimentology & Stratigraphy class. Use of these <span class="hlt">sheets</span> resulted in improved work quality, attention to detail, communication skills, and overall engagement. The <span class="hlt">sheets</span> were modeled on the work of Lynda Barry (https://www.drawnandquarterly.com/syllabus), and included a series of repeated elements: goofy/absurd newspaper clippings, marginally pertinent cartoon(s), a summary of the weeks <span class="hlt">activities</span> / goals and lectures, as well as cartoon cat, mouse and penguin drawings with innane comments, quotes and general class reminders. The pedagogical aims for these weekly <span class="hlt">sheets</span> were multifold. First, they were designed so that students could see the time and care I put in to the <span class="hlt">sheet</span> - my hope was that this would show the time and care I expected them to put in to their work. Second, I wanted to create something students would take the time to read - despite this being a 400-level class, students are rarely diligent about reading a typewritten handout. Third, I wanted to have a vehicle for engaging them in the larger world, including ethical or moral dilemmas. Fourth, I wanted the students to reflectively consider the nature of communication in science. Finally, I wanted a mechanism to focus my thoughts on the teaching and learning for the upcoming week that went beyond simply reviewing my notes and <span class="hlt">activities</span>. Student response to the WIS was positive; they read them, used them for organizing their class notes and exam review. Students arrived early for class on Mondays for the WIS - although I needed to give them time to read the <span class="hlt">sheet</span>. Comparison with previous course offerings shows improvements in student communication skills (written reports, poster presentation) and overall achievement.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JSV...413..421T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JSV...413..421T"><span>A Ffowcs Williams and Hawkings formulation for hydroacoustic analysis of propeller <span class="hlt">sheet</span> cavitation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Testa, C.; Ianniello, S.; Salvatore, F.</p> <p>2018-01-01</p> <p>A novel hydroacoustic formulation for the prediction of tonal noise emitted by marine propellers in presence of unsteady <span class="hlt">sheet</span> cavitation, is presented. The approach is based on the standard Ffowcs Williams and Hawkings equation and the use of transpiration (velocity and acceleration) terms, accounting for the time evolution of the vapour cavity attached on the blade surface. Drawbacks and potentialities of the method are tested on a marine propeller operating in a nonhomogeneous onset flow, by exploiting the hydrodynamic data from a potential-based panel method equipped with a <span class="hlt">sheet</span> cavitation model and comparing the noise predictions with those carried out by an alternative numerical approach, documented in literature. It is shown that the proposed formulation yields a one-to-one correlation between emitted noise and <span class="hlt">sheet</span> cavitation dynamics, carrying out accurate predictions in terms of noise magnitude and <span class="hlt">directivity</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20060016373&hterms=EIT&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DEIT','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20060016373&hterms=EIT&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DEIT"><span>Current <span class="hlt">Sheet</span> Evolution In The Aftermath Of A CME Event</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bemporad, A.; Poletto, G.; Seuss, S. T.; Schwardron, N. A.; Elliott, H. A.; Raymond, J. C.</p> <p>2006-01-01</p> <p>We report on SOHO UVCS observations of the coronal restructuring following a coronal mass ejection (CME) on 2002 November 26, at the time of a SOHO-Ulysses quadrature campaign. Starting about 1.5 hr after a CME in the northwest quadrant, UVCS began taking spectra at 1.7 R, covering emission from both cool and hot plasma. Observations continued, with occasional gaps, for more than 2 days. Emission in the 974.8 A line of [Fe XVIII], indicating temperatures above 6 x 10(exp 6) K, was observed throughout the campaign in a spatially limited location. Comparison with EIT images shows the [Fe XVIII] emission to overlie a growing post-flare loop system formed in the aftermath of the CME. The emission most likely originates in a current <span class="hlt">sheet</span> overlying the arcade. Analysis of the [Fe XVIII] emission allows us to infer the evolution of physical parameters in the current <span class="hlt">sheet</span> over the entire span of our observations: in particular, we give the temperature versus time in the current <span class="hlt">sheet</span> and estimate its density. At the time of the quadrature, Ulysses was <span class="hlt">directly</span> above the location of the CME and intercepted the ejecta. High ionization state Fe was detected by the Ulysses SWICS throughout the magnetic cloud associated with the CME, although its rapid temporal variation suggests bursty, rather than smooth, reconnection in the coronal current <span class="hlt">sheet</span>. The SOHO-Ulysses data set provided us with the unique opportunity of analyzing a current <span class="hlt">sheet</span> structure from its lowest coronal levels out to its in situ properties. Both the remote and in situ observations are compared with predictions of theoretical CME models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ApSS..427..678S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ApSS..427..678S"><span>Porous Ni3(NO3)2(OH)4 nano-<span class="hlt">sheets</span> for supercapacitors: Facile synthesis and excellent rate performance at high mass loadings</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shi, Mingjie; Cui, Mangwei; Kang, Litao; Li, Taotao; Yun, Shan; Du, Jing; Xu, Shoudong; Liu, Ying</p> <p>2018-01-01</p> <p>For supercapacitors, pores in electrode materials can accelerate chemical reaction kinetics by shortening ion diffusion distances and by enlarging electrolyte/electrode interfaces. This article describes a simple one-step route for the preparation of pure-phase porous Ni3(NO3)2(OH)4 nano-<span class="hlt">sheets</span> by <span class="hlt">directly</span> heating a mild Ni(NO3)2 and urea solution. During heating, urea decomposed into NH3·H2O, which provided a suitable alkaline environment for the formation of Ni3(NO3)2(OH)4 nano-<span class="hlt">sheets</span>. Meanwhile, the side product, NH4NO3, created numerous pores as a pore-forming agent. After NH4NO3 removal, the specific surface areas and pore volumes of products were boosted by ∼180-times (from 0.61 to 113.12 m2/g) and ∼90-times (from 3.40 × 10-3 to 3.17 × 10-1 m2/g), respectively. As a cathode material of supercapacitor, the porous Ni3(NO3)2(OH)4 nano-<span class="hlt">sheets</span> exhibited a high specific capacitance of 1094 F/g at an ultrahigh mass loading of 17.55 mg/cm2, leading to an impressive areal capacitance of 19.2 F/cm2. Furthermore, a Ni3(NO3)2(OH)4 nano-<span class="hlt">sheet</span>//commercial <span class="hlt">active</span> carbon asymmetric supercapacitor was constructed and delivered an energy density of 33.2 Wh/Kg at a power density of 190.5 W/Kg, based on the mass of <span class="hlt">active</span> materials on both electrodes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.C53A0822T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.C53A0822T"><span>Modeling North American Ice <span class="hlt">Sheet</span> Response to Changes in Precession and Obliquity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tabor, C.; Poulsen, C. J.; Pollard, D.</p> <p>2012-12-01</p> <p> precession on the Laurentide and Cordillera ice <span class="hlt">sheets</span> of North America. Preliminary model results show that the ice <span class="hlt">sheet</span> response to changes in obliquity are larger than for precession despite providing a smaller <span class="hlt">direct</span> insolation variation in the Northern Hemisphere high latitudes. A combination of enhanced Northern Hemisphere mid-latitude temperature gradient and longer cycle duration allow for a larger ice <span class="hlt">sheet</span> response to obliquity than would be expected from insolation forcing alone. Conversely, a shorter duration dampens the ice <span class="hlt">sheet</span> response to precession. Nevertheless, the precession cycle does cause significant changes in ice volume, a feature not observed in the Early Pleistocene δ18O records (Raymo and Nisancioglu, 2003). Future work will examine the climate response to an idealized transient orbit that includes concurrent variations in obliquity, precession, and eccentricity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19900046156&hterms=disintegration&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Ddisintegration','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19900046156&hterms=disintegration&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Ddisintegration"><span>Disintegration of liquid <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mansour, Adel; Chigier, Norman</p> <p>1990-01-01</p> <p>The development, stability, and disintegration of liquid <span class="hlt">sheets</span> issuing from a two-dimensional air-assisted nozzle is studied. Detailed measurements of mean drop size and velocity are made using a phase Doppler particle analyzer. Without air flow the liquid <span class="hlt">sheet</span> converges toward the axis as a result of surface tension forces. With airflow a quasi-two-dimensional expanding spray is formed. The air flow causes small variations in <span class="hlt">sheet</span> thickness to develop into major disturbances with the result that disruption starts before the formation of the main break-up region. In the two-dimensional variable geometry air-blast atomizer, it is shown that the air flow is responsible for the formation of large, ordered, and small chaotic 'cell' structures.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/868644','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/868644"><span>Root-growth-inhibiting <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Burton, Frederick G.; Cataldo, Dominic A.; Cline, John F.; Skiens, W. Eugene; Van Voris, Peter</p> <p>1993-01-01</p> <p>In accordance with this invention, a porous <span class="hlt">sheet</span> material is provided at intervals with bodies of a polymer which contain a 2,6-dinitroaniline. The <span class="hlt">sheet</span> material is made porous to permit free passage of water. It may be either a perforated <span class="hlt">sheet</span> or a woven or non-woven textile material. A particularly desirable embodiment is a non-woven fabric of non-biodegradable material. This type of material is known as a "geotextile" and is used for weed control, prevention of erosion on slopes, and other landscaping purposes. In order to obtain a root repelling property, a dinitroaniline is blended with a polymer which is attached to the geotextile or other porous material.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/6285534','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/6285534"><span>Root-growth-inhibiting <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Burton, F.G.; Cataldo, D.A.; Cline, J.F.; Skiens, W.E.; Van Voris, P.</p> <p>1993-01-26</p> <p>In accordance with this invention, a porous <span class="hlt">sheet</span> material is provided at intervals with bodies of a polymer which contain a 2,6-dinitroaniline. The <span class="hlt">sheet</span> material is made porous to permit free passage of water. It may be either a perforated <span class="hlt">sheet</span> or a woven or non-woven textile material. A particularly desirable embodiment is a non-woven fabric of non-biodegradable material. This type of material is known as a geotextile'' and is used for weed control, prevention of erosion on slopes, and other landscaping purposes. In order to obtain a root repelling property, a dinitroaniline is blended with a polymer which is attached to the geotextile or other porous material.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title16-vol1/pdf/CFR-2012-title16-vol1-sec460-13.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title16-vol1/pdf/CFR-2012-title16-vol1-sec460-13.pdf"><span>16 CFR 460.13 - Fact <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-01-01</p> <p>... heat flow. The higher the R-value, the greater the insulating power. Compare insulation R-values before... INSULATION § 460.13 Fact <span class="hlt">sheets</span>. If you are a manufacturer, you must give retailers and installers fact <span class="hlt">sheets</span> for the insulation products you sell to them. Each <span class="hlt">sheet</span> must contain what is listed here. You can...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title16-vol1/pdf/CFR-2010-title16-vol1-sec460-13.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title16-vol1/pdf/CFR-2010-title16-vol1-sec460-13.pdf"><span>16 CFR 460.13 - Fact <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-01-01</p> <p>... heat flow. The higher the R-value, the greater the insulating power. Compare insulation R-values before... INSULATION § 460.13 Fact <span class="hlt">sheets</span>. If you are a manufacturer, you must give retailers and installers fact <span class="hlt">sheets</span> for the insulation products you sell to them. Each <span class="hlt">sheet</span> must contain what is listed here. You can...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title16-vol1/pdf/CFR-2014-title16-vol1-sec460-13.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title16-vol1/pdf/CFR-2014-title16-vol1-sec460-13.pdf"><span>16 CFR 460.13 - Fact <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-01-01</p> <p>... heat flow. The higher the R-value, the greater the insulating power. Compare insulation R-values before... INSULATION § 460.13 Fact <span class="hlt">sheets</span>. If you are a manufacturer, you must give retailers and installers fact <span class="hlt">sheets</span> for the insulation products you sell to them. Each <span class="hlt">sheet</span> must contain what is listed here. You can...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title16-vol1/pdf/CFR-2013-title16-vol1-sec460-13.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title16-vol1/pdf/CFR-2013-title16-vol1-sec460-13.pdf"><span>16 CFR 460.13 - Fact <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-01-01</p> <p>... heat flow. The higher the R-value, the greater the insulating power. Compare insulation R-values before... INSULATION § 460.13 Fact <span class="hlt">sheets</span>. If you are a manufacturer, you must give retailers and installers fact <span class="hlt">sheets</span> for the insulation products you sell to them. Each <span class="hlt">sheet</span> must contain what is listed here. You can...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title16-vol1/pdf/CFR-2011-title16-vol1-sec460-13.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title16-vol1/pdf/CFR-2011-title16-vol1-sec460-13.pdf"><span>16 CFR 460.13 - Fact <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-01-01</p> <p>... heat flow. The higher the R-value, the greater the insulating power. Compare insulation R-values before... INSULATION § 460.13 Fact <span class="hlt">sheets</span>. If you are a manufacturer, you must give retailers and installers fact <span class="hlt">sheets</span> for the insulation products you sell to them. Each <span class="hlt">sheet</span> must contain what is listed here. You can...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1911256P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1911256P"><span>Using palaeoclimate data to improve models of the Antarctic Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Phipps, Steven; King, Matt; Roberts, Jason; White, Duanne</p> <p>2017-04-01</p> <p>Ice <span class="hlt">sheet</span> models are the most descriptive tools available to simulate the future evolution of the Antarctic Ice <span class="hlt">Sheet</span> (AIS), including its contribution towards changes in global sea level. However, our knowledge of the dynamics of the coupled ice-ocean-lithosphere system is inevitably limited, in part due to a lack of observations. Furthemore, to build computationally efficient models that can be run for multiple millennia, it is necessary to use simplified descriptions of ice dynamics. Ice <span class="hlt">sheet</span> modelling is therefore an inherently uncertain exercise. The past evolution of the AIS provides an opportunity to constrain the description of physical processes within ice <span class="hlt">sheet</span> models and, therefore, to constrain our understanding of the role of the AIS in driving changes in global sea level. We use the Parallel Ice <span class="hlt">Sheet</span> Model (PISM) to demonstrate how palaeoclimate data can improve our ability to predict the future evolution of the AIS. A 50-member perturbed-physics ensemble is generated, spanning uncertainty in the parameterisations of three key physical processes within the model: (i) the stress balance within the ice <span class="hlt">sheet</span>, (ii) basal sliding and (iii) calving of ice shelves. A Latin hypercube approach is used to optimally sample the range of uncertainty in parameter values. This perturbed-physics ensemble is used to simulate the evolution of the AIS from the Last Glacial Maximum ( 21,000 years ago) to present. Palaeoclimate records are then used to determine which ensemble members are the most realistic. This allows us to use data on past climates to <span class="hlt">directly</span> constrain our understanding of the past contribution of the AIS towards changes in global sea level. Critically, it also allows us to determine which ensemble members are likely to generate the most realistic projections of the future evolution of the AIS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/873879','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/873879"><span>Manifold free multiple <span class="hlt">sheet</span> superplastic forming</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Elmer, John W.; Bridges, Robert L.</p> <p>2001-01-01</p> <p>Fluid-forming compositions in a container attached to enclosed adjacent <span class="hlt">sheets</span> are heated to relatively high temperatures to generate fluids (gases) that effect inflation of the <span class="hlt">sheets</span>. Fluid rates to the enclosed space between the <span class="hlt">sheets</span> can be regulated by the canal from the container. Inflated articles can be produced by a continuous, rather than batch-type, process.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_18 --> <div id="page_19" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="361"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title21-vol8/pdf/CFR-2010-title21-vol8-sec880-5180.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title21-vol8/pdf/CFR-2010-title21-vol8-sec880-5180.pdf"><span>21 CFR 880.5180 - Burn <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... 21 Food and Drugs 8 2010-04-01 2010-04-01 false Burn <span class="hlt">sheet</span>. 880.5180 Section 880.5180 Food and... Burn <span class="hlt">sheet</span>. (a) Identification. A burn <span class="hlt">sheet</span> is a device made of a porous material that is wrapped aroung a burn victim to retain body heat, to absorb wound exudate, and to serve as a barrier against...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title21-vol8/pdf/CFR-2011-title21-vol8-sec880-5180.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title21-vol8/pdf/CFR-2011-title21-vol8-sec880-5180.pdf"><span>21 CFR 880.5180 - Burn <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-04-01</p> <p>... 21 Food and Drugs 8 2011-04-01 2011-04-01 false Burn <span class="hlt">sheet</span>. 880.5180 Section 880.5180 Food and... Burn <span class="hlt">sheet</span>. (a) Identification. A burn <span class="hlt">sheet</span> is a device made of a porous material that is wrapped aroung a burn victim to retain body heat, to absorb wound exudate, and to serve as a barrier against...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title21-vol8/pdf/CFR-2013-title21-vol8-sec880-5180.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title21-vol8/pdf/CFR-2013-title21-vol8-sec880-5180.pdf"><span>21 CFR 880.5180 - Burn <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-04-01</p> <p>... 21 Food and Drugs 8 2013-04-01 2013-04-01 false Burn <span class="hlt">sheet</span>. 880.5180 Section 880.5180 Food and... Burn <span class="hlt">sheet</span>. (a) Identification. A burn <span class="hlt">sheet</span> is a device made of a porous material that is wrapped aroung a burn victim to retain body heat, to absorb wound exudate, and to serve as a barrier against...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title21-vol8/pdf/CFR-2014-title21-vol8-sec880-5180.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title21-vol8/pdf/CFR-2014-title21-vol8-sec880-5180.pdf"><span>21 CFR 880.5180 - Burn <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-04-01</p> <p>... 21 Food and Drugs 8 2014-04-01 2014-04-01 false Burn <span class="hlt">sheet</span>. 880.5180 Section 880.5180 Food and... Burn <span class="hlt">sheet</span>. (a) Identification. A burn <span class="hlt">sheet</span> is a device made of a porous material that is wrapped aroung a burn victim to retain body heat, to absorb wound exudate, and to serve as a barrier against...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title21-vol8/pdf/CFR-2012-title21-vol8-sec880-5180.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title21-vol8/pdf/CFR-2012-title21-vol8-sec880-5180.pdf"><span>21 CFR 880.5180 - Burn <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-04-01</p> <p>... 21 Food and Drugs 8 2012-04-01 2012-04-01 false Burn <span class="hlt">sheet</span>. 880.5180 Section 880.5180 Food and... Burn <span class="hlt">sheet</span>. (a) Identification. A burn <span class="hlt">sheet</span> is a device made of a porous material that is wrapped aroung a burn victim to retain body heat, to absorb wound exudate, and to serve as a barrier against...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1174679','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/1174679"><span>Manifold free multiple <span class="hlt">sheet</span> superplastic forming</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Elmer, John W.; Bridges, Robert L.</p> <p>2004-01-13</p> <p>Fluid-forming compositions in a container attached to enclosed adjacent <span class="hlt">sheets</span> are heated to relatively high temperatures to generate fluids (gases) that effect inflation of the <span class="hlt">sheets</span>. Fluid rates to the enclosed space between the <span class="hlt">sheets</span> can be regulated by the canal from the container. Inflated articles can be produced by a continuous, rather than batch-type, process.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017APS..DFD.E8003C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017APS..DFD.E8003C"><span>Viscous propulsion in <span class="hlt">active</span> transversely isotropic media</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cupples, Gemma; Dyson, Rosemary; Smith, David</p> <p>2017-11-01</p> <p>Taylor's swimming <span class="hlt">sheet</span> is a classical model of microscale propulsion and pumping. Many biological fluids and substances are fibrous, having a preferred <span class="hlt">direction</span> in their microstructure; for example cervical mucus. To understand how these effects modify viscous propulsion, we extend Taylor's classical model of small-amplitude viscous propulsion of a `swimming <span class="hlt">sheet</span>' via the transversely-isotropic fluid model of Ericksen, which is linear in strain rate and possesses a distinguished <span class="hlt">direction</span>. The energetic costs of swimming are significantly altered by all rheological parameters and the initial fibre angle. Propulsion in a passive transversely-isotropic fluid enhances mean rate of working, independent of the initial fibre orientation. In this regime the mean swimming velocity is unchanged from the Newtonian case. The effect of fibre tension, or alternatively a stresslet characterising an <span class="hlt">active</span> fluid, is also considered. This stress introduces an angular dependence and dramatically changes the streamlines and flow field; fibres aligned with the swimming <span class="hlt">direction</span> increase the energetic demands of the <span class="hlt">sheet</span>. The constant fibre stress may result in a reversal of the mean swimming velocity and a negative mean rate of working if sufficiently large relative to the other parameters. Funding is provided by a Biotechnology and Biological Sciences Research Council (BBSRC) Industrial CASE Studentship (BB/L015587/1).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PhyB..537..314W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PhyB..537..314W"><span>Anisotropic carrier mobility in single- and bi-layer C3N <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, Xueyan; Li, Qingfang; Wang, Haifeng; Gao, Yan; Hou, Juan; Shao, Jianxin</p> <p>2018-05-01</p> <p>Based on the density functional theory combined with the Boltzmann transport equation with relaxation time approximation, we investigate the electronic structure and predict the carrier mobility of single- and bi-layer newly fabricated 2D carbon nitrides C3N. Although C3N <span class="hlt">sheets</span> possess graphene-like planar hexagonal structure, the calculated carrier mobility is remarkably anisotropic, which is found mainly induced by the anisotropic effective masses and deformation potential constants. Importantly, we find that both the electron and hole mobilities are considerable high, for example, the hole mobility along the armchair <span class="hlt">direction</span> of single-layer C3N <span class="hlt">sheets</span> can arrive as high as 1.08 ×104 cm2 V-1 s-1, greatly larger than that of C2N-h2D and many other typical 2D materials. Owing to the high and anisotropic carrier mobility and appropriate band gap, single- and bi-layer semiconducting C3N <span class="hlt">sheets</span> may have great potential applications in high performance electronic and optoelectronic devices.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008ArRMA.187..369C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008ArRMA.187..369C"><span>Existence and Stability of Compressible Current-Vortex <span class="hlt">Sheets</span> in Three-Dimensional Magnetohydrodynamics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Gui-Qiang; Wang, Ya-Guang</p> <p>2008-03-01</p> <p>Compressible vortex <span class="hlt">sheets</span> are fundamental waves, along with shocks and rarefaction waves, in entropy solutions to multidimensional hyperbolic systems of conservation laws. Understanding the behavior of compressible vortex <span class="hlt">sheets</span> is an important step towards our full understanding of fluid motions and the behavior of entropy solutions. For the Euler equations in two-dimensional gas dynamics, the classical linearized stability analysis on compressible vortex <span class="hlt">sheets</span> predicts stability when the Mach number M > sqrt{2} and instability when M < sqrt{2} ; and Artola and Majda’s analysis reveals that the nonlinear instability may occur if planar vortex <span class="hlt">sheets</span> are perturbed by highly oscillatory waves even when M > sqrt{2} . For the Euler equations in three dimensions, every compressible vortex <span class="hlt">sheet</span> is violently unstable and this instability is the analogue of the Kelvin Helmholtz instability for incompressible fluids. The purpose of this paper is to understand whether compressible vortex <span class="hlt">sheets</span> in three dimensions, which are unstable in the regime of pure gas dynamics, become stable under the magnetic effect in three-dimensional magnetohydrodynamics (MHD). One of the main features is that the stability problem is equivalent to a free-boundary problem whose free boundary is a characteristic surface, which is more delicate than noncharacteristic free-boundary problems. Another feature is that the linearized problem for current-vortex <span class="hlt">sheets</span> in MHD does not meet the uniform Kreiss Lopatinskii condition. These features cause additional analytical difficulties and especially prevent a <span class="hlt">direct</span> use of the standard Picard iteration to the nonlinear problem. In this paper, we develop a nonlinear approach to deal with these difficulties in three-dimensional MHD. We first carefully formulate the linearized problem for the current-vortex <span class="hlt">sheets</span> to show rigorously that the magnetic effect makes the problem weakly stable and establish energy estimates, especially high-order energy</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20150021522&hterms=methodological&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dmethodological','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20150021522&hterms=methodological&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dmethodological"><span>On the Reconstruction of Palaeo-Ice <span class="hlt">Sheets</span>: Recent Advances and Future Challenges</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stokes, Chris R.; Tarasov, Lev; Blomdin, Robin; Cronin, Thomas M.; Fisher, Timothy G.; Gyllencreutz, Richard; Hattestrand, Clas; Heyman, Jacob; Hindmarsh, Richard C. A.; Hughes, Anna L. C.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20150021522'); toggleEditAbsImage('author_20150021522_show'); toggleEditAbsImage('author_20150021522_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20150021522_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20150021522_hide"></p> <p>2015-01-01</p> <p>Reconstructing the growth and decay of palaeo-ice <span class="hlt">sheets</span> is critical to understanding mechanisms of global climate change and associated sea-level fluctuations in the past, present and future. The significance of palaeo-ice <span class="hlt">sheets</span> is further underlined by the broad range of disciplines concerned with reconstructing their behaviour, many of which have undergone a rapid expansion since the 1980s. In particular, there has been a major increase in the size and qualitative diversity of empirical data used to reconstruct and date ice <span class="hlt">sheets</span>, and major improvements in our ability to simulate their dynamics in numerical ice <span class="hlt">sheet</span> models. These developments have made it increasingly necessary to forge interdisciplinary links between sub-disciplines and to link numerical modelling with observations and dating of proxy records. The aim of this paper is to evaluate recent developments in the methods used to reconstruct ice <span class="hlt">sheets</span> and outline some key challenges that remain, with an emphasis on how future work might integrate terrestrial and marine evidence together with numerical modelling. Our focus is on pan-ice <span class="hlt">sheet</span> reconstructions of the last deglaciation, but regional case studies are used to illustrate methodological achievements, challenges and opportunities. Whilst various disciplines have made important progress in our understanding of ice-<span class="hlt">sheet</span> dynamics, it is clear that data-model integration remains under-used, and that uncertainties remain poorly quantified in both empirically-based and numerical ice-<span class="hlt">sheet</span> reconstructions. The representation of past climate will continue to be the largest source of uncertainty for numerical modelling. As such, palaeo-observations are critical to constrain and validate modelling. State-of-the-art numerical models will continue to improve both in model resolution and in the breadth of inclusion of relevant processes, thereby enabling more accurate and more <span class="hlt">direct</span> comparison with the increasing range of palaeo-observations. Thus</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70180974','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70180974"><span>On the reconstruction of palaeo-ice <span class="hlt">sheets</span>: Recent advances and future challenges</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Stokes, Chris R.; Tarasov, Lev; Blomdin, Robin; Cronin, Thomas M.; Fisher, Timothy G.; Gyllencreutz, Richard; Hattestrand, Clas; Heyman, Jakob; Hindmarsh, Richard C. A.; Hughes, Anna L. C.; Jakobsson, Martin; Kirchner, Nina; Livingstone, Stephen J.; Margold, Martin; Murton, Julian B.; Noormets, Riko; Peltier, W. Richard; Peteet, Dorothy M.; Piper, David J. W.; Preusser, Frank; Renssen, Hans; Roberts, David H.; Roche, Didier M.; Saint-Ange, Francky; Stroeven, Arjen P.; Teller, James T.</p> <p>2015-01-01</p> <p>Reconstructing the growth and decay of palaeo-ice <span class="hlt">sheets</span> is critical to understanding mechanisms of global climate change and associated sea-level fluctuations in the past, present and future. The significance of palaeo-ice <span class="hlt">sheets</span> is further underlined by the broad range of disciplines concerned with reconstructing their behaviour, many of which have undergone a rapid expansion since the 1980s. In particular, there has been a major increase in the size and qualitative diversity of empirical data used to reconstruct and date ice <span class="hlt">sheets</span>, and major improvements in our ability to simulate their dynamics in numerical ice <span class="hlt">sheet</span> models. These developments have made it increasingly necessary to forge interdisciplinary links between sub-disciplines and to link numerical modelling with observations and dating of proxy records. The aim of this paper is to evaluate recent developments in the methods used to reconstruct ice <span class="hlt">sheets</span> and outline some key challenges that remain, with an emphasis on how future work might integrate terrestrial and marine evidence together with numerical modelling. Our focus is on pan-ice <span class="hlt">sheet</span> reconstructions of the last deglaciation, but regional case studies are used to illustrate methodological achievements, challenges and opportunities. Whilst various disciplines have made important progress in our understanding of ice-<span class="hlt">sheet</span> dynamics, it is clear that data-model integration remains under-used, and that uncertainties remain poorly quantified in both empirically-based and numerical ice-<span class="hlt">sheet</span> reconstructions. The representation of past climate will continue to be the largest source of uncertainty for numerical modelling. As such, palaeo-observations are critical to constrain and validate modelling. State-of-the-art numerical models will continue to improve both in model resolution and in the breadth of inclusion of relevant processes, thereby enabling more accurate and more <span class="hlt">direct</span> comparison with the increasing range of palaeo-observations. Thus</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23276286','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23276286"><span>Graphene: powder, flakes, ribbons, and <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>James, Dustin K; Tour, James M</p> <p>2013-10-15</p> <p> fibers and in the fabrication of large area transparent electrodes. Using solid carbon sources such as polymers, food, insects, and waste, we can grow monolayer and bilayer graphene <span class="hlt">directly</span> on metal catalysts, and carbon-sources containing nitrogen can produce nitrogen-doped graphene. The resulting graphene can be transferred to other surfaces, such as metal grids, for potential use in transparent touch screens for applications in personal electronics and large area photovoltaic devices. Because the transfer of graphene from one surface to another can lead to defects, low yields, and higher costs, we have developed methods for growing graphene <span class="hlt">directly</span> on the substrates of interest. We can also produce patterned graphene to make GNRs or graphane/graphene superlattices within a single <span class="hlt">sheet</span>. These superlattices could have multiple functions for use in sensors and other devices. This Account only touches upon this burgeoning area of materials chemistry, and the field will continue to expand as researchers imagine new forms and applications of graphene.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013NatGe...6..765C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013NatGe...6..765C"><span>Dynamic behaviour of the East Antarctic ice <span class="hlt">sheet</span> during Pliocene warmth</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cook, Carys P.; van de Flierdt, Tina; Williams, Trevor; Hemming, Sidney R.; Iwai, Masao; Kobayashi, Munemasa; Jimenez-Espejo, Francisco J.; Escutia, Carlota; González, Jhon Jairo; Khim, Boo-Keun; McKay, Robert M.; Passchier, Sandra; Bohaty, Steven M.; Riesselman, Christina R.; Tauxe, Lisa; Sugisaki, Saiko; Galindo, Alberto Lopez; Patterson, Molly O.; Sangiorgi, Francesca; Pierce, Elizabeth L.; Brinkhuis, Henk; Klaus, Adam; Fehr, Annick; Bendle, James A. P.; Bijl, Peter K.; Carr, Stephanie A.; Dunbar, Robert B.; Flores, José Abel; Hayden, Travis G.; Katsuki, Kota; Kong, Gee Soo; Nakai, Mutsumi; Olney, Matthew P.; Pekar, Stephen F.; Pross, Jörg; Röhl, Ursula; Sakai, Toyosaburo; Shrivastava, Prakash K.; Stickley, Catherine E.; Tuo, Shouting; Welsh, Kevin; Yamane, Masako</p> <p>2013-09-01</p> <p>Warm intervals within the Pliocene epoch (5.33-2.58 million years ago) were characterized by global temperatures comparable to those predicted for the end of this century and atmospheric CO2 concentrations similar to today. Estimates for global sea level highstands during these times imply possible retreat of the East Antarctic ice <span class="hlt">sheet</span>, but ice-proximal evidence from the Antarctic margin is scarce. Here we present new data from Pliocene marine sediments recovered offshore of Adélie Land, East Antarctica, that reveal dynamic behaviour of the East Antarctic ice <span class="hlt">sheet</span> in the vicinity of the low-lying Wilkes Subglacial Basin during times of past climatic warmth. Sedimentary sequences deposited between 5.3 and 3.3 million years ago indicate increases in Southern Ocean surface water productivity, associated with elevated circum-Antarctic temperatures. The geochemical provenance of detrital material deposited during these warm intervals suggests <span class="hlt">active</span> erosion of continental bedrock from within the Wilkes Subglacial Basin, an area today buried beneath the East Antarctic ice <span class="hlt">sheet</span>. We interpret this erosion to be associated with retreat of the ice <span class="hlt">sheet</span> margin several hundreds of kilometres inland and conclude that the East Antarctic ice <span class="hlt">sheet</span> was sensitive to climatic warmth during the Pliocene.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017MMTA...48.2483I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017MMTA...48.2483I"><span>Multilayer Mg-Stainless Steel <span class="hlt">Sheets</span>, Microstructure, and Mechanical Properties</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Inoue, Junya; Sadeghi, Alireza; Kyokuta, Nobuhiko; Ohmori, Toshinori; Koseki, Toshihiko</p> <p>2017-05-01</p> <p>Different multilayer Mg AZ31 and SS304L steel <span class="hlt">sheet</span> combinations were prepared with different volume fractions of Mg. Isolated stress-strain curves of the Mg layers showed significant improvements in the strength and elongation of multilayer samples. Results indicated that in the most extreme situation with the lowest Mg volume fraction ( V f = 0.39), the ultimate strength was increased by 25 pct to 370 MPa and the elongation was improved by 70 pct to 0.34. Investigation of the fracture surface showed that failure occurs by the coalescence of cracks close to the interface region. The improved strength of the multilayer samples was due to the combined effect of surface crack prevention by the steel layer and the higher work-hardening rate caused by the possible increased <span class="hlt">activity</span> of non-basal systems. It is suggested that the stronger work-hardening behavior and the enhanced <span class="hlt">activity</span> of non-basal systems in the multilayer samples were due to the formation of new stress components in the transverse <span class="hlt">direction</span>. The larger the volume fraction of steel in the multilayer, the longer the distance remaining unstrained before the UTS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28346207','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28346207"><span>Quality Control: (Material) Safety Data <span class="hlt">Sheets</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Allen, Loyd V</p> <p>2017-01-01</p> <p>Safety Data <span class="hlt">Sheets</span> (formerly Material Safety Data <span class="hlt">Sheets</span>) are a system for cataloging information on chemicals, chemical compounds, and chemical mixtures and include instructions for the safe use and potential hazards associated with a particular material or product. At present, there are 16 sections of Safety Data <span class="hlt">Sheets</span>, and these sections are discussed in this article. Two United States Pharmacopeia compounding-related chapters (<795> and <800>) refer to Safety Data <span class="hlt">Sheets</span>, and this article provides a brief discussion on the terminology contained within those chapters. Copyright© by International Journal of Pharmaceutical Compounding, Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930081763','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930081763"><span>Effect of Brake Forming on the Strength of 24S-T Aluminum-alloy <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Heimerl, George J; Woods, Walter</p> <p>1946-01-01</p> <p>Tests were made to determine the effect of brake forming on the strength of 24S-T aluminum alloy <span class="hlt">sheet</span> that had been formed to an inside bend radius of three times the <span class="hlt">sheet</span> thickness. The results for both <span class="hlt">directions</span> of the grain of the material showed that the compressive yield stresses were appreciably increased, that the tensile yield stresses were moderately increased, that the ultimate tensile stresses were only slightly increased, that the elongations were considerably reduced, and that the shapes of the tensile and compressive stress-strain curves were markedly changed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AIPA....8e5023C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AIPA....8e5023C"><span>Research on Al-alloy <span class="hlt">sheet</span> forming formability during warm/hot <span class="hlt">sheet</span> hydroforming based on elliptical warm bulging test</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cai, Gaoshen; Wu, Chuanyu; Gao, Zepu; Lang, Lihui; Alexandrov, Sergei</p> <p>2018-05-01</p> <p>An elliptical warm/hot <span class="hlt">sheet</span> bulging test under different temperatures and pressure rates was carried out to predict Al-alloy <span class="hlt">sheet</span> forming limit during warm/hot <span class="hlt">sheet</span> hydroforming. Using relevant formulas of ultimate strain to calculate and dispose experimental data, forming limit curves (FLCS) in tension-tension state of strain (TTSS) area are obtained. Combining with the basic experimental data obtained by uniaxial tensile test under the equivalent condition with bulging test, complete forming limit diagrams (FLDS) of Al-alloy are established. Using a quadratic polynomial curve fitting method, material constants of fitting function are calculated and a prediction model equation for <span class="hlt">sheet</span> metal forming limit is established, by which the corresponding forming limit curves in TTSS area can be obtained. The bulging test and fitting results indicated that the <span class="hlt">sheet</span> metal FLCS obtained were very accurate. Also, the model equation can be used to instruct warm/hot <span class="hlt">sheet</span> bulging test.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19890015906','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19890015906"><span>Scaling results for the Liquid <span class="hlt">Sheet</span> Radiator (LSR)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chubb, Donald L.; Calfo, Frederick D.</p> <p>1989-01-01</p> <p>Surface tension forces at the edges of a thin liquid (approx. 100 micrometers) <span class="hlt">sheet</span> flow result in a triangularly shaped <span class="hlt">sheet</span>. Such a geometry is ideal for an external flow radiator. The experimental investigation of such <span class="hlt">sheet</span> flows was extended to large <span class="hlt">sheets</span> (width = W = 23.5 cm, length = L approx. = 3.5 m). Experimental L/W results are greater than the calculated results. However, more experimental results are necessary for a complete comparison. The calculated emissivity of a <span class="hlt">sheet</span> of Dow-Corning 705 silicone oil, which is a low temperature (300 to 400K) candidate for a liquid <span class="hlt">sheet</span> radiator (LSR), is greater than .8 for <span class="hlt">sheet</span> thicknesses greater than 100 micrometers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19720022272','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19720022272"><span>A preliminary investigation of projectile shape effects in hypervelocity impact of a double-<span class="hlt">sheet</span> structure</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Morrison, R. H.</p> <p>1972-01-01</p> <p>Impact tests of a sphere and several cylinders of various masses and fineness ratios, all of aluminum, fired into an aluminum double-<span class="hlt">sheet</span> structure at velocities near 7 km/sec, show that a cylinder, impacting in the <span class="hlt">direction</span> of its axis, is considerably more effective as a penetrator than a sphere. Impacts of three cylinders of equal mass, but different fineness ratios, produced holes through the structures' rear <span class="hlt">sheet</span>, whereas impact of a sphere of the same mass did not. Moreover, it was found that to prevent rear-<span class="hlt">sheet</span> penetration, the mass of the 1/2-fineness-ratio cylinder had to be reduced by a factor greater than three. Further tests wherein the cylinder diameter was held constant while the cylinder length was systematically reduced showed that a cylinder with a fineness ratio of 0.07 and a mass of only 1/7 that of the sphere was still capable of producing a hole in the rear <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.C21D..08R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.C21D..08R"><span>Extensive massive basal-ice structures in West Antarctica relate to ice-<span class="hlt">sheet</span> anisotropy and ice-flow</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ross, N.; Bingham, R. G.; Corr, H. F. J.; Siegert, M. J.</p> <p>2016-12-01</p> <p>Complex structures identified within both the East Antarctic and Greenland ice <span class="hlt">sheets</span> are thought to be generated by the action of basal water freezing to the ice-<span class="hlt">sheet</span> base, evolving under ice flow. Here, we use ice-penetrating radar to image an extensive series of similarly complex basal ice facies in West Antarctica, revealing a thick (>500 m) tectonised unit in an area of cold-based and relatively slow-flowing ice. We show that major folding and overturning of the unit perpendicular to ice flow elevates deep, warm ice into the mid ice-<span class="hlt">sheet</span> column. Fold axes align with present ice flow, and axis amplitudes increase down-ice, suggesting long-term consistency in the <span class="hlt">direction</span> and convergence of flow. In the absence of basal water, and the draping of the tectonised unit over major subglacial mountain ranges, the formation of the unit must be solely through the deformation of meteoric ice. Internal layer radar reflectivity is consistently greater parallel to flow compared with the perpendicular <span class="hlt">direction</span>, revealing ice-<span class="hlt">sheet</span> crystal anisotropy is associated with the folding. By linking layers to the Byrd ice-core site, we show the basal ice dates to at least the last glacial cycle and may be as old as the last interglacial. Deformation of deep-ice in this sector of WAIS, and potentially elsewhere in Antarctica, may be caused by differential shearing at interglacial-glacial boundaries, in a process analogous to that proposed for interior Greenland. The scale and heterogeneity of the englacial structures, and their subsequent impact on ice <span class="hlt">sheet</span> rheology, means that the nature of ice flow across the bulk of West Antarctica must be far more complex that is currently accounted for by any numerical ice <span class="hlt">sheet</span> model.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_19 --> <div id="page_20" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="381"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27127499','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27127499"><span>Development of a Prediction Model Based on RBF Neural Network for <span class="hlt">Sheet</span> Metal Fixture Locating Layout Design and Optimization.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Zhongqi; Yang, Bo; Kang, Yonggang; Yang, Yuan</p> <p>2016-01-01</p> <p>Fixture plays an important part in constraining excessive <span class="hlt">sheet</span> metal part deformation at machining, assembly, and measuring stages during the whole manufacturing process. However, it is still a difficult and nontrivial task to design and optimize <span class="hlt">sheet</span> metal fixture locating layout at present because there is always no <span class="hlt">direct</span> and explicit expression describing <span class="hlt">sheet</span> metal fixture locating layout and responding deformation. To that end, an RBF neural network prediction model is proposed in this paper to assist design and optimization of <span class="hlt">sheet</span> metal fixture locating layout. The RBF neural network model is constructed by training data set selected by uniform sampling and finite element simulation analysis. Finally, a case study is conducted to verify the proposed method.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4834399','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4834399"><span>Development of a Prediction Model Based on RBF Neural Network for <span class="hlt">Sheet</span> Metal Fixture Locating Layout Design and Optimization</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Wang, Zhongqi; Yang, Bo; Kang, Yonggang; Yang, Yuan</p> <p>2016-01-01</p> <p>Fixture plays an important part in constraining excessive <span class="hlt">sheet</span> metal part deformation at machining, assembly, and measuring stages during the whole manufacturing process. However, it is still a difficult and nontrivial task to design and optimize <span class="hlt">sheet</span> metal fixture locating layout at present because there is always no <span class="hlt">direct</span> and explicit expression describing <span class="hlt">sheet</span> metal fixture locating layout and responding deformation. To that end, an RBF neural network prediction model is proposed in this paper to assist design and optimization of <span class="hlt">sheet</span> metal fixture locating layout. The RBF neural network model is constructed by training data set selected by uniform sampling and finite element simulation analysis. Finally, a case study is conducted to verify the proposed method. PMID:27127499</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016GeoRL..43.9173M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016GeoRL..43.9173M"><span>High export of dissolved silica from the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Meire, L.; Meire, P.; Struyf, E.; Krawczyk, D. W.; Arendt, K. E.; Yde, J. C.; Juul Pedersen, T.; Hopwood, M. J.; Rysgaard, S.; Meysman, F. J. R.</p> <p>2016-09-01</p> <p>Silica is an essential element for marine life and plays a key role in the biogeochemistry of the ocean. Glacial <span class="hlt">activity</span> stimulates rock weathering, generating dissolved silica that is exported to coastal areas along with meltwater. The magnitude of the dissolved silica export from large glacial areas such as the Greenland Ice <span class="hlt">Sheet</span> is presently poorly quantified and not accounted for in global budgets. Here we present data from two fjord systems adjacent to the Greenland Ice <span class="hlt">Sheet</span> which reveal a large export of dissolved silica by glacial meltwater relative to other macronutrients. Upscaled to the entire Greenland Ice <span class="hlt">Sheet</span>, the export of dissolved silica equals 22 ± 10 Gmol Si yr-1. When the silicate-rich meltwater mixes with upwelled deep water, either inside or outside Greenland's fjords, primary production takes place at increased silicate to nitrate ratios. This likely stimulates the growth of diatoms relative to other phytoplankton groups.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/871928','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/871928"><span>Method for heating, forming and tempering a glass <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Boaz, Premakaran Tucker; Sitzman, Gary W.</p> <p>1998-01-01</p> <p>A method for heating, forming and tempering a glass <span class="hlt">sheet</span> including the steps of heating at least one glass <span class="hlt">sheet</span> to at least a first predetermined temperature, applying microwave energy to the glass <span class="hlt">sheet</span> to heat the glass <span class="hlt">sheet</span> to at least a second predetermined temperature, forming the glass <span class="hlt">sheet</span> to a predetermined configuration, and cooling an outer surface of the glass <span class="hlt">sheet</span> to at least a third predetermined temperature to temper the glass <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3215074','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3215074"><span>Prototypical model for tensional wrinkling in thin <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Davidovitch, Benny; Schroll, Robert D.; Vella, Dominic; Adda-Bedia, Mokhtar; Cerda, Enrique A.</p> <p>2011-01-01</p> <p>The buckling and wrinkling of thin films has recently seen a surge of interest among physicists, biologists, mathematicians, and engineers. This <span class="hlt">activity</span> has been triggered by the growing interest in developing technologies at ever-decreasing scales and the resulting necessity to control the mechanics of tiny structures, as well as by the realization that morphogenetic processes, such as the tissue-shaping instabilities occurring in animal epithelia or plant leaves, often emerge from mechanical instabilities of cell <span class="hlt">sheets</span>. Although the most basic buckling instability of uniaxially compressed plates was understood by Euler more than two centuries ago, recent experiments on nanometrically thin (ultrathin) films have shown significant deviations from predictions of standard buckling theory. Motivated by this puzzle, we introduce here a theoretical model that allows for a systematic analysis of wrinkling in <span class="hlt">sheets</span> far from their instability threshold. We focus on the simplest extension of Euler buckling that exhibits wrinkles of finite length—a <span class="hlt">sheet</span> under axisymmetric tensile loads. The first study of this geometry, which is attributed to Lamé, allows us to construct a phase diagram that demonstrates the dramatic variation of wrinkling patterns from near-threshold to far-from-threshold conditions. Theoretical arguments and comparison to experiments show that the thinner the <span class="hlt">sheet</span> is, the smaller is the compressive load above which the far-from-threshold regime emerges. This observation emphasizes the relevance of our analysis for nanomechanics applications. PMID:22042841</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1999Natur.402...63K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1999Natur.402...63K"><span>Frozen-bed Fennoscandian and Laurentide ice <span class="hlt">sheets</span> during the Last Glacial Maximum</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kleman, Johan; Hättestrand, Clas</p> <p>1999-11-01</p> <p>The areal extents of the Laurentide and Fennoscandian ice <span class="hlt">sheets</span> during the Last Glacial Maximum (about 20,000 years ago) are well known, but thickness estimates range widely, from high-domed to thin, with large implications for our reconstruction of the climate system regarding, for example, Northern Hemisphere atmospheric circulation and global sea levels. This uncertainty stems from difficulties in determining the basal temperatures of the ice <span class="hlt">sheets</span> and the shear strength of subglacial materials, a knowledge of which would better constrain reconstructions of ice-<span class="hlt">sheet</span> thickness. Here we show that, in the absence of <span class="hlt">direct</span> data, the occurrence of ribbed moraines in modern landscapes can be used to determine the former spatial distribution of frozen- and thawed-bed conditions. We argue that ribbed moraines were formed by brittle fracture of subglacial sediments, induced by the excessive stress at the boundary between frozen- and thawed-bed conditions resulting from the across-boundary difference in basal ice velocity. Maps of glacial landforms from aerial photographs of Canada and Scandinavia reveal a concentration of ribbed moraines around the ice-<span class="hlt">sheet</span> retreat centres of Quebec, Keewatin, Newfoundland and west-central Fennoscandia. Together with the evidence from relict landscapes that mark glacial areas with frozen-bed conditions, the distribution of ribbed moraines on both continents suggest that a large area of the Laurentide and Fennoscandian ice <span class="hlt">sheets</span> was frozen-based-and therefore high-domed and stable-during the Last Glacial Maximum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/675851','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/675851"><span>Method for heating, forming and tempering a glass <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Boaz, P.T.; Sitzman, G.W.</p> <p>1998-10-27</p> <p>A method for heating, forming and tempering a glass <span class="hlt">sheet</span> is disclosed including the steps of heating at least one glass <span class="hlt">sheet</span> to at least a first predetermined temperature, applying microwave energy to the glass <span class="hlt">sheet</span> to heat the glass <span class="hlt">sheet</span> to at least a second predetermined temperature, forming the glass <span class="hlt">sheet</span> to a predetermined configuration, and cooling an outer surface of the glass <span class="hlt">sheet</span> to at least a third predetermined temperature to temper the glass <span class="hlt">sheet</span>. 2 figs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1999MMTB...30..119M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1999MMTB...30..119M"><span>A mathematical model of the heat and fluid flows in <span class="hlt">direct</span>-chill casting of aluminum <span class="hlt">sheet</span> ingots and billets</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mortensen, Dag</p> <p>1999-02-01</p> <p>A finite-element method model for the time-dependent heat and fluid flows that develop during <span class="hlt">direct</span>-chill (DC) semicontinuous casting of aluminium ingots is presented. Thermal convection and turbulence are included in the model formulation and, in the mushy zone, the momentum equations are modified with a Darcy-type source term dependent on the liquid fraction. The boundary conditions involve calculations of the air gap along the mold wall as well as the heat transfer to the falling water film with forced convection, nucleate boiling, and film boiling. The mold wall and the starting block are included in the computational domain. In the start-up period of the casting, the ingot domain expands over the starting-block level. The numerical method applies a fractional-step method for the dynamic Navier-Stokes equations and the “streamline upwind Petrov-Galerkin” (SUPG) method for mixed diffusion and convection in the momentum and energy equations. The modeling of the start-up period of the casting is demonstrated and compared to temperature measurements in an AA1050 200×600 mm <span class="hlt">sheet</span> ingot.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatCh...8..563F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatCh...8..563F"><span>Experimental realization of two-dimensional boron <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Feng, Baojie; Zhang, Jin; Zhong, Qing; Li, Wenbin; Li, Shuai; Li, Hui; Cheng, Peng; Meng, Sheng; Chen, Lan; Wu, Kehui</p> <p>2016-06-01</p> <p>A variety of two-dimensional materials have been reported in recent years, yet single-element systems such as graphene and black phosphorus have remained rare. Boron analogues have been predicted, as boron atoms possess a short covalent radius and the flexibility to adopt sp2 hybridization, features that favour the formation of two-dimensional allotropes, and one example of such a borophene material has been reported recently. Here, we present a parallel experimental work showing that two-dimensional boron <span class="hlt">sheets</span> can be grown epitaxially on a Ag(111) substrate. Two types of boron <span class="hlt">sheet</span>, a β12 <span class="hlt">sheet</span> and a χ3 <span class="hlt">sheet</span>, both exhibiting a triangular lattice but with different arrangements of periodic holes, are observed by scanning tunnelling microscopy. Density functional theory simulations agree well with experiments, and indicate that both <span class="hlt">sheets</span> are planar without obvious vertical undulations. The boron <span class="hlt">sheets</span> are quite inert to oxidization and interact only weakly with their substrate. We envisage that such boron <span class="hlt">sheets</span> may find applications in electronic devices in the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JCoPh.339..126M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JCoPh.339..126M"><span>Dipole excitation of surface plasmon on a conducting <span class="hlt">sheet</span>: Finite element approximation and validation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Maier, Matthias; Margetis, Dionisios; Luskin, Mitchell</p> <p>2017-06-01</p> <p>We formulate and validate a finite element approach to the propagation of a slowly decaying electromagnetic wave, called surface plasmon-polariton, excited along a conducting <span class="hlt">sheet</span>, e.g., a single-layer graphene <span class="hlt">sheet</span>, by an electric Hertzian dipole. By using a suitably rescaled form of time-harmonic Maxwell's equations, we derive a variational formulation that enables a <span class="hlt">direct</span> numerical treatment of the associated class of boundary value problems by appropriate curl-conforming finite elements. The conducting <span class="hlt">sheet</span> is modeled as an idealized hypersurface with an effective electric conductivity. The requisite weak discontinuity for the tangential magnetic field across the hypersurface can be incorporated naturally into the variational formulation. We carry out numerical simulations for an infinite <span class="hlt">sheet</span> with constant isotropic conductivity embedded in two spatial dimensions; and validate our numerics against the closed-form exact solution obtained by the Fourier transform in the tangential coordinate. Numerical aspects of our treatment such as an absorbing perfectly matched layer, as well as local refinement and a posteriori error control are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20859726','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20859726"><span>Experience of silicone gel <span class="hlt">sheets</span> for patients with keloid scars after median sternotomy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sakuraba, Motoki; Takahashi, Nobumasa; Akahoshi, Taku; Miyasaka, Yoshikazu; Suzuki, Kenji</p> <p>2010-09-01</p> <p>It is often difficult to control hypertrophic scars and keloids with drug therapy, steroid injection, surgery, radiation therapy, laser, or wound pressing. Use of silicone gel to treat hypertrophic burn scars and fresh incisions has yielded encouraging results. We report our experience of silicone gel <span class="hlt">sheets</span> for patients with keloids following median sternotomy. Nine patients underwent a median sternotomy and received other therapies before participating in this treatment. A silicone gel <span class="hlt">sheet</span> was placed <span class="hlt">directly</span> on the keloid scar and maintained at all times. <span class="hlt">Sheets</span> were replaced every 4 weeks for a total treatment duration of 24 weeks. The scar area was measured, and subjective symptoms were determined prior to therapy and after completion of therapy. There were three men and six women, with a mean age of 45.2 years (range 22-69 years). Progression of protuberance and rub was seen in one patient. Scar redness and cramping were either diminished or unchanged in all patients. Itching progressed in two patients. After 6 months, the area of the scar relative to its initial area was 0.98 (range 0.78-1.27). Harmful events did not occur. A silicone gel <span class="hlt">sheet</span> is effective for treating keloid scars following median sternotomy. Silicone gel <span class="hlt">sheets</span> are safe and easy to use and do not aggravate any subjective symptoms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/10133199','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/10133199"><span>Energy information <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Not Available</p> <p>1993-12-02</p> <p>The National Energy Information Center (NEIC), as part of its mission, provides energy information and referral assistance to Federal, State, and local governments, the academic community, business and industrial organizations, and the general public. Written for the general public, the EIA publication Energy Information <span class="hlt">Sheets</span> was developed to provide information on various aspects of fuel production, prices, consumption and capability. The information contained herein pertains to energy data as of December 1991. Additional information on related subject matter can be found in other EIA publications as referenced at the end of each <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19860000292&hterms=TIG&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DTIG','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19860000292&hterms=TIG&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DTIG"><span>Weld Repair of Thin Aluminum <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Beuyukian, C. S.; Mitchell, M. J.</p> <p>1986-01-01</p> <p>Weld repairing of thin aluminum <span class="hlt">sheets</span> now possible, using niobium shield and copper heat sinks. Refractory niobium shield protects aluminum adjacent to hole, while copper heat sinks help conduct heat away from repair site. Technique limits tungsten/inert-gas (TIG) welding bombardment zone to melt area, leaving surrounding areas around weld unaffected. Used successfully to repair aluminum cold plates on Space Shuttle, Commercial applications, especially in sealing fractures, dents, and holes in thin aluminum face <span class="hlt">sheets</span> or clad brazing <span class="hlt">sheet</span> in cold plates, heat exchangers, coolers, and Solar panels. While particularly suited to thin aluminum <span class="hlt">sheet</span>, this process also used in thicker aluminum material to prevent surface damage near weld area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22410427-instability-current-sheets-localized-accumulation-magnetic-flux','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22410427-instability-current-sheets-localized-accumulation-magnetic-flux"><span>Instability of current <span class="hlt">sheets</span> with a localized accumulation of magnetic flux</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Pritchett, P. L.</p> <p>2015-06-15</p> <p>The longstanding problem of whether a current <span class="hlt">sheet</span> with curved magnetic field lines associated with a small “normal” B{sub z} component is stable is investigated using two-dimensional electromagnetic particle-in-cell simulations, employing closed boundary conditions analogous to those normally assumed in energy principle calculations. Energy principle arguments [Sitnov and Schindler, Geophys. Res. Lett. 37, L08102 (2010)] have suggested that an accumulation of magnetic flux at the tailward end of a thin current <span class="hlt">sheet</span> could produce a tearing instability. Two classes of such current <span class="hlt">sheet</span> configurations are probed: one with a monotonically increasing B{sub z} profile and the other with a localizedmore » B{sub z} “hump.” The former is found to be stable (in 2D) over any reasonable time scale, while the latter is prone to an ideal-like instability that shifts the hump peak in the <span class="hlt">direction</span> of the curvature normal and erodes the field on the opposite side. The growth rate of this instability is smaller by an order of magnitude than previous suggestions of an instability in an open system. An example is given that suggests that such an unstable hump configuration is unlikely to be produced by external driving of a current <span class="hlt">sheet</span> with no B{sub z} accumulation even in the presence of open boundary conditions.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AIPC.1383..927X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AIPC.1383..927X"><span>Robust Design of <span class="hlt">Sheet</span> Metal Forming Process Based on Kriging Metamodel</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xie, Yanmin</p> <p>2011-08-01</p> <p>Nowadays, <span class="hlt">sheet</span> metal forming processes design is not a trivial task due to the complex issues to be taken into account (conflicting design goals, complex shapes forming and so on). Optimization methods have also been widely applied in <span class="hlt">sheet</span> metal forming. Therefore, proper design methods to reduce time and costs have to be developed mostly based on computer aided procedures. At the same time, the existence of variations during manufacturing processes significantly may influence final product quality, rendering non-robust optimal solutions. In this paper, a small size of design of experiments is conducted to investigate how a stochastic behavior of noise factors affects drawing quality. The finite element software (LS_DYNA) is used to simulate the complex <span class="hlt">sheet</span> metal stamping processes. The Kriging metamodel is adopted to map the relation between input process parameters and part quality. Robust design models for <span class="hlt">sheet</span> metal forming process integrate adaptive importance sampling with Kriging model, in order to minimize impact of the variations and achieve reliable process parameters. In the adaptive sample, an improved criterion is used to provide <span class="hlt">direction</span> in which additional training samples can be added to better the Kriging model. Nonlinear functions as test functions and a square stamping example (NUMISHEET'93) are employed to verify the proposed method. Final results indicate application feasibility of the aforesaid method proposed for multi-response robust design.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013APS..DFD.G9010P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013APS..DFD.G9010P"><span>Experimental investigation of the stability of a moving radial liquid <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paramati, Manjula; Tirumkudulu, Mahesh</p> <p>2013-11-01</p> <p>Experiments were conducted to understand the stability of moving radial liquid <span class="hlt">sheets</span> formed by the head-on impingement of two co-linear water jets using laser induced fluorescence technique (LIF). Acoustic sinusoidal fluctuations were introduced at the jet impingement point and we measured the displacement of the center line of the liquid <span class="hlt">sheet</span> (sinuous mode) and the thickness variation (varicose mode) of the disturbed liquid <span class="hlt">sheet</span>. Our experiments show that the sinuous disturbances grow as they are convected outward in the radial <span class="hlt">direction</span> even in the smooth regime (We < 800). In the absence of the acoustic forcing, the measured thickness has the expected 1/r dependence. Interestingly, we were unable to detect any thickness variation about the pre-stimulus values in the presence of acoustic forcing suggesting that the variation in the thickness is lower than the resolution of the technique (+/- 1 μm). The growth rates of the sinuous mode determined from the wave envelope matches with the prediction of a recent theory by Tirumkudulu and Paramati (Communicated to Phys. Of Fluids, 2013) which accounts for the inertia of the liquid phase and the surface tension force in a radial liquid <span class="hlt">sheet</span> while neglecting the inertial effects due to the surrounding gas phase. The authors acknowledge the financial assistance from Indo-French Center for Pro- motion of Advanced Research and also Indian institute of technology Bombay.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AIPC.1896s0019P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AIPC.1896s0019P"><span>Properties of hot-rolled <span class="hlt">sheets</span> from ferritic steel with increased strength</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Perlovich, Yu.; Isaenkova, M.; Dobrokhotov, P.; Stolbov, S.; Bannykh, O.; Bannykh, I.; Antsyferova, M.</p> <p>2017-10-01</p> <p><span class="hlt">Sheets</span> from ferritic steel 3 mm thick with increased strength after thermal hardening were studied by use of various X-ray methods and mechanical testing. Rolling of steel was carried out at 1100°C with rather great reductions per pass, so that plastic deformation of metal spread by the significant distance from the surface. The texture of <span class="hlt">sheet</span> proved to have two sharply different layers: the inner layer of ˜40% thick with the usual rolling texture of BCC metals and the external layer with the rolling texture of FCC metals. At that, within the intermediate layer the texture is weakened. Texture formation within the external layer is conditioned by the process of dynamical deformation ageing: interstitial impurities from atmosphere block dislocations, prevent from their slip and at increased temperatures promote their collective climb. As a result, the <span class="hlt">direction</span> of lattice rotation as well as the final rolling texture change. Due to texture layering, by impact testing of the <span class="hlt">sheet</span> the plane of crack propagation must be changed when this crack reaches the inner layer, and then an additional energy for its further movement is required. Thermal hardening of the <span class="hlt">sheet</span> retains the type of rolling texture, though results in some its scattering, but at the same time the breaking point of steel grows twice owing to formation of intermetallic particles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17675353','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17675353"><span>Modeling the Alzheimer Abeta17-42 fibril architecture: tight intermolecular <span class="hlt">sheet-sheet</span> association and intramolecular hydrated cavities.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zheng, Jie; Jang, Hyunbum; Ma, Buyong; Tsai, Chung-Jun; Nussinov, Ruth</p> <p>2007-11-01</p> <p>We investigate Abeta(17-42) protofibril structures in solution using molecular dynamics simulations. Recently, NMR and computations modeled the Abeta protofibril as a longitudinal stack of U-shaped molecules, creating an in-parallel beta-<span class="hlt">sheet</span> and loop spine. Here we study the molecular architecture of the fibril formed by spine-spine association. We model in-register intermolecular beta-<span class="hlt">sheet-beta-sheet</span> associations and study the consequences of Alzheimer's mutations (E22G, E22Q, E22K, and M35A) on the organization. We assess the structural stability and association force of Abeta oligomers with different <span class="hlt">sheet-sheet</span> interfaces. Double-layered oligomers associating through the C-terminal-C-terminal interface are energetically more favorable than those with the N-terminal-N-terminal interface, although both interfaces exhibit high structural stability. The C-terminal-C-terminal interface is essentially stabilized by hydrophobic and van der Waals (shape complementarity via M35-M35 contacts) intermolecular interactions, whereas the N-terminal-N-terminal interface is stabilized by hydrophobic and electrostatic interactions. Hence, shape complementarity, or the "steric zipper" motif plays an important role in amyloid formation. On the other hand, the intramolecular Abeta beta-strand-loop-beta-strand U-shaped motif creates a hydrophobic cavity with a diameter of 6-7 A, allowing water molecules and ions to conduct through. The hydrated hydrophobic cavities may allow optimization of the <span class="hlt">sheet</span> association and constitute a typical feature of fibrils, in addition to the tight <span class="hlt">sheet-sheet</span> association. Thus, we propose that Abeta fiber architecture consists of alternating layers of tight packing and hydrated cavities running along the fibrillar axis, which might be possibly detected by high-resolution imaging.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19770005570','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19770005570"><span>Dip coating process: Silicon <span class="hlt">sheet</span> growth development for the large-area silicon <span class="hlt">sheet</span> task of the low-cost silicon solar array project</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Heaps, J. D.; Maciolek, R. B.; Zook, J. D.; Harrison, W. B.; Scott, M. W.; Hendrickson, G.; Wolner, H. A.; Nelson, L. D.; Schuller, T. L.; Peterson, A. A.</p> <p>1976-01-01</p> <p>The technical and economic feasibility of producing solar cell quality <span class="hlt">sheet</span> silicon by dip-coating one surface of carbonized ceramic substrates with a thin layer of large grain polycrystalline silicon was investigated. The dip-coating methods studied were <span class="hlt">directed</span> toward a minimum cost process with the ultimate objective of producing solar cells with a conversion efficiency of 10% or greater. The technique shows excellent promise for low cost, labor-saving, scale-up potentialities and would provide an end product of <span class="hlt">sheet</span> silicon with a rigid and strong supportive backing. An experimental dip-coating facility was designed and constructed, several substrates were successfully dip-coated with areas as large as 25 sq cm and thicknesses of 12 micron to 250 micron. There appears to be no serious limitation on the area of a substrate that could be coated. Of the various substrate materials dip-coated, mullite appears to best satisfy the requirement of the program. An inexpensive process was developed for producing mullite in the desired geometry.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20561676','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20561676"><span>Preparation of Caco-2 cell <span class="hlt">sheets</span> using plasma polymerised acrylic acid as a weak boundary layer.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Majani, Ruby; Zelzer, Mischa; Gadegaard, Nikolaj; Rose, Felicity R; Alexander, Morgan R</p> <p>2010-09-01</p> <p>The use of cell <span class="hlt">sheets</span> for tissue engineering applications has considerable advantages over single cell seeding techniques. So far, only thermoresponsive surfaces have been used to manufacture cell <span class="hlt">sheets</span> without chemically disrupting the cell-surface interactions. Here, we present a new and facile technique to prepare <span class="hlt">sheets</span> of epithelial cells using plasma polymerised acrylic acid films. The cell <span class="hlt">sheets</span> are harvested by gentle agitation of the media without the need of any additional external stimulus. We demonstrate that the plasma polymer deposition conditions affect the viability and metabolic <span class="hlt">activity</span> of the cells in the <span class="hlt">sheet</span> and relate these effects to the different surface properties of the plasma polymerised acrylic acid films. Based on surface analysis data, a first attempt is made to explain the mechanism behind the cell <span class="hlt">sheet</span> formation. The advantage of the epithelial cell <span class="hlt">sheets</span> generated here over single cell suspensions to seed a PLGA scaffold is presented. The scaffold itself, prepared using a mould fabricated via photolithography, exhibits a unique architecture that mimics closely the dimensions of the native tissue (mouse intestine). Copyright 2010 Elsevier Ltd. All rights reserved.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_20 --> <div id="page_21" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="401"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4431294','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4431294"><span>Detection of Steel Fatigue Cracks with Strain Sensing <span class="hlt">Sheets</span> Based on Large Area Electronics</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Yao, Yao; Glisic, Branko</p> <p>2015-01-01</p> <p>Reliable early-stage damage detection requires continuous monitoring over large areas of structure, and with sensors of high spatial resolution. Technologies based on Large Area Electronics (LAE) can enable <span class="hlt">direct</span> sensing and can be scaled to the level required for Structural Health Monitoring (SHM) of civil structures and infrastructure. Sensing <span class="hlt">sheets</span> based on LAE contain dense arrangements of thin-film strain sensors, associated electronics and various control circuits deposited and integrated on a flexible polyimide substrate that can cover large areas of structures. This paper presents the development stage of a prototype strain sensing <span class="hlt">sheet</span> based on LAE for crack detection and localization. Two types of sensing-<span class="hlt">sheet</span> arrangements with size 6 × 6 inch (152 × 152 mm) were designed and manufactured, one with a very dense arrangement of sensors and the other with a less dense arrangement of sensors. The sensing <span class="hlt">sheets</span> were bonded to steel plates, which had a notch on the boundary, so the fatigue cracks could be generated under cyclic loading. The sensors within the sensing <span class="hlt">sheet</span> that were close to the notch tip successfully detected the initialization of fatigue crack and localized the damage on the plate. The sensors that were away from the crack successfully detected the propagation of fatigue cracks based on the time history of the measured strain. The results of the tests have validated the general principles of the proposed sensing <span class="hlt">sheets</span> for crack detection and identified advantages and challenges of the two tested designs. PMID:25853407</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/871855','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/871855"><span>Microcomponent chemical process <span class="hlt">sheet</span> architecture</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Wegeng, Robert S.; Drost, M. Kevin; Call, Charles J.; Birmingham, Joseph G.; McDonald, Carolyn Evans; Kurath, Dean E.; Friedrich, Michele</p> <p>1998-01-01</p> <p>The invention is a microcomponent <span class="hlt">sheet</span> architecture wherein macroscale unit processes are performed by microscale components. The <span class="hlt">sheet</span> architecture may be a single laminate with a plurality of separate microcomponent sections or the <span class="hlt">sheet</span> architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one chemical process unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED495209.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED495209.pdf"><span>Participation in Sports and Civic Engagement. Fact <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Lopez, Mark Hugo; Moore, Kimberlee</p> <p>2006-01-01</p> <p>One reason to offer sports in school is to teach youth the values, skills, and habits that will make them more <span class="hlt">active</span>, engaged, and responsible citizens. Past evidence on the civic effects of sports is mixed, but points to some potential positive civic effects. This fact <span class="hlt">sheet</span> uses recent data from the 2002 National Youth Survey of Civic…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28537320','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28537320"><span>Understanding the adsorptive interactions of arsenate-iron nanoparticles with curved fullerene-like <span class="hlt">sheets</span> in <span class="hlt">activated</span> carbon using a quantum mechanics/molecular mechanics computational approach.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ha, Nguyen Ngoc; Cam, Le Minh; Ha, Nguyen Thi Thu; Goh, Bee-Min; Saunders, Martin; Jiang, Zhong-Tao; Altarawneh, Mohammednoor; Dlugogorski, Bogdan Z; El-Harbawi, Mohanad; Yin, Chun-Yang</p> <p>2017-06-07</p> <p>The prevalence of global arsenic groundwater contamination has driven widespread research on developing effective treatment systems including adsorption using various sorbents. The uptake of arsenic-based contaminants onto established sorbents such as <span class="hlt">activated</span> carbon (AC) can be effectively enhanced via immobilization/impregnation of iron-based elements on the porous AC surface. Recent suggestions that AC pores structurally consist of an eclectic mix of curved fullerene-like <span class="hlt">sheets</span> may affect the arsenic adsorption dynamics within the AC pores and is further complicated by the presence of nano-sized iron-based elements. We have therefore, attempted to shed light on the adsorptive interactions of arsenate-iron nanoparticles with curved fullerene-like <span class="hlt">sheets</span> by using hybridized quantum mechanics/molecular mechanics (QMMM) calculations and microscopy characterization. It is found that, subsequent to optimization, chemisorption between HAsO 4 2- and the AC carbon <span class="hlt">sheet</span> (endothermic process) is virtually non-existent - this observation is supported by experimental results. Conversely, the incorporation of iron nanoparticles (FeNPs) into the AC carbon <span class="hlt">sheet</span> greatly facilitates chemisorption of HAsO 4 2- . Our calculation implies that iron carbide is formed at the junction between the iron and the AC interface and this tightly chemosorbed layer prevents detachment of the FeNPs on the AC surface. Other aspects including electronic structure/properties, carbon arrangement defects and rate of adsorptive interaction, which are determined using the Climbing-Image NEB method, are also discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28164191','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28164191"><span>Particulate photocatalyst <span class="hlt">sheets</span> for Z-scheme water splitting: advantages over powder suspension and photoelectrochemical systems and future challenges.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Qian; Hisatomi, Takashi; Katayama, Masao; Takata, Tsuyoshi; Minegishi, Tsutomu; Kudo, Akihiko; Yamada, Taro; Domen, Kazunari</p> <p>2017-04-28</p> <p>Water splitting using semiconductor photocatalysts has been attracting growing interest as a means of solar energy based conversion of water to hydrogen, a clean and renewable fuel. Z-scheme photocatalytic water splitting based on the two-step excitation of an oxygen evolution photocatalyst (OEP) and a hydrogen evolution photocatalyst (HEP) is a promising approach toward the utilisation of visible light. In particular, a photocatalyst <span class="hlt">sheet</span> system consisting of HEP and OEP particles embedded in a conductive layer has been recently proposed as a new means of obtaining efficient and scalable redox mediator-free Z-scheme solar water splitting. In this paper, we discuss the advantages and disadvantages of the photocatalyst <span class="hlt">sheet</span> approach compared to conventional photocatalyst powder suspension and photoelectrochemical systems through an examination of the water splitting <span class="hlt">activity</span> of Z-scheme systems based on SrTiO 3 :La,Rh as the HEP and BiVO 4 :Mo as the OEP. This photocatalyst <span class="hlt">sheet</span> was found to split pure water much more efficiently than the powder suspension and photoelectrochemical systems, because the underlying metal layer efficiently transfers electrons from the OEP to the HEP. The photocatalyst <span class="hlt">sheet</span> also outperformed a photoelectrochemical parallel cell during pure water splitting. The effects of H + /OH - concentration overpotentials and of the IR drop are reduced in the case of the photocatalyst <span class="hlt">sheet</span> compared to photoelectrochemical systems, because the HEP and OEP are situated in close proximity to one another. Therefore, the photocatalyst <span class="hlt">sheet</span> design is well-suited to efficient large-scale applications. Nevertheless, it is also noted that the photocatalytic <span class="hlt">activity</span> of these <span class="hlt">sheets</span> drops markedly with increasing background pressure because of reverse reactions involving molecular oxygen under illumination as well as delays in gas bubble desorption. It is shown that appropriate surface modifications allow the photocatalyst <span class="hlt">sheet</span> to maintain its water</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22649126-su-radiochromic-plastic-thin-sheet-dosimeter-initial-performance','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22649126-su-radiochromic-plastic-thin-sheet-dosimeter-initial-performance"><span>SU-F-T-550: Radiochromic Plastic Thin <span class="hlt">Sheet</span> Dosimeter: Initial Performance</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Jordan, K; Adamovics, J</p> <p></p> <p>Purpose: Thin <span class="hlt">sheets</span>, of a high sensitivity formulation of radiochromic dosimeter, Presage were prepared and evaluated for optical readout. Methods: <span class="hlt">Sheets</span> of radiochromic polyurethane, 12 cm long, 10 cm wide and 0.2 cm thick were prepared with leuco crystal violet as the reporter molecule. Sample transmission was evaluated at a wavelength of 590 nm with in-house constructed instruments: optical cone beam laser CT scanner, fixed and scanning spot densitometers. Sample sequential irradiations to a total dose of 40 Gy were conducted with a modified, Theratron 60, cobalt radiotherapy machine at dose rates of 1 or 0.25 Gy per minute. Exposuremore » to ambient and readout light was minimized to limit background photochromic signals. Samples were stored at 4°C. Optical <span class="hlt">activity</span> was assessed from linearly polarized transmission images. Comparison sensitivity measurements with EBT3 film were conducted. Results: Samples were transparent, smooth and pale purple before irradiation. Radiochromic reaction was completed in less than 5 minutes. A linear dose response with a sensitivity of 0.5 cm-1Gy-1 was observed. Micrometer measurements found <span class="hlt">sheet</span> thickness variations up to 20%. Uniform dose, 2 Gy attenuation images, correlated with local <span class="hlt">sheet</span> thicknesses. Comparable measurements with EBT3 film were 3 times more sensitive at 1 Gy but above 15 Gy, EBT3 film had lower sensitivity than 0.2 cm thick Presage <span class="hlt">sheet</span> dosimeter due to its non-linear response. Conclusion: Dose sensitivity provided a 10% decrease in transmission for a 1 Gy dose. Improvements in mold design are expected to allow production of <span class="hlt">sheets</span> with less than 5% variation in thickness. Above, 10 Gy, Presage <span class="hlt">sheet</span> dosimeter performance expected to exceed EBT3 film based on linearity, sensitivity, transparency and smoothness of samples. J Adamovics is owner of Heuris Inc.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUSM.C42A..01S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUSM.C42A..01S"><span>ICESat's First Year of Measurements Over the Polar Ice <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shuman, C. A.</p> <p>2004-05-01</p> <p>NASA's Ice, Cloud and Land Elevation Satellite (ICESat) mission was developed to measure changes in elevation of the Greenland and Antarctic ice <span class="hlt">sheets</span>. Its primary mission goal is to significantly refine estimates of polar ice <span class="hlt">sheet</span> mass balance. Obtaining precise, spatially dense, ice <span class="hlt">sheet</span> elevations through time is the first step towards this goal. ICESat data will then enable study of associations between observed ice changes and dynamic or climatic forcing factors, and thus enable improved estimation of the present and future contributions of the ice <span class="hlt">sheets</span> to global sea level rise. ICESat was launched on January 12, 2003 and acquired science data from February 20th to March 29th with the first of the three lasers of the Geoscience Laser Altimeter System (GLAS). Data acquisition with the second laser began on September 25th and continued until November 18th, 2003. For one-year change detection, the second laser is scheduled for operation from approximately February 17th to March 20th, 2004. Additional operational periods will be selected to 1) enable periodic measurements through the year, and 2) to support of other NASA Earth Science Enterprise missions and <span class="hlt">activities</span>. To obtain these precise ice <span class="hlt">sheet</span> elevations, GLAS has a 1064 nm wavelength laser operating at 40 Hz with a designed range precision of about 10 cm. The laser footprints are about 70 m in diameter on the Earth's surface and are spaced every 172 m along-track. The on-board GPS receiver enables radial orbit determinations to an accuracy better than 5 cm. The star-tracking attitude-determination system will enable laser footprints to be located to 6 m horizontally when attitude calibration is completed. The orbital altitude averages 600 km at an inclination of 94 degrees with coverage extending from 86 degrees N and S latitude. The spacecraft attitude can be controlled to point the laser beam to within 50 m of surface reference tracks over the ice <span class="hlt">sheets</span> and to point off-nadir up to 5 degrees to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015MS%26E...74a2003B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015MS%26E...74a2003B"><span>Spring back of infinite honeycomb <span class="hlt">sheets</span> beyond plastic deformation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bonfanti, A.; Bhaskar, A.</p> <p>2015-02-01</p> <p>Cellular structures are promising for applications where high stiffness and strength are required with the minimal use of material. They are often used in applications where the plastic deformation plays an important role, such as those involving crashworthiness, energy absorption, and stents. The elastic analysis of a honeycomb <span class="hlt">sheet</span> has been carried out in the past [1]. The present analysis extends this classical work in the elasto-plastic regime. Recoil analysis due to elastic recovery is absent from the published literature. This work aims to develop an analytical model to calculate the spring back for a simplified case, that of an infinite honeycomb <span class="hlt">sheet</span>. An elastic-perfectly plastic material model is assumed. The recoil for a clamped beam with a load and moment applied at the free edge is analytically calculated first. This is carried out by relating the stress distribution of the cross section to the final deformed shape. The part corresponding to the elastic contribution is subsequently subtracted in order to obtain the final configuration after the external load is removed. This simple elasto-plastic analysis is then incorporated into the analysis of an infinite <span class="hlt">sheet</span> made of uniform hexagonal cells. The translational symmetry of the lattice is exploited along with the analysis of a beam under tip loading through to plastic stage and recoil. The final shape of the struts upon the removal of the remote stress is completely determined by the plastic deformation which cannot be recovered. The expression for the beam thus obtained is then used to build an analytical model for an infinite honeycomb <span class="hlt">sheet</span> loaded in both <span class="hlt">directions</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22304083-nonlinear-evolution-three-dimensional-instabilities-thin-thick-electron-scale-current-sheets-plasmoid-formation-current-filamentation','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22304083-nonlinear-evolution-three-dimensional-instabilities-thin-thick-electron-scale-current-sheets-plasmoid-formation-current-filamentation"><span>Nonlinear evolution of three-dimensional instabilities of thin and thick electron scale current <span class="hlt">sheets</span>: Plasmoid formation and current filamentation</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Jain, Neeraj; Büchner, Jörg; Max Planck Institute for Solar System Research, Justus-Von-Liebig-Weg-3, Göttingen</p> <p></p> <p>Nonlinear evolution of three dimensional electron shear flow instabilities of an electron current <span class="hlt">sheet</span> (ECS) is studied using electron-magnetohydrodynamic simulations. The dependence of the evolution on current <span class="hlt">sheet</span> thickness is examined. For thin current <span class="hlt">sheets</span> (half thickness =d{sub e}=c/ω{sub pe}), tearing mode instability dominates. In its nonlinear evolution, it leads to the formation of oblique current channels. Magnetic field lines form 3-D magnetic spirals. Even in the absence of initial guide field, the out-of-reconnection-plane magnetic field generated by the tearing instability itself may play the role of guide field in the growth of secondary finite-guide-field instabilities. For thicker current sheetsmore » (half thickness ∼5 d{sub e}), both tearing and non-tearing modes grow. Due to the non-tearing mode, current <span class="hlt">sheet</span> becomes corrugated in the beginning of the evolution. In this case, tearing mode lets the magnetic field reconnect in the corrugated ECS. Later thick ECS develops filamentary structures and turbulence in which reconnection occurs. This evolution of thick ECS provides an example of reconnection in self-generated turbulence. The power spectra for both the thin and thick current <span class="hlt">sheets</span> are anisotropic with respect to the electron flow <span class="hlt">direction</span>. The cascade towards shorter scales occurs preferentially in the <span class="hlt">direction</span> perpendicular to the electron flow.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015APS..MARG34004P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015APS..MARG34004P"><span>Thin <span class="hlt">sheets</span> achieve optimal wrapping of liquids</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paulsen, Joseph; Démery, Vincent; Davidovitch, Benny; Santangelo, Christian; Russell, Thomas; Menon, Narayanan</p> <p>2015-03-01</p> <p>A liquid drop can wrap itself in a <span class="hlt">sheet</span> using capillary forces [Py et al., PRL 98, 2007]. However, the efficiency of ``capillary origami'' at covering the surface of a drop is hampered by the mechanical cost of bending the <span class="hlt">sheet</span>. Thinner <span class="hlt">sheets</span> deform more readily by forming small-scale wrinkles and stress-focussing patterns, but it is unclear how coverage efficiency competes with mechanical cost as thickness is decreased, and what wrapping shapes will emerge. We place a thin (~ 100 nm) polymer film on a drop whose volume is gradually decreased so that the <span class="hlt">sheet</span> covers an increasing fraction of its surface. The <span class="hlt">sheet</span> exhibits a complex sequence of axisymmetric and polygonal partially- and fully- wrapped shapes. Remarkably, the progression appears independent of mechanical properties. The gross shape, which neglects small-scale features, is correctly predicted by a simple geometric approach wherein the exposed area is minimized. Thus, simply using a thin enough <span class="hlt">sheet</span> results in maximal coverage.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017APS..DFDF10001P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017APS..DFDF10001P"><span>Stabilization of Inviscid Vortex <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Protas, Bartosz; Sakajo, Takashi</p> <p>2017-11-01</p> <p>In this study we investigate the problem of stabilizing inviscid vortex <span class="hlt">sheets</span> via feedback control. Such models, expressed in terms of the Birkhoff-Rott equation, are often used to describe the Kevin-Helmholtz instability of shear layers and are known to be strongly unstable to small-scale perturbations. First, we consider the linear stability of a straight vortex <span class="hlt">sheet</span> in the periodic setting with actuation in the form of an array of point vortices or sources located a certain distance away from the <span class="hlt">sheet</span>. We establish conditions under which this system is controllable and observable. Next, using methods of the linear control theory, we synthesize a feedback control strategy which stabilizes a straight vortex <span class="hlt">sheet</span> in the linear regime. Given the poor conditioning of the discretized problem, reliable solution of the resulting algebraic Riccati equation requires the use of high-precision arithmetic. Finally, we demonstrate that this control approach also succeeds in the nonlinear regime, provided the magnitude of the initial perturbation is sufficiently small.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29929963','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29929963"><span>Universal inverse design of surfaces with thin nematic elastomer <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Aharoni, Hillel; Xia, Yu; Zhang, Xinyue; Kamien, Randall D; Yang, Shu</p> <p>2018-06-21</p> <p>Programmable shape-shifting materials can take different physical forms to achieve multifunctionality in a dynamic and controllable manner. Although morphing a shape from 2D to 3D via programmed inhomogeneous local deformations has been demonstrated in various ways, the inverse problem-finding how to program a <span class="hlt">sheet</span> in order for it to take an arbitrary desired 3D shape-is much harder yet critical to realize specific functions. Here, we address this inverse problem in thin liquid crystal elastomer (LCE) <span class="hlt">sheets</span>, where the shape is preprogrammed by precise and local control of the molecular orientation of the liquid crystal monomers. We show how blueprints for arbitrary surface geometries can be generated using approximate numerical methods and how local extrinsic curvatures can be generated to assist in properly converting these geometries into shapes. Backed by faithfully alignable and rapidly lockable LCE chemistry, we precisely embed our designs in LCE <span class="hlt">sheets</span> using advanced top-down microfabrication techniques. We thus successfully produce flat <span class="hlt">sheets</span> that, upon thermal <span class="hlt">activation</span>, take an arbitrary desired shape, such as a face. The general design principles presented here for creating an arbitrary 3D shape will allow for exploration of unmet needs in flexible electronics, metamaterials, aerospace and medical devices, and more.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24974029','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24974029"><span>Light <span class="hlt">sheet</span> microscopy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Weber, Michael; Mickoleit, Michaela; Huisken, Jan</p> <p>2014-01-01</p> <p>This chapter introduces the concept of light <span class="hlt">sheet</span> microscopy along with practical advice on how to design and build such an instrument. Selective plane illumination microscopy is presented as an alternative to confocal microscopy due to several superior features such as high-speed full-frame acquisition, minimal phototoxicity, and multiview sample rotation. Based on our experience over the last 10 years, we summarize the key concepts in light <span class="hlt">sheet</span> microscopy, typical implementations, and successful applications. In particular, sample mounting for long time-lapse imaging and the resulting challenges in data processing are discussed in detail. © 2014 Elsevier Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017QSRv..169..148P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017QSRv..169..148P"><span>Deglaciation of the Eurasian ice <span class="hlt">sheet</span> complex</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Patton, Henry; Hubbard, Alun; Andreassen, Karin; Auriac, Amandine; Whitehouse, Pippa L.; Stroeven, Arjen P.; Shackleton, Calvin; Winsborrow, Monica; Heyman, Jakob; Hall, Adrian M.</p> <p>2017-08-01</p> <p>The Eurasian ice <span class="hlt">sheet</span> complex (EISC) was the third largest ice mass during the Last Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic sea-level lowering. Whilst recent terrestrial and marine empirical insights have improved understanding of the chronology, pattern and rates of retreat of this vast ice <span class="hlt">sheet</span>, a concerted attempt to model the deglaciation of the EISC honouring these new constraints is conspicuously lacking. Here, we apply a first-order, thermomechanical ice <span class="hlt">sheet</span> model, validated against a diverse suite of empirical data, to investigate the retreat of the EISC after 23 ka BP, <span class="hlt">directly</span> extending the work of Patton et al. (2016) who modelled the build-up to its maximum extent. Retreat of the ice <span class="hlt">sheet</span> complex was highly asynchronous, reflecting contrasting regional sensitivities to climate forcing, oceanic influence, and internal dynamics. Most rapid retreat was experienced across the Barents Sea sector after 17.8 ka BP when this marine-based ice <span class="hlt">sheet</span> disintegrated at a rate of ∼670 gigatonnes per year (Gt a-1) through enhanced calving and interior dynamic thinning, driven by oceanic/atmospheric warming and exacerbated by eustatic sea-level rise. From 14.9 to 12.9 ka BP the EISC lost on average 750 Gt a-1, peaking at rates >3000 Gt a-1, roughly equally partitioned between surface melt and dynamic losses, and potentially contributing up to 2.5 m to global sea-level rise during Meltwater Pulse 1A. Independent glacio-isostatic modelling constrained by an extensive inventory of relative sea-level change corroborates our ice <span class="hlt">sheet</span> loading history of the Barents Sea sector. Subglacial conditions were predominately temperate during deglaciation, with over 6000 subglacial lakes predicted along with an extensive subglacial drainage network. Moreover, the maximum EISC and its isostatic footprint had a profound impact on the proglacial hydrological network, forming the Fleuve Manche mega-catchment which had an area of </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3465438','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3465438"><span>Dual modes of motility at the leading edge of migrating epithelial cell <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Klarlund, Jes K.</p> <p>2012-01-01</p> <p>Purse-string healing is driven by contraction of actin/myosin cables that span cells at wound edges, and it is the predominant mode of closing small round wounds in embryonic and some adult epithelia. Wounds can also heal by cell crawling, and my colleagues and I have shown previously that the presence of unconstrained, straight edges in <span class="hlt">sheets</span> of epithelial cells is a sufficient signal to induce healing by crawling. Here, it is reported that the presence of highly concave edges, which are free or physically constrained by an inert material (agarose), is sufficient to induce formation of purse strings. It was determined that neither of the two types of healing required cell damage or other potential stimuli by using the particularly gentle procedure of introducing gaps by digesting agarose blocks imbedded in the cell <span class="hlt">sheets</span>. Movement by crawling depends on signaling by the EGF receptor (EGFR); however, this was not required for purse-string contraction. A migrating epithelial cell <span class="hlt">sheet</span> usually produces finger-like projections of crawling cells. The cells between fingers contain continuous actin cables, which were also determined to contain myosin IIA and exhibit additional characteristics of purse strings. When crawling was blocked by inhibition of EGFR signaling, the concave regions continued to move, suggesting that both mechanisms contribute to propel the <span class="hlt">sheets</span> forward. Wounding epithelial cell <span class="hlt">sheets</span> causes <span class="hlt">activation</span> of the EGFR, which triggers movement by crawling. The EGFR was found to be <span class="hlt">activated</span> only at straight and convex edges, which explains how both types of movement can coexist at leading epithelial edges. PMID:23019364</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3913373','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3913373"><span>The effect of mesenchymal stem cell <span class="hlt">sheets</span> on structural allograft healing of critical-sized femoral defects in mice</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Long, Teng; Zhu, Zhenan; Awad, Hani A.; Schwarz, Edward M.; Hilton, Matthew J.; Dong, Yufeng</p> <p>2014-01-01</p> <p>Structural bone allografts are widely used in the clinic to treat critical sized bone defects, despite lacking the osteoinductive characteristics of live autografts. To address this, we generated revitalized structural allografts wrapped with mesenchymal stem/progenitor cell (MSC) <span class="hlt">sheets</span>, which were produced by expanding primary syngenic bone marrow derived cells on temperature-responsive plates, as a tissue engineered periosteum. In vitro assays demonstrated maintenance of the MSC phenotype in the <span class="hlt">sheets</span>, suggesting that short-term culturing of MSC <span class="hlt">sheets</span> is not detrimental. To test their efficacy in vivo, allografts wrapped with MSC <span class="hlt">sheets</span> were transplanted into 4-mm murine femoral defects and compared to allografts with <span class="hlt">direct</span> seeding of MSCs and allografts without cells. Evaluations consisted of x-ray plain radiography, 3D microCT, histology, and biomechanical testing at 4- and 6-weeks post-surgery. Our findings demonstrate that MSC <span class="hlt">sheets</span> induce prolonged cartilage formation at the graft-host junction and enhanced bone callus formation, as well as graft-host osteointegration. Moreover, a large periosteal callus was observed spanning the allografts with MSC <span class="hlt">sheets</span>, which partially mimics live autograft healing. Finally, biomechanical testing showed a significant increase in the structural and functional properties of MSC <span class="hlt">sheet</span> grafted femurs. Taken together, MSC <span class="hlt">sheets</span> exhibit enhanced osteogenicity during critical sized bone defect repair, demonstrating the feasibility of this tissue engineering solution for massive allograft healing. PMID:24393269</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED539211.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED539211.pdf"><span>Coos County Youth and Out-of-School <span class="hlt">Activities</span>: Patterns of Involvement and Barriers to Participation. New England Fact <span class="hlt">Sheet</span> No. 7, Fall 2012</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Sharp, Erin Hiley</p> <p>2012-01-01</p> <p>This fact <span class="hlt">sheet</span> draws from surveys administered to a cohort of 416 participants in 7th grade in 2008, again when they were in 8th grade in 2009, and most recently as 10th graders in 2011 to look at patterns of participation in structured <span class="hlt">activities</span> over time and whether male and female students differ in these patterns of participation. It also…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFM.B21F..02W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFM.B21F..02W"><span>The geomicrobiology of the Greenland Ice <span class="hlt">Sheet</span>: impact on DOC export (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wadham, J. L.; Stibal, M.; Lawson, E. C.; Barnett, M. J.; Hasan, F.; Telling, J.; Anesio, A.; Lis, G.; Cullen, D.; Butler, C.; Tranter, M.; Nienow, P. W.</p> <p>2010-12-01</p> <p>The Greenland Ice <span class="hlt">Sheet</span> (GrIS) is the largest mass of ice in the northern hemisphere, and contributes ~370 km3 in runoff annually to the Arctic Ocean. While recent work has highlighted runoff increases of up to 100% from the GrIS over the next century, very little is known about the associated impacts upon rates of sediment-bound and dissolved organic carbon export from the ice <span class="hlt">sheet</span> to the coastal ocean. This is relevant given recent work that has suggested that the high proportion of labile dissolved organic carbon (DOC) present in glacial runoff may be important in sustaining the productivity of ecosystems downstream. Here we report the phylogenetic and functional diversity of micro-organisms inhabiting the surface and basal regions of the Greenland Ice <span class="hlt">Sheet</span> (at Leverett Glacier, SW Greenland), and whose <span class="hlt">activity</span> influences the biogeochemical composition of runoff. Real time PCR data on runoff, together with 16S-rRNA bacterial clone libraries on sediments, demonstrate a subglacial microbial community that contrasts phylogenetically and functionally with the ice <span class="hlt">sheet</span> surface ecosystem. We envisage that large sectors of the subglacial environment are microbially <span class="hlt">active</span>, with overridden paleosols and in-washed surface organic matter providing a carbon substrate for a range of metabolic pathways. This includes methanogenesis which proceeds at rates similar to deep ocean sediments and via a CO2/H2 pathway. These subglacial microbial communities serve to chemically modify the DOC composition of meltwater inputs from the ice <span class="hlt">sheet</span> surface and modulate the reactivity of bulk DOC exported in runoff. Evidence for subglacial microbial influences on DOC in runoff includes elevated concentrations of dissolved carbohydrates (e.g. glucose and fructose of up to 1 μmol/L), which are preferentially exported during subglacial outburst events. We examine the temporal changes in DOC export in runoff from the ice <span class="hlt">sheet</span> over a full melt season, and consider how changes in total</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19810050965&hterms=max+planck&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dmax%2Bplanck','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19810050965&hterms=max+planck&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dmax%2Bplanck"><span>Substorm-related plasma <span class="hlt">sheet</span> motions as determined from differential timing of plasma changes at the ISEE satellites</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Forbes, T. G.; Hones, E. W., Jr.; Bame, S. J.; Asbridge, J. R.; Paschmann, G.; Sckopke, N.; Russell, C. T.</p> <p>1981-01-01</p> <p>From an ISEE survey of substorm dropouts and recoveries during the period February 5 to May 25, 1978, 66 timing events observed by the Los Alamos Scientific Laboratory/Max-Planck-Institut Fast Plasma Experiments were studied in detail. Near substorm onset, both the average timing velocity and the bulk flow velocity at the edge of the plasma <span class="hlt">sheet</span> are inward, toward the center. Measured normal to the surface of the plasma <span class="hlt">sheet</span>, the timing velocity is 23 + or - 18 km/s and the proton flow velocity is 20 + or - 8 km/s. During substorm recovery, the plasma <span class="hlt">sheet</span> reappears moving outward with an average timing velocity of 133 + or - 31 km/s; however, the corresponding proton flow velocity is only 3 + or - 7 km/s in the same <span class="hlt">direction</span>. It is suggested that the difference between the average timing velocity for the expansion of the plasma <span class="hlt">sheet</span> and the plasma bulk flow perpendicular to the surface of the <span class="hlt">sheet</span> during substorm recovery is most likely the result of surface waves moving past the position of the satellites.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017NatCh...9...39S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017NatCh...9...39S"><span>An infrared spectroscopy approach to follow β-<span class="hlt">sheet</span> formation in peptide amyloid assemblies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Seo, Jongcheol; Hoffmann, Waldemar; Warnke, Stephan; Huang, Xing; Gewinner, Sandy; Schöllkopf, Wieland; Bowers, Michael T.; von Helden, Gert; Pagel, Kevin</p> <p>2017-01-01</p> <p>Amyloidogenic peptides and proteins play a crucial role in a variety of neurodegenerative disorders such as Alzheimer's and Parkinson's disease. These proteins undergo a spontaneous transition from a soluble, often partially folded form, into insoluble amyloid fibrils that are rich in β-<span class="hlt">sheets</span>. Increasing evidence suggests that highly dynamic, polydisperse folding intermediates, which occur during fibril formation, are the toxic species in the amyloid-related diseases. Traditional condensed-phase methods are of limited use for characterizing these states because they typically only provide ensemble averages rather than information about individual oligomers. Here we report the first <span class="hlt">direct</span> secondary-structure analysis of individual amyloid intermediates using a combination of ion mobility spectrometry-mass spectrometry and gas-phase infrared spectroscopy. Our data reveal that oligomers of the fibril-forming peptide segments VEALYL and YVEALL, which consist of 4-9 peptide strands, can contain a significant amount of β-<span class="hlt">sheet</span>. In addition, our data show that the more-extended variants of each oligomer generally exhibit increased β-<span class="hlt">sheet</span> content.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_21 --> <div id="page_22" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="421"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013PhDT.......475S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013PhDT.......475S"><span>Controlling microstructure and texture in magnesium alloy <span class="hlt">sheet</span> by shear-based deformation processing</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sagapuram, Dinakar</p> <p></p> <p>Application of lightweight Mg <span class="hlt">sheet</span> is limited by its low workability, both in production of <span class="hlt">sheet</span> (typically by multistep hot and cold-rolling) and forming of <span class="hlt">sheet</span> into components. Large strain extrusion machining (LSEM), a constrained chip formation process, is used to create Mg alloy AZ31B <span class="hlt">sheet</span> in a single deformation step. The deformation in LSEM is shown to be intense simple shear that is confined to a narrow zone, which results in significant deformation-induced heating up to ~ 200°C and reduces the need for pre-heating to realize continuous <span class="hlt">sheet</span> forms. This study focuses on the texture and microstructure development in the <span class="hlt">sheet</span> processed by LSEM. Interestingly, deep, highly twinned steady-state layer develops in the workpiece subsurface due to the compressive field ahead of the shear zone. The shear deformation, in conjunction with this pre-deformed twinned layer, results in tilted-basal textures in the <span class="hlt">sheet</span> with basal planes tilted well away from the surface. These textures are significantly different from those in rolled <span class="hlt">sheet</span>, where basal planes are nearly parallel to the surface. By controlling the strain path, the basal plane inclination from the surface could be varied in the range of 32-53°. B-fiber (basal plane parallel to LSEM shear plane), associated with basal slip, is the major texture component in the <span class="hlt">sheet</span>. An additional minor C2-fiber component appears above 250°C due to the thermal <span class="hlt">activation</span> of pyramidal slip. Together with these textures, microstructure ranges from severely cold-worked to (dynamically) recrystallized type, with the corresponding grain sizes varying from ultrafine- (~ 200 nm) to fine- (2 mum) grained. Small-scale limiting dome height (LDH) confirmed enhanced formability (~ 50% increase in LDH) of LSEM <span class="hlt">sheet</span> over the conventional rolled <span class="hlt">sheet</span>. Premature, twinning-driven shear fractures are observed in the rolled <span class="hlt">sheet</span> with the basal texture. In contrast, LSEM <span class="hlt">sheet</span> with a tilted-basal texture favorably oriented for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.U22A..02H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.U22A..02H"><span>An Imminent Revolution in Modeling Interactions of Ice <span class="hlt">Sheets</span> With Climate</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hughes, T.</p> <p>2008-12-01</p> <p> by radar, seismic, and magnetic profiling, and <span class="hlt">direct</span> measurement of basal conditions by deep drilling and coring into the ice and the bed. These data allow calculating the geothermal heat flux and mapping flow of basal meltwater from geothermal sources to sinks at the termini of ice streams, which discharge up to 90 percent of the ice. James Fastook has a preliminary solution of the full momentum equation needed to model ice streams. Douglas MacAyeal has pioneered modeling catastrophic ice-shelf disintegration that releases "armadas" of icebergs into the world ocean, to extract heat from ocean surface water and thereby reduce the critical ocean-to-atmosphere heat exchange that drives global climate. Ice <span class="hlt">sheets</span> are the only component of Earth's climate machine that can destroy itself-- swiftly--and thereby radically and rapidly alter global climate and sea level.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21847608','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21847608"><span>Myosin II <span class="hlt">activity</span> is required for functional leading-edge cells and closure of epidermal <span class="hlt">sheets</span> in fish skin ex vivo.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Morita, Toshiyuki; Tsuchiya, Akiko; Sugimoto, Masazumi</p> <p>2011-09-01</p> <p>Re-epithelialization in skin wound healing is a process in which epidermal <span class="hlt">sheets</span> grow and close the wound. Although the actin-myosin system is thought to have a pivotal role in re-epithelialization, its role is not clear. In fish skin, re-epithelialization occurs around 500 μm/h and is 50 times faster than in mammalian skin. We had previously reported that leading-edge cells of the epidermal outgrowth have both polarized large lamellipodia and "purse string"-like actin filament cables in the scale-skin culture system of medaka fish, Oryzias latipes (Cell Tissue Res, 2007). The actin purse-string (APS) is a supracellular contractile machinery in which adherens junctions (AJs) link intracellular myosin II-including actin cables between neighboring cells. In this study, we developed a modified "face-to-face" scale-skin culture system as an ex vivo model to study epidermal wound healing, and examined the role of the actin-myosin system in the rapid re-epithelialization using a myosin II ATPase inhibitor, blebbistatin. A low level of blebbistatin suppressed the formation of APS and induced the dissociation of keratocytes from the leading edge without attenuating the growth of the epidermal <span class="hlt">sheet</span> or the migration rate of solitary keratocytes. AJs in the superficial layer showed no obvious changes elicited by blebbistatin. However, two epidermal <span class="hlt">sheets</span> without APSs did not make a closure with each other, which was confirmed by inhibiting the connecting AJs between the superficial layers. These results suggest that myosin II <span class="hlt">activity</span> is required for functional leading-edge cells and for epidermal closure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22299965-three-dimensional-instabilities-electron-scale-current-sheet-collisionless-magnetic-reconnection','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22299965-three-dimensional-instabilities-electron-scale-current-sheet-collisionless-magnetic-reconnection"><span>Three dimensional instabilities of an electron scale current <span class="hlt">sheet</span> in collisionless magnetic reconnection</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Jain, Neeraj; Büchner, Jörg; Max Planck Institute for Solar System Research, Justus-Von-Liebig-Weg-3, Göttingen</p> <p></p> <p>In collisionless magnetic reconnection, electron current <span class="hlt">sheets</span> (ECS) with thickness of the order of an electron inertial length form embedded inside ion current <span class="hlt">sheets</span> with thickness of the order of an ion inertial length. These ECS's are susceptible to a variety of instabilities which have the potential to affect the reconnection rate and/or the structure of reconnection. We carry out a three dimensional linear eigen mode stability analysis of electron shear flow driven instabilities of an electron scale current <span class="hlt">sheet</span> using an electron-magnetohydrodynamic plasma model. The linear growth rate of the fastest unstable mode was found to drop with themore » thickness of the ECS. We show how the nature of the instability depends on the thickness of the ECS. As long as the half-thickness of the ECS is close to the electron inertial length, the fastest instability is that of a translational symmetric two-dimensional (no variations along flow <span class="hlt">direction</span>) tearing mode. For an ECS half thickness sufficiently larger or smaller than the electron inertial length, the fastest mode is not a tearing mode any more and may have finite variations along the flow <span class="hlt">direction</span>. Therefore, the generation of plasmoids in a nonlinear evolution of ECS is likely only when the half-thickness is close to an electron inertial length.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-6-04.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-6-04.pdf"><span>17 CFR 210.6-04 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2010-04-01 2010-04-01 false Balance <span class="hlt">sheets</span>. 210.6-04... 1940, AND ENERGY POLICY AND CONSERVATION ACT OF 1975 Registered Investment Companies § 210.6-04 Balance <span class="hlt">sheets</span>. This rule is applicable to balance <span class="hlt">sheets</span> filed by registered investment companies except for...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title49-vol9/pdf/CFR-2010-title49-vol9-sec1243-2.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title49-vol9/pdf/CFR-2010-title49-vol9-sec1243-2.pdf"><span>49 CFR 1243.2 - Condensed balance <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-10-01</p> <p>... 49 Transportation 9 2010-10-01 2010-10-01 false Condensed balance <span class="hlt">sheet</span>. 1243.2 Section 1243.2... § 1243.2 Condensed balance <span class="hlt">sheet</span>. Commencing with reports for the 3 months beginning January 1, 1972, and... hereby, required to compile and file quarterly reports of balance <span class="hlt">sheet</span> items in accordance with...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title49-vol9/pdf/CFR-2011-title49-vol9-sec1243-2.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title49-vol9/pdf/CFR-2011-title49-vol9-sec1243-2.pdf"><span>49 CFR 1243.2 - Condensed balance <span class="hlt">sheet</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-10-01</p> <p>... 49 Transportation 9 2011-10-01 2011-10-01 false Condensed balance <span class="hlt">sheet</span>. 1243.2 Section 1243.2... § 1243.2 Condensed balance <span class="hlt">sheet</span>. Commencing with reports for the 3 months beginning January 1, 1972, and... hereby, required to compile and file quarterly reports of balance <span class="hlt">sheet</span> items in accordance with...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-6-04.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-6-04.pdf"><span>17 CFR 210.6-04 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2011-04-01 2011-04-01 false Balance <span class="hlt">sheets</span>. 210.6-04... 1940, AND ENERGY POLICY AND CONSERVATION ACT OF 1975 Registered Investment Companies § 210.6-04 Balance <span class="hlt">sheets</span>. This rule is applicable to balance <span class="hlt">sheets</span> filed by registered investment companies except for...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19780012128','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19780012128"><span>Subsonic longitudinal and lateral-<span class="hlt">directional</span> static aerodynamic characteristics of a general research fighter configuration employing a jet <span class="hlt">sheet</span> vortex generator</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Huffman, J. K.; Fox, C. H., Jr.; Ziegler, H.</p> <p>1978-01-01</p> <p>A configuration concept for developing vortex lift, which replaces the physical wing strake with a jet <span class="hlt">sheet</span> generated fluid strake, was investigated on a general research fighter model. The vertical and horizontal location of the jet <span class="hlt">sheet</span> with respect to the wing leading edge was studied over a momentum coefficient range from 0 to 0.24 in the Langley 7- by 10-foot high speed tunnel over a Mach number range from 0.3 to 0.8. The angle of attack range studied was from -2 to 30 deg at sideslip angles of 0, -5, and 5 deg. Test data are presented without analysis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SPIE10137E..0TM','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SPIE10137E..0TM"><span>A fast image registration approach of neural <span class="hlt">activities</span> in light-<span class="hlt">sheet</span> fluorescence microscopy images</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Meng, Hui; Hui, Hui; Hu, Chaoen; Yang, Xin; Tian, Jie</p> <p>2017-03-01</p> <p>The ability of fast and single-neuron resolution imaging of neural <span class="hlt">activities</span> enables light-<span class="hlt">sheet</span> fluorescence microscopy (LSFM) as a powerful imaging technique in functional neural connection applications. The state-of-art LSFM imaging system can record the neuronal <span class="hlt">activities</span> of entire brain for small animal, such as zebrafish or C. elegans at single-neuron resolution. However, the stimulated and spontaneous movements in animal brain result in inconsistent neuron positions during recording process. It is time consuming to register the acquired large-scale images with conventional method. In this work, we address the problem of fast registration of neural positions in stacks of LSFM images. This is necessary to register brain structures and <span class="hlt">activities</span>. To achieve fast registration of neural <span class="hlt">activities</span>, we present a rigid registration architecture by implementation of Graphics Processing Unit (GPU). In this approach, the image stacks were preprocessed on GPU by mean stretching to reduce the computation effort. The present image was registered to the previous image stack that considered as reference. A fast Fourier transform (FFT) algorithm was used for calculating the shift of the image stack. The calculations for image registration were performed in different threads while the preparation functionality was refactored and called only once by the master thread. We implemented our registration algorithm on NVIDIA Quadro K4200 GPU under Compute Unified Device Architecture (CUDA) programming environment. The experimental results showed that the registration computation can speed-up to 550ms for a full high-resolution brain image. Our approach also has potential to be used for other dynamic image registrations in biomedical applications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016PhDT........74N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016PhDT........74N"><span>Bessel light <span class="hlt">sheet</span> structured illumination microscopy</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Noshirvani Allahabadi, Golchehr</p> <p></p> <p>Biomedical study researchers using animals to model disease and treatment need fast, deep, noninvasive, and inexpensive multi-channel imaging methods. Traditional fluorescence microscopy meets those criteria to an extent. Specifically, two-photon and confocal microscopy, the two most commonly used methods, are limited in penetration depth, cost, resolution, and field of view. In addition, two-photon microscopy has limited ability in multi-channel imaging. Light <span class="hlt">sheet</span> microscopy, a fast developing 3D fluorescence imaging method, offers attractive advantages over traditional two-photon and confocal microscopy. Light <span class="hlt">sheet</span> microscopy is much more applicable for in vivo 3D time-lapsed imaging, owing to its selective illumination of tissue layer, superior speed, low light exposure, high penetration depth, and low levels of photobleaching. However, standard light <span class="hlt">sheet</span> microscopy using Gaussian beam excitation has two main disadvantages: 1) the field of view (FOV) of light <span class="hlt">sheet</span> microscopy is limited by the depth of focus of the Gaussian beam. 2) Light-<span class="hlt">sheet</span> images can be degraded by scattering, which limits the penetration of the excitation beam and blurs emission images in deep tissue layers. While two-sided <span class="hlt">sheet</span> illumination, which doubles the field of view by illuminating the sample from opposite sides, offers a potential solution, the technique adds complexity and cost to the imaging system. We investigate a new technique to address these limitations: Bessel light <span class="hlt">sheet</span> microscopy in combination with incoherent nonlinear Structured Illumination Microscopy (SIM). Results demonstrate that, at visible wavelengths, Bessel excitation penetrates up to 250 microns deep in the scattering media with single-side illumination. Bessel light <span class="hlt">sheet</span> microscope achieves confocal level resolution at a lateral resolution of 0.3 micron and an axial resolution of 1 micron. Incoherent nonlinear SIM further reduces the diffused background in Bessel light <span class="hlt">sheet</span> images, resulting in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED555956.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED555956.pdf"><span>State Arts Agency Fact <span class="hlt">Sheet</span>: Support for Arts Education</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Online Submission, 2015</p> <p>2015-01-01</p> <p>This national overview of state arts agency grants and services for arts education includes summary statistics and geographic distribution. The fact <span class="hlt">sheet</span> uses data from Final Descriptive Reports of state arts agency grant-making <span class="hlt">activities</span> submitted annually to the National Assembly of State Arts Agencies (NASAA) and the National Endowment for…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/672634','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/672634"><span>Microcomponent chemical process <span class="hlt">sheet</span> architecture</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Wegeng, R.S.; Drost, M.K.; Call, C.J.; Birmingham, J.G.; McDonald, C.E.; Kurath, D.E.; Friedrich, M.</p> <p>1998-09-22</p> <p>The invention is a microcomponent <span class="hlt">sheet</span> architecture wherein macroscale unit processes are performed by microscale components. The <span class="hlt">sheet</span> architecture may be a single laminate with a plurality of separate microcomponent sections or the <span class="hlt">sheet</span> architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one chemical process unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation. 26 figs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016ISPAr41B7..585X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ISPAr41B7..585X"><span>Extraction of Ice <span class="hlt">Sheet</span> Layers from Two Intersected Radar Echograms Near Neem Ice Core in Greenland</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xiong, S.; Muller, J.-P.</p> <p>2016-06-01</p> <p>Accumulation of snow and ice over time result in ice <span class="hlt">sheet</span> layers. These can be remotely sensed where there is a contrast in electromagnetic properties, which reflect variations of the ice density, acidity and fabric orientation. Internal ice layers are assumed to be isochronous, deep beneath the ice surface, and parallel to the <span class="hlt">direction</span> of ice flow. The distribution of internal layers is related to ice <span class="hlt">sheet</span> dynamics, such as the basal melt rate, basal elevation variation and changes in ice flow mode, which are important parameters to model the ice <span class="hlt">sheet</span>. Radar echo sounder is an effective instrument used to study the sedimentology of the Earth and planets. Ice Penetrating Radar (IPR) is specific kind of radar echo sounder, which extends studies of ice <span class="hlt">sheets</span> from surface to subsurface to deep internal ice <span class="hlt">sheets</span> depending on the frequency utilised. In this study, we examine a study site where folded ice occurs in the internal ice <span class="hlt">sheet</span> south of the North Greenland Eemian ice drilling (NEEM) station, where two intersected radar echograms acquired by the Multi-channel Coherent Radar Depth Sounder (MCoRDS) employed in the NASA's Operation IceBridge (OIB) mission imaged this folded ice. We propose a slice processing flow based on a Radon Transform to trace and extract these two sets of curved ice <span class="hlt">sheet</span> layers, which can then be viewed in 3-D, demonstrating the 3-D structure of the ice folds.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19940025623','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19940025623"><span>Experimental investigation of possible geomagnetic feedback from energetic (0.1 to 16 keV) terrestrial O(+) ions in the magnetotail current <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lennartsson, O. W.; Klumpar, D. M.; Shelley, E. G.; Quinn, J. M.</p> <p>1994-01-01</p> <p>Data from energetic ion mass spectrometers on the ISEE 1 and AMPTE/CCE spacecraft are combined with geomagnetic and solar indices to investigate, in a statistical fashion, whether energized O(+) ions of terrestrial origin constitute a source of feedback which triggers or amplifies geomagnetic <span class="hlt">activity</span> as has been suggested in the literature, by contributing a destabilizing mass increase in the magnetotail current <span class="hlt">sheet</span>. The ISEE 1 data (0.1-16 keV/e) provide in situ observations of the O(+) concentration in the central plasma <span class="hlt">sheet</span>, inside of 23 R(sub E), during the rising and maximum phases of solar cycle 21, as well as inner magnetosphere data from same period. The CCE data (0.1-17 keV/e) taken during the subsequent solar minimum all within 9 R(sub E). provide a reference for long-term variations in the magnetosphere O(+) content. Statistical correlations between the ion data and the indices, and between different indices. all point in the same <span class="hlt">direction</span>: there is probably no feedback specific to the O(+) ions, in spite of the fact that they often contribute most of the ion mass density in the tail current <span class="hlt">sheet</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED152660.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED152660.pdf"><span>Moral Dilemmas/Value <span class="hlt">Sheets</span>: Writing for Content-Centered Social Studies Classrooms.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Stahl, Robert J.; And Others</p> <p></p> <p>The purpose of the paper is to stress the development of content-centered classroom <span class="hlt">activities</span> useful for attaining values clarification and/or moral development goals. The objective is to help teachers understand the formulation of content-centered learning <span class="hlt">activities</span> so that they will be able to plan and produce their own value <span class="hlt">sheets</span> or moral…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-5-02.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-5-02.pdf"><span>17 CFR 210.5-02 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2010-04-01 2010-04-01 false Balance <span class="hlt">sheets</span>. 210.5-02... Balance <span class="hlt">sheets</span>. The purpose of this rule is to indicate the various line items and certain additional... face of the balance <span class="hlt">sheets</span> or related notes filed for the persons to whom this article pertains (see...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-5-02.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-5-02.pdf"><span>17 CFR 210.5-02 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2011-04-01 2011-04-01 false Balance <span class="hlt">sheets</span>. 210.5-02... Balance <span class="hlt">sheets</span>. The purpose of this rule is to indicate the various line items and certain additional... face of the balance <span class="hlt">sheets</span> or related notes filed for the persons to whom this article pertains (see...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5400114','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5400114"><span><span class="hlt">Sheet</span> Probability Index (SPI): Characterizing the geometrical organization of the white matter with diffusion MRI</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Tax, Chantal M.W.; Haije, Tom Dela; Fuster, Andrea; Westin, Carl-Fredrik; Viergever, Max A.; Florack, Luc; Leemans, Alexander</p> <p>2017-01-01</p> <p> assumption that the diffusion MRI peaks reflect true axons, our results would therefore indicate that pathways do not form <span class="hlt">sheet</span> structures at every crossing fiber region but instead at well-defined locations in the brain. With this framework, <span class="hlt">sheet</span> structure location, extent, and orientation could potentially serve as new structural features of brain tissue. The proposed method can be extended to quantify <span class="hlt">sheet</span> structure in <span class="hlt">directional</span> data obtained with techniques other than diffusion MRI, which is essential for further validation. PMID:27456538</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013APS..DFDD28006E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013APS..DFDD28006E"><span>Oblique impact of dense granular <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ellowitz, Jake; Guttenberg, Nicholas; Jaeger, Heinrich M.; Nagel, Sidney R.; Zhang, Wendy W.</p> <p>2013-11-01</p> <p>Motivated by experiments showing impacts of granular jets with non-circular cross sections produce thin ejecta <span class="hlt">sheets</span> with anisotropic shapes, we study what happens when two <span class="hlt">sheets</span> containing densely packed, rigid grains traveling at the same speed collide asymmetrically. Discrete particle simulations and a continuum frictional fluid model yield the same steady-state solution of two exit streams emerging from incident streams. When the incident angle Δθ is less than Δθc =120° +/-10° , the exit streams' angles differ from that measured in water <span class="hlt">sheet</span> experiments. Below Δθc , the exit angles from granular and water <span class="hlt">sheet</span> impacts agree. This correspondence is surprising because 2D Euler jet impact, the idealization relevant for both situations, is ill posed: a generic Δθ value permits a continuous family of solutions. Our finding that granular and water <span class="hlt">sheet</span> impacts evolve into the same member of the solution family suggests previous proposals that perturbations such as viscous drag, surface tension or air entrapment select the actual outcome are not correct. Currently at Department of Physics, University of Oregon, Eugene, OR 97403.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_22 --> <div id="page_23" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="441"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017PhPl...24h2903Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017PhPl...24h2903Z"><span>Electron flat-top distributions and cross-scale wave modulations observed in the current <span class="hlt">sheet</span> of geomagnetic tail</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhao, Duo; Fu, Suiyan; Parks, George K.; Sun, Weijie; Zong, Qiugang; Pan, Dongxiao; Wu, Tong</p> <p>2017-08-01</p> <p>We present new observations of electron distributions and the accompanying waves during the current <span class="hlt">sheet</span> <span class="hlt">activities</span> at ˜60 RE in the geomagnetic tail detected by the ARTEMIS (Acceleration, Reconnection, Turbulence, and Electrodynamics of the Moon's Interaction with the Sun) spacecraft. We find that electron flat-top distribution is a common feature near the neutral <span class="hlt">sheet</span> of the tailward flowing plasmas, consistent with the electron distributions that are shaped in the reconnection region. Whistler mode waves are generated by the anisotropic electron temperature associated with the electron flat-top distributions. These whistler mode waves are modulated by low frequency ion scale waves that are possibly excited by the high-energy ions injected during the current <span class="hlt">sheet</span> instability. The magnetic and electric fields of the ion scale waves are in phase with electron density variations, indicating that they are compressional ion cyclotron waves. Our observations present examples of the dynamical processes occurring during the current <span class="hlt">sheet</span> <span class="hlt">activities</span> far downstream of the geomagnetic tail.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4032586','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4032586"><span>Ammonia gas sensors based on chemically reduced graphene oxide <span class="hlt">sheets</span> self-assembled on Au electrodes</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2014-01-01</p> <p>We present a useful ammonia gas sensor based on chemically reduced graphene oxide (rGO) <span class="hlt">sheets</span> by self-assembly technique to create conductive networks between parallel Au electrodes. Negative graphene oxide (GO) <span class="hlt">sheets</span> with large sizes (>10 μm) can be easily electrostatically attracted onto positive Au electrodes modified with cysteamine hydrochloride in aqueous solution. The assembled GO <span class="hlt">sheets</span> on Au electrodes can be <span class="hlt">directly</span> reduced into rGO <span class="hlt">sheets</span> by hydrazine or pyrrole vapor and consequently provide the sensing devices based on self-assembled rGO <span class="hlt">sheets</span>. Preliminary results, which have been presented on the detection of ammonia (NH3) gas using this facile and scalable fabrication method for practical devices, suggest that pyrrole-vapor-reduced rGO exhibits much better (more than 2.7 times with the concentration of NH3 at 50 ppm) response to NH3 than that of rGO reduced from hydrazine vapor. Furthermore, this novel gas sensor based on rGO reduced from pyrrole shows excellent responsive repeatability to NH3. Overall, the facile electrostatic self-assembly technique in aqueous solution facilitates device fabrication, the resultant self-assembled rGO-based sensing devices, with miniature, low-cost portable characteristics and outstanding sensing performances, which can ensure potential application in gas sensing fields. PMID:24917701</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/874183','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/874183"><span>Thermomechanical processing of plasma sprayed intermetallic <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Hajaligol, Mohammad R.; Scorey, Clive; Sikka, Vinod K.; Deevi, Seetharama C.; Fleischhauer, Grier; Lilly, Jr., A. Clifton; German, Randall M.</p> <p>2001-01-01</p> <p>A powder metallurgical process of preparing a <span class="hlt">sheet</span> from a powder having an intermetallic alloy composition such as an iron, nickel or titanium aluminide. The <span class="hlt">sheet</span> can be manufactured into electrical resistance heating elements having improved room temperature ductility, electrical resistivity, cyclic fatigue resistance, high temperature oxidation resistance, low and high temperature strength, and/or resistance to high temperature sagging. The iron aluminide has an entirely ferritic microstructure which is free of austenite and can include, in weight %, 4 to 32% Al, and optional additions such as .ltoreq.1% Cr, .gtoreq.0.05% Zr .ltoreq.2% Ti, .ltoreq.2% Mo, .ltoreq.1% Ni, .ltoreq.0.75% C, .ltoreq.0.1% B, .ltoreq.1% submicron oxide particles and/or electrically insulating or electrically conductive covalent ceramic particles, .ltoreq.1% rare earth metal, and/or .ltoreq.3% Cu. The process includes forming a non-densified metal <span class="hlt">sheet</span> by consolidating a powder having an intermetallic alloy composition such as by roll compaction, tape casting or plasma spraying, forming a cold rolled <span class="hlt">sheet</span> by cold rolling the non-densified metal <span class="hlt">sheet</span> so as to increase the density and reduce the thickness thereof and annealing the cold rolled <span class="hlt">sheet</span>. The powder can be a water, polymer or gas atomized powder which is subjecting to sieving and/or blending with a binder prior to the consolidation step. After the consolidation step, the <span class="hlt">sheet</span> can be partially sintered. The cold rolling and/or annealing steps can be repeated to achieve the desired <span class="hlt">sheet</span> thickness and properties. The annealing can be carried out in a vacuum furnace with a vacuum or inert atmosphere. During final annealing, the cold rolled <span class="hlt">sheet</span> recrystallizes to an average grain size of about 10 to 30 .mu.m. Final stress relief annealing can be carried out in the B2 phase temperature range.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED475791.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED475791.pdf"><span>Communication Fact <span class="hlt">Sheets</span> for Parents.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Stremel, Kathleen; Bixler, Betsy; Morgan, Susanne; Layton, Kristen</p> <p></p> <p>This booklet contains 28 fact <span class="hlt">sheets</span> on communication written primarily for parents and families with a child who is deaf-blind. They attempt to address fundamental but complex issues related to the communication needs of children with vision and hearing impairments. Each fact <span class="hlt">sheet</span> targets a specific area, including: (1) communication; (2)…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-7-03.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-7-03.pdf"><span>17 CFR 210.7-03 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2010-04-01 2010-04-01 false Balance <span class="hlt">sheets</span>. 210.7-03... 1940, AND ENERGY POLICY AND CONSERVATION ACT OF 1975 Insurance Companies § 210.7-03 Balance <span class="hlt">sheets</span>. (a... otherwise permitted by the Commission, should appear on the face of the balance <span class="hlt">sheets</span> and in the notes...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-7-03.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-7-03.pdf"><span>17 CFR 210.7-03 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2011-04-01 2011-04-01 false Balance <span class="hlt">sheets</span>. 210.7-03... 1940, AND ENERGY POLICY AND CONSERVATION ACT OF 1975 Insurance Companies § 210.7-03 Balance <span class="hlt">sheets</span>. (a... otherwise permitted by the Commission, should appear on the face of the balance <span class="hlt">sheets</span> and in the notes...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3724772','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3724772"><span>Rapid Fabricating Technique for Multi-Layered Human Hepatic Cell <span class="hlt">Sheets</span> by Forceful Contraction of the Fibroblast Monolayer</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Sakai, Yusuke; Koike, Makiko; Hasegawa, Hideko; Yamanouchi, Kosho; Soyama, Akihiko; Takatsuki, Mitsuhisa; Kuroki, Tamotsu; Ohashi, Kazuo; Okano, Teruo; Eguchi, Susumu</p> <p>2013-01-01</p> <p>Cell <span class="hlt">sheet</span> engineering is attracting attention from investigators in various fields, from basic research scientists to clinicians focused on regenerative medicine. However, hepatocytes have a limited proliferation potential in vitro, and it generally takes a several days to form a <span class="hlt">sheet</span> morphology and multi-layered <span class="hlt">sheets</span>. We herein report our rapid and efficient technique for generating multi-layered human hepatic cell (HepaRG® cell) <span class="hlt">sheets</span> using pre-cultured fibroblast monolayers derived from human skin (TIG-118 cells) as a feeder layer on a temperature-responsive culture dish. Multi-layered TIG-118/HepaRG cell <span class="hlt">sheets</span> with a thick morphology were harvested on day 4 of culturing HepaRG cells by forceful contraction of the TIG-118 cells, and the resulting <span class="hlt">sheet</span> could be easily handled. In addition, the human albumin and alpha 1-antitrypsin synthesis <span class="hlt">activities</span> of TIG-118/HepaRG cells were approximately 1.2 and 1.3 times higher than those of HepaRG cells, respectively. Therefore, this technique is considered to be a promising modality for rapidly fabricating multi-layered human hepatocyte <span class="hlt">sheets</span> from cells with limited proliferation potential, and the engineered cell <span class="hlt">sheet</span> could be used for cell transplantation with highly specific functions. PMID:23923035</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23923035','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23923035"><span>Rapid fabricating technique for multi-layered human hepatic cell <span class="hlt">sheets</span> by forceful contraction of the fibroblast monolayer.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sakai, Yusuke; Koike, Makiko; Hasegawa, Hideko; Yamanouchi, Kosho; Soyama, Akihiko; Takatsuki, Mitsuhisa; Kuroki, Tamotsu; Ohashi, Kazuo; Okano, Teruo; Eguchi, Susumu</p> <p>2013-01-01</p> <p>Cell <span class="hlt">sheet</span> engineering is attracting attention from investigators in various fields, from basic research scientists to clinicians focused on regenerative medicine. However, hepatocytes have a limited proliferation potential in vitro, and it generally takes a several days to form a <span class="hlt">sheet</span> morphology and multi-layered <span class="hlt">sheets</span>. We herein report our rapid and efficient technique for generating multi-layered human hepatic cell (HepaRG® cell) <span class="hlt">sheets</span> using pre-cultured fibroblast monolayers derived from human skin (TIG-118 cells) as a feeder layer on a temperature-responsive culture dish. Multi-layered TIG-118/HepaRG cell <span class="hlt">sheets</span> with a thick morphology were harvested on day 4 of culturing HepaRG cells by forceful contraction of the TIG-118 cells, and the resulting <span class="hlt">sheet</span> could be easily handled. In addition, the human albumin and alpha 1-antitrypsin synthesis <span class="hlt">activities</span> of TIG-118/HepaRG cells were approximately 1.2 and 1.3 times higher than those of HepaRG cells, respectively. Therefore, this technique is considered to be a promising modality for rapidly fabricating multi-layered human hepatocyte <span class="hlt">sheets</span> from cells with limited proliferation potential, and the engineered cell <span class="hlt">sheet</span> could be used for cell transplantation with highly specific functions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4894304','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4894304"><span>Calcium imaging of neural circuits with extended depth-of-field light-<span class="hlt">sheet</span> microscopy</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Quirin, Sean; Vladimirov, Nikita; Yang, Chao-Tsung; Peterka, Darcy S.; Yuste, Rafael; Ahrens, Misha B.</p> <p>2016-01-01</p> <p>Increasing the volumetric imaging speed of light-<span class="hlt">sheet</span> microscopy will improve its ability to detect fast changes in neural <span class="hlt">activity</span>. Here, a system is introduced for brain-wide imaging of neural <span class="hlt">activity</span> in the larval zebrafish by coupling structured illumination with cubic phase extended depth-of-field (EDoF) pupil encoding. This microscope enables faster light-<span class="hlt">sheet</span> imaging and facilitates arbitrary plane scanning—removing constraints on acquisition speed, alignment tolerances, and physical motion near the sample. The usefulness of this method is demonstrated by performing multi-plane calcium imaging in the fish brain with a 416 × 832 × 160 µm field of view at 33 Hz. The optomotor response behavior of the zebrafish is monitored at high speeds, and time-locked correlations of neuronal <span class="hlt">activity</span> are resolved across its brain. PMID:26974063</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70038745','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70038745"><span>History of the Greenland Ice <span class="hlt">Sheet</span>: paleoclimatic insights</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Alley, Richard B.; Andrews, John T.; Brigham-Grette, J.; Clarke, G.K.C.; Cuffey, Kurt M.; Fitzpatrick, J.J.; Funder, S.; Marshall, S.J.; Miller, G.H.; Mitrovica, J.X.; Muhs, D.R.; Otto-Bliesner, B. L.; Polyak, L.; White, J.W.C.</p> <p>2010-01-01</p> <p>Paleoclimatic records show that the GreenlandIce <span class="hlt">Sheet</span> consistently has lost mass in response to warming, and grown in response to cooling. Such changes have occurred even at times of slow or zero sea-level change, so changing sea level cannot have been the cause of at least some of the ice-<span class="hlt">sheet</span> changes. In contrast, there are no documented major ice-<span class="hlt">sheet</span> changes that occurred independent of temperature changes. Moreover, snowfall has increased when the climate warmed, but the ice <span class="hlt">sheet</span> lost mass nonetheless; increased accumulation in the ice <span class="hlt">sheet</span>'s center has not been sufficient to counteract increased melting and flow near the edges. Most documented forcings and ice-<span class="hlt">sheet</span> responses spanned periods of several thousand years, but limited data also show rapid response to rapid forcings. In particular, regions near the ice margin have responded within decades. However, major changes of central regions of the ice <span class="hlt">sheet</span> are thought to require centuries to millennia. The paleoclimatic record does not yet strongly constrain how rapidly a major shrinkage or nearly complete loss of the ice <span class="hlt">sheet</span> could occur. The evidence suggests nearly total ice-<span class="hlt">sheet</span> loss may result from warming of more than a few degrees above mean 20th century values, but this threshold is poorly defined (perhaps as little as 2 °C or more than 7 °C). Paleoclimatic records are sufficiently sketchy that the ice <span class="hlt">sheet</span> may have grown temporarily in response to warming, or changes may have been induced by factors other than temperature, without having been recorded.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-9-03.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title17-vol2/pdf/CFR-2010-title17-vol2-sec210-9-03.pdf"><span>17 CFR 210.9-03 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2010-04-01 2010-04-01 false Balance <span class="hlt">sheets</span>. 210.9-03... 1940, AND ENERGY POLICY AND CONSERVATION ACT OF 1975 Bank Holding Companies § 210.9-03 Balance <span class="hlt">sheets</span>... face of the balance <span class="hlt">sheets</span> or in the notes thereto. Assets 1. Cash and due from banks. The amounts in...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-9-03.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title17-vol2/pdf/CFR-2011-title17-vol2-sec210-9-03.pdf"><span>17 CFR 210.9-03 - Balance <span class="hlt">sheets</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-04-01</p> <p>... 17 Commodity and Securities Exchanges 2 2011-04-01 2011-04-01 false Balance <span class="hlt">sheets</span>. 210.9-03... 1940, AND ENERGY POLICY AND CONSERVATION ACT OF 1975 Bank Holding Companies § 210.9-03 Balance <span class="hlt">sheets</span>... face of the balance <span class="hlt">sheets</span> or in the notes thereto. Assets 1. Cash and due from banks. The amounts in...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950038002&hterms=SPIRAL+MODEL&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3DSPIRAL%2BMODEL','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950038002&hterms=SPIRAL+MODEL&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3DSPIRAL%2BMODEL"><span>A test of source-surface model predictions of heliospheric current <span class="hlt">sheet</span> inclination</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Burton, M. E.; Crooker, N. U.; Siscoe, G. L.; Smith, E. J.</p> <p>1994-01-01</p> <p>The orientation of the heliospheric current <span class="hlt">sheet</span> predicted from a source surface model is compared with the orientation determined from minimum-variance analysis of International Sun-Earth Explorer (ISEE) 3 magnetic field data at 1 AU near solar maximum. Of the 37 cases analyzed, 28 have minimum variance normals that lie orthogonal to the predicted Parker spiral <span class="hlt">direction</span>. For these cases, the correlation coefficient between the predicted and measured inclinations is 0.6. However, for the subset of 14 cases for which transient signatures (either interplanetary shocks or bidirectional electrons) are absent, the agreement in inclinations improves dramatically, with a correlation coefficient of 0.96. These results validate not only the use of the source surface model as a predictor but also the previously questioned usefulness of minimum variance analysis across complex sector boundaries. In addition, the results imply that interplanetary dynamics have little effect on current <span class="hlt">sheet</span> inclination at 1 AU. The dependence of the correlation on transient occurrence suggests that the leading edge of a coronal mass ejection (CME), where transient signatures are detected, disrupts the heliospheric current <span class="hlt">sheet</span> but that the <span class="hlt">sheet</span> re-forms between the trailing legs of the CME. In this way the global structure of the heliosphere, reflected both in the source surface maps and in the interplanetary sector structure, can be maintained even when the CME occurrence rate is high.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008APS..MARA39007R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008APS..MARA39007R"><span>Spiraling Cracks in Thin <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Romero, Victor; Roman, Benoit; Cerda, Enrique</p> <p>2008-03-01</p> <p>A wide kind of everyday-life industrial products come in a thin package that needs to be torn open by the user, and the opening is not always easy. We built a simple setup to study crack propagation in thin <span class="hlt">sheets</span> coupled with large out-of-plane displacement : A cylindrical tool is inserted in a straight incision in a thin <span class="hlt">sheet</span>, and is pushed against the <span class="hlt">sheet</span> perpendicularly to that incision, eventually propagating a crack. When the blunt tool is continually pushed against the lip, we found that the crack follows a very robust spiraling path. Experiments may be interpreted in terms of ``Spira Mirabilis'' (logarithmic spiral). Starting with crack theory argument, we will show that the early behavior of the cut path follows a portion of a logathmic spiral, and that the path tends to another spiral with a different pitch as the crack adds more turns. Our crack experiment illustrates the fact that thin <span class="hlt">sheets</span> mechanics is deeply connected to geometry, and finally spirals characteristics allow us to measure material crack properties of the thin layer used.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4356224','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4356224"><span>Repair Mechanism of Osteochondral Defect Promoted by Bioengineered Chondrocyte <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kamei, Naosuke; Adachi, Nobuo; Hamanishi, Michio; Kamei, Goki; Mahmoud, Elhussein Elbadry; Nakano, Tomohiro; Iwata, Takanori; Yamato, Masayuki; Okano, Teruo; Ochi, Mitsuo</p> <p>2015-01-01</p> <p>Cell <span class="hlt">sheet</span> engineering has developed as a remarkable method for cell transplantation. In the field of cartilage regeneration, several studies previously reported that cartilage defects could be regenerated by transplantation of a chondrocyte <span class="hlt">sheet</span> using cell <span class="hlt">sheet</span> engineering. However, it remains unclear how such a thin cell <span class="hlt">sheet</span> could repair a deep cartilage defect. We, therefore, focused on the mechanism of cartilage repair using cell <span class="hlt">sheet</span> engineering in this study. Chondrocyte <span class="hlt">sheets</span> and synovial cell <span class="hlt">sheets</span> were fabricated using cell <span class="hlt">sheet</span> engineering, and these allogenic cell <span class="hlt">sheets</span> were transplanted to cover an osteochondral defect in a rat model. Macroscopic and histological evaluation was performed at 4 and 12 weeks after transplantation. Analysis of the gene expression of each cell <span class="hlt">sheet</span> and of the regenerated tissue at 1 week after transplantation was performed. In addition, green fluorescent protein (GFP) transgenic rats were used as donors (transplanted chondrocyte <span class="hlt">sheets</span>) or recipients (osteochondral defect models) to identify the cell origin of regenerated cartilage. Cartilage repair was significantly better in the group implanted with a chondrocyte <span class="hlt">sheet</span> than in that with a synovial cell <span class="hlt">sheet</span>. The results of gene expression analysis suggest that the possible factor contributing to cartilage repair might be TGFβ1. Cell tracking experiments using GFP transgenic rats showed that the regenerated cartilage was largely composed of cells derived from the transplanted chondrocyte <span class="hlt">sheets</span>. PMID:25396711</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19860019345','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19860019345"><span>Entrainment, transport and concentration of meteorites in polar ice <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Drewry, D. J.</p> <p>1986-01-01</p> <p>Glaciers and ice <span class="hlt">sheets</span> act as slow-moving conveyancing systems for material added to both their upper and lower surfaces. Because the transit time for most materials is extremely long the ice acts as a major global storage facility. The effects of horizontal and vertical motions on the flow patterns of Antarctic ice <span class="hlt">sheets</span> are summarized. The determination of the source areas of meteorites and their transport paths is a problem of central importance since it relates not only <span class="hlt">directly</span> to concentration mechanisms but also to the wider issues in glaciology and meteorites. The ice and snow into which a meteorite falls, and which moves with it to the concentration area, encodes information about the infall area. The principle environmental conditions being former elevation, temperature (also related to elevation), and age of the ice. This encoded information could be used to identify the infall area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19850000068&hterms=silicone+sheet&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dsilicone%2Bsheet','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19850000068&hterms=silicone+sheet&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dsilicone%2Bsheet"><span>Silicone Coating on Polyimide <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Park, J. J.</p> <p>1985-01-01</p> <p>Silicone coatings applied to polyimide <span class="hlt">sheeting</span> for variety of space-related applications. Coatings intended to protect flexible substrates of solar-cell blankets from degradation by oxygen atoms, electrons, plasmas, and ultraviolet light in low Earth orbit and outer space. Since coatings are flexible, generally useful in forming flexible laminates or protective layers on polyimide-<span class="hlt">sheet</span> products.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004JGRA..10912213S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004JGRA..10912213S"><span>Two types of energy-dispersed ion structures at the plasma <span class="hlt">sheet</span> boundary</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sauvaud, J.-A.; Kovrazhkin, R. A.</p> <p>2004-12-01</p> <p>We study two main types of ion energy dispersions observed in the energy range ˜1 to 14 keV on board the Interball-Auroral (IA) satellite at altitudes 2-3 RE at the poleward boundary of the plasma <span class="hlt">sheet</span>. The first type of structure is named velocity dispersed ion structures (VDIS). It is known that VDIS represent a global proton structure with a latitudinal width of ˜0.7-2.5°, where the ion overall energy increases with latitude. IA data allow to show that VDIS are made of substructures lasting for ˜1-3 min. Inside each substructure, high-energy protons arrive first, regardless of the <span class="hlt">direction</span> of the plasma <span class="hlt">sheet</span> boundary crossing. A near-continuous rise of the maximal and minimal energies of consecutive substructures with invariant latitude characterizes VDIS. The second type of dispersed structure is named time-of-flight dispersed ion structures (TDIS). TDIS are recurrent sporadic structures in H+ (and also O+) with a quasi-period of ˜3 min and a duration of ˜1-3 min. The maximal energy of TDIS is rather constant and reaches ≥14 keV. During both poleward and equatorward crossings of the plasma <span class="hlt">sheet</span> boundary, inside each TDIS, high-energy ions arrive first. These structures are accompanied by large fluxes of upflowing H+ and O+ ions with maximal energies up to 5-10 keV. In association with TDIS, bouncing H+ clusters are observed in quasi-dipolar magnetic field tubes, i.e., equatorward from TDIS. The electron populations generally have different properties during observations of VDIS and TDIS. The electron flux accompanying VDIS first increases smoothly and then decreases after Interball-Auroral has passed through the proton structure. The average electron energy in the range ˜0.5-2 keV is typical for electrons from the plasma <span class="hlt">sheet</span> boundary layer (PSBL). The electron fluxes associated with TDIS increases suddenly at the polar boundary of the auroral zone. Their average energy, reaching ˜5-8 keV, is typical for CPS. A statistical analysis shows that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19950004447','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19950004447"><span>Computer-aided light <span class="hlt">sheet</span> flow visualization using photogrammetry</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stacy, Kathryn; Severance, Kurt; Childers, Brooks A.</p> <p>1994-01-01</p> <p>A computer-aided flow visualization process has been developed to analyze video images acquired from rotating and translating light <span class="hlt">sheet</span> visualization systems. The computer process integrates a mathematical model for image reconstruction, advanced computer graphics concepts, and digital image processing to provide a quantitative and a visual analysis capability. The image reconstruction model, based on photogrammetry, uses knowledge of the camera and light <span class="hlt">sheet</span> locations and orientations to project two-dimensional light <span class="hlt">sheet</span> video images into three-dimensional space. A sophisticated computer visualization package, commonly used to analyze computational fluid dynamics (CFD) results, was chosen to interactively display the reconstructed light <span class="hlt">sheet</span> images with the numerical surface geometry for the model or aircraft under study. The photogrammetric reconstruction technique and the image processing and computer graphics techniques and equipment are described. Results of the computer-aided process applied to both a wind tunnel translating light <span class="hlt">sheet</span> experiment and an in-flight rotating light <span class="hlt">sheet</span> experiment are presented. The capability to compare reconstructed experimental light <span class="hlt">sheet</span> images with CFD solutions in the same graphics environment is also demonstrated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2950516','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2950516"><span>AmrZ Beta-<span class="hlt">Sheet</span> Residues Are Essential for DNA Binding and Transcriptional Control of Pseudomonas aeruginosa Virulence Genes ▿ †</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Waligora, Elizabeth A.; Ramsey, Deborah M.; Pryor, Edward E.; Lu, Haiping; Hollis, Thomas; Sloan, Gina P.; Deora, Rajendar; Wozniak, Daniel J.</p> <p>2010-01-01</p> <p>AmrZ is a putative ribbon-helix-helix (RHH) transcriptional regulator. RHH proteins utilize residues within the β-<span class="hlt">sheet</span> for DNA binding, while the α-helices promote oligomerization. AmrZ is of interest due to its dual roles as a transcriptional <span class="hlt">activator</span> and as a repressor, regulating genes encoding virulence factors associated with both chronic and acute Pseudomonas aeruginosa infection. In this study, cross-linking revealed that AmrZ forms oligomers in solution but that the amino terminus, containing an unordered region and a β-<span class="hlt">sheet</span>, were not required for oligomerization. The first 12 unordered residues (extended amino terminus) contributed minimally to DNA binding. Mutagenesis of the AmrZ β-<span class="hlt">sheet</span> demonstrated that residues 18, 20, and 22 were essential for DNA binding at both <span class="hlt">activation</span> and repressor sites, suggesting that AmrZ utilizes a similar mechanism for binding to these sites. Mice infected with amrZ mutants exhibited reduced bacterial burden, morbidity, and mortality. <span class="hlt">Direct</span> in vivo competition assays showed a 5-fold competitive advantage for the wild type over an isogenic amrZ mutant. Finally, the reduced infection phenotype of the amrZ-null strain was similar to that of a strain expressing a DNA-binding-deficient AmrZ variant, indicating that DNA binding and transcriptional regulation by AmrZ is responsible for the in vivo virulence defect. These recent infection data, along with previously identified AmrZ-regulated virulence factors, suggest the necessity of AmrZ transcriptional regulation for optimal virulence during acute infection. PMID:20709902</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_23 --> <div id="page_24" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="461"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1136209','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1136209"><span>Biodiesel Basics (Fact <span class="hlt">Sheet</span>)</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Not Available</p> <p></p> <p>This fact <span class="hlt">sheet</span> provides a brief introduction to biodiesel, including a discussion of biodiesel blends, which blends are best for which vehicles, where to buy biodiesel, how biodiesel compares to diesel fuel in terms of performance, how biodiesel performs in cold weather, whether biodiesel use will plug vehicle filters, how long-term biodiesel use may affect engines, biodiesel fuel standards, and whether biodiesel burns cleaner than diesel fuel. The fact <span class="hlt">sheet</span> also dismisses the use of vegetable oil as a motor fuel.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24393269','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24393269"><span>The effect of mesenchymal stem cell <span class="hlt">sheets</span> on structural allograft healing of critical sized femoral defects in mice.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Long, Teng; Zhu, Zhenan; Awad, Hani A; Schwarz, Edward M; Hilton, Matthew J; Dong, Yufeng</p> <p>2014-03-01</p> <p>Structural bone allografts are widely used in the clinic to treat critical sized bone defects, despite lacking the osteoinductive characteristics of live autografts. To address this, we generated revitalized structural allografts wrapped with mesenchymal stem/progenitor cell (MSC) <span class="hlt">sheets</span>, which were produced by expanding primary syngenic bone marrow derived cells on temperature-responsive plates, as a tissue-engineered periosteum. In vitro assays demonstrated maintenance of the MSC phenotype in the <span class="hlt">sheets</span>, suggesting that short-term culturing of MSC <span class="hlt">sheets</span> is not detrimental. To test their efficacy in vivo, allografts wrapped with MSC <span class="hlt">sheets</span> were transplanted into 4-mm murine femoral defects and compared to allografts with <span class="hlt">direct</span> seeding of MSCs and allografts without cells. Evaluations consisted of X-ray plain radiography, 3D microCT, histology, and biomechanical testing at 4- and 6-weeks post-surgery. Our findings demonstrate that MSC <span class="hlt">sheets</span> induce prolonged cartilage formation at the graft-host junction and enhanced bone callus formation, as well as graft-host osteointegration. Moreover, a large periosteal callus was observed spanning the allografts with MSC <span class="hlt">sheets</span>, which partially mimics live autograft healing. Finally, biomechanical testing showed a significant increase in the structural and functional properties of MSC <span class="hlt">sheet</span> grafted femurs. Taken together, MSC <span class="hlt">sheets</span> exhibit enhanced osteogenicity during critical sized bone defect repair, demonstrating the feasibility of this tissue engineering solution for massive allograft healing. Copyright © 2013 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5793571','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5793571"><span>Influence of Accumulative Roll Bonding on the Texture and Tensile Properties of an AZ31 Magnesium Alloy <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Džugan, Ján; Németh, Gergely; Lukáč, Pavel; Bohlen, Jan</p> <p>2018-01-01</p> <p>Deformation behaviour of rolled AZ31 <span class="hlt">sheets</span> that were subjected to the accumulative roll bonding was investigated. Substantially refined microstructure of samples was achieved after the first and second pass through the rolling mill. <span class="hlt">Sheets</span> texture was investigated using an X-ray diffractometer. Samples for tensile tests were cut either parallel or perpendicular to the rolling <span class="hlt">direction</span>. Tensile tests were performed at temperatures ranging from room temperature up to 300 °C. Tensile plastic anisotropy, different from the anisotropy observed in AZ31 <span class="hlt">sheets</span> by other authors, was observed. This anisotropy decreases with an increasing number of rolling passes and increasing deformation temperature. Grain refinement and texture are the crucial factors influencing the deformation behaviour. PMID:29303975</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29369624','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29369624"><span>Heterogeneous Amyloid β-<span class="hlt">Sheet</span> Polymorphs Identified on Hydrogen Bond Promoting Surfaces Using 2D SFG Spectroscopy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ho, Jia-Jung; Ghosh, Ayanjeet; Zhang, Tianqi O; Zanni, Martin T</p> <p>2018-02-08</p> <p>Two-dimensional sum-frequency generation spectroscopy (2D SFG) is used to study the structures of the pentapeptide FGAIL on hydrogen bond promoting surfaces. FGAIL is the most amyloidogenic portion of the human islet amyloid polypeptide (hIAPP or amylin). In the presence of a pure gold surface, FGAIL does not form ordered structures. When the gold is coated with a self-assembled monolayer of mercaptobenzoic acid (MBA), 2D SFG spectra reveal features associated with β-<span class="hlt">sheets</span>. Also observed are cross peaks between the FGAIL peptides and the carboxylic acid groups of the MBA monolayer, indicating that the peptides are in close contact with the surface headgroups. In the second set of samples, FGAIL peptides chemically ligated to the MBA monolayer also exhibited β-<span class="hlt">sheet</span> features but with a much simpler spectrum. From simulations of the experiments, we conclude that the hydrogen bond promoting surface catalyzes the formation of both parallel and antiparallel β-<span class="hlt">sheet</span> structures with several different orientations. When ligated, parallel <span class="hlt">sheets</span> with only a single orientation are the primary structure. Thus, this hydrogen bond promoting surface creates a heterogeneous distribution of polymorph structures, consistent with a concentration effect that allows nucleation of many different amyloid seeding structures. A single well-defined seed favors one polymorph over the others, showing that the concentrating influence of a membrane can be counterbalanced by factors that favor <span class="hlt">directed</span> fiber growth. These experiments lay the foundation for the measurement and interpretation of β-<span class="hlt">sheet</span> structures with heterodyne-detected 2D SFG spectroscopy. The results of this model system suggest that a heterogeneous distribution of polymorphs found in nature are an indication of nonselective amyloid aggregation whereas a narrow distribution of polymorph structures is consistent with a specific protein or lipid interaction that <span class="hlt">directs</span> fiber growth.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.C53C0754M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.C53C0754M"><span>Quaternary evolution of the Fennoscandian Ice <span class="hlt">Sheet</span> from 3D seismic data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Montelli, A.; Dowdeswell, J. A.; Ottesen, D.; Johansen, S. E.</p> <p>2016-12-01</p> <p>The Quaternary seismic stratigraphy and architecture of the mid-Norwegian continental shelf and slope are investigated using extensive grids of marine 2D and 3D seismic reflection data that cover more than 100,000 km2 of the continental margin. At least 26 distinct regional palaeo-surfaces have been interpreted within the stratigraphy of the Quaternary Naust Formation on the mid-Norwegian margin. Multiple assemblages of buried glacigenic landforms are preserved within the Naust Formation across most of the study area, facilitating detailed palaeo-glaciological reconstructions. We document a marine-terminating, calving Fennoscandian Ice <span class="hlt">Sheet</span> (FIS) margin present periodically on the Norwegian shelf since at least the beginning of the Quaternary. Elongate, streamlined landforms interpreted as mega-scale glacial lineations (MSGLs) have been found within the upper part of the Naust sequence N ( 1.9-1.6 Ma), sugesting the development of fast-flowing ice streams since that time. Shifts in the location of depocentres and <span class="hlt">direction</span> of features indicative of fast ice-flow suggest that several reorganisations in the FIS drainage have occurred since 1.5 Ma. Subglacial landforms reveal a complex and dynamic ice <span class="hlt">sheet</span>, with converging palaeo-ice streams and several flow-switching events that may reflect major changes in topography and internal ice-<span class="hlt">sheet</span> structure. Lack of subglacial meltwater channels suggests a largely distributed, low-volume meltwater system that drained the FIS through permeable subglacial till without leaving much erosional evidence. This regional palaeo-environmental examination of the FIS provides a useful framework for ice-<span class="hlt">sheet</span> modelling and shows that fragmentary preservation of buried surfaces and variability of ice-<span class="hlt">sheet</span> dynamics should be taken into account when reconstructing glacial history from spatially limited datasets.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1813991B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1813991B"><span>Evolution of a Greenland Ice <span class="hlt">sheet</span> Including Shelves and Regional Sea Level Variations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bradley, Sarah; Reerink, Thomas; van de Wal, Roderik S. W.; Helsen, Michiel; Goelzer, Heiko</p> <p>2016-04-01</p> <p>Observational evidence, including offshore moraines and marine sediment cores infer that at the Last Glacial maximum (LGM) the Greenland ice <span class="hlt">sheet</span> (GIS) grounded out across the Davis Strait into Baffin Bay, with fast flowing ice streams extending out to the continental shelf break along the NW margin. These observations lead to a number of questions as to weather the GIS and Laurentide ice <span class="hlt">sheet</span> (LIS) coalesced during glacial maximums, and if so, did a significant ice shelf develop across Baffin Bay and how would such a configuration impact on the relative contribution of these ice <span class="hlt">sheets</span> to eustatic sea level (ESL). Most previous paleo ice <span class="hlt">sheet</span> modelling simulations of the GIS recreated an ice <span class="hlt">sheet</span> that either did not extend out onto the continental shelf or utilised a simplified marine ice parameterisation to recreate an extended GIS, and therefore did not fully include ice shelf dynamics. In this study we simulate the evolution of the GIS from 220 kyr BP to present day using IMAU-ice; a 3D thermodynamical ice <span class="hlt">sheet</span> model which fully accounts for grounded and floating ice, calculates grounding line migration and ice shelf dynamics. As there are few observational estimates of the long-term (yrs) sub marine basal melting rates (mbm) for the GIS, we developed a mbm parameterization within IMAU-ice controlled primarily by changes in paleo water depth. We also investigate the influence of the LIS on the GIS evolution by including relative sea level forcing's derived from a Glacial Isostatic Adjustment model. We will present results of how changes in the mbm <span class="hlt">directly</span> impacts on the ice <span class="hlt">sheet</span> dynamics, timing and spatial extent of the GIS at the glacial maximums, but also on the rate of retreat and spatial extent at the Last interglacial (LIG) minimum. Results indicate that with the inclusion of ice shelf dynamics, a larger GIS is generated which is grounded out into Davis strait, up to a water depth of -750 m, but significantly reduces the GIS contribution to Last</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMPP43C2299B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMPP43C2299B"><span>Evolution of a Greenland Ice <span class="hlt">sheet</span> Including Shelves and Regional Sea Level Variations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bradley, S.; Reerink, T.; Vandewal, R.; Helsen, M.</p> <p>2015-12-01</p> <p>Observational evidence, including offshore moraines and marine sediment cores infer that at the Last Glacial maximum (LGM) the Greenland ice <span class="hlt">sheet</span> (GIS) grounded out across the Davis Strait into Baffin Bay, with fast flowing ice streams extending out to the continental shelf break along the NW margin. These observations lead to a number of questions as to weather the GIS and Laurentide ice <span class="hlt">sheet</span> (LIS) coalesced during glacial maximums, and if so, did a significant ice shelf develop across Baffin Bay and how would such a configuration impact on the relative contribution of these ice <span class="hlt">sheets</span> to eustatic sea level (ESL). Most previous paleo ice <span class="hlt">sheet</span> modelling simulations of the GIS recreated an ice <span class="hlt">sheet</span> that either did not extend out onto the continental shelf or utilised a simplified marine ice parameterisation to recreate an extended GIS, and therefore did not fully include ice shelf dynamics. In this study we simulate the evolution of the GIS from 220 kyr BP to present day using IMAU-ice; a 3D thermodynamical ice <span class="hlt">sheet</span> model which fully accounts for grounded and floating ice, calculates grounding line migration and ice shelf dynamics. There is few observational estimates of long-term (yrs) sub marine basal melting rates (mbm) for the GIS. Therefore we investigate a range of relationships to constrain the spatial and temporal parameterisation of mbm within IMAU-ice related to changes in paleo water depth, driven by changes in relative sea level and ocean temperature. We will present results of how changes in the mbm <span class="hlt">directly</span> impacts on the ice <span class="hlt">sheet</span> dynamics, timing and spatial extent of the GIS at the glacial maximums, but also on the rate of retreat and spatial extent at the Last interglacial (LIG) minimum. Initial results indicate that with the inclusion of ice shelf dynamics, a larger GIS is generated which is grounded out into Davis strait, up to a water depth of -750 m, but the total contribution to LIG ESL is reduced by up to 0.6 m.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013BGD....1019311L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013BGD....1019311L"><span>Greenland Ice <span class="hlt">Sheet</span> exports labile organic carbon to the Arctic oceans</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lawson, E. C.; Wadham, J. L.; Tranter, M.; Stibal, M.; Lis, G. P.; Butler, C. E. H.; Laybourn-Parry, J.; Nienow, P.; Chandler, D.; Dewsbury, P.</p> <p>2013-12-01</p> <p>Runoff from small glacier systems contains dissolved organic carbon (DOC), rich in protein-like, low molecular weight (LMW) compounds, designating glaciers as an important source of bioavailable carbon for downstream heterotrophic <span class="hlt">activity</span>. Fluxes of DOC and particulate organic carbon (POC) exported from large Greenland catchments, however, remain unquantified, despite the Greenland Ice <span class="hlt">Sheet</span> (GrIS) being the largest source of global glacial runoff (ca. 400 km3 yr-1). We report high and episodic fluxes of POC and DOC from a large (1200 km2) GrIS catchment during contrasting melt seasons. POC dominates organic carbon (OC) export (70-89% on average), is sourced from the ice <span class="hlt">sheet</span> bed and contains a significant bioreactive component (9% carbohydrates). A major source for the "bioavailable" (free carbohydrates) LMW-DOC fraction is microbial <span class="hlt">activity</span> on the ice <span class="hlt">sheet</span> surface, with some further addition of LMW-DOC to meltwaters by biogeochemical processes at the ice <span class="hlt">sheet</span> bed. The bioavailability of the exported DOC (30-58%) to downstream marine microorganisms is similar to that reported from other glacial watersheds. Annual fluxes of DOC and free carbohydrates during two melt seasons were similar, despite the ~ 2 fold difference in runoff fluxes, suggesting production-limited DOC sources. POC fluxes were also insensitive to an increase in seasonal runoff volumes, indicating supply-limitation of suspended sediment in runoff. Scaled to the GrIS, the combined DOC and POC fluxes (0.13-0.17 Tg C yr-1 DOC, 0.36-1.52 Tg C yr-1 mean POC) are of a similar order of magnitude to a large Arctic river system, and hence represent an important OC source to the North Atlantic, Greenland and Labrador Seas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1340580','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/1340580"><span>Micro-fluidic partitioning between polymeric <span class="hlt">sheets</span> for chemical amplification and processing</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Anderson, Brian L.</p> <p>2017-01-24</p> <p>A system for fluid partitioning for chemical amplification or other chemical processing or separations of a sample, comprising a first dispenser of a first polymeric <span class="hlt">sheet</span>, wherein the first polymeric <span class="hlt">sheet</span> contains chambers; a second dispenser of a second polymeric <span class="hlt">sheet</span> wherein the first dispenser and the second dispenser are positioned so that the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span> become parallel; a dispenser of the fluid positioned to dispense the fluid between the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span>; and a seal unit that seals the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span> together thereby sealing the sample between the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span> and partitioning the fluid for chemical amplification or other chemical processing or separations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1182597','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/1182597"><span>Micro-fluidic partitioning between polymeric <span class="hlt">sheets</span> for chemical amplification and processing</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Anderson, Brian L.</p> <p>2015-05-26</p> <p>A system for fluid partitioning for chemical amplification or other chemical processing or separations of a sample, comprising a first dispenser of a first polymeric <span class="hlt">sheet</span>, wherein the first polymeric <span class="hlt">sheet</span> contains chambers; a second dispenser of a second polymeric <span class="hlt">sheet</span> wherein the first dispenser and the second dispenser are positioned so that the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span> become parallel; a dispenser of the fluid positioned to dispense the fluid between the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span>; and a seal unit that seals the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span> together thereby sealing the sample between the first polymeric <span class="hlt">sheet</span> and the second polymeric <span class="hlt">sheet</span> and partitioning the fluid for chemical amplification or other chemical processing or separations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012JChPh.137n5104M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012JChPh.137n5104M"><span>β-<span class="hlt">sheet</span> propensity controls the kinetic pathways and morphologies of seeded peptide aggregation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Morriss-Andrews, Alex; Bellesia, Giovanni; Shea, Joan-Emma</p> <p>2012-10-01</p> <p>The effect of seeds in templating the morphology of peptide aggregates is examined using molecular dynamics simulations and a coarse-grained peptide representation. Varying the nature of the aggregate seed between β-<span class="hlt">sheet</span>, amorphous, and β-barrel seeds leads to different aggregation pathways and to morphologically different aggregates. Similar effects are seen by varying the β-<span class="hlt">sheet</span> propensity of the free peptides. For a fibrillar seed and free peptides of high β-<span class="hlt">sheet</span> propensity, fibrillar growth occurred by means of <span class="hlt">direct</span> attachment (without structural rearrangement) of free individual peptides and small ordered oligomers onto the seed. For a fibrillar seed and free peptides of low β-<span class="hlt">sheet</span> propensity, fibrillar growth occurred through a dock-lock mechanism, in which the free peptides first docked onto the seed, and then locked on, extending and aligning to join the fibril. Amorphous seeds absorbed free peptides into themselves indiscriminately, with any fibrillar rearrangement subsequent to this absorption by means of a condensation-ordering transition. Although the mechanisms observed by varying peptide β-<span class="hlt">sheet</span> propensity are diverse, the initial pathways can always be broken down into the following steps: (i) the free peptides diffuse in the bulk and attach individually to the seed; (ii) the free peptides diffuse and aggregate among themselves; (iii) the free peptide oligomers collide with the seed; and (iv) the free oligomers merge with the seed and rearrange in a manner dependent on the backbone flexibility of both the free and seed peptides. Our simulations indicate that it is possible to sequester peptides from amorphous aggregates into fibrils, and also that aggregate morphology (and thus cytoxicity) can be controlled by introducing seeds of aggregate-compatible peptides with differing β-<span class="hlt">sheet</span> propensities into the system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/9661379','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/9661379"><span>Crib <span class="hlt">sheets</span> or security blankets?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Drake, V K; Freed, P; Hunter, J M</p> <p>1998-01-01</p> <p>This article describes the sanctioned use of crib <span class="hlt">sheets</span> as a nursing intervention to decrease test anxiety when the classroom is the practice setting for psychiatric/mental health nursing faculty. The products that the students created offered additional unsuspected benefits. The faculty were convinced that the use of crib <span class="hlt">sheets</span> can be a sound intervention to reduce students' test-taking anxiety.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/874028','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/874028"><span>Enhanced methanol utilization in <span class="hlt">direct</span> methanol fuel cell</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Ren, Xiaoming; Gottesfeld, Shimshon</p> <p>2001-10-02</p> <p>The fuel utilization of a <span class="hlt">direct</span> methanol fuel cell is enhanced for improved cell efficiency. Distribution plates at the anode and cathode of the fuel cell are configured to distribute reactants vertically and laterally uniformly over a catalyzed membrane surface of the fuel cell. A conductive <span class="hlt">sheet</span> between the anode distribution plate and the anodic membrane surface forms a mass transport barrier to the methanol fuel that is large relative to a mass transport barrier for a gaseous hydrogen fuel cell. In a preferred embodiment, the distribution plate is a perforated corrugated <span class="hlt">sheet</span>. The mass transport barrier may be conveniently increased by increasing the thickness of an anode conductive <span class="hlt">sheet</span> adjacent the membrane surface of the fuel cell.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110015904','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110015904"><span>Method for shaping <span class="hlt">sheet</span> thermoplastic and the like</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Akilian, Mireille K. (Inventor); Schattenburg, Mark L. (Inventor)</p> <p>2011-01-01</p> <p>Processes and apparati for shaping <span class="hlt">sheet</span> glass or thermoplastic materials use force from a layer of a flowing fluid, such as air, between the <span class="hlt">sheet</span> and a mandrel at close to the softening temperature of the thermoplastic. The shape is preserved by cooling. The shape of the air bearing mandrel and the pressure distribution of the fluid contribute to the final shape. A process can be conducted on one or two surfaces such that the force from the air layer is on one or two surfaces of the <span class="hlt">sheet</span>. The gap size between the <span class="hlt">sheet</span> and mandrel determines the pressure profile in the gap, which also determines the final <span class="hlt">sheet</span> shape. In general, smaller gaps lead to larger viscous forces. The pressure profile depends on the shape of the mandrel, the size of the fluid gap and the <span class="hlt">sheet</span> and the fluid supply pressure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19850017733&hterms=glacier+melt&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dglacier%2Bmelt','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19850017733&hterms=glacier+melt&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dglacier%2Bmelt"><span>Potential Climatic Effects on the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bindschadler, R. A.</p> <p>1984-01-01</p> <p>The Greenland Ice <span class="hlt">Sheet</span> covers an area of 1,720,000 sq. km and contains approximately 2,600,000 cu km of ice. Most of the ice <span class="hlt">sheet</span> receives an excess of snow accumulation over the amount of ice lost to wind, meltwater run-off or other ablative processes. The majority of mass loss occurs at the margin of the ice <span class="hlt">sheet</span> as either surface melt, which flows into the sea or calving of icebergs from the tongues of outlet glaciers. Many estimates of these processes were published. An average of five published estimates is summarized. If these estimates are correct, then the Greenland Ice <span class="hlt">Sheet</span> is in approximate equilibrium and contributes 490 cu km/a of fresh water to the North Atlantic and Arctic Oceans. Climate effects, ice <span class="hlt">sheet</span> flow, and application of remote sensing to tracking of the ice <span class="hlt">sheet</span> are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-03-05/pdf/2010-4690.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-03-05/pdf/2010-4690.pdf"><span>75 FR 10267 - Federal Open Market Committee; Domestic Policy <span class="hlt">Directive</span> of January 26 and 27, 2010</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-03-05</p> <p>... the Federal Reserve's balance <span class="hlt">sheet</span> to expand significantly in coming months. The Committee <span class="hlt">directs</span>... developments regarding the System's balance <span class="hlt">sheet</span> that could affect the attainment over time of the Committee's...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title12-vol6/pdf/CFR-2011-title12-vol6-sec615-5211.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title12-vol6/pdf/CFR-2011-title12-vol6-sec615-5211.pdf"><span>12 CFR 615.5211 - Risk categories-balance <span class="hlt">sheet</span> assets.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-01-01</p> <p>... 12 Banks and Banking 6 2011-01-01 2011-01-01 false Risk categories-balance <span class="hlt">sheet</span> assets. 615.5211...—balance <span class="hlt">sheet</span> assets. Section 615.5210(c) specifies certain balance <span class="hlt">sheet</span> assets that are not assigned to the risk categories set forth below. All other balance <span class="hlt">sheet</span> assets are assigned to the percentage...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title12-vol6/pdf/CFR-2010-title12-vol6-sec615-5211.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title12-vol6/pdf/CFR-2010-title12-vol6-sec615-5211.pdf"><span>12 CFR 615.5211 - Risk categories-balance <span class="hlt">sheet</span> assets.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-01-01</p> <p>... 12 Banks and Banking 6 2010-01-01 2010-01-01 false Risk categories-balance <span class="hlt">sheet</span> assets. 615.5211...—balance <span class="hlt">sheet</span> assets. Section 615.5210(c) specifies certain balance <span class="hlt">sheet</span> assets that are not assigned to the risk categories set forth below. All other balance <span class="hlt">sheet</span> assets are assigned to the percentage...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/489060-nonlinear-breakup-liquid-sheets','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/489060-nonlinear-breakup-liquid-sheets"><span>Nonlinear breakup of liquid <span class="hlt">sheets</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Jazayeri, S.A.; Li, X.</p> <p>1997-07-01</p> <p>Sprays formed from the disintegration of liquid <span class="hlt">sheets</span> have extensive practical applications, ranging from chemical and pharmaceutical processes to power generation and propulsion systems. A knowledge of the liquid <span class="hlt">sheet</span> breakup process is essential to the understanding of fundamental mechanism of liquid atomization and spray formation processes. The breakup of liquid <span class="hlt">sheets</span> has been investigated in terms of hydrodynamic stability via linear analysis by Squire, Hagerty and Shea, Li, etc. nonlinear effect has been studied by Clark and Dombrowski up to the second order, and by Rangel and Sirignano through numerical simulation employing vortex discretization method. As shown by Taubmore » for the breakup of circular liquid jets, the closer to the breakup region, the higher the order of nonlinear analysis has to be for adequate description of the breakup behavior. As pointed out by Bogy, a nonlinear analysis up to the third order is generally sufficient to account for the inherent nonlinear nature of the breakup process. Therefore, a third-order nonlinear analysis has been carried out in this study to investigate the process of liquid <span class="hlt">sheet</span> disruption preceding the spray formation.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29421562','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29421562"><span>Exogenous ROS-induced cell <span class="hlt">sheet</span> transfer based on hematoporphyrin-polyketone film via a one-step process.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Koo, Min-Ah; Lee, Mi Hee; Kwon, Byeong-Ju; Seon, Gyeung Mi; Kim, Min Sung; Kim, Dohyun; Nam, Ki Chang; Park, Jong-Chul</p> <p>2018-04-01</p> <p>To date, most of invasive cell <span class="hlt">sheet</span> harvesting methods have used culture surface property variations, such as wettability, pH, electricity, and magnetism, to induce cell detachment. These methods that rely on surface property changes are effective when cell detachment prior to application is necessary, but of limited use when used for cell <span class="hlt">sheet</span> transfer to target regions. The study reports a new reactive oxygen species (ROS)-induced strategy based on hematoporphyrin-incorporated polyketone film (Hp-PK film) to transfer cell <span class="hlt">sheets</span> <span class="hlt">directly</span> to target areas without an intermediate harvesting process. After green LED (510 nm) irradiation, production of exogenous ROS from the Hp-PK films induces cell <span class="hlt">sheet</span> detachment and transfer. The study suggests that ROS-induced cell detachment property of the Hp-PK film is closely related to conformational changes of extracellular matrix (ECM) proteins. Also, this strategy with the Hp-PK film can be applied by regulating production rate of exogenous ROS in various types of cells, including fibroblasts, mesenchymal stem cells and keratinocytes. In conclusion, ROS-induced method using the Hp-PK film can be used for one-step cell <span class="hlt">sheet</span> transplantation and has potential in biomedical applications. Copyright © 2018 Elsevier Ltd. All rights reserved.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_24 --> <div id="page_25" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="481"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140016762','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140016762"><span>Increased Tensile Strength of Carbon Nanotube Yarns and <span class="hlt">Sheets</span> through Chemical Modification and Electron Beam Irradiation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Miller, Sandi G.; Williams, Tiffany S.; Baker, James S.; Sola, Francisco; Lebron-Colon, Marisabel; McCorkle, Linda S.; Wilmoth, Nathan G.; Gaier, James; Chen, Michelle; Meador, Michael A.</p> <p>2014-01-01</p> <p>The inherent strength of individual carbon nanotubes offers considerable opportunity for the development of advanced, lightweight composite structures. Recent work in the fabrication and application of carbon nanotube (CNT) forms such as yarns and <span class="hlt">sheets</span> has addressed early nanocomposite limitations with respect to nanotube dispersion and loading; and has pushed the technology toward structural composite applications. However, the high tensile strength of an individual CNT has not <span class="hlt">directly</span> translated to macro-scale CNT forms where bulk material strength is limited by inter-tube electrostatic attraction and slippage. The focus of this work was to assess post processing of CNT <span class="hlt">sheet</span> and yarn to improve the macro-scale strength of these material forms. Both small molecule functionalization and e-beam irradiation was evaluated as a means to enhance tensile strength and Youngs modulus of the bulk CNT material. Mechanical testing results revealed a tensile strength increase in CNT <span class="hlt">sheets</span> by 57 when functionalized, while an additional 48 increase in tensile strength was observed when functionalized <span class="hlt">sheets</span> were irradiated; compared to unfunctionalized <span class="hlt">sheets</span>. Similarly, small molecule functionalization increased yarn tensile strength up to 25, whereas irradiation of the functionalized yarns pushed the tensile strength to 88 beyond that of the baseline yarn.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRC..122.5022M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRC..122.5022M"><span>Large-scale experimental observations of <span class="hlt">sheet</span> flow on a sandbar under skewed-asymmetric waves</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mieras, Ryan S.; Puleo, Jack A.; Anderson, Dylan; Cox, Daniel T.; Hsu, Tian-Jian</p> <p>2017-06-01</p> <p>A novel large wave flume experiment was conducted on a fixed, barred beach with a sediment pit on the sandbar, allowing for the isolation of small-scale bed response to large-scale forcing. Concurrent measurements of instantaneous <span class="hlt">sheet</span> layer sediment concentration profiles and near-bed velocity profiles were obtained on a sandbar for the first time. Two sediment distributions were used with median grain diameters, d50, of 0.17 and 0.27 mm. <span class="hlt">Sheet</span> flow occurred primarily under wave crests, where <span class="hlt">sheet</span> thickness increased with increasing wave height. A proportionality constant, Λ, was used to relate maximum Shields parameter to maximum <span class="hlt">sheet</span> thickness (normalized by d50), with bed shear stress computed using the quadratic drag law. An enhanced <span class="hlt">sheet</span> layer thickness was apparent for the smaller sediment experiments (Λ = 18.7), when <span class="hlt">directly</span> compared to closed-conduit oscillatory flow tunnel data (Λ = 10.6). However, Λ varied significantly (5 < Λ < 31) depending on the procedure used to estimate grain roughness, ks, and wave friction factor, fw. Three models for ks were compared (keeping the model for fw fixed): constant ks = 2.5d50, and two expressions dependent on flow intensity, derived from steady and oscillatory <span class="hlt">sheet</span> flow experiments. Values of ks/d50 varied by two orders of magnitude and exhibited an inverse relationship with Λ, where Λ ˜ 30 for ks/d50 of O(1) while Λ ˜ 5 for ks/d50 of O(100). Two expressions for fw were also tested (with the steady flow-based model for ks), yielding a difference of 69% (Λ ˜ 13 versus Λ ˜ 22).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.C51B0713H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.C51B0713H"><span>Probability based hydrologic catchments of the Greenland Ice <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hudson, B. D.</p> <p>2015-12-01</p> <p>Greenland Ice <span class="hlt">Sheet</span> melt water impacts ice <span class="hlt">sheet</span> flow dynamics, fjord and coastal circulation, and sediment and biogeochemical fluxes. Melt water exiting the ice <span class="hlt">sheet</span> also is a key term in its mass balance. Because of this, knowledge of the area of the ice <span class="hlt">sheet</span> that contributes melt water to a given outlet (its hydrologic catchment) is important to many ice <span class="hlt">sheet</span> studies and is especially critical to methods using river runoff to assess ice <span class="hlt">sheet</span> mass balance. Yet uncertainty in delineating ice <span class="hlt">sheet</span> hydrologic catchments is a problem that is rarely acknowledged. Ice <span class="hlt">sheet</span> catchments are delineated as a function of both basal and surface topography. While surface topography is well known, basal topography is less certain because it is dependent on radar surveys. Here, I a present a Monte Carlo based approach to delineating ice <span class="hlt">sheet</span> catchments that quantifies the impact of uncertain basal topography. In this scheme, over many iterations I randomly vary the ice <span class="hlt">sheet</span> bed elevation within published error bounds (using Morlighem et al., 2014 bed and bed error datasets). For each iteration of ice <span class="hlt">sheet</span> bed elevation, I calculate the hydraulic potentiometric surface and route water over its path of 'steepest' descent to delineate the catchment. I then use all realizations of the catchment to arrive at a probability map of all major melt water outlets in Greenland. I often find that catchment size is uncertain, with small, random perturbations in basal topography leading to large variations in catchments size. While some catchments are well defined, others can double or halve in size within published basal topography error bars. While some uncertainty will likely always remain, this work points to locations where studies of ice <span class="hlt">sheet</span> hydrology would be the most successful, allows reinterpretation of past results, and points to where future radar surveys would be most advantageous.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22587046-residual-stress-induced-grain-growth-twinned-grains-its-effect-formability-magnesium-alloy-sheet-room-temperature','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22587046-residual-stress-induced-grain-growth-twinned-grains-its-effect-formability-magnesium-alloy-sheet-room-temperature"><span>Residual-stress-induced grain growth of twinned grains and its effect on formability of magnesium alloy <span class="hlt">sheet</span> at room temperature</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Kim, Se-Jong; Kim, Daeyong, E-mail: daeyong@kims.re.kr; Lee, Keunho</p> <p>2015-11-15</p> <p>A magnesium alloy <span class="hlt">sheet</span> was subjected to in-plane compression along with a vertical load to avoid buckling during compression. Pre-compressed specimens machined from the <span class="hlt">sheet</span> were annealed at different temperatures and the changes in microstructure and texture were observed using electron back scattered diffraction (EBSD). Twinned grains preferentially grew during annealing at 300 °C, so that a strong texture with the < 0001 > <span class="hlt">direction</span> parallel to the transverse <span class="hlt">direction</span> developed. EBSD analysis confirmed that the friction caused by the vertical load induced inhomogeneous distribution of residual stress, which acted as an additional driving force for preferential grain growth ofmore » twinned grain during annealing. The annealed specimen showed excellent formability. - Highlights: • A magnesium alloy <span class="hlt">sheet</span> subjected to in-plane compression under a vertical load • The vertical load induced inhomogeneous distribution of the residual stress. • The residual stress acted as an additional driving force for grain growth. • The annealed specimen with strong non-basal texture showed excellent formability.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014APS..DFDH15008P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014APS..DFDH15008P"><span>Wrapping a liquid drop with a thin elastic <span class="hlt">sheet</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paulsen, Joseph; Démery, Vincent; Davidovitch, Benny; Santangelo, Chris; Russell, Thomas; Menon, Narayanan</p> <p>2014-11-01</p> <p>We study the wrapping of a liquid drop by an initially-planar ultrathin (~ 100 nm) circular <span class="hlt">sheet</span>. These elastic <span class="hlt">sheets</span> can completely relax compressive stresses by forming wrinkles. In the experiment, we find that when a small fraction of the drop is covered, the overall shape of the <span class="hlt">sheet</span> (i.e. averaging over the wrinkles) is axisymmetric. As we shrink the drop further, the <span class="hlt">sheet</span> develops radial folds that break the axisymmetry of the <span class="hlt">sheet</span> and the drop. Our data are consistent with a model where the <span class="hlt">sheet</span> selects the shape that minimizes the exposed liquid surface area. We thus identify a ``geometric wrapping'' regime, where the partially-wrapped shape depends only on the relative radii of the <span class="hlt">sheet</span> and the drop; the global breaking of axisymmetry is independent of the elastic energy of the deformed <span class="hlt">sheet</span>. This regime requires that bending energy is negligible compared to surface energy, in contrast to the ``capillary origami'' regime where the static shape of the drop comes from a balance of bending and capillary forces.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMSH54A..05S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMSH54A..05S"><span>Exploring reconnection, current <span class="hlt">sheets</span>, and dissipation in a laboratory MHD turbulence experiment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schaffner, D. A.</p> <p>2015-12-01</p> <p>The Swarthmore Spheromak Experiment (SSX) can serve as a testbed for studying MHD turbulence in a controllable laboratory setting, and in particular, explore the phenomena of reconnection, current <span class="hlt">sheets</span> and dissipation in MHD turbulence. Plasma with turbulently fluctuating magnetic and velocity fields can be generated using a plasma gun source and launched into a flux-conserving cylindrical tunnel. No background magnetic field is applied so internal fields are allowed to evolve dynamically. Point measurements of magnetic and velocity fluctuations yield broadband power-law spectra with a steepening breakpoint indicative of the onset of a dissipation scale. The frequency range at which this steepening occurs can be correlated to the ion inertial scale of the plasma, a length which is characteristic of the size of current <span class="hlt">sheets</span> in MHD plasmas and suggests a connection to dissipation. Observation of non-Gaussian intermittent jumps in magnetic field magnitude and angle along with measurements of ion temperature bursts suggests the presence of current <span class="hlt">sheets</span> embedded within the turbulent plasma, and possibly even <span class="hlt">active</span> reconnection sites. Additionally, structure function analysis coupled with appeals to fractal scaling models support the hypothesis that current <span class="hlt">sheets</span> are associated with dissipation in this system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22364859-initiation-eruption-process-magnetic-flux-rope-from-solar-active-region-noaa-earth-directed-cme','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22364859-initiation-eruption-process-magnetic-flux-rope-from-solar-active-region-noaa-earth-directed-cme"><span>INITIATION AND ERUPTION PROCESS OF MAGNETIC FLUX ROPE FROM SOLAR <span class="hlt">ACTIVE</span> REGION NOAA 11719 TO EARTH-<span class="hlt">DIRECTED</span> CME</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Vemareddy, P.; Zhang, J., E-mail: vema@prl.res.in</p> <p></p> <p>An eruption event launched from the solar <span class="hlt">active</span> region (AR) NOAA 11719 is investigated based on coronal EUV observations and photospheric magnetic field measurements obtained from the Solar Dynamic Observatory. The AR consists of a filament channel originating from a major sunspot and its south section is associated with an inverse-S sigmoidal system as observed in Atmospheric Imaging Assembly passbands. We regard the sigmoid as the main body of the flux rope (FR). There also exists a twisted flux bundle crossing over this FR. This overlying flux bundle transforms in shape similar to kink-rise evolution, which corresponds with the risemore » motion of the FR. The emission measure and temperature along the FR exhibits an increasing trend with its rising motion, indicating reconnection in the thinning current <span class="hlt">sheet</span> underneath the FR. Net magnetic flux of the AR, evaluated at north and south polarities, showed decreasing behavior whereas the net current in these fluxes exhibits an increasing trend. Because the negative (positive) flux has a dominant positive (negative) current, the chirality of AR flux system is likely negative (left handed) in order to be consistent with the chirality of inverse S-sigmoidal FR. This analysis of magnetic fields of the source AR suggests that the cancelling fluxes are prime factors of the monotonous twisting of the FR system, reaching to a critical state to trigger kink instability and rise motion. This rise motion may have led to the onset of the torus instability, resulting in an Earth-<span class="hlt">directed</span> coronal mass ejection, and the progressive reconnection in the thinning current <span class="hlt">sheet</span> beneath the rising FR led to the M6.5 flare.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=241667','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=241667"><span><span class="hlt">Direct</span> Determination of <span class="hlt">Activities</span> for Microorganisms of Chesapeake Bay Populations</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Tabor, Paul S.; Neihof, Rex A.</p> <p>1984-01-01</p> <p>We used three methods in determination of the metabolically <span class="hlt">active</span> individual microorganisms for Chesapeake Bay surface and near-bottom populations over a period of a year. Synthetically <span class="hlt">active</span> bacteria were recognized as enlarged cells in samples amended with nalidixic acid and yeast extract and incubated for 6 h. Microorganisms with <span class="hlt">active</span> electron transport systems were identified by the reduction of a tetrazolium salt electron acceptor. Microorganisms <span class="hlt">active</span> in uptake of amino acids, thymidine, and acetate were determined by microautoradiography. In conjunction with enumeration of <span class="hlt">active</span> organisms, a total <span class="hlt">direct</span> count was made for each sample preparation by epifluorescence microscopy. For the majority of samples, numbers of amino acid uptake-<span class="hlt">active</span> organisms were greater than numbers of organisms determined to be <span class="hlt">active</span> by other <span class="hlt">direct</span> measurements. Within a sample, the numbers of uptake-<span class="hlt">active</span> organisms (amino acids or thymidine) and electron transport system-<span class="hlt">active</span> organisms were significantly different for 68% of the samples. Numbers of synthetically <span class="hlt">active</span> bacteria were generally less than numbers determined by the other <span class="hlt">direct</span> <span class="hlt">activity</span> measurements. The distribution of total counts in the 11 samplings showed a seasonal pattern, with significant dependence on in situ water temperature, increasing from March to September and then decreasing through February. Synthetically <span class="hlt">active</span> bacteria and amino acid uptake-<span class="hlt">active</span> organisms showed a significant dependence on in situ temperature, independent of the function of temperature on total counts. Numbers of <span class="hlt">active</span> organisms determined by at least one of the methods used exceeded 25% of the total population of all samplings, and from June through September, >85% of the total population was found to be <span class="hlt">active</span> by at least one <span class="hlt">direct</span> <span class="hlt">activity</span> measurement. Thus, <span class="hlt">active</span> rather than dormant organisms compose a major portion of the microbial population in this region of Chesapeake Bay. PMID:16346659</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/16346659','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/16346659"><span><span class="hlt">Direct</span> determination of <span class="hlt">activities</span> for microorganisms of chesapeake bay populations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tabor, P S; Neihof, R A</p> <p>1984-11-01</p> <p>We used three methods in determination of the metabolically <span class="hlt">active</span> individual microorganisms for Chesapeake Bay surface and near-bottom populations over a period of a year. Synthetically <span class="hlt">active</span> bacteria were recognized as enlarged cells in samples amended with nalidixic acid and yeast extract and incubated for 6 h. Microorganisms with <span class="hlt">active</span> electron transport systems were identified by the reduction of a tetrazolium salt electron acceptor. Microorganisms <span class="hlt">active</span> in uptake of amino acids, thymidine, and acetate were determined by microautoradiography. In conjunction with enumeration of <span class="hlt">active</span> organisms, a total <span class="hlt">direct</span> count was made for each sample preparation by epifluorescence microscopy. For the majority of samples, numbers of amino acid uptake-<span class="hlt">active</span> organisms were greater than numbers of organisms determined to be <span class="hlt">active</span> by other <span class="hlt">direct</span> measurements. Within a sample, the numbers of uptake-<span class="hlt">active</span> organisms (amino acids or thymidine) and electron transport system-<span class="hlt">active</span> organisms were significantly different for 68% of the samples. Numbers of synthetically <span class="hlt">active</span> bacteria were generally less than numbers determined by the other <span class="hlt">direct</span> <span class="hlt">activity</span> measurements. The distribution of total counts in the 11 samplings showed a seasonal pattern, with significant dependence on in situ water temperature, increasing from March to September and then decreasing through February. Synthetically <span class="hlt">active</span> bacteria and amino acid uptake-<span class="hlt">active</span> organisms showed a significant dependence on in situ temperature, independent of the function of temperature on total counts. Numbers of <span class="hlt">active</span> organisms determined by at least one of the methods used exceeded 25% of the total population of all samplings, and from June through September, >85% of the total population was found to be <span class="hlt">active</span> by at least one <span class="hlt">direct</span> <span class="hlt">activity</span> measurement. Thus, <span class="hlt">active</span> rather than dormant organisms compose a major portion of the microbial population in this region of Chesapeake Bay.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19830000108&hterms=baxter&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dbaxter','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19830000108&hterms=baxter&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dbaxter"><span>Reinforcement for Stretch Formed <span class="hlt">Sheet</span> Metal</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lea, J. B.; Baxter, C. R.</p> <p>1983-01-01</p> <p>Tearing of aluminum <span class="hlt">sheet</span> metal durinng stretch forming prevented by flame spraying layer of aluminum on edges held in stretch-forming machine. Technique improves grip of machine on metal and reinforced <span class="hlt">sheet</span> better able to with stand concentration of force in vicinity of grips.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005JMFM....7S.254S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005JMFM....7S.254S"><span>On Compressible Vortex <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Secchi, Paolo</p> <p>2005-05-01</p> <p>We introduce the main known results of the theory of incompressible and compressible vortex <span class="hlt">sheets</span>. Moreover, we present recent results obtained by the author with J. F. Coulombel about supersonic compressible vortex <span class="hlt">sheets</span> in two space dimensions. The problem is a nonlinear free boundary hyperbolic problem with two difficulties: the free boundary is characteristic and the Lopatinski condition holds only in a weak sense, yielding losses of derivatives. Under a supersonic condition that precludes violent instabilities, we prove an energy estimate for the boundary value problem obtained by linearization around an unsteady piecewise solution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1020234-role-polyalanine-domains-sheet-formation-spider-silk-block-copolymers','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1020234-role-polyalanine-domains-sheet-formation-spider-silk-block-copolymers"><span>Role of Polyalanine Domains in -<span class="hlt">Sheet</span> Formation in Spider Silk Block Copolymers</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Rabotyagova, O.; Cebe, P; Kaplan, D</p> <p>2010-01-01</p> <p>Genetically engineered spider silk-like block copolymers were studied to determine the influence of polyalanine domain size on secondary structure. The role of polyalanine block distribution on {beta}-<span class="hlt">sheet</span> formation was explored using FT-IR and WAXS. The number of polyalanine blocks had a <span class="hlt">direct</span> effect on the formation of crystalline {beta}-<span class="hlt">sheets</span>, reflected in the change in crystallinity index as the blocks of polyalanines increased. WAXS analysis confirmed the crystalline nature of the sample with the largest number of polyalanine blocks. This approach provides a platform for further exploration of the role of specific amino acid chemistries in regulating the assembly of {beta}-sheetmore » secondary structures, leading to options to regulate material properties through manipulation of this key component in spider silks.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ClDy...50.2881S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ClDy...50.2881S"><span>Influence of glacial ice <span class="hlt">sheets</span> on the Atlantic meridional overturning circulation through surface wind change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sherriff-Tadano, Sam; Abe-Ouchi, Ayako; Yoshimori, Masakazu; Oka, Akira; Chan, Wing-Le</p> <p>2018-04-01</p> <p>Coupled modeling studies have recently shown that the existence of the glacial ice <span class="hlt">sheets</span> intensifies the Atlantic meridional overturning circulation (AMOC). However, most models show a strong AMOC in their simulations of the Last Glacial Maximum (LGM), which is biased compared to reconstructions that indicate both a weaker and stronger AMOC during the LGM. Therefore, a detailed investigation of the mechanism behind this intensification of the AMOC is important for a better understanding of the glacial climate and the LGM AMOC. Here, various numerical simulations are conducted to focus on the effect of wind changes due to glacial ice <span class="hlt">sheets</span> on the AMOC and the crucial region where the wind modifies the AMOC. First, from atmospheric general circulation model experiments, the effect of glacial ice <span class="hlt">sheets</span> on the surface wind is evaluated. Second, from ocean general circulation model experiments, the influence of the wind stress change on the AMOC is evaluated by applying wind stress anomalies regionally or at different magnitudes as a boundary condition. These experiments demonstrate that glacial ice <span class="hlt">sheets</span> intensify the AMOC through an increase in the wind stress at the North Atlantic mid-latitudes, which is induced by the North American ice <span class="hlt">sheet</span>. This intensification of the AMOC is caused by the increased oceanic horizontal and vertical transport of salt, while the change in sea ice transport has an opposite, though minor, effect. Experiments further show that the Eurasian ice <span class="hlt">sheet</span> intensifies the AMOC by <span class="hlt">directly</span> affecting the deep-water formation in the Norwegian Sea.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.epa.gov/compliance/final-npdes-electronic-reporting-rule-fact-sheet','PESTICIDES'); return false;" href="https://www.epa.gov/compliance/final-npdes-electronic-reporting-rule-fact-sheet"><span>Final NPDES Electronic Reporting Rule Fact <span class="hlt">Sheet</span></span></a></p> <p><a target="_blank" href="http://www.epa.gov/pesticides/search.htm">EPA Pesticide Factsheets</a></p> <p></p> <p></p> <p>Fact <span class="hlt">sheet</span> explaining the National Pollution Discharge Elimination System (NPDES) Electronic Reporting Rule. The fact <span class="hlt">sheet</span> provides information on the purpose of the rule, benefits and implementation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFM.C14B..01B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFM.C14B..01B"><span>Rewriting Ice <span class="hlt">Sheet</span> "Glacier-ology"</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bindschadler, R.</p> <p>2006-12-01</p> <p>The revolution in glaciology driven by the suite of increasingly sophisticated satellite instruments has been no more extreme than in the area of ice dynamics. Years ago, glaciologists were (probably unwittingly) selective in what properties of mountain glaciers were also applied to ice <span class="hlt">sheets</span>. This reinforced the view that they responded slowly to their environment. Notions of rapid response driven by the ideas of John Mercer, Bill Budd and Terry Hughes were politely rejected by the centrists of mainstream glaciological thought. How the tables have turned--and by the ice <span class="hlt">sheets</span> themselves, captured in the act of rapidly changing by modern remote sensors! The saw-toothed record of sea-level change over past glacial-interglacial cycles required the existence of rapid ice loss processes. Satellite based observations, supported by hard-earned field observations have extended the time scale over which ice <span class="hlt">sheets</span> can suddenly change to ever shorter intervals: from centuries, to decades, to years to even minutes. As changes continue to be observed, the scientific community is forced to consider new or previously ignored processes to explain these observations. The penultimate goal of ice-<span class="hlt">sheet</span> dynamics is to credibly predict the future of both the Greenland and Antarctic ice <span class="hlt">sheets</span>. In this important endeavor, there is no substitute for our ability to observe. Without the extensive data sets provided by remote sensing, numerical models can be neither tested nor improved. The impact of remote sensing on our existing ability to predict the future must be compared to our probable state of knowledge and ability were these data never collected. Among many satellite observed phenomena we would be largely or wholly ignorant of are the recent acceleration of ice throughout much of coastal Greenland; the sudden disintegration of multiple ice shelves along the Antarctic Peninsula; and the dramatic thinning and acceleration of the Amundsen Sea sector of West Antarctica. These</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5456546','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5456546"><span>Buckling Behavior of Substrate Supported Graphene <span class="hlt">Sheets</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Yang, Kuijian; Chen, Yuli; Pan, Fei; Wang, Shengtao; Ma, Yong; Liu, Qijun</p> <p>2016-01-01</p> <p>The buckling of graphene <span class="hlt">sheets</span> on substrates can significantly degrade their performance in materials and devices. Therefore, a systematic investigation on the buckling behavior of monolayer graphene <span class="hlt">sheet</span>/substrate systems is carried out in this paper by both molecular mechanics simulations and theoretical analysis. From 70 simulation cases of simple-supported graphene <span class="hlt">sheets</span> with different sizes under uniaxial compression, two different buckling modes are investigated and revealed to be dominated by the graphene size. Especially, for graphene <span class="hlt">sheets</span> with length larger than 3 nm and width larger than 1.1 nm, the buckling mode depends only on the length/width ratio. Besides, it is revealed that the existence of graphene substrate can increase the critical buckling stress and strain to 4.39 N/m and 1.58%, respectively, which are about 10 times those for free-standing graphene <span class="hlt">sheets</span>. Moreover, for graphene <span class="hlt">sheets</span> with common size (longer than 20 nm), both theoretical and simulation results show that the critical buckling stress and strain are dominated only by the adhesive interactions with substrate and independent of the graphene size. Results in this work provide valuable insight and guidelines for the design and application of graphene-derived materials and nano-electromechanical systems. PMID:28787831</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930004962','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930004962"><span>Current status of liquid <span class="hlt">sheet</span> radiator research</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chubb, Donald L.; Calfo, Frederick D.; Mcmaster, Matthew S.</p> <p>1993-01-01</p> <p>Initial research on the external flow, low mass liquid <span class="hlt">sheet</span> radiator (LSR), has been concentrated on understanding its fluid mechanics. The surface tension forces acting at the edges of the <span class="hlt">sheet</span> produce a triangular planform for the radiating surface of width, W, and length, L. It has been experimentally verified that (exp L)/W agrees with the theoretical result, L/W = (We/8)exp 1/2, where We is the Weber number. Instability can cause holes to form in regions of large curvature such as where the edge cylinders join the <span class="hlt">sheet</span> of thickness, tau. The W/tau limit that will cause hole formation with subsequent destruction of the <span class="hlt">sheet</span> has yet to be reached experimentally. Although experimental measurements of <span class="hlt">sheet</span> emissivity have not yet been performed because of limited program scope, calculations of the emissivity and <span class="hlt">sheet</span> lifetime is determined by evaporation losses were made for two silicon based oils; Dow Corning 705 and Me(sub 2). Emissivities greater than 0.75 are calculated for tau greater than or equal to 200 microns for both oils. Lifetimes for Me(sub 2) are much longer than lifetimes for 705. Therefore, Me(sub 2) is the more attractive working fluid for higher temperatures (T greater than or equal to 400 K).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15458633','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15458633"><span>Anatomy of an amyloidogenic intermediate: conversion of beta-<span class="hlt">sheet</span> to alpha-<span class="hlt">sheet</span> structure in transthyretin at acidic pH.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Armen, Roger S; Alonso, Darwin O V; Daggett, Valerie</p> <p>2004-10-01</p> <p>The homotetramer of transthyretin (TTR) dissociates into a monomeric amyloidogenic intermediate that self-assembles into amyloid fibrils at low pH. We have performed molecular dynamics simulations of monomeric TTR at neutral and low pH at physiological (310 K) and very elevated temperature (498 K). In the low-pH simulations at both temperatures, one of the two beta-<span class="hlt">sheets</span> (strands CBEF) becomes disrupted, and alpha-<span class="hlt">sheet</span> structure forms in the other <span class="hlt">sheet</span> (strands DAGH). alpha-<span class="hlt">sheet</span> is formed by alternating alphaL and alphaR residues, and it was first proposed by Pauling and Corey. Overall, the simulations are in agreement with the available experimental observations, including solid-state NMR results for a TTR-peptide amyloid. In addition, they provide a unique explanation for the results of hydrogen exchange experiments of the amyloidogenic intermediate-results that are difficult to explain with beta-structure. We propose that alpha-<span class="hlt">sheet</span> may represent a key pathological conformation during amyloidogenesis. Copyright 2004 Elsevier Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=wind+AND+energy+AND+texas&id=ED363712','ERIC'); return false;" href="https://eric.ed.gov/?q=wind+AND+energy+AND+texas&id=ED363712"><span>Technology Systems. Laboratory <span class="hlt">Activities</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Brame, Ray; And Others</p> <p></p> <p>This guide contains 43 modules of laboratory <span class="hlt">activities</span> for technology education courses. Each module includes an instructor's resource <span class="hlt">sheet</span> and the student laboratory <span class="hlt">activity</span>. Instructor's resource <span class="hlt">sheets</span> include some or all of the following elements: module number, course title, <span class="hlt">activity</span> topic, estimated time, essential elements, objectives,…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17434737','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17434737"><span>The use of a daily goals <span class="hlt">sheet</span> to improve communication in the paediatric intensive care unit.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Phipps, Lorri M; Thomas, Neal J</p> <p>2007-10-01</p> <p>To assess the impact of the implementation of a daily goals <span class="hlt">sheet</span> upon nursing perception of communication in an academic, tertiary care paediatric intensive care unit (PICU). Prospective, longitudinal, before-and-after intervention surveys. University affiliated 12-bed PICU. Bedside nurses. A questionnaire was administered to PICU nurses addressing their perception of communication. Following this questionnaire, the use of a daily goals <span class="hlt">sheet</span> was instituted. A second questionnaire was administered one year later. Mann-Whitney Rank Sum Test was used to compare differences of the graded outcome variables. The primary outcome was the perception of communication taken from a nursing perspective. Eighty-five percent of nurses felt the daily goals <span class="hlt">sheet</span> led to improved communication between physicians and nurses in the PICU. All questions related to communication demonstrated a positive influence of the goals <span class="hlt">sheet</span>, with the perception of the PICU staff working as a team reaching statistical significance (p=0.05). The perception of the care of one surgical service being attending physician <span class="hlt">directed</span> also significantly improved after the institution of the goals <span class="hlt">sheet</span> (p=0.04). The institution of a daily goals <span class="hlt">sheet</span> led to an improvement in nursing perception of communication. Future studies are required to determine if this change in process has a demonstrable effect on health care outcomes of critically ill children, or whether this tool can have the same beneficial effects in other academic and non-academic PICUs.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_25 --> <div class="footer-extlink text-muted" style="margin-bottom:1rem; text-align:center;">Some links on this page may take you to non-federal websites. 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