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Sample records for cai tien giong

  1. Skinner and CAI.

    ERIC Educational Resources Information Center

    Chandler, Harry N.

    1984-01-01

    The author cites comments of B.F. Skinner supporting the benefits of carefully constructed computer assisted instruction (CAI) programs. Preliminary studies on military populations suggesting the value of CAI are discussed, as is the collection of information about software. (CL)

  2. Developing Large CAI Packages.

    ERIC Educational Resources Information Center

    Reed, Mary Jac M.; Smith, Lynn H.

    1983-01-01

    When developing large computer-assisted instructional (CAI) courseware packages, it is suggested that there be more attentive planning to the overall package design before actual lesson development is begun. This process has been simplified by modifying the systems approach used to develop single CAI lessons, followed by planning for the…

  3. Competition in Individualized CAI.

    ERIC Educational Resources Information Center

    Hativa, Nira; And Others

    1993-01-01

    Examines the effects of competition and cooperation on learning through computer-assisted instruction (CAI). A questionnaire was administered to 457 Israeli fourth graders who used two CAI arithmetic systems. The characteristics of the systems are discussed, and the results of the survey are correlated to students' gender and achievement levels.…

  4. A Modular CAI System.

    ERIC Educational Resources Information Center

    Van Der Mast, Charles

    The experimental CAI system which is being tested at Delft University of Technology is structured in a modular manner to account for high changeability. The concept formulated for this project was the outcome of research into technological, organizational, and educational developments in CAI, and the enumeration of the common aspects of the…

  5. Experience with the CAIS

    NASA Technical Reports Server (NTRS)

    Tighe, Michael F.

    1986-01-01

    Intermetrics' experience is that the Ada package construct, which allows separation of specification and implementation allows specification of a CAIS that is transportable across varying hardware and software bases. Additionally, the CAIS is an excellent basis for providing operating system functionality to Ada applications. By allowing the Byron APSE to be moved easily from system to system, and allowing significant re-writes of underlying code. Ada and the CAIS provide portability as well as transparency to change at the application operating system interface level.

  6. Carbon, CAIs and chondrules

    NASA Technical Reports Server (NTRS)

    Ash, R. D.; Russell, S. S.

    1994-01-01

    It has been shown that C is present in CAI's and chondrules. It can be distinguished from matrix C both by its thermal stability and isotopic composition, which implies that it was not introduced after parent body accretion. It is concluded that C must have been present in the chondrule and CAI precursor material. Therefore any models of chondrule and CAI formation and inferences drawn about solar system conditions during these events must take into account the consequences of the presence of C on inclusion chemistry, mineralogy, and oxidation state.

  7. The CAIS 2 Project

    NASA Technical Reports Server (NTRS)

    Legrand, Sue; Thall, Richard

    1986-01-01

    The Common APSE Interface Set (CAIS) is a proposed MIL-STD intended to promote the portability of Ada Programming Support Environment (APSE) tools written in Ada. The standardized interfaces define a virtual operating system, from which portable tools derive their basic services, e.g., file management, input/output, communications, and process control. In the Ada world, such a virtual operating system is called a Kernel Ada Programming Support Environment (KAPSE). The CAIS is a standardized interface between KAPSEs and tools. The CAIS has been proposed as a starting point for standard interfaces to be used in the NASA Software Support Environment (SSE) for the Space Station Program. The status of the CAIS standardization effort and plans for further development are described.

  8. The Ontario CAI Network.

    ERIC Educational Resources Information Center

    Olivier, W. P.

    The evolution and current operation of the Ontario Computer Assisted Instruction (CAI) Network are described. Sponsored by the Ontario Institute for Studies in Education and including 11 community colleges in Ontario, the network has computer installations and access devices throughout the province. Initial development work was done using a…

  9. Maxi CAI with a Micro.

    ERIC Educational Resources Information Center

    Gerhold, George; And Others

    This paper describes an effective microprocessor-based CAI system which has been repeatedly tested by a large number of students and edited accordingly. Tasks not suitable for microprocessor based systems (authoring, testing, and debugging) were handled on larger multi-terminal systems. This approach requires that the CAI language used on the…

  10. Teacher's Handbook for CAI Courses.

    ERIC Educational Resources Information Center

    Suppes, Patrick; And Others

    The handbooks for the most widely used computer-assisted instruction (CAI) courses now available on computer terminals at the Institute for Mathematical Studies in the Social Sciences at Stanford University are presented. Handbooks are included for the following courses: Strands Drill-and-practice (arithmetic fundamentals for fourth grade), Logic…

  11. Timing Students' Answers in CAI.

    ERIC Educational Resources Information Center

    Hativa, Nira; And Others

    1991-01-01

    Discussion of limiting response time for students' answers focuses on a study of Israeli elementary students that investigated the effects on their performance of increasing the response time in computer-assisted instruction (CAI) for arithmetic drill and practice. Effects on high- versus low-aptitude students, and younger versus older, are…

  12. CAI in Advanced Literature Class.

    ERIC Educational Resources Information Center

    Hinton, Norman

    1981-01-01

    Ways that computer assisted instruction (CAI) can be useful in teaching English at upperclass and graduate levels are considered, with illustrations from PLATO lessons that have been composed and programmed. One lesson takes advantage of PLATO's graphic design capabilities, which enabled the teacher to design the runic figures and to show them in…

  13. Evaluating CAI Material for the Microcomputer.

    ERIC Educational Resources Information Center

    Ashmore, Timothy M.

    The relative worth of any evaluation instrument depends on user needs and the material being evaluated. Potential users of a good computer assisted instruction (CAI) instrument include purchasers, authors, reviewers, and publishers of CAI materials. Although each user has unique needs, a good instrument will serve both to educate and discriminate,…

  14. Some "Facts" about CAI: 1976 in Depth.

    ERIC Educational Resources Information Center

    Kearsley, Greg P.

    This report presents information about the state of the art in Computer Assisted Instruction (CAI) in 1976. This information takes the form of quantitative data (mostly frequency distributions), on the number and average completion time of CAI programs according to subject matter, author, language, instructional strategies, sources, and central…

  15. The Screen Display Syntax for CAI.

    ERIC Educational Resources Information Center

    Richards, Boyd F.; Salisbury, David F.

    1987-01-01

    Describes four storyboard techniques frequently used in designing computer assisted instruction (CAI) programs, and explains screen display syntax (SDS), a new technique combining the major advantages of the storyboard techniques. SDS was developed to facilitate communication among designers, programmers, and editors working on a large CAI basic…

  16. A unified framework for producing CAI melting, Wark-Lovering rims and bowl-shaped CAIs

    NASA Astrophysics Data System (ADS)

    Liffman, Kurt; Cuello, Nicolas; Paterson, David A.

    2016-10-01

    Calcium-Aluminium inclusions (CAIs) formed in the Solar system, some 4567 million years ago. CAIs are almost always surrounded by Wark-Lovering rims (WLRs), which are a sequence of thin, mono/bi-mineralic layers of refractory minerals, with a total thickness in the range of 1-100 microns. Recently, some CAIs have been found that have tektite-like bowl-shapes. To form such shapes, the CAI must have travelled through a rarefied gas at hypersonic speeds. We show how CAIs may have been ejected from the inner solar accretion disc via the centrifugal interaction between the solar magnetosphere and the inner disc rim. They subsequently punched through the hot, inner disc rim wall at hypersonic speeds. This re-entry heating partially or completely evaporated the CAIs. Such evaporation could have significantly increased the metal abundances of the inner disc rim. High speed movement through the inner disc produced WLRs. To match the observed thickness of WLRs required metal abundances at the inner disc wall that are of order 10 times that of standard solar abundances. The CAIs cooled as they moved away from the protosun, the deduced CAI cooling rates are consistent with the CAI cooling rates obtained from experiment and observation. The speeds and gas densities required to form bowl-shaped CAIs are also consistent with the expected speeds and gas densities for larger, ˜1 cm, CAIs punching through an inner accretion disc wall.

  17. A risk management approach to CAIS development

    NASA Technical Reports Server (NTRS)

    Hart, Hal; Kerner, Judy; Alden, Tony; Belz, Frank; Tadman, Frank

    1986-01-01

    The proposed DoD standard Common APSE Interface Set (CAIS) was developed as a framework set of interfaces that will support the transportability and interoperability of tools in the support environments of the future. While the current CAIS version is a promising start toward fulfilling those goals and current prototypes provide adequate testbeds for investigations in support of completing specifications for a full CAIS, there are many reasons why the proposed CAIS might fail to become a usable product and the foundation of next-generation (1990'S) project support environments such as NASA's Space Station software support environment. The most critical threats to the viability and acceptance of the CAIS include performance issues (especially in piggybacked implementations), transportability, and security requirements. To make the situation worse, the solution to some of these threats appears to be at conflict with the solutions to others.

  18. CAIS. Condition Assessment Information System

    SciTech Connect

    Oak, J.C.

    1996-09-30

    CAIS is used by Architects and Engineers to gather facility condition assessment data. This data consist of architectural, civil, structural, electrical, and mechanical systems and components that are a part of the inspected facility. Data is collected using a hand-held, pen-based computer system which is preprogrammed for detailed inventories of individual components. The program is deficiency based for collecting data for repair and replacement observations. Observations are recorded on checklists preformatted to individual site needs, allowing for comments on unusual conditions to be documented on site. Data is transferred to a central database, where it can be reviewed, costed, and reported on using different scenarios. Information can be transferred to the DOE operations offices as well as to the DOE FIMS database for each site.

  19. CAIs in Semarkona (LL3.0)

    NASA Technical Reports Server (NTRS)

    Mishra, R. K.; Simon, J. I.; Ross, D. K.; Marhas, K. K.

    2016-01-01

    Calcium, Aluminum-rich inclusions (CAIs) are the first forming solids of the Solar system. Their observed abundance, mean size, and mineralogy vary quite significantly between different groups of chondrites. These differences may reflect the dynamics and distinct cosmochemical conditions present in the region(s) of the protoplanetary disk from which each type likely accreted. Only about 11 such objects have been found in L and LL type while another 57 have been found in H type ordinary chondrites, compared to thousands in carbonaceous chondrites. At issue is whether the rare CAIs contained in ordinary chondrites truly reflect a distinct population from the inclusions commonly found in other chondrite types. Semarkona (LL3.00) (fall, 691 g) is the most pristine chondrite available in our meteorite collection. Here we report petrography and mineralogy of 3 CAIs from Semarkona

  20. Re-Os Systematics in the Allende CAI: Big AL

    NASA Astrophysics Data System (ADS)

    Chen, J. H.; Papanastassiou, D. A.; Wasserburg, G. J.

    1999-03-01

    A sample of coarse-grained Allende CAI, Big Al analyzed using reverse aqua regia, plots on the IIA iron meteorite reference isochron, suggesting a very small time difference between the formation of CAIs, chondrites, and iron.

  1. Jurassic evolution of the Tien-Shan

    SciTech Connect

    Bebeshev, I.I.

    1994-09-01

    Complex studies led to identification of three stages in Jurassic deposits. The stages reflect development periods of the studied deposits. Each stage is represented by a paleogeographic map that indicates the evolution of ancient landforms in the Tien-Shan region in time and space.

  2. The Relevance of AI Research to CAI.

    ERIC Educational Resources Information Center

    Kearsley, Greg P.

    This article provides a tutorial introduction to Artificial Intelligence (AI) research for those involved in Computer Assisted Instruction (CAI). The general theme is that much of the current work in AI, particularly in the areas of natural language understanding systems, rule induction, programming languages, and socratic systems, has important…

  3. CAI Use by Developmental Studies Students.

    ERIC Educational Resources Information Center

    Crumb, Glenn H.; Monroe, Eula Ewing

    This study, conducted with college developmental studies students, explored possible relationships between individualized computer-assisted instruction (CAI) in basic mathematics skills and each of two variables; mathematics knowledge and anxiety toward mathematics. Both experimental (N=5) and control (N=12) groups made significant gains in…

  4. Tien Shan Geohazards Database: Earthquakes and landslides

    NASA Astrophysics Data System (ADS)

    Havenith, H. B.; Strom, A.; Torgoev, I.; Torgoev, A.; Lamair, L.; Ischuk, A.; Abdrakhmatov, K.

    2015-11-01

    In this paper we present new and review already existing landslide and earthquake data for a large part of the Tien Shan, Central Asia. For the same area, only partial databases for sub-regions have been presented previously. They were compiled and new data were added to fill the gaps between the databases. Major new inputs are products of the Central Asia Seismic Risk Initiative (CASRI): a tentative digital map of active faults (even with indication of characteristic or possible maximum magnitude) and the earthquake catalogue of Central Asia until 2009 that was now updated with USGS data (to May 2014). The new compiled landslide inventory contains existing records of 1600 previously mapped mass movements and more than 1800 new landslide data. Considering presently available seismo-tectonic and landslide data, a target region of 1200 km (E-W) by 600 km (N-S) was defined for the production of more or less continuous geohazards information. This target region includes the entire Kyrgyz Tien Shan, the South-Western Tien Shan in Tajikistan, the Fergana Basin (Kyrgyzstan, Tajikistan and Uzbekistan) as well as the Western part in Uzbekistan, the North-Easternmost part in Kazakhstan and a small part of the Eastern Chinese Tien Shan (for the zones outside Kyrgyzstan and Tajikistan, only limited information was available and compiled). On the basis of the new landslide inventory and the updated earthquake catalogue, the link between landslide and earthquake activity is analysed. First, size-frequency relationships are studied for both types of geohazards, in terms of Gutenberg-Richter Law for the earthquakes and in terms of probability density function for the landslides. For several regions and major earthquake events, case histories are presented to outline further the close connection between earthquake and landslide hazards in the Tien Shan. From this study, we concluded first that a major hazard component is still now insufficiently known for both types of geohazards

  5. GPS survey of the western Tien Shan

    NASA Technical Reports Server (NTRS)

    Molnar, Peter H.

    1994-01-01

    This report summarizes the background, field work, data collection and analysis, and future plans associated with a collaborative GPS experiment in the Tien Shan of the former Soviet Union. This project involves the amalgamation of two, separately funded projects, which were proposed separately by PIs Hamburger and Reilinger (NSF number EAR-9115159 and NASA number NAG5-1941) and Molnar and Hager (NSF number EAR9117889 and NASA number NAG5-1947). In addition, the work is being conducted under the auspices of the US-USSR Agreement on Cooperation in the Field of Environmental Protection, with support from the United States Geological Survey.

  6. NALDA (Naval Aviation Logistics Data Analysis) CAI (computer aided instruction)

    SciTech Connect

    Handler, B.H. ); France, P.A.; Frey, S.C.; Gaubas, N.F.; Hyland, K.J.; Lindsey, A.M.; Manley, D.O. ); Hunnum, W.H. ); Smith, D.L. )

    1990-07-01

    Data Systems Engineering Organization (DSEO) personnel developed a prototype computer aided instruction CAI system for the Naval Aviation Logistics Data Analysis (NALDA) system. The objective of this project was to provide a CAI prototype that could be used as an enhancement to existing NALDA training. The CAI prototype project was performed in phases. The task undertaken in Phase I was to analyze the problem and the alternative solutions and to develop a set of recommendations on how best to proceed. The findings from Phase I are documented in Recommended CAI Approach for the NALDA System (Duncan et al., 1987). In Phase II, a structured design and specifications were developed, and a prototype CAI system was created. A report, NALDA CAI Prototype: Phase II Final Report, was written to record the findings and results of Phase II. NALDA CAI: Recommendations for an Advanced Instructional Model, is comprised of related papers encompassing research on computer aided instruction CAI, newly developing training technologies, instructional systems development, and an Advanced Instructional Model. These topics were selected because of their relevancy to the CAI needs of NALDA. These papers provide general background information on various aspects of CAI and give a broad overview of new technologies and their impact on the future design and development of training programs. The paper within have been index separately elsewhere.

  7. GPS survey of the western Tien Shan

    NASA Technical Reports Server (NTRS)

    Hager, Bradford H.; Molnar, Peter H.; Hamburger, Michael W.; Reilinger, Robert E.

    1995-01-01

    There were two major developments in 1994 in our collaborative GPS experiment in the Tien Shan of the Former Soviet Union (FSU). Both were motivated by our expectation that we will ultimately obtain better science at lower cost if we involve our colleagues in the FSU more deeply in (1) the collection and (2) the analysis of data. As an experimental test of the concept of having our local collaborators carry out the field work semi-autonomously, we sent 6 MIT receivers to the Tien Shan for a period of 3 months. To enable our collaborators to have the capability for data analysis, we provided computers for two data analysis centers and organized a two-week training session. This report emphasizes the rationale for deeper involvement of FSU scientists, describes the training sessions, discusses the data collection, and presents the results. We also discuss future plans. More detailed discussion of background, general scientific objectives, discussions with collaborators, and results for the campaigns in 1992 and 1993 have been given in previous reports.

  8. Research on TRIZ and CAIs Application Problems for Technology Innovation

    NASA Astrophysics Data System (ADS)

    Li, Xiangdong; Li, Qinghai; Bai, Zhonghang; Geng, Lixiao

    In order to realize application of invent problem solve theory (TRIZ) and computer aided innovation software (CAIs) , need to solve some key problems, such as the mode choice of technology innovation, establishment of technology innovation organization network(TION), and achievement of innovative process based on TRIZ and CAIs, etc.. This paper shows that the demands for TRIZ and CAIs according to the characteristics and existing problem of the manufacturing enterprises. Have explained that the manufacturing enterprises need to set up an open TION of enterprise leading type, and achieve the longitudinal cooperation innovation with institution of higher learning. The process of technology innovation based on TRIZ and CAIs has been set up from researching and developing point of view. Application of TRIZ and CAIs in FY Company has been summarized. The application effect of TRIZ and CAIs has been explained using technology innovation of the close goggle valve product.

  9. Physical properties of CAI-rich asteroids

    NASA Astrophysics Data System (ADS)

    Tanga, P.; Devogele, M.; Cellino, A.; Pinilla-Alonso, N.; Campins, H.; Bus, S. J.

    2015-12-01

    Some L-type asteroids (collectively called "Barbarians") are known to exhibit an anomalous polarimetric behavior, whose origin - still to be elucidated - can be related to compositional and/or scattering effects. The fact that these asteroids belong to the same taxonomic class (following the De Meo 2009 classification, including NIR) implies that composition must play a role. Sunshine et al. 2008 showed that these asteroids contain high amounts of CAIs, possibly hinting to a formation in an early proto-planetary environment, very rich in refractory material. On the base of this evidence, we started an observational campaign to increase the data coverage of these objects, by obtaining new NIR spectra, photometric and polarimetric measurements. Our first results show that the peculiar features are not restricted to polarimetry. In particular we show the existence of an anomalous distribution of the rotation periods, and a possible relation between CAI abundance and albedos determined by WISE. We tentatively discuss a possible scenario justifying the different observed features.

  10. Oxygen Isotopes of CAIs from Unequilibrated Enstatite Chondrites: Characteristics and Implications

    NASA Technical Reports Server (NTRS)

    Guan, Y.; McKeegan, K. D.; MacPherson, G. J.

    2000-01-01

    Ion microprobe analyses of ten CAIs from enstatite chondrites show large O-16 excesses similar to CAIs in carbonaceous and ordinary chondrites, supporting the idea that most CAIs formed in a restricted nebular locale.

  11. A CAI Study of Learning Geologic Time and Evolution.

    ERIC Educational Resources Information Center

    Young, James P.; Stolurow, Lawrence M.

    Twenty-two college students in science education were given an adjunctive computer-assisted instruction (CAI) program by means of typewriter consoles and computer-controlled colored slide presentations of critical information. Students were pretested, told how to respond at the student console, taught by the Harvard CAI System, and posttested. The…

  12. Effect of CAI on Achievement of LD Students in English

    ERIC Educational Resources Information Center

    Sivaram, R. T.; Ramar, R.

    2014-01-01

    The present experimental study was undertaken with three objectives in view, (i) to identify students with language learning disabilities (ii) to develop CAI software to teach LD students through computer-assisted instruction and (iii) to measure the effectiveness of CAI with special reference to LD students. Two matched groups of LD students were…

  13. High School Students Participate in a CAI Study Skills Program.

    ERIC Educational Resources Information Center

    Gadzella, Bernadette M.

    A 10-module computer-assisted instruction (CAI) program on study skills was field tested to determine its effectiveness with high school students, using 50 advanced seniors in a large Texas high school as subjects. The program consisted of a study skills pretest, the CAI modules, a notebook on study skills, and a posttest. The modules were…

  14. Marshall McLuhan and the Case Against CAI.

    ERIC Educational Resources Information Center

    Hirvela, Alan

    1988-01-01

    Presents some of the conventional arguments against computer assisted instruction (CAI) in language education and explores humanistic concerns raised in the works of Marshall McLuhan. It is concluded that CAI is introduced into the instructional process before proper research has demonstrated that this method of teaching is not harmful for…

  15. Creation and Distribution of CAIs in the Protoplanetary Nebula

    NASA Technical Reports Server (NTRS)

    Cuzzi, J. N.; Davis, S. S.; Dobrovolskis, A. R.

    2003-01-01

    CaAl rich refractory mineral inclusions (CAIs) found at 1 - 10% mass fraction in primitive chondrites appear to be several million years older than the dominant (chondrule) components in the same parent bodies. A prevalent concern is that it is difficult to retain CAIs for this long against gas-drag-induced radial drift into the sun. We assess a hot inner (turbulent) nebula context for CAI formation, using analytical models of nebula evolution and particle diffusion. We show that outward radial diffusion in a weakly turbulent nebula can prevent significant numbers of CAI-size particles from being lost into the sun for times of 1 - 3 x 10(exp 6) years. To match the CAI abundances quantitatively, we advocate an enhancement of the inner hot nebula in silicate-forming material, due to rapid inward migration of very primitive, silicate and carbon rich, meter-sized objects. 'Combustion' of the carbon into CO would make the CAI formation environment more reduced than solar, as certain observations imply. Abundant CO might also play a role in mass-independent chemical fractionation of oxygen isotopes as seen in CAIs and associated primitive, high-temperature condensates.

  16. Astrophysics of CAI formation as revealed by silicon isotope LA-MC-ICPMS of an igneous CAI

    NASA Astrophysics Data System (ADS)

    Shahar, Anat; Young, Edward D.

    2007-05-01

    Silicon isotope ratios of a typical CAI from the Leoville carbonaceous chondrite, obtained in situ by laser ablation MC-ICPMS, together with existing 25Mg/ 24Mg data, reveal a detailed picture of the astrophysical setting of CAI melting and subsequent heating. Models for the chemical and isotopic effects of evaporation of the molten CAI are used to produce a univariant relationship between PH 2 and time during melting. The result shows that this CAI was molten for a cumulative time of no more than 70 days and probably less than 15 days depending on temperature. The object could have been molten for an integrated time of just a few hours if isotope ratio zoning was eliminated after melting by high subsolidus temperatures (e.g., > 1300 K) for ˜ 500 yr. In all cases subsolidus heating sufficient to produce diffusion-limited isotope fractionation at the margin of the solidified CAI is required. These stable isotope data point to a two-stage history for this igneous CAI involving melting for a cumulative timescale of hours to months followed by subsolidus heating for years to hundreds of years. The thermobarometric history deduced from combining Si and Mg isotope ratio data implicates thermal processing in the disk, perhaps by passage through shockwaves, following melting. This study underscores the direct link between the meaning of stable isotope ratio zoning, or lack thereof, and the inferred astrophysical setting of melting and subsequent processing of CAIs.

  17. A CAI in the Ivuna CI1 Chondrite

    NASA Technical Reports Server (NTRS)

    Frank, David R.; Zolensky, M.; Martinez, J.; Mikouchi, T.; Ohsumi, K.; Hagiya, K.; Satake, W.; Le, L.; Ross, D.; Peslier, A.

    2011-01-01

    We have recently discovered the first well-preserved calcium aluminum-rich inclusion (CAI) in a CI1 chondrite (Ivuna). Previously, all CI1 chondrites were thought to be devoid of preserved CAI and chondrules due to the near total aqueous alteration to which their parent body (bodies) have been subjected. The CAI is roughly spherical, but with a slight teardrop geometry and a maximum diameter of 170 microns (fig. 1). It lacks any Wark-Lovering Rim. Incipient aqueous alteration, and probably shock, have rendered large portions of the CAI poorly crystalline. It is extremely fine-grained, with only a few grains exceeding 10 microns. We have performed electron microprobe analyses (EPMA), FEG-SEM imaging and element mapping, as well as electron back-scattered diffraction (EBSD) and synchrotron X-ray diffraction (SXRD) in order to determine the fundamental characteristics of this apparently unique object.

  18. Lunar and Planetary Science XXXV: Chondrules and CAIs

    NASA Technical Reports Server (NTRS)

    2004-01-01

    The session "Chondrules and CAI's" included the following reports:Metallic Chondrules in NWA 1390 (H3-6): Clues to Their History from Metallic Cu; Relationship Between Bulk Chemical Composition and Formation Age of Chondrules in Bishunpur and Krymka; Relict Forsterite in Chondrules: Implications for Cooling Rates; An Evaluation of Quantitative Methods of Determining the Degree of Melting Experienced by a Chondrule; Rare Earth Element Fractionation in Chondrules; Mineralogy and Petrology of Chondrules in Carbonaceous Chondrite NWA 770; Isotopic Cosmobarometry: A Synthesis of Concepts and Implications for Chondrule and CAI Formation Mechanisms; Further Investigations of Minor Element Distributions in Spinels in Type B CAIs; and Trace Element Compositions of the Sublayers Making Up W-L Rims on CAI .

  19. NEW TITANIUM ISOTOPE DATA FOR ALLENDE AND EFREMOVKA CAIs

    SciTech Connect

    Leya, Ingo; Schoenbaechler, Maria; Kraehenbuehl, Urs; Halliday, Alex N.

    2009-09-10

    We measured the titanium (Ti) isotope composition, i.e., {sup 50}Ti/{sup 47}Ti, {sup 48}Ti/{sup 47}Ti, and {sup 46}Ti/{sup 47}Ti, in five calcium-rich-aluminum-rich refractory inclusions (CAIs) from the oxidized CV3 chondrite Allende and in two CAIs from the reduced CV3 chondrite Efremovka. Our data indicate that CAIs are enriched in {sup 50}Ti/{sup 47}Ti and {sup 46}Ti/{sup 47}Ti and are slightly depleted in {sup 48}Ti/{sup 47}Ti compared to normal Ti defined by ordinary chondrites, eucrites, ureilites, mesosiderites, Earth, Moon, and Mars. Some CAIs have an additional {sup 50}Ti excess of {approx}8{epsilon} relative to bulk carbonaceous chondrites, which are enriched in {sup 50}Ti by {approx}2{epsilon} relative to terrestrial values, leading to a total excess of {approx}10{epsilon}. This additional {sup 50}Ti excess is correlated with nucleosynthetic anomalies found in {sup 62}Ni and {sup 96}Zr, all indicating an origin from a neutron-rich stellar source. Bulk carbonaceous chondrites show a similar trend, however, the extent of the anomalies is either less than or similar to the smallest anomalies seen in CAIs. Mass balance calculations suggest that bulk Allende Ti possibly consists of a mixture of at least two Ti components, anomalous Ti located in CAIs and a normal component possibly for matrix and chondrules. This argues for a heterogeneous distribution of Ti isotopes in the solar system. The finding that anomalous Ti is concentrated in CAIs suggests that CAIs formed in a specific region of the solar system and were, after their formation, not homogeneously redistributed within the solar system. Combining the CAI data with improved model predictions for early solar system irradiation effects indicates that a local production scenario for the relatively short lived radionuclides can be excluded, because the production of, e.g., {sup 10}Be, {sup 26}Al, and {sup 41}Ca, would result in a significant collateral shift in Ti isotopes, which is not seen in the

  20. Numerical simulation and validation of SI-CAI hybrid combustion in a CAI/HCCI gasoline engine

    NASA Astrophysics Data System (ADS)

    Wang, Xinyan; Xie, Hui; Xie, Liyan; Zhang, Lianfang; Li, Le; Chen, Tao; Zhao, Hua

    2013-02-01

    SI-CAI hybrid combustion, also known as spark-assisted compression ignition (SACI), is a promising concept to extend the operating range of CAI (Controlled Auto-Ignition) and achieve the smooth transition between spark ignition (SI) and CAI in the gasoline engine. In this study, a SI-CAI hybrid combustion model (HCM) has been constructed on the basis of the 3-Zones Extended Coherent Flame Model (ECFM3Z). An ignition model is included to initiate the ECFM3Z calculation and induce the flame propagation. In order to precisely depict the subsequent auto-ignition process of the unburned fuel and air mixture independently after the initiation of flame propagation, the tabulated chemistry concept is adopted to describe the auto-ignition chemistry. The methodology for extracting tabulated parameters from the chemical kinetics calculations is developed so that both cool flame reactions and main auto-ignition combustion can be well captured under a wider range of thermodynamic conditions. The SI-CAI hybrid combustion model (HCM) is then applied in the three-dimensional computational fluid dynamics (3-D CFD) engine simulation. The simulation results are compared with the experimental data obtained from a single cylinder VVA engine. The detailed analysis of the simulations demonstrates that the SI-CAI hybrid combustion process is characterised with the early flame propagation and subsequent multi-site auto-ignition around the main flame front, which is consistent with the optical results reported by other researchers. Besides, the systematic study of the in-cylinder condition reveals the influence mechanism of the early flame propagation on the subsequent auto-ignition.

  1. Effects of CAI on the Academic Performance and Attitudes of College Students

    ERIC Educational Resources Information Center

    Luyben, Paul D.; Hipworth, Kristin; Pappas, Thomas

    2003-01-01

    Although computer-assisted instruction (CAI) favorably affects academic performance and attitudes toward instruction, most CAI programs target mastery but not fluency. This study used a within-subjects, crossover design to compare the effects of CAI that included fluency training with traditional study (TS) conditions on test performance and…

  2. Computer-Assisted Instruction in Clinical Education: A Roadmap to Increasing CAI Implementation

    ERIC Educational Resources Information Center

    Berman, Norman B.; Fall, Leslie H.; Maloney, Christopher G.; Levine, David A.

    2008-01-01

    This reflection is based on the premise that clinical education can be improved by more widespread use of computer-assisted instruction (CAI) and that a roadmap will enable more medical educators to begin using CAI. The rationale for CAI use includes many of its inherent features such as incorporation of multimedia and interactivity yet the use of…

  3. Development of CAI Presentations for Science Teaching and Overview of Research Findings

    ERIC Educational Resources Information Center

    Ranade, Mridula D.

    2006-01-01

    Research suggests that information and communication technologies (ICT) used in the form of computer assisted instruction (CAI) may benefit student learning. There is, however, limited research about the application of CAI in non-Western educational contexts. Here I describe the use of CAI in the learning of science in India. Evaluation of student…

  4. Effectiveness of CAI Package on Achievement in Physics of IX Standard Students

    ERIC Educational Resources Information Center

    Maheswari, I. Uma; Ramakrishnan, N.

    2015-01-01

    The present study is an experimental one in nature, to find out the effectiveness of CAI package on in Physics of IX std. students. For this purpose a CAI package was developed and validated. The validated CAI package formed an independent variable of this study. The dependent variable is students' achievements in physics content. In order to find…

  5. MONIFORMS as Authoring Aids for the PLATO IV CAI System.

    ERIC Educational Resources Information Center

    Schulz, Russel E.

    An analysis of portions of the HumRRO (Human Resources Research Organization) developed computer-assisted instruction (CAI) course in COBOL programing, and a survey of representatives from Advanced Research Project Agency (ARPA) PLATO IV installations indicated a need for authoring aids that could be prepared and programed easily and quickly. The…

  6. An Intelligent CAI Monitor and Generative Tutor. Interim Report.

    ERIC Educational Resources Information Center

    Koffman, Elliot B.; And Others

    Design techniques for generative computer-assisted-instructional (CAI) systems are described in this report. These are systems capable of generating problems for students and of deriving and monitoring solutions; problem difficulty, instructional pace, and depth of monitoring are all individually tailored and parts of the solution algorithms can…

  7. Focal Manual for CAI Coding on the TSS/8 System.

    ERIC Educational Resources Information Center

    Kirbs, H. Dewey; And Others

    Basic information is provided in this manual for coding drill-and-practice CAI (computer-assisted instruction) applications in the language FOCAL (Formulating On-line Calculations in Algebraic Language). This language is available on the Digital Equipment Corporation Time-Sharing 8 system (TSS/8). While FOCAL is oriented toward solution of…

  8. Conjunctival mucin deficiency in complete androgen insensitivity syndrome (CAIS).

    PubMed

    Mantelli, Flavio; Moretti, Costanzo; Micera, Alessandra; Bonini, Stefano

    2007-06-01

    Sex steroid hormones are essential for a healthy ocular surface and the androgen receptor impairment found in patients with complete androgen insensitivity syndrome (CAIS) has been described to cause meibomian gland dysfunction and functional dry eye for lipid tear film layer instability. However, it has not been reported if the mucous layer is also affected. A 37-year-old CAIS patient with persistent symptoms of dry eye underwent ophthalmological examination and was evaluated for qualitative and quantitative tear function tests and conjunctival cytology. Samples obtained from the conjunctival epithelium were stained for histology and immunohistochemistry and compared with three age-matched female controls. Western blot and relative real-time RT-PCR for MUC1 and MUC5AC were also performed on these samples. Immunohistochemistry, Western blot and relative real-time RT-PCR showed a decrease in the expression of MUC1 and MUC5AC in CAIS. Changes in the tear film mucous layer were accompanied by a reduction in the tear film break up time test. This is the first report describing mucous layer alteration associated with androgen receptor impairment. Decreased mucin levels contribute in explaining the tear film instability in CAIS and should be considered an additional cause of dry eye in sex steroid hormone pathology.

  9. CAISYS-8- A CAI Language Developed For A Minicomputer.

    ERIC Educational Resources Information Center

    Holm, Cheryl; And Others

    The University of Texas Medical Branch developed a minicomputer-based computer-assisted instruction (CAI) system which employed a teacher oriented software package called CAISYS-8, consisting of a highly modularized teaching compiler and operating system. CAISYS-8 used instructional quanta which generalized the flow of information to and from the…

  10. Distribution and Origin of 36Cl In Allende CAIs

    SciTech Connect

    Matzel, J P; Jacobsen, B; Hutcheon, I D; Krot, A N; Nagashima, K; Yin, Q; Ramon, E C; Weber, P; Wasserburg, G J

    2009-12-11

    The abundance of short-lived radionuclides (SLRs) in early solar system materials provide key information about their nucleosynthetic origin and can constrain the timing of early solar system events. Excesses of {sup 36}S ({sup 36}S*) correlated with {sup 35}Cl/{sup 34}S ratios provide direct evidence for in situ decay of {sup 36}Cl ({tau}{sub 1/2} {approx} 0.3 Ma) and have been reported in sodalite (Na{sub 8}Al{sub 6}Si{sub 6}O{sub 24}Cl{sub 2}) and wadalite (Ca{sub 6}Al{sub 5}Si{sub 2}O{sub 16}Cl{sub 3}) in CAIs and chondrules from the Allende and Ningqiang CV carbonaceous chondrites. While previous studies demonstrate unequivocally that {sup 36}Cl was extant in the early solar system, no consensus on the origin or initial abundance of {sup 36}Cl has emerged. Understanding the origin of {sup 36}Cl, as well as the reported variation in the initial {sup 36}Cl/{sup 35}Cl ratio, requires addressing when, where and how chlorine was incorporated into CAIs and chondrules. These factors are key to distinguishing between stellar nucleosynthesis or energetic particle irradiation for the origin of {sup 36}Cl. Wadalite is a chlorine-rich secondary mineral with structural and chemical affinities to grossular. The high chlorine ({approx}12 wt%) and very low sulfur content (<<0.01 wt%) make wadalite ideal for studies of the {sup 36}Cl-{sup 36}S system. Wadalite is present in Allende CAIs exclusively in the interior regions either in veins crosscutting melilite or in zones between melilite and anorthite associated with intergrowths of grossular, monticellite, and wollastonite. Wadalite and sodalite most likely resulted from open-system alteration of primary minerals with a chlorine-rich fluid phase. We recently reported large {sup 36}S* correlated with {sup 35}Cl/{sup 34}S in wadalite in Allende Type B CAI AJEF, yielding a ({sup 36}Cl/{sup 35}Cl){sub 0} ratio of (1.7 {+-} 0.3) x 10{sup -5}. This value is the highest reported {sup 36}Cl/{sup 35}Cl ratio and is {approx}5 times

  11. Search for 41K Excess in Efremovka CAIs

    NASA Astrophysics Data System (ADS)

    Srinivasan, G.; Ulyanov, A. A.; Goswami, J. N.

    1993-07-01

    We have used the ion microprobe to measure K isotopic composition of refractory phases in Efremovka CAIs to look for the possible presence of K excess from the decay of extinct radionuclide Ca (halflife = 0.13 Ma). The presence of Ca at the time of CAI formation, if established, will allow us to place a lower limit on the time interval between the last injection of freshly synthesized matter into the solar nebula and the formation of some of the first solid objects (CAIs) in the solar system. Several attempts have been made earlier to detect 41K excess in Allende CAIs [1-4]. We have further investigated this problem by analyzing the Efremovka CAIs for two reasons. First, both the petrographic and magnesium isotopic systematics suggest the Efremovka CAIs to be less altered compared to the Allende CAIs making them an ideal and perhaps better sample for this study. Second, the presence of large perovskite (~10 micrometers) allowed us to analyse this phase, which was not included in earlier studies. The major difficulty in accurately measuring 41K, which was identified in earlier studies, is the unresolvable (40Ca42Ca)++ interference, which was found to be matrix dependent [4]. In addition, one can also have interfernce from the (40CaH)+ peak. In our operating condition the interference from the hydride peak can be neglected (Fig. 1, which appears in the hard copy). We have analyzed terrestrial perovskite (K <= 20 ppm) to determine the (40Ca42Ca)++ correction term, and its equivalence with (40Ca43Ca)++ ion signal at mass 41.5 [4]. In perovskite, the (40Ca42Ca)++ signal constitutes ~80% of the signal at 41K and we could estimate this interference with confidence. A value of (2.7 +- 0.1) x 10^-5 was obtained for the ratio [(40Ca42Ca)++/42Ca+], which is similar to the measured [(40Ca43Ca)++/43Ca+] ratio of (2.4 +- 0.2) x 10^-5. We have therefore used the measured value for the latter ratio in the analyzed phases to correct for the doubly charged interference at mass 41

  12. Climatic and hydrologic changes in the Tien Shan, central Asia

    SciTech Connect

    Aizen, V.B.; Aizen, E.M.; Melack, J.M.; Dozier, J.

    1997-06-01

    The authors analyze climatic hydrologic data from 110 sites collected from the middle of the twentieth century to the present in the Tien Shan, one of the largest mountain systems of central Asia. In spite of a few confounding interregional variations in the temporal changes of surface air temperature, precipitation, runoff, glacier mass, and snow thickness in the Tien Shan, it has been possible to establish statistically significant long-range, with slightly lower values below 2000-m elevation. The precipitation in the Tien Shan increased 1.2 mm yr{sup -1} over the past half-century. The precipitation increase is larger at low altitudes in the northern and western regions than at altitudes above 2000 m. A decrease in snow resources occurred almost everywhere in the Tien Shan; the maximum snow thickness an snow duration have decreased on average 10 cm and 9 days, respectively. The annual runoff is the type of precipitation (liquid or solid). Over the last few decades, periods of glacier decline have coincided with declining river runoff. 45 refs., 8 figs., 2 tabs.

  13. INVESTIGATION OF CRUSTAL MOTION IN THE TIEN SHAN USING INSAR

    SciTech Connect

    Mellors, R J

    2011-02-25

    The northern Tien Shan of Central Asia is an area of active mid-continent deformation. Although far from a plate boundary, this region has experienced 5 earthquakes larger than magnitude 7 in the past century and includes one event that may as be as large as Mw 8.0. Previous studies based on GPS measurements indicate on the order of 23 mm/yr of shortening across the entire Tien Shan and up to 15 mm/year in the northern Tien Shan (Figure 1). The seismic moment release rate appears comparable with the geodetic measured slip, at least to first order, suggesting that geodetic rates can be considered a proxy for accumulation rates of stress for seismic hazard estimation. Interferometric synthetic aperture radar may provide a means to make detailed spatial measurements and hence in identifying block boundaries and assisting in seismic hazard. Therefore, we hoped to define block boundaries by direct measurement and by identifying and resolving earthquake slip. Due to political instability in Kyrgzystan, the existing seismic network has not performed as well as required to precisely determine earthquake hypocenters in remote areas and hence InSAR is highly useful. In this paper we present the result of three earthquake studies and show that InSAR is useful for refining locations of teleseismically located earthquakes. ALOS PALSAR data is used to investigate crustal motion in the Tien Shan mountains of Central Asia. As part of the work, considerable software development was undertaken to process PALSAR data. This software has been made freely available. Two damaging earthquakes have been imaged in the Tien Shan and the locations provided by ALOS InSAR have helped to refine seismological velocity models. A third earthquake south of Kyrgyzstan was also imaged. The use of InSAR data and especially L band is therefore very useful in providing groundtruth for earthquake locations.

  14. Observations from a prototype implementation of the Common APSE Interface Set (CAIS)

    NASA Technical Reports Server (NTRS)

    Mcclimens, M.; Bowerman, R.; Howell, C.; Gill, H.; Hutchison, R.

    1985-01-01

    This paper presents an overview of the Common Ada Programming Support Environment (APSE) Interface Set (CAIS), its purpose, and its history. The paper describes an internal research and development effort at the Mitre Corporation to implement a prototype version of the current CAIS specification and to rehost existing Ada software development tools onto the CAIS prototype. Based on this effort, observations are made on the maturity and functionality of the CAIS. These observations support the government's current policy of publicizing the CAIS specification as a baseline for public review in support of its evolution into a standard which can be mandated for use as Ada is today.

  15. Oxygen Isotope Measurements of a Rare Murchison Type A CAI and Its Rim

    NASA Technical Reports Server (NTRS)

    Matzel, J. E. P.; Simon, J. I.; Hutcheon, I. D.; Jacobsen, B.; Simon, S. B.; Grossman, L.

    2013-01-01

    Ca-, Al-rich inclusions (CAIs) from CV chondrites commonly show oxygen isotope heterogeneity among different mineral phases within individual inclusions reflecting the complex history of CAIs in both the solar nebula and/or parent bodies. The degree of isotopic exchange is typically mineral-specific, yielding O-16-rich spinel, hibonite and pyroxene and O-16-depleted melilite and anorthite. Recent work demonstrated large and systematic variations in oxygen isotope composition within the margin and Wark-Lovering rim of an Allende Type A CAI. These variations suggest that some CV CAIs formed from several oxygen reservoirs and may reflect transport between distinct regions of the solar nebula or varying gas composition near the proto-Sun. Oxygen isotope compositions of CAIs from other, less-altered chondrites show less intra-CAI variability and 16O-rich compositions. The record of intra-CAI oxygen isotope variability in CM chondrites, which commonly show evidence for low-temperature aqueous alteration, is less clear, in part because the most common CAIs found in CM chondrites are mineralogically simple (hibonite +/- spinel or spinel +/- pyroxene) and are composed of minerals less susceptible to O-isotopic exchange. No measurements of the oxygen isotope compositions of rims on CAIs in CM chondrites have been reported. Here, we present oxygen isotope data from a rare, Type A CAI from the Murchison meteorite, MUM-1. The data were collected from melilite, hibonite, perovskite and spinel in a traverse into the interior of the CAI and from pyroxene, melilite, anorthite, and spinel in the Wark-Lovering rim. Our objectives were to (1) document any evidence for intra-CAI oxygen isotope variability; (2) determine the isotopic composition of the rim minerals and compare their composition(s) to the CAI interior; and (3) compare the MUM-1 data to oxygen isotope zoning profiles measured from CAIs in other chondrites.

  16. Replacement textures in CAI and implications regarding planetary metamorphism

    NASA Technical Reports Server (NTRS)

    Meeker, G. P.; Wasserburg, G. J.; Armstrong, J. T.

    1983-01-01

    Formation by a secondary metamorphic event, rather than primary crystallization from a melt or a sequential nebular condensation, is indicated by textural and chemical features of five coarse grained, Ca- and Al-rich inclusions (CAI) from the Allende meteorite which contain embayed pyroxene surrounded by melilite. It is suggested that the most probable environment for a metamorphic process (requiring the addition of Ca derived from calcite or from the introduction of a fluid phase) is that of a small planetary body, rather than the solar nebula. These results are compatible with O isotopic heterogeneities within CAI, and offer a mechanism for the production of lower temperature alteration phases, together with the rim phases found in these inclusions.

  17. CAIS standard manual. System number 32. Central cooling plants

    SciTech Connect

    1995-04-28

    At this installation the list of facilities to be surveyed will be addressed on the basis of 32 unique systems that form the CAIS Engineering Deficiency Standards and Inspection Methods document. Each system deals with a specific technical aspect of the facility to be surveyed. Within each system a further breakdown is made to subsystems, each having a specific list of components. Specific observations of the listed defects are provided so as to allow the entry of observed quantification data. A DOD CAIS manual is provided for each of the 32 systems with an internal organization. The System Tree is a graphical representation of the Work Breakdown Structure, showing system, subsystem and component relationships for the Central Cooling Plants.

  18. CAIS standard manual. System number 24. Natural gas distribution system

    SciTech Connect

    1995-04-28

    At this installation the list of facilities to be surveyed, including infrastructure, will be addressed on the basis of 32 unique systems that form the CAIS Engineering Deficiency Standards and Inspection Methods document. Each system deals with a specific technical aspect of the facility to be surveyed. Within each system a further breakdown is made to subsystems, each having a related list of components. Detailed observations of the listed defects are provided so as to allow the entry of observed quantification data. A DOD CAIS manual is provided for each of the 32 systems with an internal organization. The System Tree is a graphical representation of the Work Breakdown Structure, showing system, subsystem and component relationships for the Natural Gas Distribution System.

  19. CAIS standard manual. System number 28. Central heating plants

    SciTech Connect

    1995-04-28

    At this installation the list of facilities to be surveyed will be addressed on the basis of 32 unique systems that form the CAIS Engineering Deficiency Standards and Inspection Methods document. Each system deals with a specific technical aspect of the facility to be surveyed. Within each system a further breakdown is made to subsystems, each having a specific list of components. Specific observations of the listed defects are provided so as to allow the entry of observed quantification data. A DOD CAIS manual is provided for each of the 32 systems with an internal organization. The System Tree is a graphical representation of the Work Breakdown Structure, showing system, subsystem and component relationships for the Central Heating Plants.

  20. CAIS standard manual. System number 27. Petroleum fuel facilities

    SciTech Connect

    1995-04-28

    At this installation the list of facilities to be surveyed, including infrastructure, will be addressed on the basis of 32 unique systems that form the CAIS Engineering Deficiency Standards and Inspection Methods document. Each system deals with a specific technical aspect of the facility to be surveyed. Within each system a further breakdown is made to subsystems, each having a related list of components. Detailed observations of the listed defects are provided so as to allow the entry of observed quantification data. A DOD CAIS manual is provided for each of the 32 systems with an internal organization. The System Tree is a graphical representation of the Work Breakdown Structure, showing system, subsystem and component relationships for the Industrial Gas Storage and Distribution System.

  1. Silicon Isotopic Fractionation of CAI-like Vacuum Evaporation Residues

    SciTech Connect

    Knight, K; Kita, N; Mendybaev, R; Richter, F; Davis, A; Valley, J

    2009-06-18

    Calcium-, aluminum-rich inclusions (CAIs) are often enriched in the heavy isotopes of magnesium and silicon relative to bulk solar system materials. It is likely that these isotopic enrichments resulted from evaporative mass loss of magnesium and silicon from early solar system condensates while they were molten during one or more high-temperature reheating events. Quantitative interpretation of these enrichments requires laboratory determinations of the evaporation kinetics and associated isotopic fractionation effects for these elements. The experimental data for the kinetics of evaporation of magnesium and silicon and the evaporative isotopic fractionation of magnesium is reasonably complete for Type B CAI liquids (Richter et al., 2002, 2007a). However, the isotopic fractionation factor for silicon evaporating from such liquids has not been as extensively studied. Here we report new ion microprobe silicon isotopic measurements of residual glass from partial evaporation of Type B CAI liquids into vacuum. The silicon isotopic fractionation is reported as a kinetic fractionation factor, {alpha}{sub Si}, corresponding to the ratio of the silicon isotopic composition of the evaporation flux to that of the residual silicate liquid. For CAI-like melts, we find that {alpha}{sub Si} = 0.98985 {+-} 0.00044 (2{sigma}) for {sup 29}Si/{sup 28}Si with no resolvable variation with temperature over the temperature range of the experiments, 1600-1900 C. This value is different from what has been reported for evaporation of liquid Mg{sub 2}SiO{sub 4} (Davis et al., 1990) and of a melt with CI chondritic proportions of the major elements (Wang et al., 2001). There appears to be some compositional control on {alpha}{sub Si}, whereas no compositional effects have been reported for {alpha}{sub Mg}. We use the values of {alpha}Si and {alpha}Mg, to calculate the chemical compositions of the unevaporated precursors of a number of isotopically fractionated CAIs from CV chondrites whose

  2. Oxygen Isotope Variations at the Margin of a CAI Records Circulation Within the Solar Nebula

    NASA Astrophysics Data System (ADS)

    Simon, Justin I.; Hutcheon, Ian D.; Simon, Steven B.; Matzel, Jennifer E. P.; Ramon, Erick C.; Weber, Peter K.; Grossman, Lawrence; DePaolo, Donald J.

    2011-03-01

    Micrometer-scale analyses of a calcium-, aluminum-rich inclusion (CAI) and the characteristic mineral bands mantling the CAI reveal that the outer parts of this primitive object have a large range of oxygen isotope compositions. The variations are systematic; the relative abundance of 16O first decreases toward the CAI margin, approaching a planetary-like isotopic composition, then shifts to extremely 16O-rich compositions through the surrounding rim. The variability implies that CAIs probably formed from several oxygen reservoirs. The observations support early and short-lived fluctuations of the environment in which CAIs formed, either because of transport of the CAIs themselves to distinct regions of the solar nebula or because of varying gas composition near the proto-Sun.

  3. Oxygen isotope variations at the margin of a CAI records circulation within the solar nebula.

    PubMed

    Simon, Justin I; Hutcheon, Ian D; Simon, Steven B; Matzel, Jennifer E P; Ramon, Erick C; Weber, Peter K; Grossman, Lawrence; DePaolo, Donald J

    2011-03-04

    Micrometer-scale analyses of a calcium-, aluminum-rich inclusion (CAI) and the characteristic mineral bands mantling the CAI reveal that the outer parts of this primitive object have a large range of oxygen isotope compositions. The variations are systematic; the relative abundance of (16)O first decreases toward the CAI margin, approaching a planetary-like isotopic composition, then shifts to extremely (16)O-rich compositions through the surrounding rim. The variability implies that CAIs probably formed from several oxygen reservoirs. The observations support early and short-lived fluctuations of the environment in which CAIs formed, either because of transport of the CAIs themselves to distinct regions of the solar nebula or because of varying gas composition near the proto-Sun.

  4. Some "Facts" About CAI: A Quantitative Analysis of the 1976 Index to Computer Based Instruction

    ERIC Educational Resources Information Center

    Kearsley, Greg P.

    1976-01-01

    Descriptive quantitative data on various aspects of CAI are reported, including subject matter, author languages, instructional strategies, level of instruction, sources, and central processors. (Author)

  5. Coordinated Oxygen Isotopic and Petrologic Studies of CAIS Record Varying Composition of Protosolar

    NASA Technical Reports Server (NTRS)

    Simon, Justin I.; Matzel, J. E. P.; Simon, S. B.; Weber, P. K.; Grossman, L.; Ross, D. K.; Hutcheon, I. D.

    2012-01-01

    Ca-, Al-rich inclusions (CAIs) record the O-isotope composition of Solar nebular gas from which they grew [1]. High spatial resolution O-isotope measurements afforded by ion microprobe analysis across the rims and margin of CAIs reveal systematic variations in (Delta)O-17 and suggest formation from a diversity of nebular environments [2-4]. This heterogeneity has been explained by isotopic mixing between the O-16-rich Solar reservoir [6] and a second O-16-poor reservoir (probably nebular gas) with a "planetary-like" isotopic composition [e.g., 1, 6-7], but the mechanism and location(s) where these events occur within the protoplanetary disk remain uncertain. The orientation of large and systematic variations in (Delta)O-17 reported by [3] for a compact Type A CAI from the Efremovka reduced CV3 chondrite differs dramatically from reports by [4] of a similar CAI, A37 from the Allende oxidized CV3 chondrite. Both studies conclude that CAIs were exposed to distinct, nebular O-isotope reservoirs, implying the transfer of CAIs among different settings within the protoplanetary disk [4]. To test this hypothesis further and the extent of intra-CAI O-isotopic variation, a pristine compact Type A CAI, Ef-1 from Efremovka, and a Type B2 CAI, TS4 from Allende were studied. Our new results are equally intriguing because, collectively, O-isotopic zoning patterns in the CAIs indicate a progressive and cyclic record. The results imply that CAIs were commonly exposed to multiple environments of distinct gas during their formation. Numerical models help constrain conditions and duration of these events.

  6. The Vibrio cholerae quorum-sensing autoinducer CAI-1: analysis of the biosynthetic enzyme CqsA

    SciTech Connect

    Kelly, R.; Bolitho, M; Higgins, D; Lu, W; Ng, W; Jeffrey, P; Rabinowitz, J; Semmelhack, M; Hughson, F; Bassler, B

    2009-01-01

    Vibrio cholerae, the bacterium that causes the disease cholera, controls virulence factor production and biofilm development in response to two extracellular quorum-sensing molecules, called autoinducers. The strongest autoinducer, called CAI-1 (for cholera autoinducer-1), was previously identified as (S)-3-hydroxytridecan-4-one. Biosynthesis of CAI-1 requires the enzyme CqsA. Here, we determine the CqsA reaction mechanism, identify the CqsA substrates as (S)-2-aminobutyrate and decanoyl coenzyme A, and demonstrate that the product of the reaction is 3-aminotridecan-4-one, dubbed amino-CAI-1. CqsA produces amino-CAI-1 by a pyridoxal phosphate-dependent acyl-CoA transferase reaction. Amino-CAI-1 is converted to CAI-1 in a subsequent step via a CqsA-independent mechanism. Consistent with this, we find cells release {ge}100 times more CAI-1 than amino-CAI-1. Nonetheless, V. cholerae responds to amino-CAI-1 as well as CAI-1, whereas other CAI-1 variants do not elicit a quorum-sensing response. Thus, both CAI-1 and amino-CAI-1 have potential as lead molecules in the development of an anticholera treatment.

  7. Learner Control of Instructional Sequencing within an Adaptive Tutorial CAI Environment. Technical Report 75-7.

    ERIC Educational Resources Information Center

    Seidel, Robert J.; And Others

    A study to test the effects of learner control of the sequencing of instructional tasks when using computer-assisted instruction (CAI) systems is described. Using a series of CAI modules to teach the COBOL programing language to military personnel, students were able to control various aspects of their learning environment. Among the research…

  8. A Study of Effectiveness of Computer Assisted Instruction (CAI) over Classroom Lecture (CRL) at ICS Level

    ERIC Educational Resources Information Center

    Kaousar, Tayyeba; Choudhry, Bushra Naoreen; Gujjar, Aijaz Ahmed

    2008-01-01

    This study was aimed to evaluate the effectiveness of CAI vs. classroom lecture for computer science at ICS level. The objectives were to compare the learning effects of two groups with classroom lecture and computer-assisted instruction studying the same curriculum and the effects of CAI and CRL in terms of cognitive development. Hypotheses of…

  9. Less Equals More: Coaching/Prompting CAI as a Tool Technology.

    ERIC Educational Resources Information Center

    Cooper, Ted L.

    Recent reviews of computer-assisted instruction (CAI) in various journals suggest that the technological and economic barriers to its adoption and use may be overcome in the very near future, and that CAI will be feasible in a number of educational settings. Computer hardware costs have dropped dramatically in recent years, and a variety of…

  10. Student Conceptions of, and Attitudes toward, Specific Features of a CAI System.

    ERIC Educational Resources Information Center

    Hativa, Nira

    1989-01-01

    Describes study of Israeli elementary school students that examined student attitudes toward computer-assisted instruction (CAI) designed to provide drill and practice in arithmetic. Attitudes are compared in relation to students' aptitude, gender, grade level, and socioeconomic status, and implications for the design of CAI systems are discussed.…

  11. Distribution of vanadium and melting of opaque assemblages in Efremovka CAI's

    NASA Technical Reports Server (NTRS)

    Casanova, I.; Grossman, L.

    1993-01-01

    A petrographic and chemical study of compact Type A CAI's from the Efremovka CV3 chondrite strongly suggests that the opaque assemblages (OA's) that they contain were molten at temperatures below the CAI silicate solidus, and that the V-rich magnetite presently observed in association with OA's formed by in situ oxidation of their FeNi.

  12. Can CAI Help? The Crisis of Content in Educational Psychology Courses.

    ERIC Educational Resources Information Center

    Clark, Michael C.

    Computer technology per se is not a solution to the problem of the current "crisis in content" in teacher education programs. Computer assisted instruction (CAI) is defined as the on-line interaction of a student with a computer program for purposes of instruction. The drill-and-practice and tutorial CAI programs serve merely as a medium for…

  13. The Effects of the Locus of CAI Control Strategies on the Learning of Mathematics Rules.

    ERIC Educational Resources Information Center

    Goetzfried, Leslie; Hannafin, Michael J.

    1985-01-01

    Effects of the locus of computer assisted instruction (CAI) strategies on low achievers' learning accuracy and efficiency were studied. Externally controlled adaptive, individually based learner control with advisement, and linear control design strategies were used. Effects were examined for CAI strategy, prior achievement, and sex of student.…

  14. Effects of Computer Assisted Instruction (CAI) on Secondary School Students' Performance in Biology

    ERIC Educational Resources Information Center

    Yusuf, Mudasiru Olalere; Afolabi, Adedeji Olufemi

    2010-01-01

    This study investigated the effects of computer assisted instruction (CAI) on secondary school students' performance in biology. Also, the influence of gender on the performance of students exposed to CAI in individualised or cooperative learning settings package was examined. The research was a quasi experimental involving a 3 x 2 factorial…

  15. Audio-Tutorial and CAI Aids for Problem Solving in Introductory Chemistry

    ERIC Educational Resources Information Center

    Lower, Stephen K.

    1970-01-01

    Starting from a successful audio-tutorial program, the author initiated a computer assisted tutorial program in solving chemistry problems. Discusses the advantages of computer assisted instruction (CAI) over audiotapes and the advantages of both over conventional instructional methods. Presents a flow chart of a CAI program on a calorimetry…

  16. INAA of CAIs from the Maralinga CK4 chondrite: Effects of parent body thermal metamorphism

    NASA Technical Reports Server (NTRS)

    Lindstrom, D. J.; Keller, L. P.; Martinez, R. R.

    1993-01-01

    Maralinga is an anomalous CK4 carbonaceous chondrite which contains numerous Ca-, Al-rich inclusions (CAI's) unlike the other members of the CK group. These CAI's are characterized by abundant green hercynitic spinel intergrown with plagioclase and high-Ca clinopyroxene, and a total lack of melilite. Instrumental Neutron Activation Analysis (INAA) was used to further characterize the meteorite, with special focus on the CAI's. High sensitivity INAA was done on eight sample disks about 100-150 microns in diameter obtained from a normal 30 micron thin section with a diamond microcoring device. The CAI's are enriched by 60-70X bulk meteorite values in Zn, suggesting that the substantial exchange of Fe for Mg that made the spinel in the CAI's hercynitic also allowed efficient scavenging of Zn from the rest of the meteorite during parent body thermal metamorphism. Less mobile elements appear to have maintained their initial heterogeneity.

  17. Design Specification for Test and Evaluation of the NATO Common Ada Programming Support Environment (APSE) Interface Set (CAIS) Implementation

    DTIC Science & Technology

    1989-02-23

    testing (i.e., testing of individual interfaces) for a critical subset of the SWG CAIS interfaces. The second category of testing activities includes...for correctness in the functionality of critical interfaces. These critical interfaces are defined in Section 2.2. The second category, usability...QUEUE-MANAGEMENT CAM-.STANDARD None CAM- DEFENITIONS CAMSJO..DEINITJONS CAI IST-MANAGEMENT CAIS.ACCESS-.CONTROL- MANAGEMENT CAIS-SCROLL-TERMNAL-10 CA1S

  18. Ozone and nitrogen dioxide above the northern Tien Shan

    NASA Technical Reports Server (NTRS)

    Arefev, Vladimir N.; Volkovitsky, Oleg A.; Kamenogradsky, Nikita E.; Semyonov, Vladimir K.; Sinyakov, Valery P.

    1994-01-01

    The results of systematic perennial measurements of the total ozone (since 1979) and nitrogen dioxide column (since 1983) in the atmosphere in the European-Asian continent center above the mountainmass of the Tien Shan are given. This region is distinguished by a great number of sunny days during a year. The observation station is at the Northern shore of Issyk Kul Lake (42.56 N 77.04 E 1650 m above the sea level). The measurement results are presented as the monthly averaged atmospheric total ozone and NO2 stratospheric column abundances (morning and evening). The peculiarities of seasonal variations of ozone and nitrogen dioxide atmospheric contents, their regular variances with a quasi-biennial cycles and trends have been noticed. Irregular variances of ozone and nitrogen dioxide atmospheric contents, i.e. their positive and negative anomalies in the monthly averaged contents relative to the perennial averaged monthly means, have been analyzed. The synchronous and opposite in phase anomalies in variations of ozone and nitrogen dioxide atmospheric contents were explained by the transport and zonal circulation in the stratosphere (Kamenogradsky et al., 1990).

  19. Two Generations of Sodic Metasomatism in an Allende Type B CAI

    NASA Technical Reports Server (NTRS)

    Ross, D. K.; Simon, J. I.; Simon, S. B.; Grossman, L.

    2015-01-01

    Calcium-Aluminum rich inclusions (CAI) in Allende, along with other chondritic compo-nents, experienced variable amounts and types of alter-ation of their mineralogy and chemistry. In CAIs, one of the principal types of alteration led to the depo-sition of nepheline and sodalite. Here we extend initial obervations of alteration in an Allende CAI, focus-ing on occurences of nepheline and a nepheline-like phase with unusally high Ca (referred to as "calcic nepheline" in this abstract). Detailed petrographic and microchemical observations of alteration phases in an Allende Type B CAI (TS4) show that two separate generations of "nepheline", with very distinct composi-tions, crystallized around the margins and in the interi-or of this CAI. We use observations of micro-faults as potential temporal markers, in order to place constraints on the timing of alteration events in Allende. These observa-tions of micro-faulting that truncate and offset one gen-eration of "nepheline" indicate that some "nepheline" crystallized before incorporation of the CAI into the Allende parent-body. Some of the sodic metasomatism in some Allende CAIs occurred prior to Allende par-ent-body assembly. The earlier generation of "calcic-nepheline" has a very distinctive, calcium-rich compo-sition, and the second generation is low in calcium, and matches the compositions of nephelines found in near-by altered chondrules, and in the Allende matrix.

  20. Microstructural Investigation of a Wark-Lovering Rim on a Vigarano CAI

    NASA Technical Reports Server (NTRS)

    Han, J.; Keller, L. P.; Needham, A. W.; Messenger, S.; Simon, J. I.

    2015-01-01

    Wark-Lovering (WL) rims are thin multi-layered mineral sequences that surround many CAIs. These rim layers consist of the primary minerals found in the CAI interiors, but vary in their mineralogy. Several models for their origin have been proposed including condensation, reaction with a nebular gas, evaporation, or combinations of these. However, there still is little consensus on how and when the rims formed. Here, we describe the microstructure and mineralogy of a WL rim on a type B CAI from the Vigarano CV(sub red) chondrite using FIB/TEM to better understand the astrophysical significance of WL rim formation.

  1. Thermotectonic evolution of the northern Kyrgyz Tien Shan intrusives

    NASA Astrophysics Data System (ADS)

    Glorie, Stijn; de Grave, Johan; Buslov, Mikhail

    2010-05-01

    The northern Kyrgyz Tien Shan (nKTS) encloses a large number of granitoid intrusions. These plutons intruded during the Palaeozoic and are geodynamical related to either Caledonian or Hercynian collisions. The most voluminous, i.e. the Caledonian intrusion phase is associated with the evolution and closure of the Early Palaeozoic Terskey Ocean (branch of the Turkestan Ocean). Hercynian plutons, smaller in both abundance and dimensions, are thought to have formed during the final closure of the Turkestan Ocean when the Tarim microcontinent eventually collided with the Kazakhstan plate. In the Late Palaeozoic - Early Mesozoic, the nKTS experienced tectonic quiescence. This geodynamic environment abruptly changed in the Mesozoic, when the Central Asian Orogenic System - including the nKTS - was reactivated as an intracontinental orogen (Cimmerian orogeny). The granitoids embedded in the basement record this phase as a cooling event. This cooling is a consequence of denudation and exhumation of the nKTS basement associated with this orogeny. The Late Mesozoic - Early Cenozoic introduced again a period of thermal stability. In the Cenozoic, a new phase of cooling, linked to renewed denudation as a tectonic far-field effect of the India-Eurasia collision, affected the nKTS basement. In this study, we dated each of the aforementioned events and reveal the thermotectonic history of the nKTS granitoids from emplacement to exhumation. Zircon SHRIMP and LA-ICP-MS U/Pb concordia ages suggest a Middle to Late Ordovician crystallization age (440-470 Ma) for the Caledonian intrusion phase, however the presence of additional Early Ordovician - Cambrian U/Pb samples, points towards a more prolonged production of granitoids during the entire Early Palaeozoic. Hercynian samples are constrained to the Late Carboniferous - Permian (260-300 Ma). 40Ar/39Ar stepwise heating plateau-ages (biotite: 400-440 Ma; K-feldspar: 235-375 Ma) bear witness to rapid Silurian - Early Devonian post

  2. Coordinated Oxygen Isotopic and Petrologic Studies of CAIs Record Varying Composition of Protosolar Gas

    NASA Astrophysics Data System (ADS)

    Simon, J. I.; Matzel, J. E. P.; Simon, S. B.; Weber, P. K.; Grossman, L.; Ross, D. K.; Hutcheon, I. D.

    2012-03-01

    High-resolution O-isotopic zoning profiles obtained by NanoSIMS indicate a progressive and cyclic record of exchange between CAIs and distinct nebular gases. Numerical models are used to constrain conditions and duration of these exchange events.

  3. Effects of Computer-Assisted Instruction (CAI) on 11th Graders' Attitudes to Biology and CAI and Understanding of Reproduction in Plants and Animals.

    ERIC Educational Resources Information Center

    Soyibo, Kola; Hudson, Ann

    2000-01-01

    Investigates whether the use of the combination of lecture, discussion, and computer-assisted instruction (CAI) significantly improved students' attitudes toward biology and their understanding of reproduction in plants and animals. Studies grade 11 Jamaican female students (n=77) from two traditional high schools in Kingston. (Contains 19…

  4. A Discussion of Behavioral Technology Laboratories CAI Projects In Relation to a CAI Test-Bed Concept. Technical Report Number 71.

    ERIC Educational Resources Information Center

    Rigney, Joseph W.

    The elements of an instructional system are discussed and some literature bearing on these is reviewed. The discussion is intended to stimulate thought about an instructional system as a computer-assisted instructional (CAI) test-bed and to point out some noteworthy laboratory research results, particularly in cognitive psychology. Following this,…

  5. Fine-Gained CAIs in Comet Samples: Moderate Refractory Character and Comparison to Small Refractory Inclusions in Chondrites

    NASA Technical Reports Server (NTRS)

    Joswiak, D. J.; Brownlee, D. E.; Nguyen, A. N.; Messenger, S

    2017-01-01

    Examination of >200 comet Wild 2 particles collected by the Stardust (SD) mission shows that the CAI abundance of comet Wild 2's rocky material is near 1% and that nearly 50% of all bulbous tracks will contain at least one recognizable CAI fragment. A similar abundance to Wild 2 is found in a giant cluster IDP thought to be of cometary origin. The properties of these CAIs and their comparison with meteoritic CAIs provide important clues on the role of CAIs in the early Solar System (SS) and how they were transported to the edge of the solar nebula where Kuiper Belt comets formed. Previously, only two CAIs in comet Wild 2 had been identified and studied in detail. Here we present 2 new Wild 2 CAIs and 2 from a giant cluster cometary IDP, describe their mineralogical characteristics and show that they are most analogous to nodules in spinel-rich, fine-grained inclusions (FGIs) observed in CV3 and other chondrites. Additionally, we present new O isotope measurements from one CAI from comet Wild 2 and show that its oxygen isotopic composition is similar to some FGIs. This is only the second CAI from Wild 2 in which O isotopes have been measured.

  6. Evidence for extinct 135Cs from Ba isotopes in Allende CAIs?

    NASA Astrophysics Data System (ADS)

    Bermingham, K. R.; Mezger, K.; Desch, S. J.; Scherer, E. E.; Horstmann, M.

    2014-05-01

    The abundance and distribution of isotopes throughout the Solar System can be used to constrain the number and type of nucleosynthetic events that contributed material to the early nebula. Barium is particularly well suited to quantifying the degree of isotope heterogeneity in the Solar System because it comprises seven stable isotopes that were synthesized by three different nucleosynthetic processes (s-, r-, and p-processes), all of which contributed material to the Solar System. There is also potential contribution to 135Ba from short-lived radioisotope 135Cs, conclusive evidence for which is yet to be reported. Four Allende (CV3) Ca,Al-rich inclusions (CAI 1, CAI 2, CAI 4, CAI 5) and one Allende dark inclusion (DI) were analyzed for Ba isotope variability. Two CAIs (CAI 2 and CAI 5) display 135Ba excesses that are not accompanied by 137Ba anomalies. Calcium-aluminum-rich inclusion 1 displays a 135Ba excess that is possibly coupled with a 137Ba excess, and the remaining refractory inclusions (CAI 2 and DI) have terrestrial Ba isotope compositions. These Ba isotope data are presented in conjunction with published whole rock Ba isotope data from individual Allende CAIs. The enrichment in 135Ba and absence of coupled 137Ba excesses in CAI 2 and CAI 5 is interpreted to indicate that the anomalies are not purely nucleosynthetic in origin but also contain contributions (16-48 ppm) from the decay of short-lived 135Cs. The majority of Allende CAIs studied to date may also have similar contributions from 135Cs on the basis of higher than expected 135Ba excesses if the Ba isotope anomalies were purely nucleosynthetic in origin. The 135Ba anomalies appear not to be coupled with superchondritic Cs/Ba, which may imply that the contribution to 135Ba did not occur via in situ decay of live 135Cs. However, it is feasible that the CAIs had a superchondritic Cs/Ba during decay of 135Cs, but Cs was subsequently removed from the system during aqueous alteration on the parent body

  7. The ethnoecology of Caiçara metapopulations (Atlantic Forest, Brazil): ecological concepts and questions

    PubMed Central

    Begossi, Alpina

    2006-01-01

    The Atlantic Forest is represented on the coast of Brazil by approximately 7,5% of remnants, much of these concentrated on the country's SE coast. Within these southeastern remnants, we still find the coastal Caiçaras who descend from Native Indians and Portuguese Colonizers. The maintenance of such populations, and their existence in spite of the deforestation that occurred on the Atlantic Forest coast, deserves especial attention and analysis. In this study, I address, in particular, the Caiçaras who live on the coast of São Paulo and Rio de Janeiro States, illustrating with examples of coastal inhabitants from other areas, such as Bahia State (NE coast) and of other forested areas (riverine caboclos of the Amazon). The major focus of this study, based on previous research, performed since 1986 in several populations or villages of the Atlantic Forest coast, is to understand the resilience of the Caiçaras, which is analyzed using ecological concepts, such as metapopulation, resilience and adaptive cycles. The Caiçara populations are located on islands (Búzios, Comprida, Grande, Ilhabela, Jaguanum, Gipóia) and on the coast (Bertioga, Puruba, Picinguaba, among others). Information gathered about the Caiçaras regarding the economic cycles of the local regions, along with ecological, historical and economic data available, are used to understand such resilience, and are complemented with comparative examples from the Brazilian Amazon and with variables such as the local restrictions imposed by environmental governmental agencies. PMID:17010204

  8. Do comets have chondrules and CAIs? Evidence from the Leonid meteors

    NASA Astrophysics Data System (ADS)

    Swindle, Timothy D.; Campins, Humberto

    2004-10-01

    Chondrules, silicate spheres typically 0.1 to 1 mm in diameter, are the most abundant constituents in the most common meteorites falling on Earth, the ordinary chondrites. In addition, many primitive meteorites have calcium-aluminum-rich inclusions (CAIs). The question of whether comets have chondrules or CAIs is relevant to understanding what the interior of a comet is like and what a cometary meteorite might be like. In addition, one prominent model for forming chondrules and CAIs, the X-wind model, predicts their presence in comets, while most other models do not. At present, the best way to search for chondrules and CAIs in comets is through meteor showers derived from comets, in particular, the Leonid meteor shower. Evidence potentially could be found in the overall mass distribution of the shower, in chemical analyses of meteors, or in light curves. There is no evidence for a chondrule abundance in the Leonid meteors similar to that found in chondritic meteorites. There is intriguing evidence for chondrule- or CAI-sized objects in a small fraction of the light curves, but further work is required to generate a definitive test.

  9. Mineralogy and Petrology of EK-459-5-1, A Type B1 CAI from Allende

    NASA Technical Reports Server (NTRS)

    Jeffcoat, C. R.; Kerekgyarto, A. G.; Lapen, T. J.; Andreasen, R.; Righter, M.; Ross, D. K.

    2015-01-01

    Calcium-aluminum-rich inclusions (CAIs) are a type of coarse-grained clast composed of Ca-, Al-, and Mg-rich silicates and oxides found in chondrite meteorites. Type B (CAIs) are exclusively found in the CV chondrite meteorites and are the most well studied type of inclusion found in chondritic meteorites. Type B1 CAIs are distinguished by a nearly monomineralic rim of melilite that surrounds an interior predominantly composed of melilite, fassaite (Ti and Al-rich clinopyroxene), anorthite, and spinel with varying amounts of other minor primary and secondary phases. The formation of Type B CAIs has received considerable attention in the course of CAI research and quantitative models, experimental results and observations from Type B inclusions remain largely in disagreement. Recent experimental results and quantitative models have shown that the formation of B1 mantles could have occurred by the evaporative loss of Si and Mg during the crystallization of these objects. However, comparative studies suggest that the lower bulk SiO2 compositions in B1s result in more prior melilite crystallization before the onset of fassaite and anorthite crystallization leading to the formation of thick melilite rich rims in B1 inclusions. Detailed petrographic and cosmochemical studies of these inclusions will further our understanding of these complex objects.

  10. The Formation Of The First Solids In The Solar System: An Investigation Of CAI Diversity

    NASA Astrophysics Data System (ADS)

    Taillifet, Esther; Baillié, K.; Charnoz, S.; Aléon, J.

    2012-10-01

    Chondritic meteorites are primitive bodies and therefore an important source of information on the first moments of planets formation. Chondrites contain several materials especially calcium and aluminum rich inclusions (CAIs), known to be the oldest objects of the solar system (4.567 Gyr - Amelin et al., 2002; Connelly et al., 2008) and thus the first solids to be formed. CAIs appear in various textures, sizes and compositions in chondrites. Though, all of them should have formed at high temperature (1300-1800 K) in the same region of the solar nebula by condensation from the gas (e.g. Grossman, 1972; Yoneda & Grossman, 1995; Petaev & Wood, 1998; Ebel & Grossman 2000). To answer this problem we study the CAI formation within the solar nebula using numerical simulations. For this work we developed a self consistent thermodynamical model of the solar nebula (see associated talk from Baillié et. al ) based on previous works (Calvet et. al, 1991; Hueso & Guillot, 2005; Dullemond, Dominik and Natta, 2001). Using this model, we simulate the young system with Lagrangian Implicit Disk Transport code (LIDT - Charnoz et. al, 2010). We will focus on the very first instants of the CAIs within the few years following their condensation. We will report our first results in terms of thermal history and investigate if turbulence-driven transport may explain the CAI diversity.

  11. Experimental Determination of Li, Be and B Partitioning During CAI Crystallization

    SciTech Connect

    Ryerson, F J; Brenan, J M; Phinney, D L

    2005-01-12

    The main focus of the work is to develop a better understanding of the distribution of the elements B, Be and Li in melilite, fassaitic clinop clinopy-roxene, anorthite and spinel, which are the primary constituents of calcium-aluminum-rich inclusions (CAIs). These elements are the parent or decay products of short-lived nuclides (specifically, {sup 7}Be and {sup 10}Be) formed by cosmic ray spallation reactions on silicon and oxygen. Recent observations suggest that some CAIs contain ''fossil'' {sup 7}Be and {sup 10}Be in the form of ''excess'' amounts of their decay products (B and Li). The exact timing of {sup 7}Be and {sup 10}Be production is unknown, but if it occurred early in CAI history, it could constrain the birthplace of CAIs to be within a limited region near the infant sun. Other interpretations are possible, however, and bear little significance to early CAI genesis. In order to interpret the anomalies as being ''primary'', and thus originating at high temperature, information on the intermineral partitioning of both parent and daughter elements is required.

  12. The ethnoecology of Caiçara metapopulations (Atlantic Forest, Brazil): ecological concepts and questions.

    PubMed

    Begossi, Alpina

    2006-09-29

    The Atlantic Forest is represented on the coast of Brazil by approximately 7.5% of remnants, much of these concentrated on the country's SE coast. Within these southeastern remnants, we still find the coastal Caiçaras who descend from Native Indians and Portuguese Colonizers. The maintenance of such populations, and their existence in spite of the deforestation that occurred on the Atlantic Forest coast, deserves special attention and analysis. In this study, I address, in particular, the Caiçaras who live on the coast of São Paulo and Rio de Janeiro States, illustrating with examples of coastal inhabitants from other areas, such as Bahia State (NE coast) and of other forested areas (riverine caboclos of the Amazon). The major focus of this study, based on previous research, performed since 1986 in several populations or villages of the Atlantic Forest coast, is to understand the resilience of the Caiçaras, which is analyzed using ecological concepts, such as metapopulation, resilience and adaptive cycles. The Caiçara populations are located on islands (Búzios, Comprida, Grande, Ilhabela, Jaguanum, Gipóia) and on the coast (Bertioga, Puruba, Picinguaba, among others). Information gathered about the Caiçaras regarding the economic cycles of the local regions, along with ecological, historical and economic data available, are used to understand such resilience, and are complemented with comparative examples from the Brazilian Amazon and with variables such as the local restrictions imposed by environmental governmental agencies.

  13. A FIB/TEM Study of a Complex Wark-Lovering Rim on a Vigarano CAI

    NASA Technical Reports Server (NTRS)

    Keller, L. P.; Needham, A. W.; Messenger, S.

    2013-01-01

    Wark-Lovering (WL) rims are thin multilayered mineral sequences that surround most Ca, Al-rich inclusions (CAIs). Several processes have been proposed for WL rim formation, including condensation, flash-heating or reaction with a nebular reservoir, or combinations of these [e.g. 1-7], but no consensus exists. Our previous coordinated transmission electron microscope (TEM) and NanoSIMS O isotopic measurements showed that a WL rim experienced flash heating events in a nebular environment with planetary O isotopic composition, distinct from the (16)O-rich formation environment [6]. Our efforts have focused on CAIs from the CV(sub red) chondrites, especially Vigarano, because these have escaped much of the parent body alteration effects that are common in CAIs from CV(sub ox) group.

  14. Verification of new cloud discrimination algorithm using GOSAT TANSO-CAI in the Amazon

    NASA Astrophysics Data System (ADS)

    Oishi, Y.; Ishida, H.; Nakajima, T. Y.

    2015-12-01

    Greenhouse gases Observing SATellite (GOSAT) was launched in 2009 to measure the global atmospheric CO2 and CH4 concentrations. GOSAT is equipped with two sensors: the Thermal And Near-infrared Sensor for carbon Observation-Fourier Transform Spectrometer (TANSO-FTS) and the Cloud and Aerosol Imager (TANSO-CAI). The presence of clouds in the instantaneous field-of-view (IFOV) of the FTS leads to incorrect estimates of the concentrations. Thus, the FTS data which are suspected to be cloud-contaminated must be identified using a CAI cloud discrimination algorithm and rejected. Conversely, overestimation of clouds leads to reduce the amount of the FTS data which can be used to estimate the greenhouse gases concentrations. It becomes a serious problem in the region of tropical rainforest such as the Amazon, where there are very few remaining FTS data by cloud cover. The preparation for the launch of the GOSAT-2 in fiscal 2017 has been progressing. To improve the accuracy of estimates of the greenhouse gases concentrations, we need to refine the existing CAI cloud discrimination algorithm. For the reason, a new cloud discrimination algorithm using support vector machines (SVM) was developed. Visual inspections can use the locally optimized thresholds, though the existing CAI cloud discrimination algorithm uses the common thresholds all over the world. Thus, it is certain that the accuracy of visual inspections is better than these algorithms in the limited region without areas such as ice and snow, where it is difficult to discriminate between clouds and ground surfaces. In this study we evaluated the accuracy of the new cloud discrimination algorithm by comparing with the existing CAI cloud discrimination algorithm and visual inspections of the same CAI images in the Amazon. We will present our latest results.

  15. Deriving High Resolution UV Aerosol Optical Depth over East Asia using CAI-OMI Joint Retrieval

    NASA Astrophysics Data System (ADS)

    Go, S.; Kim, J.; KIM, M.; Lee, S.

    2015-12-01

    Monitoring aerosols using near UV spectral region have been successfully performed over decades by Ozong Monitoring Instruments (OMI) with benefit of strong aerosol signal over continuous dark surface reflectance, both land and ocean. However, because of big foot print of OMI, the cloud contamination error was a big issue in the UV aerosol algorithm. In the present study, high resolution UV aerosol optical depth (AOD) over East Asia was derived by collaborating the Greenhouse gases Observing SATellite/Thermal And Near infrared Sensor for carbon Observation (GOSAT/TANSO)-Cloud and Aerosol Imager (CAI) and OMI together. AOD of 0.1 degree grid resolution was retrieved using CAI band 1 (380nm) by bring OMI lv.2 aerosol type, single scattering albedo, and aerosol layer peak height in 1 degree grid resolution. Collocation of the two dataset within the 0.5 degree grid with time difference of OMI and CAI less than 5 minute was selected. Selected region becomes wider as it goes to the higher latitude. Also, calculated degradation factor of 1.57 was applied to CAI band1 (380nm) by comparing normalized radiance and Lambertian Equivalent Reflectivity (LER) of both sensors. The calculated degradation factor was reasonable over dark scene, but inconsistent over cirrus cloud and bright area. Then, surface reflectance was developed by compositing CAI LER minimum data over three month period, since the infrequent sampling rate associated with the three-day recursion period of GOSAT and the narrow CAI swath of 1000 km. To retrieve AOD, look up table (LUT) was generated using radiative transfer model VLIDORT NGST. Finally, the retrieved AOD was validated with AERONET ground based measurement data during the Dragon-NE Asia campaign in 2012.

  16. Arginine oscillation explains Na+ independence in the substrate/product antiporter CaiT.

    PubMed

    Kalayil, Sissy; Schulze, Sabrina; Kühlbrandt, Werner

    2013-10-22

    Most secondary-active transporters transport their substrates using an electrochemical ion gradient. In contrast, the carnitine transporter (CaiT) is an ion-independent, l-carnitine/γ-butyrobetaine antiporter belonging to the betaine/carnitine/choline transporter family of secondary transporters. Recently determined crystal structures of CaiT from Escherichia coli and Proteus mirabilis revealed an inverted five-transmembrane-helix repeat similar to that in the amino acid/Na(+) symporter LeuT. The ion independence of CaiT makes it unique in this family. Here we show that mutations of arginine 262 (R262) make CaiT Na(+)-dependent. The transport activity of R262 mutants increased by 30-40% in the presence of a membrane potential, indicating substrate/Na(+) cotransport. Structural and biochemical characterization revealed that R262 plays a crucial role in substrate binding by stabilizing the partly unwound TM1' helix. Modeling CaiT from P. mirabilis in the outward-open and closed states on the corresponding structures of the related symporter BetP reveals alternating orientations of the buried R262 sidechain, which mimic sodium binding and unbinding in the Na(+)-coupled substrate symporters. We propose that a similar mechanism is operative in other Na(+)/H(+)-independent transporters, in which a positively charged amino acid replaces the cotransported cation. The oscillation of the R262 sidechain in CaiT indicates how a positive charge triggers the change between outward-open and inward-open conformations as a unifying critical step in LeuT-type transporters.

  17. Oxygen reservoirs in the early solar nebula inferred from an Allende CAI.

    PubMed

    Young, E D; Russell, S S

    1998-10-16

    Ultraviolet laser microprobe analyses of a calcium-aluminum-rich inclusion (CAI) from the Allende meteorite suggest that a line with a slope of exactly 1.00 on a plot of delta (17)O against delta (18)O represents the primitive oxygen isotope reservoir of the early solar nebula. Most meteorites are enriched in (17)O and (18)O relative to this line, and their oxygen isotope ratios can be explained by mass fractionation or isotope exchange initiating from the primitive reservoir. These data establish a link between the oxygen isotopic composition of the abundant ordinary chondrites and the primitive (16)O-rich component of CAIs.

  18. Oxygen reservoirs in the early solar nebula inferred from an allende CAI

    PubMed

    Young; Russell

    1998-10-16

    Ultraviolet laser microprobe analyses of a calcium-aluminum-rich inclusion (CAI) from the Allende meteorite suggest that a line with a slope of exactly 1.00 on a plot of delta17O against delta18O represents the primitive oxygen isotope reservoir of the early solar nebula. Most meteorites are enriched in 17O and 18O relative to this line, and their oxygen isotope ratios can be explained by mass fractionation or isotope exchange initiating from the primitive reservoir. These data establish a link between the oxygen isotopic composition of the abundant ordinary chondrites and the primitive 16O-rich component of CAIs.

  19. Processing of refractory meteorite inclusions (CAIs) in parent-body atmospheres

    NASA Technical Reports Server (NTRS)

    Podolak, Morris; Bunch, T. E.; Cassen, Pat; Reynolds, Ray T.; Chang, S.

    1990-01-01

    Ca-Al-rich inclusions (CAIs) in refractory meteorites are shown to have been subject to partial melting during a suitably high gas density/small scale height regime arising during gasdynamic deceleration in a temporary atmosphere around an accreting parent body. The presence of dust in such an atmosphere would have increased the pressure gradient with height, lowering the boiloff rate, and permitting dust particles to become trapped in the partially melted material. CAIs may therefore be studied as probes of a primitive atmosphere.

  20. Thermal and chemical evolution in the early solar system as recorded by FUN CAIs: Part I - Petrology, mineral chemistry, and isotopic composition of Allende FUN CAI CMS-1

    NASA Astrophysics Data System (ADS)

    Williams, C. D.; Ushikubo, T.; Bullock, E. S.; Janney, P. E.; Hines, R. R.; Kita, N. T.; Hervig, R. L.; MacPherson, G. J.; Mendybaev, R. A.; Richter, F. M.; Wadhwa, M.

    2017-03-01

    Detailed petrologic, geochemical and isotopic analyses of a new FUN CAI from the Allende CV3 meteorite (designated CMS-1) indicate that it formed by extensive melting and evaporation of primitive precursor material(s). The precursor material(s) condensed in a 16O-rich region (δ17O and δ18O ∼ -49‰) of the inner solar nebula dominated by gas of solar composition at total pressures of ∼10-3-10-6 bar. Subsequent melting of the precursor material(s) was accompanied by evaporative loss of magnesium, silicon and oxygen resulting in large mass-dependent isotope fractionations in these elements (δ25Mg = 30.71-39.26‰, δ29Si = 14.98-16.65‰, and δ18O = -41.57 to -15.50‰). This evaporative loss resulted in a bulk composition similar to that of compact Type A and Type B CAIs, but very distinct from the composition of the original precursor condensate(s). Kinetic fractionation factors and the measured mass-dependent fractionation of silicon and magnesium in CMS-1 suggest that ∼80% of the silicon and ∼85% of the magnesium were lost from its precursor material(s) through evaporative processes. These results suggest that the precursor material(s) of normal and FUN CAIs condensed in similar environments, but subsequently evolved under vastly different conditions such as total gas pressure. The chemical and isotopic differences between normal and FUN CAIs could be explained by sorting of early solar system materials into distinct physical and chemical regimes, in conjunction with discrete heating events, within the protoplanetary disk.

  1. Gender Role, Gender Identity and Sexual Orientation in CAIS ("XY-Women") Compared With Subfertile and Infertile 46,XX Women.

    PubMed

    Brunner, Franziska; Fliegner, Maike; Krupp, Kerstin; Rall, Katharina; Brucker, Sara; Richter-Appelt, Hertha

    2016-01-01

    The perception of gender development of individuals with complete androgen insensitivity syndrome (CAIS) as unambiguously female has recently been challenged in both qualitative data and case reports of male gender identity. The aim of the mixed-method study presented was to examine the self-perception of CAIS individuals regarding different aspects of gender and to identify commonalities and differences in comparison with subfertile and infertile XX-chromosomal women with diagnoses of Mayer-Rokitansky-Küster-Hauser syndrome (MRKHS) and polycystic ovary syndrome (PCOS). The study sample comprised 11 participants with CAIS, 49 with MRKHS, and 55 with PCOS. Gender identity was assessed by means of a multidimensional instrument, which showed significant differences between the CAIS group and the XX-chromosomal women. Other-than-female gender roles and neither-female-nor-male sexes/genders were reported only by individuals with CAIS. The percentage with a not exclusively androphile sexual orientation was unexceptionally high in the CAIS group compared to the prevalence in "normative" women and the clinical groups. The findings support the assumption made by Meyer-Bahlburg ( 2010 ) that gender outcome in people with CAIS is more variable than generally stated. Parents and professionals should thus be open to courses of gender development other than typically female in individuals with CAIS.

  2. Revision of the Oriental leafhopper genus Destinoides Cai & He (Hemiptera: Cicadellidae: Ledrinae), with a new synonym and two new combinations.

    PubMed

    Sun, Jing; Webb, Michael D; Zhang, Yalin

    2014-04-08

    The leafhopper genus Destinoides Cai & He is revised to include two species D. latifrons (Walker 1851, Ledra) n. comb. and D. conspicuus (Distant 1907, Petalocephala) n. comb. Destinoides fasciata Cai & He, 2000 is placed as a junior synonym of D. latifrons, syn. nov. These two species are redescribed and illustrated in detail and a key is given based on the males.

  3. Stable Magnesium Isotope Variation in Melilite Mantle of Allende Type B1 CAI EK 459-5-1

    NASA Technical Reports Server (NTRS)

    Kerekgyarto, A. G.; Jeffcoat, C. R.; Lapen, T. J.; Andreasen, R.; Righter, M.; Ross, D. K.

    2014-01-01

    Ca-Al-rich inclusions (CAIs) are the earliest formed crystalline material in our solar system and they record early Solar System processes. Here we present petrographic and delta Mg-25 data of melilite mantles in a Type B1 CAI that records early solar nebular processes.

  4. Structural framework of a major intracontinental orogenic termination zone: The easternmost Tien Shan, China

    USGS Publications Warehouse

    Cunningham, D.; Owen, L.A.; Snee, L.W.; Li, J.

    2003-01-01

    The Barkol Tagh and Karlik Tagh ranges of the easternmost Tien Shan are a natural laboratory for studying the fault architecture of an active termination zone of a major intracontinental mountain range. Barkol and Karlik Tagh and lesser ranges to the north are bounded by active thrust faults that locally deform Quaternary sediments. Major thrusts in Karlik Tagh connect along strike to the east with the left-lateral Gobi-Tien Shan Fault System in SW Mongolia. From a Mongolian perspective. Karlik Tagh represents a large restraining bend for this regional strike-slip fault system, and the entire system of thrusts and strike-slip faults in the Karlik Tagh region defines a horsetail splay fault geometry. Regionally, there appears to be a kinematic transition from thrust-dominated deformation in the central Tien Shan to left-lateral transpressional deformation in the easternmost Tien Shan. This transition correlates with a general eastward decrease in mountain belt width and average elevation and a change in the angular relationship between the NNE-directed maximum horizontal stress in the region and the pre-existing basement structural grain, which is northwesterly in the central Tien Shan (orthogonal to SHmax) but more east-west in the eastern Tien Shan (acute angular relationship with SHmax . Ar-Ar ages indicate that major range-bounding thrusts in Barkol and Karlik Tagh are latest Permian-Triassic ductile thrust zones that underwent brittle reactivation in the Late Cenozoic. It is estimated that the modern mountain ranges of the extreme easternmost Tien Shan could have been constructed by only 10-15 km of Late Cenozoic horizontal shortening.

  5. Performance assessment of the cellulose absorption index (CAI) method for estimating crop residue cover

    Technology Transfer Automated Retrieval System (TEKTRAN)

    Accurate and quick field estimation of crop residues are important for carbon sequestration and biofuel production programs. Landscape-scale assessment of this vital information has promoted the use of remote sensing technology. The cellulose absorption index (CAI) technique has outperformed other ...

  6. Heterogeneity of Mg Isotopes and Variable ^26Al/^27Al Ratio in FUN CAIs

    NASA Astrophysics Data System (ADS)

    Park, C.; Nagashima, K.; Hutcheon, I. D.; Wasserburg, G. J.; Papanastassiou, D. A.; Davis, A. M.; Huss, G. R.; Krot, A. N.

    2013-09-01

    We report high-precision Mg-isotope data of individual minerals from the Axtell 2271, BG82DH8, EK1-4-1, C1, TE, and CG14 FUN CAIs, which shows variations in both Mg-isotope ratio and ^26Al/^27Al ratio.

  7. Learner Control of Instructional Sequencing Within an Adaptive Tutorial CAI Environment

    ERIC Educational Resources Information Center

    Seidel, Robert J.; And Others

    1978-01-01

    This study was designed to test effects of a specified degree of learner control over the sequencing of instructional materials in a self contained tutorial CAI course in COBOL programming. Findings describe contributions and interactions of learner controlled variables with respect to instructional effectiveness and efficiency. (RAO)

  8. Role of Computer Assisted Instruction (CAI) in an Introductory Computer Concepts Course.

    ERIC Educational Resources Information Center

    Skudrna, Vincent J.

    1997-01-01

    Discusses the role of computer assisted instruction (CAI) in undergraduate education via a survey of related literature and specific applications. Describes an undergraduate computer concepts course and includes appendices of instructions, flowcharts, programs, sample student work in accounting, COBOL instructional model, decision logic in a…

  9. Using CAI To Enhance the Peer Acceptance of Mainstreamed Students with Mild Disabilities.

    ERIC Educational Resources Information Center

    Culliver, Concetta; Obi, Sunday

    This study applied computer-assisted instruction (CAI) techniques to improve peer acceptance among 92 mainstreamed students with mild disabilities from 10 to 13 years of age. Participants in the treatment group received their generalized curriculum program (including mathematics, language arts, reading, health, social studies, and science)…

  10. C.A.I. as a Means for Educational Justice in Primary Schools: A Greek Experience.

    ERIC Educational Resources Information Center

    Raptis, Nicos

    This study examines the effects of computer assisted instruction (CAI) on the inequalities in education among children of less privileged backgrounds. A natural science lesson was taught to 116 children at the fifth level of the Greek primary school. Subjects went to two different public schools, one of which was in a privileged area, and the…

  11. Making C.A.I. Make a Difference in College Teaching.

    ERIC Educational Resources Information Center

    Lower, Stephen K.

    An explanation for the failure of technology and computer-assisted instruction (CAI) in particular to make much headway in education is that even when innovations are introduced in the classroom, their potentials are not exploited; rather, they are used in traditional ways. The integration of new technologies with other classroom activities is…

  12. Socioeconomic Status, Aptitude, and Gender Differences in CAI Gains of Arithmetic.

    ERIC Educational Resources Information Center

    Hativa, Nira; Shorer, Dvora

    1989-01-01

    A report is given of a study which examined the effects of computer-assisted instruction (CAI) in mathematics on 99 disadvantaged and 112 advantaged Israeli students. Higher performance levels and larger gains were found for advantaged over disadvantaged students, for high achievers over low achievers, and for boys over girls. (IAH)

  13. A Cross-National CAI Tool To Support Learning Operations Decision-Making and Market Analysis.

    ERIC Educational Resources Information Center

    Mockler, Robert J.; Afanasiev, Mikhail Y.; Dologite, Dorothy G.

    1999-01-01

    Describes bicultural (United States and Russia) development of a computer-aided instruction (CAI) tool to learn management decision-making using information systems technologies. The program has been used with undergraduate and graduate students in both countries; it integrates free and controlled market concepts and combines traditional computer…

  14. The Use of C.A.I. in the Language Program at Gallaudet.

    ERIC Educational Resources Information Center

    Madachy, James L.; Miller, J. Douglas

    Employing an English-as-a-second-language approach, Gallaudet College has developed 101 computer assisted instruction (CAI) lessons to help deaf students master basic English structures. These lessons begin with a pretest and then branch to appropriate explanations and drills. Some are accompanied by coordinated presentations in sign language. In…

  15. Melilite-Rich CAIs and Wark-Lovering Rims Formed from a Common Oxygen Reservoir

    NASA Astrophysics Data System (ADS)

    Bodénan, J.-D.; Starkey, N. A.; Russell, S. S.; Wright, I. P.; Franchi, I. A.

    2013-09-01

    O isotopic ratio profiles in CAIs from the unaltered meteorites Léoville and QUE 99177 and their Wark-Lovering rims show no variation, indicating that they sampled the same O isotopic reservoir that persisted until the end of WL rim formation.

  16. Consumption of fa cai Nostoc soup: a potential for BMAA exposure from Nostoc cyanobacteria in China?

    PubMed

    Roney, Britton R; Renhui, Li; Banack, Sandra Anne; Murch, Susan; Honegger, Rosmarie; Cox, Paul Alan

    2009-01-01

    Grown in arid regions of western China the cyanobacterium Nostoc flagelliforme--called fa cai in Mandarin and fat choy in Cantonese--is wild-harvested and used to make soup consumed during New Year's celebrations. High prices, up to $125 USD/kg, led to overharvesting in Inner Mongolia, Ningxia, Gansu, Qinghai, and Xinjiang. Degradation of arid ecosystems, desertification, and conflicts between Nostoc harvesters and Mongol herdsmen concerned the Chinese environmental authorities, leading to a government ban of Nostoc commerce. This ban stimulated increased marketing of a substitute made from starch. We analysed samples purchased throughout China as well as in Chinese markets in the United States and the United Kingdom. Some were counterfeits consisting of dyed starch noodles. A few samples from California contained Nostoc flagelliforme but were adulterated with starch noodles. Other samples, including those from the United Kingdom, consisted of pure Nostoc flagelliforme. A recent survey of markets in Cheng Du showed no real Nostoc flagelliforme to be marketed. Real and artificial fa cai differ in the presence of beta-N-methylamino-L-alanine (BMAA). Given its status as a high-priced luxury food, the government ban on collection and marketing, and the replacement of real fa cai with starch substitutes consumed only on special occasions, it is anticipated that dietary exposure to BMAA from fa cai will be reduced in the future in China.

  17. Toward a Market Success for CAI; An Overview of the TICCIT Program.

    ERIC Educational Resources Information Center

    Stetten, Kenneth J.

    A new computer-assisted instruction (CAI) system for college teaching is being tested in two locations by the MITRE Corporation. The system, called TICCIT (Time-Share Interactive Computer-Controlled Information Television), now interacts with more than 100 students, each moving at his own pace, for four semesters of community college math and…

  18. The Effect of Adaptive, Advisement, and Linear CAI Control Strategies on the Learning of Mathematics Rules.

    ERIC Educational Resources Information Center

    Goetzfried, Leslie; Hannafin, Michael

    This study examined the effects of the locus of three computer assisted instruction (CAI) strategies on the accuracy and efficiency of mathematics rule and application learning of 47 low-achieving seventh grade students in remedial mathematics classes. The instructional task was a mathematics rule lesson concerning divisibility by the numbers two,…

  19. CAI for the Visually Handicapped: Promising Collaboration Between Two and Four-Year Schools.

    ERIC Educational Resources Information Center

    Wilkinson, William K.; And Others

    This report describes the efforts of the Office of Research and Extension of the North Carolina State University (NCSU) School of Education to develop vocal computer-assisted instruction (CAI) tutorials for blind junior college students, the rationale behind those efforts, the costs and means of funding for the project, and suggested ways in which…

  20. A Pseudo-Language for Creating CAI Programs on APL Systems

    ERIC Educational Resources Information Center

    Gucker, Edward J.

    1973-01-01

    Encourages the use of APL as a language for computer assisted instruction (CAI) instead of such languages as BASIC or COURSEWRITER. Describes a set of APL functions that can simulate to some extent the features of COURSEWRITER, while permitting a more experienced course author to use the full mathematical power of APL. (Author/JF)

  1. Web Pages: An Effective Method of Providing CAI Resource Material in Histology.

    ERIC Educational Resources Information Center

    McLean, Michelle

    2001-01-01

    Presents research that introduces computer-aided instruction (CAI) resource material as an integral part of the second-year histology course at the University of Natal Medical School. Describes the ease with which this software can be developed, using limited resources and available skills, while providing students with valuable learning…

  2. Case Study: Using VDO or CAI in Studying Methods of Proof

    ERIC Educational Resources Information Center

    Chundang, Ungsana; Setteechaichana, Patcharin

    2012-01-01

    The objective of the research is to study the effectiveness of the students' performance and the attitude of the students towards using VDO (MTH 225 principle of mathematics) or CAI (MTH 225 principle of mathematics) in studying the topic "Methods of Proof", of 74 students. The students would be categorized into: group A, students who…

  3. Has Computer Assisted Instruction (CAI) Been a Financial Failure? Studies in Economic Education No. 3.

    ERIC Educational Resources Information Center

    Daellenbach, Lawrence A.; And Others

    A course in macroeconomics was used to investigate the cost effectiveness of computer-assisted instruction (CAI). The experimental design used an experimental section in which the students had the opportunity to use the computer to the intensity of their choice, choosing from tutorial lessons, games, and simulations. The students in the control…

  4. Dynamic support of the Tien Shan lithosphere based on flexural and rheological modeling

    NASA Astrophysics Data System (ADS)

    Jiang, Xiaodian

    2014-10-01

    The Tien Shan is a high, young and seismically active intracontinental mountain belt in central Asia that has been uplifted approximately 3 km over the past 10 Ma. A flexural analysis using Bouguer gravity and topographic data was used to determine the dynamic lithospheric mechanisms that are responsible for the topographic uplift and crustal thickening of the range. Bouguer gravity anomalies were used to constrain flexural models for isostatic compensation associated with the large relief of the Tien Shan. This is explained by significant underthrusting of a continuous elastic plate below the Tien Shan, with an effective elastic thicknesses (Te) that gradually changes from 40 to 50 km in the Tarim and Junggar basins and the Kazakh plate to 20-23 km beneath the Tien Shan. Horizontal shortening due to folding and thrusting of the upper-middle crust causes uplift and crustal thickening of the margin of the Tien Shan. The regional and local compensation occur at the eastern and western parts of the Tien Shan respectively. Rheological modeling using a simple geothermal structure for the Tien Shan reveals that the base of the strong upper crust of Tibet is at a depth of 30-35 km, which is consistent with the depths of 7776 earthquakes between 1970 and 2011, which serve as constraints on the brittle failure domain of the area. The Moho depths are used to determine the thickness of the lower crust (17-25 km) and to understand the mobility of the lower-crustal flow of the Tien Shan. The tendency for the strong upper crust to flow over the weak, ductile lower crust (or middle-lower crust) depends on the thickness of the lower crust. In other words, its strength depends on the depths of the base of the upper crust and the Moho. The larger the difference, the easier it is for the upper crust to flow relative to the strong upper-mantle lithosphere. The crustal deformation is decoupled from deformation of the upper-mantle lithosphere by the weak, ductile lower crust of the Tien

  5. Chronology of chrondrule and CAI formation: Mg-Al isotopic evidence

    NASA Technical Reports Server (NTRS)

    Macpherson, G. J.; Davis, A. M.

    1994-01-01

    Details of the chondrule and Ca-Al-rich inclusion (CAI) formation during the earliest history of the solar system are imperfectly known. Because CAI's are more 'refractory' than ferromagnesian chondrules and have the lowest recorded initial Sr-87/Sr-86 ratios of any solar system materials, the expectation is that CAI's formed earlier than chondrules. But it is not known, for example, if CAI formation had stopped by the time chondrule formation began. Conventional (absolute) age-dating techniques cannot adequately resolve small age differences (less than 10(exp 6) years) between objects of such antiquity. One approach has been to look at systematic differences in the daughter products of short-lived radionuclides such as Al-26 and I-129. Unfortunately, neither system appears to be 'well-behaved.' One possible reason for this circumstance is that later secondary events have partially reset the isotopic systems, but a viable alternative continues to be large-scale (nebular) heterogeneity in initial isotopic abundances, which would of course render the systems nearly useless as chronometers. In the past two years the nature of this problem has been redefined somewhat. Examination of the Al-Mg isotopic database for all CAI's suggests that the vast majority of inclusions originally had the same initial Al-26/Al-27 abundance ratio, and that the ill-behaved isotopic systematics now observed are the results of later partial reequilibration due to thermal processing. Isotopic heterogeneities did exist in the nebula, as demonstrated by the existence of so-called FUN inclusions in CV3 chondrites and isotopically anomalous hibonite grains in CM2 chondrites, which had little or no live Al-26 at the time of their formation. But, among the population of CV3 inclusions at least, FUN inclusions appear to have been a relatively minor nebular component.

  6. An ion microprobe study of CAIs from CO3 meteorites. [Abstract only

    NASA Technical Reports Server (NTRS)

    Russell, S. S.; Greenwood, R. C.; Fahey, A. J.; Huss, G. R.; Wasserburg, G. J.

    1994-01-01

    When attempting to interpret the history of Ca, Al-rich inclusions (CAIs) it is often difficult to distinguish between primary features inherited from the nebula and those produced during secondary processing on the parent body. We have undertaken a systematic study of CAIs from 10 CO chondrites, believed to represent a metamorphic sequence with the goal of distinguishing primary and secondary features. ALHA 77307 (3.0), Colony (3.0), Kainsaz (3.1), Felix (3.2), ALH 82101 (3.3), Ornans (3.3), Lance (3.4), ALHA 77003 (3.5), Warrenton (3.6), and Isna (3.7) were examined by Scanning Electron Microscopy (SEM) and optical microscopy. We have identified 141 CAIs within these samples, and studied in detail the petrology of 34 inclusions. The primary phases in the lower petrologic types are spinel, melilite, and hibonite. Perovskite, FeS, ilmenite, anorthite, kirschsteinite, and metallic Fe are present as minor phases. Melilite becomes less abundant in higher petrologic types and was not detected in chondrites of type 3.5 and above, confirming previous reports that this mineral easily breaks down during heating. Iron, an element that would not be expected to condense at high temperatures, has a lower abundance in spinel from low-petrologic-type meteorites than those of higher grade, and CaTiO3 is replaced by FeTiO3 in meteorites of higher petrologic type. The abundance of CAIs is similar in each meteorite. Eight inclusions have been analyzed by ion probe. The results are summarized. The results obtained to date show that CAIs in CO meteorites, like those from other meteorite classes, contain Mg* and that Mg in some inclusions has been redistributed.

  7. High-Throughput Proteomic Approaches to the Elucidation of Potential Biomarkers of Chronic Allograft Injury (CAI)

    PubMed Central

    Cassidy, Hilary; Slyne, Jennifer; Frain, Helena; Slattery, Craig; Ryan, Michael P.; McMorrow, Tara

    2013-01-01

    This review focuses on the role of OMICs technologies, concentrating in particular on proteomics, in biomarker discovery in chronic allograft injury (CAI). CAI is the second most prevalent cause of allograft dysfunction and loss in the first decade post-transplantation, after death with functioning graft (DWFG). The term CAI, sometimes referred to as chronic allograft nephropathy (CAN), describes the deterioration of renal allograft function and structure as a result of immunological processes (chronic antibody-mediated rejection), and other non-immunological factors such as calcineurin inhibitor (CNI) induced nephrotoxicity, hypertension and infection. Current methods for assessing allograft function are costly, insensitive and invasive; traditional kidney function measurements such as serum creatinine and glomerular filtration rate (GFR) display poor predictive abilities, while the current “gold-standard” involving histological diagnosis with a renal biopsy presents its own inherent risks to the overall health of the allograft. As early as two years post-transplantation, protocol biopsies have shown more than 50% of allograft recipients have mild CAN; ten years post-transplantation more than 50% of the allograft recipients have progressed to severe CAN which is associated with diminishing graft function. Thus, there is a growing medical requirement for minimally invasive biomarkers capable of identifying the early stages of the disease which would allow for timely intervention. Proteomics involves the study of the expression, localization, function and interaction of the proteome. Proteomic technologies may be powerful tools used to identify novel biomarkers which would predict CAI in susceptible individuals. In this paper we will review the use of proteomics in the elucidation of novel predictive biomarkers of CAI in clinical, animal and in vitro studies. PMID:28250402

  8. Empirical Relationship between particulate matter and Aerosol Optical Depth over Northern Tien-Shan, Central Asia

    EPA Science Inventory

    Measurements were obtained at two sites in northern Tien-Shan in Central Asia during a 1-year period beginning July 2008 to examine the statistical relationship between aerosol optical depth (AOD) and of fine [PM2.5, particles less than 2.5 μm aerodynamic diameter (AD)] and coars...

  9. Teaching earth sciences: should we implement teacher-directed or student-controlled CAI in the secondary classroom?

    NASA Astrophysics Data System (ADS)

    Chang, Chun-Yen

    2003-04-01

    While previous studies and meta analyses have primarily focused on the comparative efficacy of computer assisted instruction (CAI) versus traditional instruction, there have been relatively fewer examples of research exploring how various teaching formats of CAI influence student science learning outcomes in the secondary classroom. In this paper this issue is addressed by comparing teacher-directed CAI (TDCAI) and student-controlled CAI (SCCAI) in a compulsory earth science course in a secondary school in Taiwan. Data collection instruments included the Earth Science Achievement Test and the Attitudes Toward Earth Science Inventory. A multivariate analysis of covariance suggested that TDCAI students had significantly higher score gains than SCCAI students on the set of achievement and attitude measures. It is therefore suggested that TDCAI-based instruction is an alternative in teaching basic science concepts in the secondary classroom.

  10. Heterogeneity of a metal particle enriched with refractory elements in the CAI Efremovka CV chondrite

    NASA Astrophysics Data System (ADS)

    Fisenko, A. V.; Ignatenko, K. I.; Lavrukhina, A. K.

    1990-03-01

    This paper describes the morphology and mineral composition of a macroscopic-size (about 0.5 mm) metallic particle found in a type-B1 CAI fragment from the Efremovka chondrite. Results of mineralographic and chemical analyses showed that the particle consists of two different metallic particles. One of these (EM1A), which is of a hypidiomorphic shape, is composed mainly of taenite and kamacite and contains micron-size inclusions of vanadium oxide. The other particle (EM1) is of ellipsoidal form and, besides taenite and kamacite, is enriched by phosphides; it also contains inclusions of vanadium sulfide and oxide. The EM particle is surrounded by a border of opaque minerals including kulsonite, chromite, and Ca phosphate. The characteristics of this particle have no analogs among the known metal particles in CAI or other carbonaceous chondrites.

  11. Alternative communication network designs for an operational Plato 4 CAI system

    NASA Technical Reports Server (NTRS)

    Mobley, R. E., Jr.; Eastwood, L. F., Jr.

    1975-01-01

    The cost of alternative communications networks for the dissemination of PLATO IV computer-aided instruction (CAI) was studied. Four communication techniques are compared: leased telephone lines, satellite communication, UHF TV, and low-power microwave radio. For each network design, costs per student contact hour are computed. These costs are derived as functions of student population density, a parameter which can be calculated from census data for one potential market for CAI, the public primary and secondary schools. Calculating costs in this way allows one to determine which of the four communications alternatives can serve this market least expensively for any given area in the U.S. The analysis indicates that radio distribution techniques are cost optimum over a wide range of conditions.

  12. Al-rich Chondrules: Petrologic Basis for Their Diversity, and Relation to Type C CAIs

    NASA Technical Reports Server (NTRS)

    MacPherson, G. J.; Huss, G. R.

    2003-01-01

    Al-rich chondrules share mineralogical and chemical properties with, and are intermediate in a volatility sense between, CAIs and ferromagnesian chondrules. In some way they must be petrogenetic links between the two. A recent upsurge of interest in Al-rich chondrules is due to their constituent plagioclase feldspar and Al-rich glass being amenable to successful ion microprobe searches for radiogenic Mg-26, the decay product of Al-26 (t(sub 1/2) = 720,000 y). This has allowed estimates to be made of the time duration between CAI formation and the onset of Al-rich (and possibly, by extension, ferromagnesian) chondrule formation, on the order of 1.5-2.5 million years.

  13. CAIS standard manual. System number 26. Industrial gas storage and distribution systems

    SciTech Connect

    1995-04-28

    At this installation the list of facilities to be surveyed, including infrastructure, will be addressed on the basis of 32 unique systems that form the CAIS Engineering Deficiency Standards and Inspection Methods document. Each system deals with a specific technical aspect of the facility to be surveyed. Within each system a further breakdown is made to subsystems, each having a related list of components. Detailed observations of the listed defects are provided so as to allow the entry of observed quantification data. A DOD CAIS manual is provided for each of the 32 systems with an internal organization. The System Tree is a graphical representation of the Work Breakdown Structure, showing system, subsystem and component relationships for the Industrial Gas Storage and Distribution System.

  14. CAIS standard manual. System number 25. Coal site handling and storage

    SciTech Connect

    1995-04-28

    At this installation the list of facilities to be surveyed, including infrastructure, will be addressed on the basis of 32 unique systems that form the CAIS Engineering Deficiency Standards and Inspection Methods document. Each system deals with a specific technical aspect of the facility to be surveyed. Within each system a further breakdown is made to subsystems, each having a related list of components. Detailed observations of the listed defects are provided so as to allow the entry of observed quantification data. A DOD CAIS manual is provided for each of the 32 systems with an internal organization. The System Tree is a graphical representation of the Work Breakdown Structure, showing system, subsystem and component relationships for the Coal Site Handling and Storage Svstem.

  15. Evaluation of the Vesicating Properties of Neutralized Chemical Agent Identification Set (CAIS) Components

    DTIC Science & Technology

    1997-06-01

    euthanasia, 17 TABLE 2. SYNOPSIS OF PHASE II AND PHASE 111 TESTING PROCEDURES Phase II. A total of I I hairless guinea pigs ( HGPs ) were used in this...24 HGPs were used, dosing six to eight sites per animal with a 1 hr duration of exposure. All animals were examined 24 hr following exposure and...The "blue" wastestream, that CAIS component containing neat HD neutralized with DCDMH, has been found to cause microvesication in HGPs at dosing

  16. Limited subsolidus diffusion in type B1 CAI: Evidence from Ti distribution in spinel

    NASA Technical Reports Server (NTRS)

    Meeker, G. P.; Quick, J. E.; Paque, Julie M.

    1993-01-01

    Most models of calcium aluminum-rich inclusions (CAI) have focused on early stages of formation by equilibrium crystallization of a homogeneous liquid. Less is known about the subsolidus cooling history of CAI. Chemical and isotopic heterogeneties on a scale of tens to hundreds of micrometers (e.g. MacPherson et al. (1989) and Podosek, et al. (1991)) suggest fairly rapid cooling with a minimum of subsolidus diffusion. However, transmission electron microscopy indicates that solid state diffusion may have been an important process at a smaller scale (Barber et al. 1984). If so, chemical evidence for diffusion could provide constraints on cooling times and temperatures. With this in mind, we have begun an investigation of the Ti distribution in spinels from two type B1 CAI from Allende to determine if post-crystallization diffusion was a significant process. The type B1 CAIs, 3529Z and 5241 have been described by Podosek et al. (1991) and by El Goresy et al. (1985) and MacPherson et al. (1989). We have analyzed spinels in these inclusions using the electron microprobe. These spinels are generally euhedral, range in size from less than 10 to 15 micron and are poikilitically enclosed by millimeter-sized pyroxene, melilite, and anorthite. Analyses were obtained from both the mantles and cores of the inclusions. Compositions of pyroxene in the vicinity of individual spinel grains were obtained by analyzing at least two points on opposite sides of the spinel and averaging the compositions. The pyroxene analyses were obtained within 15 microns of the spinel-pyroxene interface. No compositional gradients were observed within single spinel crystals. Ti concentrations in spinels included within pyroxene, melilite, and anorthite are presented.

  17. Numerical investigation of CAI Combustion in the Opposed- Piston Engine with Direct and Indirect Water Injection

    NASA Astrophysics Data System (ADS)

    Pyszczek, R.; Mazuro, P.; Teodorczyk, A.

    2016-09-01

    This paper is focused on the CAI combustion control in a turbocharged 2-stroke Opposed-Piston (OP) engine. The barrel type OP engine arrangement is of particular interest for the authors because of its robust design, high mechanical efficiency and relatively easy incorporation of a Variable Compression Ratio (VCR). The other advantage of such design is that combustion chamber is formed between two moving pistons - there is no additional cylinder head to be cooled which directly results in an increased thermal efficiency. Furthermore, engine operation in a Controlled Auto-Ignition (CAI) mode at high compression ratios (CR) raises a possibility of reaching even higher efficiencies and very low emissions. In order to control CAI combustion such measures as VCR and water injection were considered for indirect ignition timing control. Numerical simulations of the scavenging and combustion processes were performed with the 3D CFD multipurpose AVL Fire solver. Numerous cases were calculated with different engine compression ratios and different amounts of directly and indirectly injected water. The influence of the VCR and water injection on the ignition timing and engine performance was determined and their application in the real engine was discussed.

  18. Application of Global Positioning Measurements to Continental Collision in the Pamir-Tien Shan Region, Central Asia and GPS Survey of the Western Tien Shan

    NASA Technical Reports Server (NTRS)

    Hamburger, Michael W.; Reilinger, Robert E.; Hager, Bradford H.; Molnar, Peter

    1997-01-01

    In this report, we summarize what we have accomplished with five years of funding from NASA under its DOSE program, and with a comparable level of funding from NSF. We describe the development of a GPS network in the Tien Shan of Kyrgyzstan and Kazakhstan of the former Soviet Union, the analysis of data, and the main results. This discussion presents the state of the current network, which has grown significantly since the termination of our DOSE grants, with continued support both from NSF through its continental dynamics program and from NASA's SENH program. Although grants from NASA's DOSE program did not support this growth not directly, it did so indirectly by building the infrastructure that has enabled further expansion in an area where otherwise there would be only a small GPS presence. We note how the network has grown over time, but the emphasis of this discussion is on the quantity and quality of measurements that we have made.

  19. Rare Earth Element Measurements of Melilite and Fassaite in Allende Cai by Nanosims

    NASA Technical Reports Server (NTRS)

    Ito, M.; Messenger, Scott

    2009-01-01

    The rare earth elements (REEs) are concentrated in CAIs by approx. 20 times the chondritic average [e.g., 1]. The REEs in CAIs are important to understand processes of CAI formation including the role of volatilization, condensation, and fractional crystallization [1,2]. REE measurements are a well established application of ion microprobes [e.g., 3]. However the spatial resolution of REE measurements by ion microprobe (approx.20 m) is not adequate to resolve heterogeneous distributions of REEs among/within minerals. We have developed methods for measuring REE with the NanoSIMS 50L at smaller spatial scales. Here we present our initial measurements of REEs in melilite and fassaite in an Allende Type-A CAI with the JSC NanoSIMS 50L. We found that the key parameters for accurate REE abundance measurements differ between the NanoSIMS and conventional SIMS, in particular the oxide-to-element ratios, the relative sensitivity factors, the energy distributions, and requisite energy offset. Our REE abundance measurements of the 100 ppm REE diopside glass standards yielded good reproducibility and accuracy, 0.5-2.5 % and 5-25 %, respectively. We determined abundances and spatial distributions of REEs in core and rim within single crystals of fassaite, and adjacent melilite with 5-10 m spatial resolution. The REE abundances in fassaite core and rim are 20-100 times CI abundance but show a large negative Eu anomaly, exhibiting a well-defined Group III pattern. This is consistent with previous work [4]. On the other hand, adjacent melilite shows modified Group II pattern with no strong depletions of Eu and Yb, and no Tm positive anomaly. REE abundances (2-10 x CI) were lower than that of fassaite. These patterns suggest that fassaite crystallized first followed by a crystallization of melilite from the residual melt. In future work, we will carry out a correlated study of O and Mg isotopes and REEs of the CAI in order to better understand the nature and timescales of its

  20. Oxygen isotopes in the early protoplanetary disk inferred from pyroxene in a classical type B CAI

    NASA Astrophysics Data System (ADS)

    Aléon, Jérôme

    2016-04-01

    A major unanswered question in solar system formation is the origin of the oxygen isotopic dichotomy between the Sun and the planets. Individual Calcium-Aluminum-rich inclusions (CAIs) from CV chondrites exhibit almost the full isotopic range, but how their composition evolved is still unclear, which prevents robust astrochemical conclusions. A key issue is notably the yet unsolved origin of the 16O-rich isotopic composition of pyroxene in type B CAIs. Here, I report an in-situ oxygen isotope study of the archetypal type B CAI USNM-3529-Z from Allende with emphasis on the isotopic composition of pyroxene and its isotopic and petrographic relationships with other major minerals. The O isotopic composition of pyroxene is correlated with indicators of magmatic growth, indicating that the pyroxene evolved from a 16O-poor composition and became progressively enriched in 16O during its crystallization, contrary to the long held assumption that pyroxene was initially 16O-rich. This variation is well explained by isotopic exchange between a 16O-poor partial melt having the isotopic composition of melilite and a 16O-rich gas having the isotopic composition of spinel, during pyroxene crystallization. The isotopic evolution of 3529-Z is consistent with formation in an initially 16O-rich environment where spinel and gehlenitic melilite crystallized, followed by a 16O-depletion associated with melilite partial melting and recrystallization and finally a return to the initial 16O-rich environment before pyroxene crystallization. This strongly suggests that the environment of CAI formation was globally 16O-rich, with local 16O-depletions systematically associated with high temperature events. The Al/Mg isotopic systematics of 3529-Z further indicates that this suite of isotopic changes occurred in the first 150 000 yr of the solar system, during the main CAI formation period. A new astrophysical setting is proposed, where the 16O-depletion occurs in an optically thin surface

  1. Source processes of strong earthquakes in the North Tien-Shan region

    NASA Astrophysics Data System (ADS)

    Kulikova, G.; Krueger, F.

    2013-12-01

    Tien-Shan region attracts attention of scientists worldwide due to its complexity and tectonic uniqueness. A series of very strong destructive earthquakes occurred in Tien-Shan at the turn of XIX and XX centuries. Such large intraplate earthquakes are rare in seismology, which increases the interest in the Tien-Shan region. The presented study focuses on the source processes of large earthquakes in Tien-Shan. The amount of seismic data is limited for those early times. In 1889, when a major earthquake has occurred in Tien-Shan, seismic instruments were installed in very few locations in the world and these analog records did not survive till nowadays. Although around a hundred seismic stations were operating at the beginning of XIX century worldwide, it is not always possible to get high quality analog seismograms. Digitizing seismograms is a very important step in the work with analog seismic records. While working with historical seismic records one has to take into account all the aspects and uncertainties of manual digitizing and the lack of accurate timing and instrument characteristics. In this study, we develop an easy-to-handle and fast digitization program on the basis of already existing software which allows to speed up digitizing process and to account for all the recoding system uncertainties. Owing to the lack of absolute timing for the historical earthquakes (due to the absence of a universal clock at that time), we used time differences between P and S phases to relocate the earthquakes in North Tien-Shan and the body-wave amplitudes to estimate their magnitudes. Combining our results with geological data, five earthquakes in North Tien-Shan were precisely relocated. The digitizing of records can introduce steps into the seismograms which makes restitution (removal of instrument response) undesirable. To avoid the restitution, we simulated historic seismograph recordings with given values for damping and free period of the respective instrument and

  2. Tectonic evolution of Kazakhstan and Tien Shan in Neoproterozoic and Early-Middle Paleozoic

    NASA Astrophysics Data System (ADS)

    Samygin, S. G.; Kheraskova, T. N.; Kurchavov, A. M.

    2015-05-01

    Geological information on Kazakhstan and the Tien Shan obtained up to the present time has been considered and integrated in order to demonstrate the main features of continental massifs, basins with oceanic crust, island arcs, marginal volcanic-plutonic belts, and transform fault zones differing in type and age. We ascertained the character and probable causes of their evolution and transformations resulting in the origination and development of mosaic structural assembly at margin of the Paleoasian ocean that existed from Neoproterozoic. The main stages of the geodynamic history of Paleozoides in Kazakhstan and Tien Shan are characterized, and a model of the probable course of regional tectonic events has been proposed. This model is illustrated by published paleomagnetic data and a series of paleotectonic reconstructions for time intervals 950-900, 850-800, 750-700, 650-630, 570-550, 530-515, 500-470, 460-440, and 390-380 Ma.

  3. Tomographic Imaging of the Crust and Upper Mantle Beneath the Western Tien Shan

    NASA Astrophysics Data System (ADS)

    Li, Z.; Roecker, S.

    2007-12-01

    We combine P and S wave arrival times from the recent MANAS deployment of broad band sensors with the prior GENGHIS deployment and analogue observations from the Kyrgyz Institute of Seismology to generate a high resolution (5-20 km) image of elastic wavespeeds in the crust and upper mantle beneath the western Tien Shan. The total data set consists of 29,006 P and 21,491 S arrivals from 2176 local events along with 27,196 P arrivals from 2631 teleseismic events recorded at 144 stations. Near surface structure is constrained by a combination of arrival times from local and regional events, Moho depths determined from receiver functions, and travel times from the 2007 MANAS active source profile. Our principal finding is a large high wavespeed region in the mantle beneath most of western Tien Shan dipping to the north to depths as great as 600 km. This region appears to be continuous to shallow depths and surfaces at the southern range front near where the Tarim Basin is being overthrust by the Kokshal range. This result suggests that the Tarim Basin continues to actively subduct beneath the Tien Shan. We do not see any similar feature associated with underthrusting of the Kazach shield to the south. We also inverted a subset of regionally located events for Pn wavespeed and anisotropy. Similar to the larger scale results, Pn wavespeeds in the uppermost mantle are 3-4 percent lower than normal under most of the Tien Shan. The fast direction of Pn anisotropy is predominantly north-south in agreement with the sparser sampling of previous SKS studies. Taken with the tomographic image, we suggest that the anisotropy is most likely due to flow in the asthenosphere induced by the subduction of the Tarim basin.

  4. Tectonic interaction between the Pamir and Tien Shan observed by GPS

    NASA Astrophysics Data System (ADS)

    Zubovich, A.; Schöne, T.; Metzger, S.; Mosienko, O.; Mukhamediev, Sh.; Sharshebaev, A.; Zech, C.

    2016-02-01

    The complex tectonic interplay between the Central Asian Southwest Tien Shan and the north advancing Pamir as well as the role of the Pamir Frontal Thrust (PFT) separating these two orogens along the intervening Alai Valley is yet unclear. In this paper we present data of the newly installed Western Alai GPS profile (WAGP), capturing the deformation signal of both mountain ranges. The 20 km long WAGP records a maximum displacement rate of 9.3 ± 0.8 mm yr-1. The lion's share of displacement (6.0 ± 0.8 mm yr-1) is accommodated between the two stations located directly north and south of the PFT in 5 km distance. The WAGP data nicely complement the existing South Tien Shan and the Pamir GPS network data, which we present here in a combined reference frame and use it as input for horizontal block rotation/strain models. The model results show that both the Southwest Tien Shan and the Pamir behave as uniformly strained blocks and rotate counterclockwise (with respect to Eurasia) by 0.93 ± 0.11° Myr-1 and 0.62 ± 0.05° Myr-1, respectively. The Southwest Tien Shan undergoes NNE-SSW shortening of -22.1 ± 1.5 × 10-9 year-1 with an insignificant perpendicular extension. The Pamir is shortening with a rate of -10.2 ± 3.8 × 10-9 year-1 in a NNE-SSW direction, which is nearly 2.5 times less than its lateral extension rate. A band of increased deformation along the PFT is bounded to the north by the northern rim of the Alai Valley and extends up to 30-50 km south into the Pamir.

  5. Calcium-aluminum-rich inclusions with fractionation and unknown nuclear effects (FUN CAIs): I. Mineralogy, petrology, and oxygen isotopic compositions

    NASA Astrophysics Data System (ADS)

    Krot, Alexander N.; Nagashima, Kazuhide; Wasserburg, Gerald J.; Huss, Gary R.; Papanastassiou, Dimitri; Davis, Andrew M.; Hutcheon, Ian D.; Bizzarro, Martin

    2014-11-01

    We present a detailed characterization of the mineralogy, petrology, and oxygen isotopic compositions of twelve FUN CAIs, including C1 and EK1-4-1 from Allende (CV), that were previously shown to have large isotopic fractionation patterns for magnesium and oxygen, and large isotopic anomalies of several elements. The other samples show more modest patterns of isotopic fractionation and have smaller but significant isotopic anomalies. All FUN CAIs studied are coarse-grained igneous inclusions: Type B, forsterite-bearing Type B, compact Type A, and hibonite-rich. Some inclusions consist of two mineralogically distinct lithologies, forsterite-rich and forsterite-free/poor. All the CV FUN CAIs experienced postcrystallization open-system iron-alkali-halogen metasomatic alteration resulting in the formation of secondary minerals commonly observed in non-FUN CAIs from CV chondrites. The CR FUN CAI GG#3 shows no evidence for alteration. In all samples, clear evidence of oxygen isotopic fractionation was found. Most samples were initially 16O-rich. On a three-oxygen isotope diagram, various minerals in each FUN CAI (spinel, forsterite, hibonite, dmisteinbergite, most fassaite grains, and melilite (only in GG#3)), define mass-dependent fractionation lines with a similar slope of ∼0.5. The different inclusions have different Δ17O values ranging from ∼-25‰ to ∼-16‰. Melilite and plagioclase in the CV FUN CAIs have 16O-poor compositions (Δ17O ∼-3‰) and plot near the intercept of the Allende CAI line and the terrestrial fractionation line. We infer that mass-dependent fractionation effects of oxygen isotopes in FUN CAI minerals are due to evaporation during melt crystallization. Differences in Δ17O values of mass-dependent fractionation lines defined by minerals in individual FUN CAIs are inferred to reflect differences in Δ17O values of their precursors. Differences in δ18O values of minerals defining the mass-dependent fractionation lines in several FUN CAIs

  6. OXYGEN ISOTOPIC COMPOSITIONS OF THE ALLENDE TYPE C CAIs: EVIDENCE FOR ISOTOPIC EXCHANGE DURING NEBULAR MELTING AND ASTEROIDAL THERMAL METAMORPHISM

    SciTech Connect

    Krot, A N; Chaussidon, M; Yurimoto, H; Sakamoto, N; Nagashima, K; Hutcheon, I D; MacPherson, G J

    2008-02-21

    Based on the mineralogy and petrography, coarse-grained, igneous, anorthite-rich (Type C) calcium-aluminum-rich inclusions (CAIs) in the CV3 carbonaceous chondrite Allende have been recently divided into three groups: (i) CAIs with melilite and Al,Ti-diopside of massive and lacy textures (coarse grains with numerous rounded inclusions of anorthite) in a fine-grained anorthite groundmass (6-1-72, 100, 160), (ii) CAI CG5 with massive melilite, Al,Ti-diopside and anorthite, and (iii) CAIs associated with chondrule material: either containing chondrule fragments in their peripheries (ABC, TS26) or surrounded by chondrule-like, igneous rims (93) (Krot et al., 2007a,b). Here, we report in situ oxygen isotopic measurements of primary (melilite, spinel, Al,Ti-diopside, anorthite) and secondary (grossular, monticellite, forsterite) minerals in these CAIs. Spinel ({Delta}{sup 17}O = -25{per_thousand} to -20{per_thousand}), massive and lacy Al,Ti-diopside ({Delta}{sup 17}O = -20{per_thousand} to -5{per_thousand}) and fine-grained anorthite ({Delta}{sup 17}O = -15{per_thousand} to -2{per_thousand}) in 100, 160 and 6-1-72 are {sup 16}O-enriched relative spinel and coarse-grained Al,Ti-diopside and anorthite in ABC, 93 and TS26 ({Delta}{sup 17}O ranges from -20{per_thousand} to -15{per_thousand}, from -15{per_thousand} to -5{per_thousand}, and from -5{per_thousand} to 0{per_thousand}, respectively). In 6-1-72, massive and lacy Al,Ti-diopside grains are {sup 16}O-depleted ({Delta}{sup 17}O {approx} -13{per_thousand}) relative to spinel ({Delta}{sup 17}O = -23{per_thousand}). Melilite is the most {sup 16}O-depleted mineral in all Allende Type C CAIs. In CAI 100, melilite and secondary grossular, monticellite and forsterite (minerals replacing melilite) are similarly {sup 16}O-depleted, whereas grossular in CAI 160 is {sup 16}O-enriched ({Delta}{sup 17}O = -10{per_thousand} to -6{per_thousand}) relative to melilite ({Delta}{sup 17}O = -5{per_thousand} to -3{per_thousand}). We infer

  7. Comparison of Gosat CAI and SPOT Vgt Ndvi Data with Different Season and Land Cover in East Asia

    NASA Astrophysics Data System (ADS)

    Liu, Y.; Wang, X.; Guo, M.; Tani, H.

    2011-08-01

    The Normalized Difference Vegetation Index (NDVI) has become one of the most widely used indices in remote sensing applications in a variety of fields. Many studies have compared the NDVI values for different satellite sensors. Nowadays, the Greenhouse Gases Observing Satellite (GOSAT) was successfully launched on January 23, 2009. It is used to monitor greenhouse gases on the Earth's surface and also has a sensor, the Cloud Aerosol Imager (CAI), that senses red and near infrared spectrums. It can also process NDVI data. Therefore, we are first compare GOSAT CAI and SPOT VGT NDVI data in different seasonal and land cover in East Asian, to explore the relationship between the two types of datasets, and to discuss the possibility of extending SPOT VGT data using GOSAT CAI NDVI data for the same area. We used GOSAT CAI Level 3 data to derive 10-day composite NDVI values for the East Asia region for November 2009 and January, April and July 2010 using the maximum value composite (MVC) method. We compared these values with 10-day composite SPOT VGT NDVI data for the same period. The results show that the correlation coefficients of regression analysis generally revealed a strong correlation between NDVI from the two sensors in November 2009 and January, April and July 2010 (0.88, 0.85, 0.77 and 0.74, respectively). The differences place may be affected by cloud cover. From the combined analysis of seasonal changes and land cover, we found that the correlations between the SPOT VGT and the GOSAT CAI NDVI data are less affected by seasonal change and the SPOT VGT data is more sensitive to high vegetation coverage than the GOSAT CAI data. In the future, through continued monitoring and processing by cloud removal technology, the accuracy of GOSAT CAI NDVI data will be further improved and thus be more widely used.

  8. Temporal and Spatial Heterogeneities in the Solar Nebula Reflected in Rb-Sr and Sm-Nd Systematics of Al3S4, an Allende Type B CAI

    NASA Astrophysics Data System (ADS)

    Marks, N. E.; Borg, L. E.; Hutcheon, I. D.; Jacobsen, B.; Clayton, R. N.; Mayeda, T. K.

    2012-03-01

    We have measured the Rb-Sr, ^1^7^4Sm-^1^4^3Nd and ^1^4^7Sm-^1^4^2Nd isotope compositions of a type B CAI. These data indicate that CAIs and Earth have the same ^1^4^2Nd/^1^4^4Nd composition and that carbonaceous chondrites are distinct from both Earth and CAIs.

  9. The isotopic homogeneity in the early solar system: Revisiting the CAI oxygen isotopic anomaly

    NASA Astrophysics Data System (ADS)

    Ozima, M.; Yamada, A.

    2009-12-01

    Since the first discovery of the mass-independently fractionated oxygen isotopes in anhydrous, high temperature Ca-Al rich inclusion minerals in carbonaceous meteorites (CAIs) by Clayton et al. (1), their common occurrence in primitive meteorites has generally been regarded to reflect some fundamental process prevalent in the early solar nebula. The CAI oxygen isotopic composition is uniquely characterized by (i) large mass independent isotopic fractionation and (ii) their isotopic data in an oxygen three isotope plot (δ17O - δ18O (δ17O ≡ {(17O/16O)/(17O/16O)SMOW - 1} × 1000) yield nearly a straight line with a slope 1.0. In establishing these characteristics, ion microprobe analyses has played a central role, especially an isotopic mapping technique (isotopography) was crucial (e.g., 2). The extraordinary oxygen isotopic ratio in CAIs is widely attributed to the self-shielding absorption of UV radiation in CO, one of the dominant chemical compounds in the early solar nebula (3). However, the self-shielding scenario necessarily leads to the unusual prediction that a mean solar oxygen isotopic composition differs from most of planetary bodies including Earth, Moon, and Mars. If the self-shielding process were indeed responsible to the CAI oxygen isotopic anomaly, this would require a fundamental revision of the current theory of the origin of the solar system, which generally assumes the initial total vaporization of nebula material to give rise to isotopic homogenization. The GENESIS mission launched in 2001(4), which collected oxygen in the solar wind was hoped to resolve the isotopic composition of the Sun. However, because of difficulties in correcting for instrumental and more importantly for intrinsic isotopic fractionation between the SW and the Sun, a final answer is yet to be seen (5). Here, we show on the basis of the oxygen isotopic fractionation systematics that the self shielding hypothesis cannot explain the key characteristics of the CAI oxygen

  10. Characterization of Meteorites by Focused Ion Beam Sectioning: Recent Applications to CAIs and Primitive Meteorite Matrices

    NASA Technical Reports Server (NTRS)

    Christoffersen, Roy; Keller, Lindsay P.; Han, Jangmi; Rahman, Zia; Berger, Eve L.

    2015-01-01

    Focused ion beam (FIB) sectioning has revolutionized preparation of meteorite samples for characterization by analytical transmission electron microscopy (TEM) and other techniques. Although FIB is not "non-destructive" in the purest sense, each extracted section amounts to no more than nanograms (approximately 500 cubic microns) removed intact from locations precisely controlled by SEM imaging and analysis. Physical alteration of surrounding material by ion damage, fracture or sputter contamination effects is localized to within a few micrometers around the lift-out point. This leaves adjacent material intact for coordinate geochemical analysis by SIMS, microdrill extraction/TIMS and other techniques. After lift out, FIB sections can be quantitatively analyzed by electron microprobe prior to final thinning, synchrotron x-ray techniques, and by the full range of state-of-the-art analytical field-emission scanning transmission electron microscope (FE-STEM) techniques once thinning is complete. Multiple meteorite studies supported by FIB/FE-STEM are currently underway at NASA-JSC, including coordinated analysis of refractory phase assemblages in CAIs and fine-grained matrices in carbonaceous chondrites. FIB sectioning of CAIs has uncovered epitaxial and other overgrowth relations between corundum-hibonite-spinel consistent with hibonite preceding corundum and/or spinel in non-equilibrium condensation sequences at combinations of higher gas pressures, dust-gas enrichments or significant nebular transport. For all of these cases, the ability of FIB to allow for coordination with spatially-associated isotopic data by SIMS provides immense value for constraining the formation scenarios of the particular CAI assemblage. For carbonaceous chondrites matrix material, FIB has allowed us to obtain intact continuous sections of the immediate outer surface of Murchison (CM2) after it has been experimentally ion processed to simulate solar wind space weathering. The surface

  11. An oxygen isotope study of Wark-Lovering rims on type A CAIs in primitive carbonaceous chondrites

    NASA Astrophysics Data System (ADS)

    Bodénan, Jean-David; Starkey, Natalie A.; Russell, Sara S.; Wright, Ian P.; Franchi, Ian A.

    2014-09-01

    Calcium-aluminium-rich Inclusions (CAIs) and the thin Wark-Lovering (WL) rims of minerals surrounding them offer a record of the nature of changing conditions during the earliest stages of Solar System formation. Considerable heterogeneity in the gas composition in the immediate vicinity of the proto-Sun had previously been inferred from oxygen isotopic variations in the WL rim of a CAI from Allende (Simon et al., 2011). However, high precision and high spatial resolution oxygen isotope measurements presented in this study show that WL rim and pristine core minerals of individual CAIs from meteorites that had experienced only low degrees of alteration or low grade metamorphism (one from Léoville (reduced CV3), two in QUE 99177 (CR3.0) and two in ALHA 77307 (CO3.0)) are uniformly 16O-rich. This indicates that the previously observed variations are the result of secondary processes, most likely on the asteroid parent body, and that there were no temporal or spatial variations in oxygen isotopic composition during CAI and WL rim formation. Such homogeneity across three groups of carbonaceous chondrites lends further support for a common origin for the CAIs in all chondrites. 16O-poor oxygen reservoirs such as those associated with chondrule formation, were probably generated by UV photo-dissociation involving self-shielding mechanisms and must have occurred elsewhere in outer regions of the solar accretion disk.

  12. Constraints on the Origin of Chondrules and CAIs from Short-Lived and Long-Lived Radionuclides

    SciTech Connect

    Kita, N T; Huss, G R; Tachibana, S; Amelin, Y; Nyquist, L E; Hutcheon, I D

    2005-10-24

    The high time resolution Pb-Pb ages and short-lived nuclide based relative ages for CAIs and chondrules are reviewed. The solar system started at 4567.2 {+-} 0.6Ma inferred from the high precision Pb-Pb ages of CAIs. Time scales of CAIs ({le}0.1Myr), chondrules (1-3Myr), and early asteroidal differentiation ({ge}3Myr) inferred from {sup 26}Al relative ages are comparable to the time scale estimated from astronomical observations of young star; proto star, classical T Tauri star and week-lined T Tauri star, respectively. Pb-Pb ages of chondrules also indicate chondrule formation occur within 1-3 Myr after CAIs. Mn-Cr isochron ages of chondrules are similar to or within 2 Myr after CAI formation. Chondrules from different classes of chondrites show the same range of {sup 26}Al ages in spite of their different oxygen isotopes, indicating that chondrule formed in the localized environment. The {sup 26}Al ages of chondrules in each chondrite class show a hint of correlation with their chemical compositions, which implies the process of elemental fractionation during chondrule formation events.

  13. FIB-NanoSIMS-TEM Coordinated Study of a Wark-Lovering Rim in a Vigarano Type A CAI

    NASA Technical Reports Server (NTRS)

    Cai, A.; Ito, M.; Keller, L. P.; Ross, D. K.; Nakamura-Messenger, K.

    2010-01-01

    Wark-Lovering (WL) rims are thin multi layered mineral sequences that surround most Ca, Al-rich inclusions (CAIs). Unaltered WL rims are composed of the same primary high temperature minerals as CAIs, such as melilite, spinel, pyroxene, hibonite, perovskite, anorthite and olivine. It is still unclear whether the rim minerals represent a different generation formed by a separate event from their associated CAIs or are a byproduct of CAI formation. Several models have been proposed for the origins of WL rims including condensation, flashheating, reaction of a CAI with a Mg-Si-rich reservoir (nebular gas or solid); on the basis of mineralogy, abundances of trace elements, O and Mg isotopic studies. Detailed mineralogical characterizations of WL rims at micrometer to nanometer scales have been obtained by TEM observations, but so far no coordinated isotopic - mineralogical studies have been performed. Thus, we have applied an O isotopic imaging technique by NanoSIMS 50L to investigate heterogeneous distributions of O isotopic ratios in minerals within a cross section of a WL rim prepared using a focused ion beam (FIB) instrument. After the isotopic measurements, we determine the detailed mineralogy and microstructure of the same WL FIB section to gain insight into its petrogenesis. Here we present preliminary results from O isotopic and elemental maps by NanoSIMS and mineralogical analysis by FE-SEM of a FIB section of a WL rim in the Vigarano reduced CV3 chondrite.

  14. Opaque minerals in CAIs, and classification of the Axtell (CV3) chondrite

    NASA Astrophysics Data System (ADS)

    Casanova, I.; Simon, S. B.

    1994-07-01

    Axtell is a new CV3 chondrite from Texas. Preliminary studies of its Ca-Al rich Inclusions (CAIs) were reported. The mineralogy and chemical compositions of opaque minerals in four Axtell CAIs are distinct from their analogs in other inclusions from CV3 chondrites. Metallic NiFe (awaruite) is the dominant phase in opaque assemblages from Axtell inclusions, and occurs as well-rounded particles of sizes between about 1 and 20 microns. Their compositions (in atom %) are N63-67Fe31-33Co2-3 in AX-4, AX-7, and AX-9, and Ni74Fe23Co2 in AX-5. None of the awaruite grains contains measurable amounts (greater than 200 ppm by weight) of the platinum-group elements analyzed for Ru, W, Mo, Re, Os, Ir, and Pt. With very few exceptions, the awaruite particles studied are surrounded by or intergrown with V-free magnetite (detection limit = 400 ppm). In contrast with Allende, the dominant sulfide phase in Axtell inclusions is troilite (Ni less than or = 0.02-0.3%, by weight); pentlandite is scarce, occurring only sporadically as small grains associated with metallic FeNi (just a few particles of 5-15 microns were found in AX-5, AX-4, and AX-7, and none in AX-9). Also, an isolated 10-microns grain of millerite (NiS; Fe = 0.6 wt%) has been identified in AX-5. Unlike Allende inclusions, Axtell CAIs do not contain sulfide veins. Two remarkably large PGE-rich sulfide grains have been recognized: one spherical 12-microns particle in AX-4 (AX-4A, in melilite, close to the edge of the inclusion) and another irregularly shaped 25-microns grain in AX-9 (AX-9A, in melilite inside a spinel palisade). Study of the elemental distribution by wavelength-dispersive X-ray mapping and analysis and backscattered electron imaging suggests that these are single minerals and not multiphase assemblages. Microprobe analyses of chondrule olivines and low-Ca pyroxenes yield average Fa and Fs contents of 6.7 and 1.0 mol% respectively. These compositions suggest that Axtell is more similar to the CV3 chondrites

  15. Problem Solving Process Research of Everyone Involved in Innovation Based on CAI Technology

    NASA Astrophysics Data System (ADS)

    Chen, Tao; Shao, Yunfei; Tang, Xiaowo

    It is very important that non-technical department personnel especially bottom line employee serve as innovators under the requirements of everyone involved in innovation. According the view of this paper, it is feasible and necessary to build everyone involved in innovation problem solving process under Total Innovation Management (TIM) based on the Theory of Inventive Problem Solving (TRIZ). The tools under the CAI technology: How TO mode and science effects database could be very useful for all employee especially non-technical department and bottom line for innovation. The problem solving process put forward in the paper focus on non-technical department personnel especially bottom line employee for innovation.

  16. New Evidence for 26Al in CAI and Chondrules from Type 3 Ordinary Chondrites

    NASA Astrophysics Data System (ADS)

    Srinivasan, G.; Russell, S. S.; MacPherson, G. J.; Huss, G. R.; Wasserburg, G. J.

    1996-03-01

    We have known since 1976 that 26A1 (tl/2 = 7.2 x 105 yrs) was alive in the early solar system, at a level of (26Al/27Al)o z 5 x 10-5 in calcium-aluminum inclusions (CAI). However, several outstanding questions remain. Little evidence for 26A1 has been found in other chondritic material, and none has been found in differentiated meteorites. These results might imply that 26A1 was heterogeneously distributed in the nebula or by mineralogic site in nebular dust, or they might reflect differences in time of formation. There are strict limitations on finding evidence of 26A1 in normal chondrules with bulk Al/Mg ~ 0.1, since even quenched, perfectly preserved, late-stage glasses would have low Al/Mg. Primary plagioclase crystals provide the only possibility, but these only crystallize rarely in melts within the compositional range of normal chondrules. Also, metamorphism can erase the evidence in high-AI/Mg phases. To address these issues, we have conducted a search for chondrules and CAI with high-Al/Mg phases suitable for ion-probe measurement in type 3 ordinary chondrites. Previous work has revealed evidence for 26Al in a plagioclase bearing, olivine-pyroxene class from Semarkona (LL3.0; (26Al/27Al)o = 7.7+/-2.1 x 10-6)), a plagioclase-rich object from Bovedy (L3.7?; 2.5+/-1.2 x 10-7), in separated plagioclase from St. Marguerite (H4; 2.0+/-0.6 x 10-7), an isolated hibonite grain from Dhajala (H3.8; 8.4+0.5 x 10-6), and in Al2O3 and hibonite grains ((26Al/27Al)o = 2-5 x 10-5; [GRH, unpublished]) from acid residues of Semarkona, Bishunpur (LL3.1), and Krymka (LL3.1). We have identified and measured Al-Mg isotope systematics in two CAI and seven chondrules from ordinary chondrites of low metamorphic grade and have found clear evidence for 26A1 in both CAI and in two chondrules.

  17. Intelligent CAI.

    DTIC Science & Technology

    1975-10-01

    of industria !, technological, and sociological interest- invaluable information for executives and professionals who must keep up to date. The...BEVERAGE 1A HOT CHOCOLATE MB TEA IBI WITH LEMON HB2 WITH SUGAR AND CREAM 1C COFFEE 11 SUBSTITUTE WOR’ JN &TATCIKMT Before we end this

  18. Ca-Fe and Alkali-Halide Alteration of an Allende Type B CAI: Aqueous Alteration in Nebular or Asteroidal Settings

    NASA Technical Reports Server (NTRS)

    Ross, D. K.; Simon, J. I.; Simon, S. B.; Grossman, L.

    2012-01-01

    Ca-Fe and alkali-halide alteration of CAIs is often attributed to aqueous alteration by fluids circulating on asteroidal parent bodies after the various chondritic components have been assembled, although debate continues about the roles of asteroidal vs. nebular modification processes [1-7]. Here we report de-tailed observations of alteration products in a large Type B2 CAI, TS4 from Allende, one of the oxidized subgroup of CV3s, and propose a speculative model for aqueous alteration of CAIs in a nebular setting. Ca-Fe alteration in this CAI consists predominantly of end-member hedenbergite, end-member andradite, and compositionally variable, magnesian high-Ca pyroxene. These phases are strongly concentrated in an unusual "nodule" enclosed within the interior of the CAI (Fig. 1). The Ca, Fe-rich nodule superficially resembles a clast that pre-dated and was engulfed by the CAI, but closer inspection shows that relic spinel grains are enclosed in the nodule, and corroded CAI primary phases interfinger with the Fe-rich phases at the nodule s margins. This CAI also contains abundant sodalite and nepheline (alkali-halide) alteration that occurs around the rims of the CAI, but also penetrates more deeply into the CAI. The two types of alteration (Ca-Fe and alkali-halide) are adjacent, and very fine-grained Fe-rich phases are associated with sodalite-rich regions. Both types of alteration appear to be replacive; if that is true, it would require substantial introduction of Fe, and transport of elements (Ti, Al and Mg) out of the nodule, and introduction of Na and Cl into alkali-halide rich zones. Parts of the CAI have been extensively metasomatized.

  19. Extending the granularity of representation and control for the MIL-STD CAIS 1.0 node model

    NASA Technical Reports Server (NTRS)

    Rogers, Kathy L.

    1986-01-01

    The Common APSE (Ada 1 Program Support Environment) Interface Set (CAIS) (DoD85) node model provides an excellent baseline for interfaces in a single-host development environment. To encompass the entire spectrum of computing, however, the CAIS model should be extended in four areas. It should provide the interface between the engineering workstation and the host system throughout the entire lifecycle of the system. It should provide a basis for communication and integration functions needed by distributed host environments. It should provide common interfaces for communications mechanisms to and among target processors. It should provide facilities for integration, validation, and verification of test beds extending to distributed systems on geographically separate processors with heterogeneous instruction set architectures (ISAS). Additions to the PROCESS NODE model to extend the CAIS into these four areas are proposed.

  20. In Situ Trace Element Analysis of an Allende Type B1 CAI: EK-459-5-1

    NASA Technical Reports Server (NTRS)

    Jeffcoat, C. R.; Kerekgyarto, A.; Lapen, T. J.; Andreasen, R.; Righter, M.; Ross, D. K.

    2014-01-01

    Variations in refractory major and trace element composition of calcium, aluminum-rich inclusions (CAIs) provide constraints on physical and chemical conditions and processes in the earliest stages of the Solar System. Previous work indicates that CAIs have experienced complex histories involving, in many cases, multiple episodes of condensation, evaporation, and partial melting. We have analyzed major and trace element abundances in two core to rim transects of the melilite mantle as well as interior major phases of a Type B1 CAI (EK-459-5-1) from Allende by electron probe micro-analyzer (EPMA) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) to investigate the behavior of key trace elements with a primary focus on the REEs Tm and Yb.

  1. Timing and process of river and lake terrace formation in the Kyrgyz Tien Shan

    NASA Astrophysics Data System (ADS)

    Burgette, Reed J.; Weldon, Ray J.; Abdrakhmatov, Kanatbek Ye.; Ormukov, Cholponbek; Owen, Lewis A.; Thompson, Stephen C.

    2017-03-01

    Well-preserved flights of river and lake terraces traverse an actively deforming rangefront, and form a link between glaciated mountains and a large intermontane lake in the Issyk-Kul basin of the Kyrgyz Tien Shan. We investigated the history and geometry of these lake and river terraces using geologic mapping, surveying, and radiocarbon and terrestrial cosmogenic nuclide dating. A prominent late Pleistocene highstand of the lake occurred over at least the period of 43-25 ka, followed by a period of deep regression and subsequent rise of the lake to the modern sill level in the late Holocene. Major aggradation of the most prominent latest Quaternary river terrace along the Ak-Terek and Barskaun rivers likely started at ∼70-60 ka, coincident to the local last glacial maximum in this region. In contrast to some models of aggradation and incision, the rivers appear to have stayed near the top of the fill for >20 ka, incising subtly below the top of this fill by ∼37 ka, locally. Deep incision likely did not occur until the peak deglaciation in the latest Pleistocene. Older dated terrace surfaces are consistent with one major terrace-forming event per glacial, constant deformation and incision rates, and typical fluvial gradients lower than the modern incising streams. The dating confirms regional terrace correlations for the most prominent late Quaternary terraces, but correlating higher terraces is complicated by spatially varying uplift rates and preferential terrace preservation between basins in the Tien Shan.

  2. Basin evolution in a folding lithosphere: Altai-Sayan and Tien Shan belts in Central Asia

    NASA Astrophysics Data System (ADS)

    Delvaux, D.; Cloetingh, S.; Beekman, F.; Sokoutis, D.; Burov, E.; Buslov, M. M.; Abdrakhmatov, K. E.

    2013-08-01

    Central Asia is a classical example for continental lithospheric folding. In particular, the Altay-Sayan belt in South-Siberia and the Kyrgyz Tien Shan display a special mode of lithospheric deformation, involving decoupled lithospheric mantle folding and upper crustal folding and faulting. Both areas have a heterogenous crust with a long history of accretion-collision, subsequently reactivated as a far-field effect of the Indian-Eurasian collision. Thanks to the youthfulness of the tectonic deformation in this region (peak deformation in late Pliocene-early Pleistocene), the surface expression of lithospheric deformation is well documented by the surface topography and superficial tectonic structures. A review of the paleostress data and tectono-stratigraphic evolution of the Kurai-Chuya basin in Siberian Altai, Zaisan basin in Kazakh South Altai and Issyk-Kul basin in Kyrgyz Tien Shan suggests that they were initiated in an extensional context and inverted by a combination of fault-controlled deformation and flexural folding. In these basins, fault-controlled deformation alone appears largely insufficient to explain their architecture. Lithospheric buckling inducing surface tilting, uplift and subsidence also played an important role. They form typical basins in a folding lithosphere (FLB). Their characteristic basin fill and symmetry, inner structure, folding wavelength and amplitude, thermal regime, time frame are examined in relation to basement structure, stress field, strain rate, timing of deformation, and compared to existing modelling results.

  3. Full Waveform 2.5D Teleseismic Surface Wave Tomography with Application to the Tien Shan

    NASA Astrophysics Data System (ADS)

    Roecker, S. W.; Priestley, K. F.; Baker, B. I.

    2011-12-01

    We adapt the 2.5D spectral domain finite difference waveform tomography algorithm of Roecker et al. (2010) to permit the analysis of teleseismically recorded surface waves. The teleseismic body wave technique of generating synthetic waveforms by specifying an analytic solution for a background wavefield in a 1D model and solving for a scattered field excited by this background is equally applicable to surface waves. We use the locked mode approach of Gomberg and Masters (1988) to calculate the background Greens functions at each point of the finite difference (FD) grid. Because of the much greater concentration of energy at the surface, we adopt the cell-based FD operators of Min et al. (2004) to calculate the free surface boundary conditions, and the generalized stretching function of Komatitch and Martin (2007) to improve the absorption in the PML. We use this algorithm to analyze broad band seismograms of events in Sumatra recorded by the MANAS array in the Tien Shan. Our results show that the upper mantle beneath much of the central Tien Shan has shear wavespeeds at least 10% lower than the lithosphere beneath the Tarim basin to the south or the Kazach shield to the north. At the same time, there appears to be a remnant lithospheric lid beneath the Kyrgyz range in the north, an observation consistent with previous receiver function studies in this area.

  4. Thermal maturity patterns in New York State using CAI and %Ro

    USGS Publications Warehouse

    Weary, D.J.; Ryder, R.T.; Nyahay, R.E.

    2001-01-01

    New conodont alteration index (CAI) and vitrinite reflectance (%Ro) data collected from drill holes in the Appalachian basin of New York State allow refinement of thermal maturity maps for Ordovician and Devonian rocks. CAI isotherms on the new maps show a pattern that approximates that published by Harris et al. (1978) in eastern and western New York, but it differs in central New York, where the isotherms are shifted markedly westward by more than 100 km and are more tightly grouped. This close grouping of isograds reflects a steeper thermal gradient than previously noted by Harris et al. (1978) and agrees closely with the abrupt west-to-east increase in thermal maturity across New York noted by Johnsson (1986). These data show, in concordance with previous studies, that thermal maturity levels in these rocks are higher than can be explained by simple burial heating beneath the present thickness of overburden. The Ordovician and Devonian rocks of the Appalachian Basin in New York must have been buried by very thick post-Devonian sediments (4-6 km suggested by Sarwar and Friedman 1995) or were exposed to a higher-than-normal geothermal flux caused by crustal extension, or a combination of the two.

  5. An experimental study of fuel injection strategies in CAI gasoline engine

    SciTech Connect

    Hunicz, J.; Kordos, P.

    2011-01-15

    Combustion of gasoline in a direct injection controlled auto-ignition (CAI) single-cylinder research engine was studied. CAI operation was achieved with the use of the negative valve overlap (NVO) technique and internal exhaust gas re-circulation (EGR). Experiments were performed at single injection and split injection, where some amount of fuel was injected close to top dead centre (TDC) during NVO interval, and the second injection was applied with variable timing. Additionally, combustion at variable fuel-rail pressure was examined. Investigation showed that at fuel injection into recompressed exhaust fuel reforming took place. This process was identified via an analysis of the exhaust-fuel mixture composition after NVO interval. It was found that at single fuel injection in NVO phase, its advance determined the heat release rate and auto-ignition timing, and had a strong influence on NO{sub X} emission. However, a delay of single injection to intake stroke resulted in deterioration of cycle-to-cycle variability. Application of split injection showed benefits of this strategy versus single injection. Examinations of different fuel mass split ratios and variable second injection timing resulted in further optimisation of mixture formation. At equal share of the fuel mass injected in the first injection during NVO and in the second injection at the beginning of compression, the lowest emission level and cyclic variability improvement were observed. (author)

  6. Characterizing Pyroxene Reaction Space in Calcium-Aluminum Rich Inclusions: Oxidation During CAI Rim Formation

    NASA Astrophysics Data System (ADS)

    Dyl, K. A.; Young, E. D.

    2009-12-01

    We define the reaction space that controls changes in pyroxene composition in CAIs and Wark-Lovering (WL) rims in an oxidizing solar nebula. Ti-rich pyroxenes in CAIs record a sub-solar oxygen fugacity (Ti3+/Ti4+~1.5). WL rim pyroxenes in the CAI Leoville 144A have a distinctly lower oxidation state.This difference supports WL rim condensation in an environment of increasing O2(g) and Mg(g) (Simon et al. 2005). We used the following phase components to identify four linearly independent reactions (Thompson 1982): diopside, CaTs (Al2Mg-1Si-1), T3 (Ti3+AlMg-1Si-1), T4 (Ti4+Al2Mg-1Si-2), En (MgCa-1), perovskite, O(g), Mg(g), SiO(g), and Ca(g). Compositional variation in this system is dominated by two reactions. The first is oxidation of Ti3+ via reaction with O and Mg in the gas phase: 1.5 O(g) + Mg(g) → ¼ Di + [Ti4+Mg3/4Ti3+-1Ca-1/4Si-1/2] (1). Pyroxene is produced and En is introduced. The second reaction (2) is perovskite formation. It is observed in the WL rim of Leoville 144A, and experiments confirm that an elevated Ti component converts pyroxene to perovskite(Gupta et al. 1973). MgCa-1 is the third linearly independent reaction (3). They combine to give: ½ Di + x Ca(g)→ x Mg(g)+ Pv + [Mg1/2-xSiTi4+-1Ca-1/2+x](2,3). Unlike (1), pyroxene is consumed in this reaction. The parameter x defines the extent of Mg-Ca exchange. When x > 0.5, WL rim formation occurs in an environment where Mg is volatile and Ca condenses. The reaction space defined by reactions (1) and (2,3) describes the transition from CAI interior to WL rims. WL rim pyroxene Ti contents, [CaTs], and Ca < 1 pfu are all explained in this space. The fourth linearly independent reaction is SiO(g):1/8 Di + ¼ Mg(g)→ ¾ SiO(g) + [Mg3/8Ca1/8Ti4+Ti3+-1Si-1/2](4). Silica reduction forms Ti4+, releasing SiO(g). (4) does not describe the oxidation of Ti3+ in WL rim pyroxene, but (1) - (4) results in En formation directly from the gas phase. This may explain WL rim analyses that have Si contents in excess

  7. High precision Al-Mg systematics of forsterite-bearing Type B CAIs from CV3 chondrites

    NASA Astrophysics Data System (ADS)

    MacPherson, G. J.; Bullock, E. S.; Tenner, T. J.; Nakashima, D.; Kita, N. T.; Ivanova, M. A.; Krot, A. N.; Petaev, M. I.; Jacobsen, S. B.

    2017-03-01

    In order to further elucidate possible temporal relationships between different varieties of calcium-, aluminum-rich inclusions (CAIs), we measured the aluminum-magnesium isotopic systematics of seven examples of the rare type known as forsterite-bearing Type B (FoB) inclusions from four different CV3 carbonaceous chondrites: Allende, Efremovka, NWA 3118, and Vigarano. The primary phases (forsterite, Al-Ti-rich diopside, spinel, melilite, and anorthite) in each inclusion were analyzed in situ using high-precision secondary ion mass-spectrometry (SIMS). In all cases, minerals with low Al/Mg ratios (all except anorthite) yield well-defined internal Al-Mg isochrons, with a range of initial 26Al/27Al ratios [(26Al/27Al)0] ranging from (5.30 ± 0.22) × 10-5 down to (4.17 ± 0.43) × 10-5. Anorthite in all cases is significantly disturbed relative to the isochrons defined by the other phases in the same CAIs, and in several cases contains no resolved excesses of radiogenic 26Mg (δ26Mg∗) even at 27Al/24Mg ratios greater than 1000. The fact that some FoBs preserve (26Al/27Al)0 of ∼5.2 × 10-5, close to the canonical value of (5.23 ± 0.13) × 10-5 inferred from bulk magnesium-isotope measurements of CV CAIs (B. Jacobsen et al., 2008), demonstrates that FoBs began forming very early, contemporaneous with other more-refractory CAIs. The range of (26Al/27Al)0 values further shows that FoBs continued to be reprocessed over ∼200,000 years of nebular history, consistent with results obtained for other types of igneous CAIs in CV chondrites. The absence of any correlation between of CAI + FoB formation or reprocessing times with bulk composition or CAI type means that there is no temporal evolutionary sequence between the diverse CAI types. The initial δ26Mg∗ value in the most primitive FoB (SJ101) is significantly lower than the canonical solar system value of -0.040 ± 0.029‰.

  8. Calcium and Titanium Isotope Fractionation in CAIS: Tracers of Condensation and Inheritance in the Early Solar Protoplanetary Disk

    NASA Technical Reports Server (NTRS)

    Simon, J. I.; Jordan, M. K.; Tappa, M. J.; Kohl, I. E.; Young, E. D.

    2016-01-01

    The chemical and isotopic compositions of calcium-aluminum-rich inclusions (CAIs) can be used to understand the conditions present in the protoplantary disk where they formed. The isotopic compositions of these early-formed nebular materials are largely controlled by chemical volatility. The isotopic effects of evaporation/sublimation, which are well explained by both theory and experimental work, lead to enrichments of the heavy isotopes that are often exhibited by the moderately refractory elements Mg and Si. Less well understood are the isotopic effects of condensation, which limits our ability to determine whether a CAI is a primary condensate and/or retains any evidence of its primordial formation history.

  9. Microstructures of Hibonite From an ALH A77307 (CO3.0) CAI: Evidence for Evaporative Loss of Calcium

    NASA Technical Reports Server (NTRS)

    Han, Jangmi; Brearley, Adrian J.; Keller, Lindsay P.

    2014-01-01

    Hibonite is a comparatively rare, primary phase found in some CAIs from different chondrite groups and is also common in Wark-Lovering rims [1]. Hibonite is predicted to be one of the earliest refractory phases to form by equilibrium condensation from a cooling gas of solar composition [2] and, therefore, can be a potential recorder of very early solar system processes. In this study, we describe the microstructures of hibonite from one CAI in ALH A77307 (CO3.0) using FIB/TEM techniques in order to reconstruct its formational history.

  10. Developing the Coach Analysis and Intervention System (CAIS): establishing validity and reliability of a computerised systematic observation instrument.

    PubMed

    Cushion, Christopher; Harvey, Stephen; Muir, Bob; Nelson, Lee

    2012-01-01

    We outline the evolution of a computerised systematic observation tool and describe the process for establishing the validity and reliability of this new instrument. The Coach Analysis and Interventions System (CAIS) has 23 primary behaviours related to physical behaviour, feedback/reinforcement, instruction, verbal/non-verbal, questioning and management. The instrument also analyses secondary coach behaviour related to performance states, recipient, timing, content and questioning/silence. The CAIS is a multi-dimensional and multi-level mechanism able to provide detailed and contextualised data about specific coaching behaviours occurring in complex and nuanced coaching interventions and environments that can be applied to both practice sessions and competition.

  11. A Comparative Study to Evaluate the Effectiveness of Computer Assisted Instruction (CAI) versus Class Room Lecture (CRL) for Computer Science at ICS Level

    ERIC Educational Resources Information Center

    Kausar, Tayyaba; Choudhry, Bushra Naoreen; Gujjar, Aijaz Ahmed

    2008-01-01

    This study was aimed to evaluate the effectiveness of CAI vs. classroom lecture for computer science at ICS level. The objectives were to compare the learning effects of two groups with class room lecture and computer assisted instruction studying the same curriculum and the effects of CAI and CRL in terms of cognitive development. Hypothesis of…

  12. A Comparative Study to Evaluate the Effectiveness of Computer Assisted Instruction (CAI) versus Class Room Lecture (RL) for Computer Science at ICS Level

    ERIC Educational Resources Information Center

    Kausar, Tayyaba; Choudhry, Bushra Naoreen; Gujjar, Aijaz Ahmed

    2008-01-01

    This study was aimed to evaluate the effectiveness of CAI vs. classroom lecture for computer science at ICS level. The objectives were to compare the learning effects of two groups with class room lecture and computer assisted instruction studying the same curriculum and the effects of CAI and CRL in terms of cognitive development. Hypothesis of…

  13. A One Year Post-program Assessment of a Computer-Assisted Instruction (CAI) Weight Management Program for Industrial Employees: Lessons Learned.

    ERIC Educational Resources Information Center

    Dennison, Kathryn F.; And Others

    1996-01-01

    This study examined whether a computer-assisted instruction (CAI) nutrition program would help employees maintain weight loss and dietary intake improvements over time. Subjects received either no nutrition education, education with microcomputer use, or education without microcomputers. Posttesting found greater weight loss for CAI participants,…

  14. Climatic vs. Seismic Controlled Rockglacier Advances in Northern Tien Shan - Insights from Lichenometry

    NASA Astrophysics Data System (ADS)

    Rosenwinkel, S.; Korup, O.; Landgraf, A.; Dzhumabaeva, A.

    2014-12-01

    Glaciers and permafrost landforms in high mountain areas are of major importance for storing and providing fresh water for the surroundings, especially in arid or semi-arid areas as Central Asia. Rockglaciers have been traditionally used as landform proxies of the distribution of alpine permafrost. In the northern Tien Shan mountains, the most distinct lobes of >200 rockglaciers that we mapped from satellite imagery occur at minimum elevations between 2500 and 3700 m. However, individual and particularly low-lying lobes extend down to well below 3000 m, and seem difficult to reconcile with regional paleoclimatic fluctuations. To support ground based and satellite imagery estimates on rockglacier advances (1 to 10 m/yr) and to gain information on their morphological characteristics, we present results of terrestrial LiDAR measurements on six rockglaciers in four steep mountain valleys in the Kyrgyz and Kazakh Tien Shan. Having the ability to destabilize, and thus provide massive sediment input from hillslopes, we hypothesize that strong earthquakes may also have influenced the formation or advance of some of the region's rockglaciers. This hypothesis is based on the observation that the tectonically active area was affected by a series of major earthquakes in the late 19th and earliest 20th centuries, which have subsequently triggered numerous landslides and rock falls. Using lichenometry, we aim to resolve age patterns on lobes of different rockglaciers located both, in the vicinity and distal from large young historic earthquakes. This method has been used successfully to reconstruct glaciation histories, and paleoseismicity. To gain information about and to compare advance histories of the rockglaciers from the relative ages of their lobes, we compiled a dataset of several thousand lichen diameter measurements of different species (e.g., Rhizocarpon geographicum, Aspicilia tianshanica, Lecanora muralis, and Xanthoria elegans). Results show that lichen age

  15. Source parameters for 11 earthquakes in the Tien Shan, central Asia, determined by P and SH waveform inversion

    NASA Technical Reports Server (NTRS)

    Nelson, Michael R.; Mccaffrey, Robert; Molnar, Peter

    1987-01-01

    The style and the distribution of faulting occurring today in the Tien Shan region were studied, by digitizing long-period World-Wide Standard Seismograph Network P and SH waveforms of 11 of the largest Tien Shan earthquakes between 1965 and 1982 and then using a least squares inversion routine to constrain their fault plane solutions and depths. The results of the examination indicate that north-south shortening is presently occurring in the Tien Shan, with the formation of basement uplifts flanked by moderately dipping thrust faults. The present-day tectonics of the Tien Shan seem to be analogous to those of the Rocky Mountains in Colorado, Wyoming, and Utah during the Laramide orogeny in Late Cretaceous and Early Tertiary time.

  16. Dissolved Chemical Ions in an Ice Core of Grigoriev Ice Cap, Kyrgyz Tien Shan

    NASA Astrophysics Data System (ADS)

    SHUN, A.; Takeuchi, N.; Sera, S.; Fujita, K.; Okamoto, S.; Naoki, K.; Aizen, V. B.

    2012-12-01

    Snow and ice of glaciers contain various chemical ions supplied through the atmosphere and preserve them for a long period of time. Thus, analysis of soluble ions in glaciers is important to reveal material circulation and climate change in the cryosphere. Many glaciers are distributed over the mountains of the Central Asia. Chemical analysis of ice cores recovered from there play an important role to understand the atmosphere and material circulation peculiar to the Eurasian Continent. In this study, we analyzed the concentration of major ions in the ice core drilled on Grigoriev Ice Cap, Kyrgys Tien Shan, located in the northwestern part of Central Asia. We aim to understand material circulation in this area based on the chemical records. Then, we have attempted to reconstruct the environmental change of Central Asia, combining the chronology, hydrogen and oxygen stable isotope ratio, and density of dust in the ice core analyzed by prior researches. In this study, we used 2,176 samples of a snow pit and ice core from the surface to bed (86.87 m total length) on the top of Grigoriev Ice Cap (4,660 m high), Kyrgys Tien Shan in September, 2007. Samples were cut every 1-5 cm and scraped thinly, and transported frozen to Chiba University, Japan. After that, we dispensed those for various experiments, and analyzed the concentration of major ions using ion chromatography. By the way, it is estimated that the date of the bottom of this ice core is approximately 12,000 years ago by prior researches. The concentration of major ions dissolved in the ice core of Grigoriev Ice Cap revealed that Ca is the most dominant species in the measured ions and it accounted for more than 50 % (Eq ratio) of the mean of the entire core. This suggests that CaCO3 included in mineral dust derived from deserts around Tien Shan strongly influence the chemical composition of the Ice Cap. In addition, this composition is similar to those of Urumqi No.1 Glacier (Tien Shan), Mustagh Ata Glacier

  17. Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)

    NASA Astrophysics Data System (ADS)

    Sorg, A. F.; Bolch, T.; Stoffel, M.; Solomina, O.; Beniston, M.

    2012-12-01

    Climate-driven changes in glacier-fed streamflow regimes have direct implications on freshwater supply, irrigation and hydropower potential. Reliable information about current and future glaciation and runoff is crucial for water allocation and, hence, for social and ecological stability. Although the impacts of climate change on glaciation and runoff have been addressed in previous work undertaken in the Tien Shan (known as the 'water tower of Central Asia'), a coherent, regional perspective of these findings has not been presented until now. In our study, we explore the range of changes in glaciation in different climatic regions of the Tien Shan based on existing data. We show that the majority of Tien Shan glaciers experienced accelerated glacier wasting since the mid-1970s and that glacier shrinkage is most pronounced in peripheral, lower-elevation ranges near the densely populated forelands, where summers are dry and where snow and glacial meltwater is essential for water availability. The annual glacier area shrinkage rates since the middle of the twentieth century are 0.38-0.76% per year in the outer ranges, 0.15-0.40% per year in the inner ranges and 0.05-0.31% per year in the eastern ranges. This regionally non-uniform response to climate change implies that glacier shrinkage is less severe in the continental inner ranges than in the more humid outer ranges. Glaciers in the inner ranges react with larger time lags to climate change, because accumulation and thus mass turnover of the mainly cold glaciers are relatively small. Moreover, shrinkage is especially pronounced on small or fragmented glaciers, which are widely represented in the outer regions. The relative insensitivity of glaciers in the inner ranges is further accentuated by the higher average altitude, as the equilibrium line altitude ranges from 3'500 to 3'600 masl in the outer ranges to 4'400 masl in the inner ranges. For our study, we used glacier change assessments based both on direct data

  18. Tien Shan geohazards database: Landslides versus other geomorphic features, seismic versus climatic triggering

    NASA Astrophysics Data System (ADS)

    Havenith, Hans-Balder; Strom, Alexander

    2015-04-01

    Recently, we compiled a new landslide inventory for the Tien Shan, Central Asia, containing about 3500 mapped mass movements within a target region of 1200 km (E-W) by 600 km (N-S). While compiling this inventory, we met several problems: which features need to be combined to identify a landslide - combination of scarp and depositional area? Are all deposits below scarps landslide deposits? Should we map scarps as a landslide feature even if no deposits are found below it? How to clearly distinguish landslide from moraine deposits in the higher mountain areas? ... and finally, as the Tien Shan is prone to strong earthquakes (and comparatively less to severe climatic events), can we consider that most giant landslides are triggered by large seismic events .. and, then, could they be used a paleoseismic markers? Identification problems are partly due to the low resolution of imagery that was used for the landslide mapping (mainly based on Google Earth imagery); the other main reason for related uncertainties is the likely great age (> 1000 years) of the mapped features (even though conservation of geomorphic features can be considered as good in those semi-arid areas - much better than in the Alps). For some of those 'old' features, the uncertainty of their origin remained even after having visited the sites. The tendency was that 'landslide geologists' generally considered the mapped features as landslide deposits while some other geoscientists preferred the moraine hypothesis. The problem of the possible seismic origin of proved landslide morphologies is either directly solved if the triggering earthquake event is known (in recent historical times, after 1885) or indirectly in the other (more frequent) case. We consider that most giant landslides (>107 m3) in the Tien Shan had been triggered by earthquakes - while most occurred in 'pre-historic' times (here, before 1885) and a direct proof is thus missing. Actually, several hard rock slopes and many soft rock

  19. Adding the Long-Term Perspective: Tien Shan's Glacier Mass Change during 1961-2012

    NASA Astrophysics Data System (ADS)

    Farinotti, D.; Longuevergne, L.; Moholdt, G.; Duethmann, D.; Bolch, T.; Vorogushyn, S.; Guntner, A.; Gafurov, A.

    2014-12-01

    The Tien Shan, Central Asia's major mountain range, has recently been the focus of a series of studies targeting changes in meteorological variables, glacier mass and extent, as well as runoff. Reviews have repeatedly highlighted the importance of glacier melt for total runoff on the one hand, but the scarcity of direct glaciological observation on the other. At the regional to global scale, the lack of such direct observations has been tackled by using remotely sensed products such as satellite gravimetry and altimetry, but the covered time frame is typically in the order of one decade, thus hampering robust assessments. Here, an ensemble of approaches based on the Gravity Recovery and Climate Experiment (GRACE), the Ice, Cloud and land Elevation Satellite (ICESat), and in-situ glacier mass balance measurements is used for estimating glacier mass changes in the Tien Shan during the last decade, and for validating a glacier mass balance model that we subsequently use for reconstructing a continuous mass balance time series over the last half-century. The model ensemble is designed to take into account a wide range of uncertainty sources including often-neglected differences such as data sources or model structure. We cross-validate our different approaches during the period 2003-2009, and find an average glacier mass change of -6.1±4.4 Gt/a, thus confirming previously published estimates. We use the glaciological modelling approach to extend our estimates over the period 1961-2012, and gain insights in the spatial and temporal evolution of the regional glacier melt. Estimated melt rates are in turn used for assessing the contribution of glacier melt to the total runoff of major hydrological basins, and indicate that the contribution from glaciers has likely been overestimated in a series of previous studies.

  20. Linking CAI abundance to polarimetric response in a population of ancient asteroids

    NASA Astrophysics Data System (ADS)

    Devogele, Maxime; Tanga, Paolo; Bendjoya, Philippe; Rivet, Jean-Pierre; Surdej, Jean; Bus, Schelte J.; Sunshine, Jessica M.; Cellino, Alberto; Campins, Humberto; Licandro, Javier; Pinilla-Alonso, Noemi; Carry, Benoit

    2016-10-01

    Polarimetry constitutes one of the fundamental tools for characterizing the surface texture and composition of airless Solar System bodies. In 2006, polarimetric observations led to the discovery of a new type of asteroids, which displays a peculiar polarimetric response. These asteroids are collectively known as "Barbarians", from (234) Barbara the first discovered one.The most commonly accepted explanation for this perculiar polarization response seems to be the presence of a high percentage of fluffy-type Calcium Aluminium-rich Inclusions (CAIs), whose optical properties could produce the observed polarization. Their reflectance spectra also exibit an absorption feature in the near-infrared around 2.1-2.2 microns, that is characteristic of this peculiar group.Based on these results, we organized a systematic polarimetric and near-infrared observational campaign of known Barbarians or candidate asteroids. These campaigns include members of the family of 1040 Klumpkea, 2085 Henan and 729 Watsonia, which are known to contain Barbarian and/or L-type asteroids also suspected to have such a polarimetric behaviour. We have made use of the ToPo polarimeter at the 1m telescope of the Centre pédagogique Planète et Univers (C2PU, Observatoire de la Côte d'Azur, France). The spectroscopic observations in the near-infrared were obtained with the SpeX instrument at the NASA's InfraRed Telescope Facility (IRTF).By combining polarimetry and spectroscopy we find a correlation between the abundance of CAIs and the inversion angle of the phase-polarization curve of Barbarian asteroids. This is the first time that a direct link has been established between a specific polarimetric response and the surface composition of asteroids. In addition, we find a considerable variety of CAI abundance from one object to the other, consistent with a wide range of possible albedos. Since these asteroids constitute a reservoir of primitive Solar System material, understanding their origin can

  1. Phenotypic diversity and correlation between white-opaque switching and the CAI microsatellite locus in Candida albicans.

    PubMed

    Hu, Jian; Guan, Guobo; Dai, Yu; Tao, Li; Zhang, Jianzhong; Li, Houmin; Huang, Guanghua

    2016-08-01

    Candida albicans is a commensal fungal pathogen that is often found as part of the human microbial flora. The aim of the present study was to establish a relationship between diverse genotypes and phenotypes of clinical isolates of C. albicans. Totally 231 clinical isolates were collected and used for genotyping and phenotypic switching analysis. Based on the microsatellite locus (CAI) genotyping assay, 65 different genotypes were identified, and some dominant types were found in certain human niches. For example, the genotypes of 30-44 and 30-45 were enriched in vaginal infection samples. C. albicans has a number of morphological forms including the single-celled yeasts, multicellular filaments, white, and opaque cell types. The relationship between the CAI genotype and the ability to undergo phenotypic switching was examined in the clinical isolates. We found that the strains with longer CAA/G repeats in both alleles of the CAI locus were more opaque competent. We also discovered that some MTL heterozygous (a/alpha) isolates could undergo white-opaque switching when grown on regular culture medium (containing glucose as the sole carbon source). Our study establishes a link between phenotypic switching and genotypes of the CAI microsatellite locus in clinical isolates of C. albicans.

  2. Teaching Critical Thinking Skills with CAI: A Design by Two Researchers Shows Computers Can Make a Difference.

    ERIC Educational Resources Information Center

    Bass, George M., Jr.; Perkins, Harvey W.

    1984-01-01

    Describes a project which involved designing a nine-week course utilizing computer assisted instruction (CAI) to teach seventh graders critical thinking skills. Results indicate measurable gains were made in the critical thinking skills of verbal analogy and inductive/deductive reasoning, although no consistent gains were made in logical reasoning…

  3. Changes in flavour and microbial diversity during natural fermentation of suan-cai, a traditional food made in Northeast China.

    PubMed

    Wu, Rina; Yu, Meiling; Liu, Xiaoyu; Meng, Lingshuai; Wang, Qianqian; Xue, Yating; Wu, Junrui; Yue, Xiqing

    2015-10-15

    We measured changes in the main physical and chemical properties, flavour compounds and microbial diversity in suan-cai during natural fermentation. The results showed that the pH and concentration of soluble protein initially decreased but were then maintained at a stable level; the concentration of nitrite increased in the initial fermentation stage and after reaching a peak it decreased significantly to a low level by the end of fermentation. Suan-cai was rich in 17 free amino acids. All of the free amino acids increased in concentration to different degrees, except histidine. Total free amino acids reached their highest levels in the mid-fermentation stage. The 17 volatile flavour components identified at the start of fermentation increased to 57 by the mid-fermentation stage; esters and aldehydes were in the greatest diversity and abundance, contributing most to the aroma of suan-cai. Bacteria were more abundant and diverse than fungi in suan-cai; 14 bacterial species were identified from the genera Leuconostoc, Bacillus, Pseudomonas and Lactobacillus. The predominant fungal species identified were Debaryomyces hansenii, Candida tropicalis and Penicillium expansum.

  4. Hunting and use of terrestrial fauna used by Caiçaras from the Atlantic Forest coast (Brazil)

    PubMed Central

    2009-01-01

    Background The Brazilian Atlantic Forest is considered one of the hotspots for conservation, comprising remnants of rain forest along the eastern Brazilian coast. Its native inhabitants in the Southeastern coast include the Caiçaras (descendants from Amerindians and European colonizers), with a deep knowledge on the natural resources used for their livelihood. Methods We studied the use of the terrestrial fauna in three Caiçara communities, through open-ended interviews with 116 native residents. Data were checked through systematic observations and collection of zoological material. Results The dependence on the terrestrial fauna by Caiçaras is especially for food and medicine. The main species used are Didelphis spp., Dasyprocta azarae, Dasypus novemcinctus, and small birds (several species of Turdidae). Contrasting with a high dependency on terrestrial fauna resources by native Amazonians, the Caiçaras do not show a constant dependency on these resources. Nevertheless, the occasional hunting of native animals represents a complimentary source of animal protein. Conclusion Indigenous or local knowledge on native resources is important in order to promote local development in a sustainable way, and can help to conserve biodiversity, particularly if the resource is sporadically used and not commercially exploited. PMID:19930595

  5. A Model Driven Question-Answering System for a CAI Environment. Final Report (July 1970 to May 1972).

    ERIC Educational Resources Information Center

    Brown, John S.; And Others

    A question answering system which permits a computer-assisted instruction (CAI) student greater initiative in the variety of questions he can ask is described. A method is presented to represent the dynamic processes of a subject matter area by augmented finite state automata, which permits efficient inferencing about dynamic processes and…

  6. From Corporate Social Responsibility, through Entrepreneurial Orientation, to Knowledge Sharing: A Study in Cai Luong (Renovated Theatre) Theatre Companies

    ERIC Educational Resources Information Center

    Tuan, Luu Trong

    2015-01-01

    Purpose: This paper aims to examine the role of antecedents such as corporate social responsibility (CSR) and entrepreneurial orientation in the chain effect to knowledge sharing among members of Cai Luong theatre companies in the Vietnamese context. Knowledge sharing contributes to the depth of the knowledge pool of both the individuals and the…

  7. Computer-Assisted Instruction (CAI) in Language Arts: Investigating the Influence of Teacher Knowledge and Attitudes on the Learning Environment

    ERIC Educational Resources Information Center

    Davis, Jamie M.

    2009-01-01

    The integration of Computer-Assisted Instruction (CAI) into the language arts classroom can greatly assist teachers meet the needs of diverse literacy learners. However, this new technology does not come without some concerns, including but not limited to ease of implementation, funding for new hardware and software, appropriate teacher support,…

  8. Investigating Learning Achievements of Thai High School Students in a Sequences and Series Lesson Delivered on CAI-Based Materials

    ERIC Educational Resources Information Center

    Chundang, Ungsana; Singhaprink, Wipawaan; Pongpullponsak, Adisak; Tantipisalkul, Tasanee; Praekhaow, Puchong

    2012-01-01

    The current experimental research aims to investigate students' learning outcomes in classes in which the interactive CAI (computer-assisted instruction)-based materials were implemented. It also aims to compare the learning outcomes of the students based on regions in which their school is located. The participants were 326 Matthayom-4 students…

  9. Hypertext and three-dimensional computer graphics in an all digital PC-based CAI workstation.

    PubMed Central

    Schwarz, D. L.; Wind, G. G.

    1991-01-01

    In the past several years there has been an enormous increase in the number of computer-assisted instructional (CAI) applications. Many medical educators and physicians have recognized the power and utility of hypertext. Some developers have incorporated simple diagrams, scanned monochrome graphics or still frame photographs from a laser disc or CD-ROM into their hypertext applications. These technologies have greatly increased the role of the microcomputer in education and training. There still remain numerous applications for these tools which are yet to be explored. One of these exciting areas involves the use of three-dimensional computer graphics. An all digital platform increases application portability. Images Figure 1 Figure 2 Figure 3 Figure 4 PMID:1807767

  10. Two years since SSAMS: Status of 14C AMS at CAIS

    NASA Astrophysics Data System (ADS)

    Ravi Prasad, G. V.; Cherkinsky, Alexander; Culp, Randy A.; Dvoracek, Doug K.

    2015-10-01

    The NEC 250 kV single stage AMS accelerator (SSAMS) was installed two years ago at the Center for Applied Isotope Studies (CAIS), University of Georgia. The accelerator is primarily being used for radiocarbon measurements to test the authenticity of natural and bio-based samples while all other samples such as geological, atmospheric, marine and archaeological. are run on the 500 kV, NEC 1.5SDH-1 model tandem accelerator, which has been operating since 2001. The data obtained over a six months period for OXI, OXII, ANU sucrose and FIRI-D are discussed. The mean value of ANU sucrose observed to be slightly lower than the consensus value. The processed blanks on SSAMS produce lower apparent age compared to the tandem accelerator as expected.

  11. A FIB/TEM/Nanosims Study of a Wark-Lovering Rim on an Allende CAI

    NASA Technical Reports Server (NTRS)

    Keller, L. P.; Needham, A. W.; Messenger, S.

    2014-01-01

    Ca- Al-rich inclusions (CAIs) are commonly surrounded by Wark-Lovering (WL) rims - thin (approx. 50 micrometers) multilayered sequences - whose mineralogy is dominated by high temperature minerals similar to those that occur in the cores of CAIs [1]. The origins of these WL rims involved high temperature events in the early nebula such as condensation, flashheating or reaction with a nebular reservoir, or combinations of these processes. These rims formed after CAI formation but prior to accretion into their parent bodies. We have undertaken a coordinated mineralogical and isotopic study of WL rims to determine the formation conditions of the individual layers and to constrain the isotopic reservoirs they interacted with during their history. We focus here on the spinel layer, the first-formed highest- temperature layer in the WL rim sequence. Results and Discussion: We have performed mineralogical, chemical and isotopic analyses of an unusual ultrarefractory inclusion from the Allende CV3 chondrite (SHAL) consisting of an approx. 500 micrometers long single crystal of hibonite and co-existing coarsegrained perovskite. SHAL is partially surrounded by WL rim. We previously reported on the mineralogy, isotopic compositions and trace elements in SHAL [2-4]. The spinel layer in the WL rim is present only on the hibonite and terminates abruptly at the contact with the coarse perovskite. This simple observation shows that the spinel layer is not a condensate in this case (otherwise spinel would have condensed on the perovskite as well). The spinel layer appears to have formed by gas-phase corrosion of the hibonite by Mg-rich vapors such that the spinel layer grew at the expense of the hibonite. We also found that the spinel layer has the same 16Orich composition as the hibonite. The spinel layer is polycrystalline and individual crystals do not show a crystallographic relationship with the hibonite. An Al-diopside layer overlies the spinel layer, and is present on both

  12. Secondary processing of chondrules and refractory inclusions (CAIs) by gasdynamic heating

    NASA Technical Reports Server (NTRS)

    Podolak, M.; Prialnik, D.; Bunch, T. E.; Cassen, P.; Reynolds, R.

    1993-01-01

    Results of calculations performed to determine the conditions necessary for producing the opaque rims on chondrules and CAI rims by high-speed entry into the transient atmosphere of an accreting meteorite parent body are presented. The sensitivity of these results to variations in critical parameters is investigated. The range of entry velocities which can produce such rims is shown to depend on the size, melting temperature, and thermal conductivity of the particles. For particles greater than 2 mm in radius, with thermal conductivities of 20,000 ergs/sm s K or lower, entry velocities of about 3 km/s suffice. For particle sizes less than 1 mm in radius, the range of encounter velocities that can produce rims is narrow or vanishing, regardless of the thermal conductivity, unless the melting temperature in the outer part of the chondrule has been reduced by compositional heterogeneity.

  13. Retrieval of UV Aerosol Index using backscattered monochromatic radiance measured by GOSAT CAI

    NASA Astrophysics Data System (ADS)

    Go, S.; Kim, J.; KIM, M.; Park, S. S.

    2014-12-01

    UV Aerosol Index(AI) using backscattered radiance at a single channel has been retrieved. In the current UV AI algorithm, two UV channels are used to contrast the absorbing aerosol loaded atmosphere to Rayleigh scattering condition. There have been needs to retrieve information of absorbing aerosol from a single UV channel, such as GOSAT CAI. 30-day minimum composite method, however, makes the process possible to construct the condition with the use of only single UV channel. Also, absorption by aerosol changes with respect to AOD and wavelength for different aerosol types. Therefore, single channel aerosol index(SAI) can detect absorbing aerosol qualitatively. Correlation coefficient of SAI to current UV AI indicate significant value, showing possibility of detecting highly absorbing aerosols. The application of a cloud screening makes the presence of absorbing aerosols even more clear. Radiative transfer calculations using VLIDORT were performed to test the sensitivity of SAI and UV AI to aerosol optical properties, showing that highly absorbing aerosol results in meaningful SAI. Results from dust case study in East Asia show reasonable performance of SAI for the region with single scattering albedo below 0.90. This study concludes with a comparison of SAI from GOSAT lv.1b data to OMI UVAI data, where reasonable agreement and low false detection was found for dust cases in East Asia. The SAI value of -0.2 to 0.0 from GOSAT-CAI was comparable to OMI dust threshold value of 0.7. These findings corroborate the suitability of SAI as a for detecting absorbing aerosols for satellite instrument with a single UV channel.

  14. Geodynamics of late Paleozoic magmatism in the Tien Shan and its framework

    NASA Astrophysics Data System (ADS)

    Biske, Yu. S.; Konopelko, D. L.; Seltmann, R.

    2013-07-01

    The Devonian-Permian history of magmatic activity in the Tien Shan and its framework has been considered using new isotopic datings. It has been shown that the intensity of magmatism and composition of igneous rocks are controlled by interaction of the local thermal upper mantle state (plumes) and dynamics of the lithosphere on a broader regional scale (plate motion). The Kazakhstan paleocontinent, which partly included the present-day Tien Shan and Kyzylkum, was formed in the Late Ordovician-Early Silurian as a result of amalgamation of ancient continental masses and island arcs. In the Early Devonian, heating of the mantle resulted in the within-plate basaltic volcanism in the southern framework of the Kazakhstan paleocontinent (Turkestan paleoocean) and development of suprasubduction magmatism over an extensive area at its margin. In the Middle-Late Devonian, the margins of the Turkestan paleoocean were passive; the area of within-plate oceanic magmatism shifted eastward, and the active margin was retained at the junction with the Balkhash-Junggar paleoocean. A new period of active magmatism was induced by an overall shortening of the region under the settings of plate convergence. The process started in the Early Carboniferous at the Junggar-Balkhash margin of the Kazakhstan paleocontinent and the southern (Paleotethian) margin of the Karakum-Tajik paleocontinent. In the Late Carboniferous, magmatism developed along the northern boundary of the Turkestan paleoocean, which was closing between them. The disappearance of deepwater oceanic basins by the end of the Carboniferous was accompanied by collisional granitic magmatism, which inherited the paleolocations of subduction zones. Postcollision magmatism fell in the Early Permian with a peak at 280 Ma ago. In contrast to Late Carboniferous granitic rocks, the localization of Early Permian granitoids is more independent of collision sutures. The magmatism of this time comprises: (1) continuation of the

  15. Reconstruction of glacial lake outburst floods in northern Tien Shan: Implications for hazard assessment

    NASA Astrophysics Data System (ADS)

    Zaginaev, V.; Ballesteros-Cánovas, J. A.; Erokhin, S.; Matov, E.; Petrakov, D.; Stoffel, M.

    2016-09-01

    Glacier lake outburst floods (GLOFs) and related debris flows are among the most significant natural threats in the Tien Shan Mountains of Kyrgyzstan and have even caused the loss of life and damage to infrastructure in its capital Bishkek. An improved understanding of the occurrence of this process is essential so as to be able to design reliable disaster risk reduction strategies, even more so in view of ongoing climate change and scenarios of future evolutions. Here, we apply a dendrogeomorphic approach to reconstruct past debris-flow activity on the Aksay cone (Ala-Archa valley, Kyrgyz range), where outbursting glacier lakes and intense rainfalls have triggered huge debris flows over the past decades. A total of 96 Picea abies (L.) Karst. trees growing on the cone and along the main channel have been selected based on the evidence of past debris-flow damage in their trunks; these trees were then sampled using increment borers. The dating of past events was based on the assessment of growth disturbances (GD) in the tree-ring records and included the detection of injuries, tangential rows of traumatic resin ducts, reaction wood, and abrupt growth changes. In total, 320 GD were identified in the tree-ring samples. In combination with aerial imagery and geomorphic recognition in the field, reactions in trees and their position on the cone have allowed reconstruction of the main spatial patterns of past events on the Aksay cone. Our findings suggest that at least 27 debris flows have occurred on the site between 1877 and 2015 and point to the occurrence of at least 17 events that were not documented prior to this study. We also observe high process activity during the 1950s and 1960s, with major events on the cone in 1950, 1966, and 1968, coinciding with phases of slight glacier advance. The spatial analyses of events also point to two different spatial patterns, suggesting that quite dissimilar magnitudes probably occurred during glacier lake outburst floods and

  16. The Whole Tien Shan Glacier Area Changes Between 1973 and 2003 Estimated From Corona and ASTER Satellite Imagery

    NASA Astrophysics Data System (ADS)

    Surazakov, A. B.; Aizen, V. B.; Aizen, E. M.

    2007-12-01

    Changes in glacier covered area of the Tien Shan Mountains (western, central and eastern) was estimated between 1973-2003 using Corona KH-9 (9 m) and ASTER (15 m) imagery. Large spatial coverage of a single Corona KH-9 photograph (almost eight ASTER images) and accurate geometric qualities of the KH-9 frame- mapping camera provide a unique opportunity for reconstruction of the glacier covered area during the last 30 years with comparable spatial resolution. The images were orthorectified using SRTM DEM with void areas filled with ASTER DEM and ground control points collected from 1:25,000 and 1:50,000 topographic maps. The Corona and ASTER orthorectification RMS residuals were in the same order of 7-15 m. Glacier boundaries were derived using segmentation of ASTER 3N/4 band ratio and manual digitizing with error-checking in stereo viewing. Since the middle of 1970s, Tien Shan was experiencing abrupt increase in air temperature, that accelerated glacier recession particularly in the mountain ranges lower than 5,000 m a.s.l. From 1973 to 2003 all Tien Shan glaciers have significant recession trend. The most notable recession has been observed in the western and southern Tien Shan: from 20% to 17.1% of the total glacier area. The eastern and northern Tien Shan glaciers have lost 12.6% - 11% of their total area while the largest and highest (up to 7,000 m) central Tien Shan remained nearly the same glacierized area: only 1% of the total glacier area reduction. The large dendritic glaciers in the central Tien Shan are heavily covered by moraine debris, which protect glaciers from intensive ablation. The Tien Shan mountain ranges longitudinally spans more than 2,000 km and glaciers exist in different geo-morphological and climatic conditions determining the difference in glacier recession. However, the Tien Shan glacier surface has decreased in all regions and has to be measured by GPS and satellite altimetry to estimate real changes in glacier ice water resources.

  17. VARIABLE AND EXTREME IRRADIATION CONDITIONS IN THE EARLY SOLAR SYSTEM INFERRED FROM THE INITIAL ABUNDANCE OF {sup 10}Be IN ISHEYEVO CAIs

    SciTech Connect

    Gounelle, Matthieu; Chaussidon, Marc; Rollion-Bard, Claire

    2013-02-01

    A search for short-lived {sup 10}Be in 21 calcium-aluminum-rich inclusions (CAIs) from Isheyevo, a rare CB/CH chondrite, showed that only 5 CAIs had {sup 10}B/{sup 11}B ratios higher than chondritic correlating with the elemental ratio {sup 9}Be/{sup 11}B, suggestive of in situ decay of this key short-lived radionuclide. The initial ({sup 10}Be/{sup 9}Be){sub 0} ratios vary between {approx}10{sup -3} and {approx}10{sup -2} for CAI 411. The initial ratio of CAI 411 is one order of magnitude higher than the highest ratio found in CV3 CAIs, suggesting that the more likely origin of CAI 411 {sup 10}Be is early solar system irradiation. The low ({sup 26}Al/{sup 27}Al){sub 0} [{<=} 8.9 Multiplication-Sign 10{sup -7}] with which CAI 411 formed indicates that it was exposed to gradual flares with a proton fluence of a few 10{sup 19} protons cm{sup -2}, during the earliest phases of the solar system, possibly the infrared class 0. The irradiation conditions for other CAIs are less well constrained, with calculated fluences ranging between a few 10{sup 19} and 10{sup 20} protons cm{sup -2}. The variable and extreme value of the initial {sup 10}Be/{sup 9}Be ratios in carbonaceous chondrite CAIs is the reflection of the variable and extreme magnetic activity in young stars observed in the X-ray domain.

  18. A compound Ca-, Al-rich inclusion from CV3 chondrite Northwest Africa 3118: Implications for understanding processes during CAI formation

    NASA Astrophysics Data System (ADS)

    Ivanova, Marina A.; Lorenz, Cyril A.; Krot, Alexander N.; MacPherson, Glenn J.

    2015-09-01

    A calcium-aluminum-rich inclusion 3N from the Northwest Africa (NWA) 3118 CV3 carbonaceous chondrite is a unique cm-sized compound object, primarily a forsterite-bearing type B (FoB) CAI, that encloses at least 26 smaller CAIs of different types, including compact type A (CTA), B, C, and an ultra-refractory inclusion. Relative to typical type A and B CAIs found elsewhere, the bulk compositions of the types A and B CAIs within 3N more closely match the bulk compositions predicted by equilibrium condensation of a gas of solar composition. Being trapped within the FoB melt may have protected them from melt evaporation that affected most "stand-alone" CAIs. 3N originated either as an aggregate of many smaller (mostly types A, B, C) CAIs plus accreted Fo-bearing material (like an amoeboid olivine aggregate) which experienced partial melting of the whole, or else as a FoB melt droplet that collided with and trapped many smaller solid CAIs. In the former case, 3N recorded the earliest accretion of pebble-sized bodies known. In the latter case, the presence of a large number of individual refractory inclusions within 3N suggests a very high local density of refractory solids in the immediate region of the host CAI during the brief time while it was melted. Collisions would have occurred on time scales of hours at most, assuming a melt solidification interval for the host CAI of 300-400 °C (maximum) and a cooling rate of ~10 °C/h.

  19. Seismic Microzoning of Cap-Haïtien: Effects of Lithological Site and Liquefaction

    NASA Astrophysics Data System (ADS)

    Gilles, R.; Jeudy, B.; Prepetit, C.; Bertil, D.; Roulle, A.; Noury, G.

    2014-12-01

    After the earthquake of January 12, 2010 in Haiti, the Haitian Government has resolved to implement a program of seismic microzonation for most vulnerable cities in the country by the way of prevention. Metropolitan Port-au-Prince and five cities in the North of Haiti including Cap-Haitien were included in this program. The seismic microzonation is an important tool for the knowledge of the seismic risk. It is based on the collection of geological, geophysical and geotechnical data. It describes a specific class of soil associated with each type of soil. Its goal is to map the homogenous zones of soil to effects of site lithology, topographic site effects, liquefaction and ground movements. This work is based on two aspects of the studies of microzoning for the city of Cap-Haïtien: effects of lithological site and Liquefaction. The zoning of site effects is to identify and map the areas with consistent geological and geomechanical characteristics and homogeneous seismic response; the objective is to provide, in each zone, seismic movements adapted. Five classes of soil at site effects were distinguished. Associated responses spectra were obtained by a 1D nonlinear analysis using CyberQuake software (Modaressi et al. 1997 BRGM). The zoning of the liquefaction present the liquefaction potential of different areas. Three levels of risk of liquefaction were found during this study that a large part of the city is strongly liquefiable.

  20. [Termites (Isoptera) in forest ecosystems of Cat Tien National Park (Southern Vietnam)].

    PubMed

    Beliaeva, N V; Tiunov, A V

    2010-01-01

    The species composition and termite community populations were studied and the total land termites biomass was estimated in five forest habitats of Cat Tien National Park, Southern Vietnam. Twenty-four species of two families, Rhinotermitidae (1 species) and Termitidae (23 species), the predominant representatives of the subfamily Macrotermitinae, were found in mounds and in soil samples. On the test plots the density of termite mounds averaged 68 per hectare, primarily the mounds of three Macrotermes species. Destructive sampling allowed estimation of the caste composition and total community biomass based on six termite mounds of the prevailing species (Globitermes sulphureus, Microcerotermes burmanicus, Macrotermes carbonarius, M. gilvus, M. malaccensis, and Hypotermes obscuriceps). The total number of termites in the nests ranged from 65 000 to 3 150 000 individuals with the total biomass ranging from 185 to 2440 g live weight. The total abundance of nesting Macrotermes species alone could conservatively be estimated as 2.5 million individuals and 20.5 kg live weight per hectare. The number of soil- and litter-feeding termites averaged for the test plots was estimated at about 60 ind./m2. Four species dominating on the test plots (M. carbonarius, M. gilvus, M. malaccensis, and H. obscuriceps) belong to active tree litter feeders.

  1. Stress drop in the sources of intermediate-magnitude earthquakes in northern Tien Shan

    NASA Astrophysics Data System (ADS)

    Sycheva, N. A.; Bogomolov, L. M.

    2014-05-01

    The paper is devoted to estimating the dynamical parameters of 14 earthquakes with intermediate magnitudes (energy class 11 to 14), which occurred in the Northern Tien Shan. For obtaining the estimates of these parameters, including the stress drop, which could be then applied in crustal stress reconstruction by the technique suggested by Yu.L. Rebetsky (Schmidt Institute of Physics of the Earth, Russian Academy of Sciences), we have improved the algorithms and programs for calculating the spectra of the seismograms. The updated products allow for the site responses and spectral transformations during the propagation of seismic waves through the medium (the effect of finite Q-factor). By applying the new approach to the analysis of seismograms recorded by the seismic KNET network, we calculated the radii of the sources (Brune radius), scalar seismic moment, and stress drop (release) for the studied 14 earthquakes. The analysis revealed a scatter in the source radii and stress drop even among the earthquakes that have almost identical energy classes. The stress drop by different earthquakes ranges from one to 75 bar. We have also determined the focal mechanisms and stress regime of the Earth's crust. It is worth noting that during the considered period, strong seismic events with energy class above 14 were absent within the segment covered by the KNET stations.

  2. Ordovician-Carboniferous tectono-sedimentary evolution of the North Nuratau region, Uzbekistan (Westernmost Tien Shan)

    NASA Astrophysics Data System (ADS)

    McCann, T.; Nurtaev, B.; Kharin, V.; Valdivia-Manchego, M.

    2013-04-01

    The Tien Shan is a c. 2500 km long orogenic belt of which the Nuratau region of eastern Uzbekistan forms the western part. Petrographical and field analysis of the Ordovician-Carboniferous succession in the North Nuratau region provided the basis for a reconstruction of the depositional settings along part of the northern margin of the Alai continent and their evolution during the period of closure of the Turkestan Ocean, which separated the Alai and the Kazakh-Kyrgyz continents. Initial sedimentation (Ordovician) was broadly carbonate dominated, although by Mid-Late Ordovician times siliciclastic input predominated in some areas. These variations, between clastic- and carbonate-dominated regions may have been related to tectonic activity within the Alai continent. Carbonate sedimentation was reestablished in the ?Wenlock, with broad shelf systems forming along the continental margin. Volcanic activity in the Early Devonian records a period of tectonic instability, and this was followed by the reestablishment of the carbonate mosaic, albeit with a greater degree of instability (as indicated by stratigraphic gaps) than in the Silurian. This pattern extended up into the Carboniferous culminating in backarc-related magmatic activity. Final closure of the Turkestan Ocean involved significant folding and thrusting, as well as a major change from compressional to strike-slip movement.

  3. Morphogenetic features of soils in the Cat Tien National Park, southern Vietnam

    NASA Astrophysics Data System (ADS)

    Khokhlova, O. S.; Myakshina, T. N.; Kuznetsov, A. N.; Gubin, S. V.

    2017-02-01

    Morphogenetic features of soils on the selected plots in the Cat Tien National Park in southern Vietnam have been studied with the use of a set of morphological, analytical, and instrumental methods. The lithological factor and topographic position play the leading role in the development of the particular genetic soil features. The soils can be subdivided into four groups according to these factors. The soils developing from volcanic deposits with a predominance of tephra can be classified as thin clayey brown tropical soils (Dystric Skeletic Rhodic Cambisols (Clayic)), and the soils developed from less weathered colluvial derivatives of basalts with some admixture of tephra can be classified as dark-humus clayey tropical soils (Skeletic Greyzemic Umbrisols (Clayic)). Very poor soils developed from the eluvium of argillites are classified as thin weakly developed clayey tropical soils (Dystric Regosols (Clayic)). The soils forming from the alluvial sediments of different textures are classified as alluvial loamy sandy soils (Dystric Fluvisols (Arenic, Drainic)) and as alluvial clay loamy soils (Eutric Fluvisols (Episiltic, Endoclayic)).

  4. Alpine tectonics of granites in basement of Ysyk-Köl Basin, northern Tien Shan

    NASA Astrophysics Data System (ADS)

    Leonov, M. G.; Przhiyalgovsky, E. S.; Lavrushina, E. V.; Poleshchuk, A. V.; Rybin, A. K.

    2016-07-01

    The Ysyk-Köl Basin filled with Lower Jurassic-Quaternary sedimentary rocks is the largest intermontane negative structural unit of the northern Tien Shan. The basement of this basin is composed of Precambrian-Paleozoic rocks, largely of Ordovician and Silurian granitoids exposed in mountain ranges of the basin framework and as separate anticlinal domes situated in areas occupied by the Mesozoic-Cenozoic sedimentary cover. The postmagmatic tectonic internalstructure of the Chonkurchak (Chunkurchak), Kyzyl-Choku, Kyzyl-Bulak, and Prishib massifs emplaced in the basement, as well as their relationships to the sedimentary cover, are described in the paper. The study was carried out using the morphostructural method, detailed geological mapping, structural kinematic analysis, and petrographic examination of rocks. The internalstructure of Paleozoic granites in the basement and indications of their 3D tectonic flow are characterized. It is shown that granites underwent 3D deformation after their emplacement in the consolidated crust, and this process had a substantial influence on tectonic processes at the plate and orogenic stages of regional evolution.

  5. Tectonic and sedimentary evolution of the Ili Basin (northern Tien Shan, Kazakhstan)

    NASA Astrophysics Data System (ADS)

    Kley, J.; Voigt, T.; Seib, N.; Kober, M.

    2010-12-01

    The Tien Shan active intraplate orogen of Central Asia exhibits strong along-strike variations in structure. Its northern front in southeastern Kazakhstan is characterized by a fragmented array of anticlinal basement highs whose wavelengths range from c. 5 to 30 km. Range-bounding faults are mostly E- to ENE-trending thrust or reverse faults and SE-trending dextral strike-slip faults. Faults of large displacement (more than several tens of meters) are conspicuously absent. The synclinal lows between the basement highs preserve Cenozoic strata of Oligocene to Quaternary age, probably deposited in a once continuous basin (the Ili Basin) and recording the entire history of Tien Shan uplift. Very gentle, long-wavelength folds affect the Cenozoic strata. As far as visible, the basement is always folded conformably. The basin fill starts in the middle Oligocene (mammal fossils; Indricotherium horizon). The facies of these oldest deposits is characterized by fluvial deposits of a large river system and varying flood-plain deposits with intense soil formation (calcretes and gypsisols). Transport directions and quartz content of the sediments suggest they were not sourced from the nearby mountain ranges present today. The fluvial succession is followed by late Oligocene to early Miocene lake deposits which reflect the transition from an evaporitic lake/playa system to freshwater lacustrine conditions. The Oligocene to Early Miocene deposits are limited to a small area in the core of the Aktau anticline and show no relationship to the sediment succession overlying the basement in the uplifts surrounding the Aktau mountains in the north and west. There, alluvial and fluvial deposits of middle Miocene(?) age rest on deeply weathered paleosurfaces. Transport is mainly to the south. Changes in colour, grain size and ratio of channel to interchannel deposits probably reflect climatic changes. Rapid facies and thickness-changes allow the reconstruction of several alluvial fans

  6. Towards an improved glacier monitoring program in the Kyrgyz Tien Shan and Pamir Mountains

    NASA Astrophysics Data System (ADS)

    Barandun, Martina; Huss, Matthias; Azisov, Erlan; Gafurov, Abror; Vorogushyn, Sergiy; Usubaliev, Ryskul; Kronenberg, Marlene; Hoelzle, Martin

    2014-05-01

    The monitoring of glacier mass balance in remote regions is important to understand the response of glaciers to climate change. The coverage of monitored glaciers in Central Asia has been very limited for the past 15 years; however the necessity of enhanced understanding regarding glacier dynamics and long term evolution in this particular region is crucial. Moisture availability importantly determines glacier response. Glaciers located in the Northern Tien Shan and Pamir Mountains are likely not to be directly influenced by monsoon such as most monitored Peri-Himalayan glaciers. However, not only scientific reasons make glacier monitoring to be of great relevance, also the link to political and socio-economic constraints on water scarcity carries high importance. First steps towards the establishment of a new glacier monitoring network were performed in 2010/2011 and since then modernization and extension of the monitoring strategies are continuously aspired. Close cooperation of international and local scientists build the basis of the program. Today four glaciers located in the Kyrgyz Tien Shan (Golubin Glacier, Suek Zapadniy Glacier, Glacier No. 354) and the North-Western Pamir (Abramov Glacier) are regularly monitored. The network is planned to be extended in the next years to cover selected glaciers in Uzbekistan and Tajikistan. Further, we intend to develop new approaches to remotely monitor sub-seasonal glacier mass balance at a regional scale. In-situ mass balance measurements are taken at all four glaciers continuously in late summer. Automatic weather stations installed at Abramov Glacier in 2011 and at Golubin Glacier in 2013 deliver daily meteorological data allowing the application of a simple mass balance model driven with local precipitation and temperature data. Model calibration is performed using glaciological measurements and results are validated with snowline observations based on remote imagery. Automatic cameras at Abramov Glacier take

  7. Cenozoic tectonic history of the Western Tien Shan constrained by low-temperature thermochronology

    NASA Astrophysics Data System (ADS)

    Bande, Alejandro; Sobel, Edward; Mikolaichuk, Alexander

    2014-05-01

    The NW-SE trending dextral Talas-Fergana fault (TFF) separates the Western Tien Shan from the Central Kyrgyz Tien Shan. This ~2000 km long structure extends from western Tarim basin in the southeast to the Turgay basin in the northwest. The TFF formed in the late Paleozoic - Early Mesozoic and was reactivated in the Jurassic and Cenozoic. Cenozoic displacement only occurred along the southern segment of the fault and is poorly constrained; Thomas et al. (1993) suggested 100 ± 60 km Cenozoic displacement based on vertical-axis rotation of Tertiary red beds in the Fergana basin. AFT analysis was carried out on 26 samples collected from vertical profiles and spot samples in the Chatkal, Shandalash, Ugam, Talas and Fergana Ranges associated with structures that merge with the northern active end of the TFF with the goal of constraining the timing of slip. Sampling and thermal modeling of the Talas Range, on the east side of the TFF, show that the range was rapidly being exhumed by the latest Oligocene both near the TFF and at its northern termination. Based on this data and the geometrical relation of the TFF and the structural lineaments of the Talas Range, we interpret the zone as a transpressional pop-up structure kinematically-related to the TFF. A vertical profile in the Shandalash Range, directly to the west across the TFF, suggests a rapid exhumation event at Oligo-Miocene boundary. In this sector, the geometrical relationship of the reverse faults with the main TFF suggests a restraining bend connected to the TFF. Moreover, the timing of exhumation in these two areas suggests that strike-slip movement along the TFF is responsible for the uplift of the Talas pop-up and the development of restraining bends in the Ugam, Shandalash and Chatkal Ranges. Farther south along the west side of the TFF, we collected a vertical profile in the Fergana range in the hanging wall of a thrust sheet that roots into the TFF. A kink in an age-elevation plot suggests the onset of

  8. Tien Shan geohazards database: earthquake and landslide size-frequency statistics

    NASA Astrophysics Data System (ADS)

    Havenith, Hans-Balder

    2015-04-01

    Recently compiled landslide and earthquake data covering a large part of the Tien Shan, Central Asia, are analysed with respect to their size-frequency behaviour. For the same area, only partial databases for sub-regions had been presented previously. They were combined and new data were added to fill the gaps between the databases. The new compiled landslide inventory contains existing records of 1600 previously identified mass movements and more than 1800 new landslide data mapped over a target region of 1200 km (E-W) by 600 km (N-S). On the basis of the new landslide inventory and an updated earthquake catalogue (> 10000 records), the link between landslide and earthquake activity is analysed. Here we focus on the size-frequency relationships developed for both types of geohazards, in terms of Gutenberg-Richter Law for the earthquakes and in terms of probability density function for the landslides. Some similarities can be found in the spatially changing b-value of earthquake events and the power law exponent of the landslide data - lowest values are found in mountain areas where very large mass movements had occurred near major fault zones. The supra-regional landslide inventory will also be compared with sub-regional ones. For one of them, we also possess a multi-temporal landslide inventory and assessed landslide size-frequency relationships for each time period. Those show a decreasing power law exponent with time - due to the coalescence of smaller landslides to form fewer larger ones. However, at (supra-)regional scale, temporal data are very scarce; thus, a major hazard component is still insufficiently known and scaling in time is almost impossible. We may only counteract this problem by dating rockslides and any large mass movement. Finally, we would like to emphasize the role of coupling effects related to various types of geohazards that may also be expressed by similarities between size-frequency relationships.

  9. New complex EAS installation of the Tien Shan mountain cosmic ray station

    NASA Astrophysics Data System (ADS)

    Chubenko, A. P.; Shepetov, A. L.; Antonova, V. P.; Beisembayev, R. U.; Borisov, A. S.; Dalkarov, O. D.; Kryakunova, O. N.; Mukashev, K. M.; Mukhamedshin, R. A.; Nam, R. A.; Nikolaevsky, N. F.; Pavlyuchenko, V. P.; Piscal, V. V.; Puchkov, V. S.; Ryabov, V. A.; Sadykov, T. Kh.; Saduev, N. O.; Salikhov, N. M.; Shaulov, S. B.; Stepanov, A. V.; Vildanov, N. G.; Vildanova, L. I.; Vildanova, M. I.; Zastrozhnova, N. N.; Zhukov, V. V.

    2016-10-01

    In this paper we present a description of the new complex installation for the study of extensive air showers which was created at the Tien Shan mountain cosmic ray station, as well as the results of the test measurements made there in 2014-2016. At present, the system for registration of electromagnetic shower component consists of ∼100 detector points built on the basis of plastic scintillator plates with the sensitive area of 0.25 m2 and 1 m2, spread equidistantly over ∼104m2 space. The dynamic range of scintillation amplitude measurements is currently about (3 - 7) ·104, and there is a prospect of it being extended up to ∼106. The direction of shower arrival is defined by signal delays from a number of the scintillators placed cross-wise at the periphery of the detector system. For the investigation of nuclear active shower components a multi-tier 55 m2 ionization-neutron calorimeter with a sum absorber thickness of ∼1000 g/cm2, typical spatial resolution of the order of 10 cm, and dynamic range of ionization measurement channel about ∼105 was created. Also, the use of saturation-free neutron detectors is anticipated for registration of the high- and low-energy hadron components in the region of shower core. A complex of underground detectors is designed for the study of muonic and penetrative nuclear-active components of the shower. The full stack of data acquisition, detector calibration, and shower parameters restoration procedures are now completed, and the newly obtained shower size spectrum and lateral distribution of shower particles occur in agreement with conventional data. Future studies in the field of 1014 -1017 eV cosmic ray physics to be held at the new shower installation are discussed.

  10. Ca-Fe and Alkali-Halide Alteration of an Allende Type B CAI: Aqueous Alteration in Nebular or Asteroidal Settings?

    NASA Astrophysics Data System (ADS)

    Ross, D. K.; Simon, J. I.; Simon, S. B.; Grossman, L.

    2012-03-01

    Petrographic and chemical observations of secondary alteration products in a CAI constrain the physical and temporal setting of the alteration. Andradite, hedenbergite, sodalite, and nepheline alteration pre-dated assembly of the Allende chondrite parent body.

  11. An experimental study of the combustion characteristics in SCCI and CAI based on direct-injection gasoline engine

    SciTech Connect

    Lee, C.H.; Lee, K.H.

    2007-08-15

    Emissions remain a critical issue affecting engine design and operation, while energy conservation is becoming increasingly important. One approach to favorably address these issues is to achieve homogeneous charge combustion and stratified charge combustion at lower peak temperatures with a variable compression ratio, a variable intake temperature and a trapped rate of the EGR using NVO (negative valve overlap). This experiment was attempted to investigate the origins of these lower temperature auto-ignition phenomena with SCCI and CAI using gasoline fuel. In case of SCCI, the combustion and emission characteristics of gasoline-fueled stratified-charge compression ignition (SCCI) engine according to intake temperature and compression ratio was examined. We investigated the effects of air-fuel ratio, residual EGR rate and injection timing on the CAI combustion area. In addition, the effect of injection timing on combustion factors such as the start of combustion, its duration and its heat release rate was also investigated. (author)

  12. Association between atmospheric circulation patterns and firn-ice core records from the Inilchek glacierized area, central Tien Shan, Asia

    USGS Publications Warehouse

    Aizen, V.B.; Aizen, E.M.; Melack, J.M.; Kreutz, K.J.; Cecil, L.D.

    2004-01-01

    Glacioclimatological research in the central Tien Shan was performed in the summers of 1998 and 1999 on the South Inilchek Glacier at 5100-5460 m. A 14.36 m firn-ice core and snow samples were collected and used for stratigraphic, isotopic, and chemical analyses. The firn-ice core and snow records were related to snow pit measurements at an event scale and to meteorological data and synoptic indices of atmospheric circulation at annual and seasonal scales. Linear relationships between the seasonal air temperature and seasonal isotopic composition in accumulated precipitation were established. Changes in the ??18O air temperature relationship, in major ion concentration and in the ratios between chemical species, were used to identify different sources of moisture and investigate changes in atmospheric circulation patterns. Precipitation over the central Tien Shan is characterized by the lowest ionic content among the Tien Shan glaciers and indicates its mainly marine origin. In seasons of minimum precipitation, autumn and winter, water vapor was derived from the and and semiarid regions in central Eurasia and contributed annual maximal solute content to snow accumulation in Tien Shan. The lowest content of major ions was observed in spring and summer layers, which represent maximum seasonal accumulation when moisture originates over the Atlantic Ocean and Mediterranean and Black Seas. Copyright 2004 by the American Geophysical Union.

  13. Willy: A prize noble Ur-Fremdling - Its history and implications for the formation of Fremdlinge and CAI

    NASA Technical Reports Server (NTRS)

    Armstrong, J. T.; El Goresy, A.; Wasserburg, G. J.

    1985-01-01

    The structure and composition of Willy, a 150-micron-diameter Fremdling in CAI 5241 from the Allende meteorite, are investigated using optical, secondary-electron, and electron-backscatter microscopy and electron-microprobe analysis. The results are presented in diagrams, maps, tables, graphs, and micrographs and compared with those for other Allende Fremdlinge. Willy is found to have a concentric-zone structure comprising a complex porous core of magnetite, metal, sulfide, scheelite, and other minor phases; a compact magnetite-apatite mantle; a thin (20 microns or less) reaction-assemblage zone; and a dense outer rim of fassaite with minor spinel. A multistage formation sequence involving changes in T and fO2 and preceding the introduction of Willy into the CAI (which itself preceded CAI spinel and silicate formation) is postulated, and it is inferred from the apparent lack of post-capture recrystallization that Willy has not been subjected to temperatures in excess of 600 C and may represent the precursor material for many other Fremdlinge.

  14. Numerical Investigation Into Effect of Fuel Injection Timing on CAI/HCCI Combustion in a Four-Stroke GDI Engine

    NASA Astrophysics Data System (ADS)

    Cao, Li; Zhao, Hua; Jiang, Xi; Kalian, Navin

    2006-02-01

    The Controlled Auto-Ignition (CAI) combustion, also known as Homogeneous Charge Compression Ignition (HCCI), was achieved by trapping residuals with early exhaust valve closure in conjunction with direct injection. Multi-cycle 3D engine simulations have been carried out for parametric study on four different injection timings in order to better understand the effects of injection timings on in-cylinder mixing and CAI combustion. The full engine cycle simulation including complete gas exchange and combustion processes was carried out over several cycles in order to obtain the stable cycle for analysis. The combustion models used in the present study are the Shell auto-ignition model and the characteristic-time combustion model, which were modified to take the high level of EGR into consideration. A liquid sheet breakup spray model was used for the droplet breakup processes. The analyses show that the injection timing plays an important role in affecting the in-cylinder air/fuel mixing and mixture temperature, which in turn affects the CAI combustion and engine performance.

  15. Heating during solar nebula formation and Mg isotopic fractionation in precursor grains of CAIs and chondrules

    NASA Technical Reports Server (NTRS)

    Sasaki, S.; Nagahara, H.; Kitagami, K.; Nakagawa, Y.

    1994-01-01

    In some Ca-Al-rich inclusion (CAI) grains, mass-dependent isotopic fractionations of Mg, Si, and O are observed and large Mg isotopic fractionation is interpreted to have been produced by cosmochemical processes such as evaporation and condensation. Mass-dependent Mg isotopic fractionation was found in olivine chondrules of Allende meteorites. Presented is an approximate formula for the temperature of the solar nebula that depends on heliocentric distance and the initial gas distribution. Shock heating during solar nebula formation can cause evaporative fractionation within interstellar grains involved in a gas at the inner zone (a less than 3 AU) of the disk. Alternatively collision of late-accreting gas blobs might cause similar heating if Sigma(sub s) and Sigma are large enough. Since the grain size is small, the solid/gas mass ratio is low and solar (low P(sub O2)), and the ambient gas pressure is low, this heating event could not produce chondrules themselves. Chondrule formation should proceed around the disk midplane after dust grains would grow and sediment to increase the solid/gas ratio there. The heating source there is uncertain, but transient rapid accretion through the disk could release a large amount of heat, which would be observed as FU Orionis events.

  16. I-Xe measurements of CAIs and chondrules from the CV3 chondrites Mokoia and Vigarano

    NASA Astrophysics Data System (ADS)

    Whitby, J. A.; Russell, S. S.; Turner, G.; Gilmour, J. D.

    2004-08-01

    I-Xe analyses were carried out for chondrules and refractory inclusions from the two CV3 carbonaceous chondrites Mokoia and Vigarano (representing the oxidized and reduced subgroups, respectively). Although some degree of disturbance to the I-Xe system is evident in all of the samples, evidence is preserved of aqueous alteration of CAIs in Mokoia 1 Myr later than the I-Xe age of the Shallowater standard and of the alteration of a chondrule (V3) from Vigarano ~0.7 Myr later than Shallowater. Other chondrules in Mokoia and Vigarano experienced disturbance of the I-Xe system millions of years later and, in the case of one Vigarano chondrule (VS1), complete resetting of the I-Xe system after decay of essentially all 129I, corresponding to an age more than 80 Myr after Shallowater. Our interpretation is that accretion and processing to form the Mokoia and Vigarano parent bodies must have continued for at least 4 Myr and 80 Myr, respectively. The late age of a chondrule that shows no evidence for any aqueous alteration or significant thermal processing after its formation leads us to postulate the existence of an energetic chondrule-forming mechanism at a time when nebular processes are not expected to be important.

  17. Depth localized azimuthal anisotropy from SKS and P receiver functions: The Tien Shan

    NASA Astrophysics Data System (ADS)

    Vinnik, L. P.; Aleshin, I. M.; Kiselev, S. G.; Kosarev, G. L.; Makeyeva, L. I.

    2007-06-01

    Shear wave splitting in the seismic SKS phase provides a unique possibility to judge on deformations at depths inaccessible for direct observations. Fast S wave polarization direction in collisional belts is often parallel to the trend of the belt, although deformations of the mantle lithosphere in low-angle thrusts would lead to the fast polarization direction normal to the trend of the belt. These considerations suggested that the upper mantle in collisional belts is decoupled from the crust. However, SKS technique is notable by a poor depth resolution, and usually it assumes that the fast polarization direction is the same at any depth, which is hard to justify. Here, to investigate depth dependent azimuthal anisotropy in the mantle, we invert jointly P receiver functions and SKS particle motions at a number of seismograph stations. The technique involves azimuthal filtering of the receiver functions and provides a criterion to discriminate between the effects of azimuthal anisotropy and lateral heterogeneity of isotropic medium. A search for the optimum models is conducted with a technique similar to simulated annealing. Testing with synthetics demonstrates that this approach is robust. The results for 10 seismograph stations in the Tien Shan, the world's most active intracontinental collisional belt in Central Asia, reveal a pronounced change in the patterns of azimuthal anisotropy at a depth around 100 km. In the mantle lithosphere (at depths less than 100 km), anisotropy is relatively weak and fast wave polarization direction varies laterally in a broad range. This layer is not necessarily decoupled from the crust: its anisotropy can be a combined effect of present day thrusting and of deformations of the geologic past. In the lower layer (asthenosphere) the average azimuth of fast wave polarization is close to the trend of the belt, whereas magnitude of S wave anisotropy is stable and large (between 5 and 6 per cent). This anisotropy is a likely result of

  18. Inhibition of metastasis, angiogenesis, and tumor growth by Chinese herbal cocktail Tien-Hsien Liquid

    PubMed Central

    2010-01-01

    Background Advanced cancer is a multifactorial disease that demands treatments targeting multiple cellular pathways. Chinese herbal cocktail which contains various phytochemicals may target multiple dys-regulated pathways in cancer cells and thus may provide an alternative/complementary way to treat cancers. Previously we reported that the Chinese herbal cocktail Tien-Hsien Liguid (THL) can specifically induce apoptosis in various cancer cells and have immuno-modulating activity. In this study, we further evaluated the anti-metastatic, anti-angiogenic and anti-tumor activities of THL with a series of in vitro and in vivo experiments. Methods The migration and invasion of cancer cells and endothelial cells was determined by Boyden chamber transwell assays. The effect of THL on pulmonary metastasis was done by injecting CT-26 colon cancer cells intravenously to syngenic mice. The in vitro and in vivo microvessel formation was determined by the tube formation assay and the Matrigel plug assay, respectively. The in vivo anti-tumor effect of THL was determined by a human MDA-MB-231 breast cancer xenograft model. The expression of metalloproteinase (MMP)-2, MMP-9, and urokinase plasminogen activator (uPA) was measured by gelatin zymography. The expression of HIF-1α and the phosphorylation of ERK1/2 were determined by Western blot. Results THL inhibited the migration and invasion ability of various cancer cells in vitro, decreased the secretion of MMP-2, MMP-9, and uPA and the activity of ERK1/2 in cancer cells, and suppressed pulmonary metastasis of CT-26 cancer cells in syngenic mice. Moreover, THL inhibited the migration, invasion, and tube formation of endothelial cells in vitro, decreased the secretion of MMP-2 and uPA in endothelial cells, and suppressed neovascularization in Matrigel plugs in mice. Besides its inhibitory effect on endothelial cells, THL inhibited hypoxia-induced HIF-1α and vascular endothelial growth factor-A expression in cancer cells. Finally

  19. Autonomous geodynamics of the Pamir-Tien Shan junction zone from seismology data

    NASA Astrophysics Data System (ADS)

    Lukk, A. A.; Shevchenko, V. I.; Leonova, V. G.

    2015-11-01

    The geodynamics of the Tajik Depression, the junction zone of the Pamirs and Tien Shan, is typically considered in the context of plate tectonic concept, which implies intense subhorizontal compression of the zone resulting from the subduction of the Indian and Eurasian lithospheric plates. This convergence has been reliably confirmed by the GPS measurements. However, the joint analysis of the geological structure, seismicity, and geodimeter measurements conducted during a few years at the Garm geodynamical testing site of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, demonstrates a widening of the Tajik Depression instead of its shortening, as should be expected from the subhorizontal compression predominant in the present-day stress-state of this region. This conclusion, together with the data from the other regions, suggests that, along with the plate tectonic mechanisms, there are also other, local, autonomous drivers that contribute to the tectogenesis of this region. Besides, the probable existence of these autonomous sources within the Tajik Depression directly follows from the seismology data. Among them is the crustal spreading within the depression suggested by the seismotectonic displacements in the focal mechanisms of the earthquakes. These displacements are directed in different azimuths off the axial's most subsided part of the depression at a depth of 20-30 km. Above this region the distribution of seismotectonic deformations (STD) is chaotic. This pattern of deformation is barely accounted for by a simple model of subhorizontal compression of the Earth's crust in the region. In our opinion, these features of the seismotectonic deformation in the crust within the studied part of the Tajik Depression is probably associated with the gain in the volume of the rocks due to the inflow of the additional material, which is supplied from the bottom crust or upper mantle by the deep fluids. This increase in the rock volume

  20. Hercynian post-collisional magmatism in the context of Paleozoic magmatic evolution of the Tien Shan orogenic belt

    NASA Astrophysics Data System (ADS)

    Seltmann, Reimar; Konopelko, Dmitry; Biske, Georgy; Divaev, Farid; Sergeev, Sergei

    2011-10-01

    The Hercynian Tien Shan (Tianshan) orogen formed during Late Palaeozoic collision between the Karakum-Tarim and the Kazakhstan paleo-continents. In order to constrain timing of Hercynian post-collisional magmatism, 27 intrusions were sampled for U-Pb zircon dating along a ca. 2000 km - long profile in Uzbekistan and Kyrgyzstan. The samples were dated utilizing sensitive high resolution ion microprobe (SHRIMP-II). The obtained ages, together with previously published age data, allowed the timing of Hercynian post-collisional magmatism to be constrained and interpreted in the context of the Paleozoic magmatic evolution of the region. Apart from Hercynian post-collisional magmatism, two older magmatic episodes have been recognized, and the following sequence of events has been established: (1) approximately 10 Ma after cessation of continuous Caledonian magmatism a number of Late Silurian-Early Devonian intrusions were emplaced in the Middle and Northern Tien Shan terranes between 420 and 390 Ma. The intrusions probably formed in an extensional back arc setting during coeval subduction under the margins of Caledonian Paleo-Kazakhstan continent; (2) the next relatively short Late Carboniferous episode of subduction under Paleo-Kazakhstan was registered in the Kurama range of the Middle Tien Shan. Calc-alkaline volcanics and granitoids with ages 315-300 Ma have distinct metallogenic affinities typical for subduction-related rocks and are not found anywhere outside the Middle Tien Shan terrane west of the Talas-Farghona fault; (3) the Early Permian Hercynian post-collisional magmatism culminated after the closure of the Paleo-Turkestan ocean and affected the whole region across terrane boundaries. The post-collisional intrusions formed within a relatively short time span between 295 and 280 Ma. The model for Hercynian post-collisional evolution suggests that after collision the Tien Shan was affected by trans-crustal strike-slip motions which provided suitable conduits

  1. Results from the 2009 Investigations at the Global Change Observatory "Gottfried Merzbacher" (Tien Shan, Kyrgyz Republic)

    NASA Astrophysics Data System (ADS)

    Häusler, Hermann; Leber, Diethard; Scheibz, Jürgen; Kopecny, Alexander; Wetzel, Hans-Ulrich; Echtler, Helmut; Moldobekov, Bolot

    2010-05-01

    The Global Change Observatory "Gottfried Merzbacher", which was installed near the former confluence of the Southern and Northern Inylchek Glacier, served as a platform for intensive field work in August 2009. "Peremitschka" (meaning "the area between") is a test site in front of the retreating Northern Inylchek Glacier, which regularly is flooded by the increasing glacier-dammed Lake Merzbacher, before it bursts out. Mapping the micro-geomorphology and conducting electrical resistivity tomography (ERT) profiles resulted in a sound interpretation of the surface morphology and of subsurface layers of the Peremitschka plain, which probably is underlain by both, permafrost and dead ice of the retreating Northern Inylchek Glacier. The flat 780 meters long high resolution ERT-profile reveals an undulated multilayer resistivity distribution. The uppermost 3-5 m of the profile show low resistivities ranging from 10 to about 200 ohm.m, indicating fine clastic sediments. In this area the surface of the whole test area is covered by silt and sand, the weathered material from the surrounding hills, which mainly consist of shists and calcareous shists of Upper Silurian to Lower Devonian age (Jamansu-Formation). The second "layer" below this low resistivity zone is characterized by resistivities up to 30.000 ohm.m to the final depth of the profile in approximately 45 m, and probably portraits permafrost overlying dead ice of the retreating Northern Inylchek Glacier. The geophysical measurements enable sound interpretations of the local geomorphology which consequently can be mapped in remote sensing images as flooded plain directly underlain by melting permafrost. Time series analysis of oblique aerial photos and remote sensing images allowed for a detailed reconstruction of the glacier retreat from 1943 to nowadays. It is still under discussion, however, if the Northern Inylchek Glacier surged in the late 1990ies. Compared to other regions in the Tien Shan range the youngest

  2. Evidence for divalent vanadium in Allende CAI fassaite and implications for formation conditions

    SciTech Connect

    Sutton, S.R.; Simon, S.; Grossman, L.; Delaney, J.S.; Beckett, J.; Newville, M.; Eng, P.; Rivers, M.L.

    2005-04-22

    Fassaite, a Ti-rich, Al-rich clinopyroxene, is a major mineral in Type B refractory inclusions in carbonaceous chondrites. Stoichiometric treatment of electron microprobe data reveals that Ti{sup 3+}/Ti{sup 4+} is {approx}1 in the fassaite, and experimental work shows that this implies crystallization at fO{sub 2} of {approx}10{sup -19} at 1200 C, very close to the fO{sub 2} of a gas of solar composition. Many fassaite grains are strongly zoned in Ti, whose abundance decreases from core to rim, probably as a result of the compatibility of Ti{sup 3+} in fassaite during crystallization of the molten Ca-rich, Al-rich inclusions (CAIs). Superimposed on these profiles are zones where Ti and V contents spike upward together, within which the Ti{sup 3+}/Ti{sup 4+} ratio also increases significantly. Because Ti{sup 3+} is more compatible than Ti{sup 4+}, the spikes are thought to be caused by variable fO{sub 2} during crystallization. Thermodynamic calculations show that VO and V{sub 2}O{sub 3} are in equilibrium at approximately the same T-fO{sub 2} conditions as Ti{sup 3+} and Ti{sup 4+}, but whether variable fO{sub 2} can be responsible for the V spikes is unclear, since V{sup 2+} would not be expected to be more compatible than V{sup 3+} in clinopyroxene. We report here on our initial results from using x-ray absorption near edge structure (XANES) spectroscopy to determine the oxidation state of V in the zoned Allende fassaite and synthetic pyroxene. The ultimate goal is to place constraints on the oxygen fugacity history of the nebular environment during the crystallization of individual fassaite grains by also determining the pyroxene/liquid partitioning behavior of V as a function of oxidation state.

  3. An investigative study into the effectiveness of using computer-aided instruction (CAI) as a laboratory component of college-level biology: A case study

    NASA Astrophysics Data System (ADS)

    Barrett, Joan Beverly

    Community colleges serve the most diverse student populations in higher education. They consist of non-traditional, part-time, older, intermittent, and mobile students of different races, ethnic backgrounds, language preferences, physical and mental abilities, and learning style preferences. Students who are academically challenged may have diverse learning characteristics that are not compatible with the more traditional approaches to the delivery of instruction. With this need come new ways of solving the dilemma, such as Computer-aided Instruction (CAI). This case study investigated the use of CAI as a laboratory component of college-level biology in a small, rural community college setting. The intent was to begin to fill a void that seems to exist in the literature regarding the role of the faculty in the development and use of CAI. In particular, the investigator was seeking to understand the practice and its effectiveness, especially in helping the under prepared student. The case study approach was chosen to examine a specific phenomenon within a single institution. Ethnographic techniques, such as interviewing, documentary analysis, life's experiences, and participant observations were used to collect data about the phenomena being studied. Results showed that the faculty was primarily self-motivated and self-taught in their use of CAI as a teaching and learning tool. The importance of faculty leadership and collegiality was evident. Findings showed the faculty confident that expectations of helping students who have difficulties with mathematical concepts have been met and that CAI is becoming the most valuable of learning tools. In a traditional college classroom, or practice, time is the constant (semesters) and competence is the variable. In the CAI laboratory time became the variable and competence the constant. The use of CAI also eliminated hazardous chemicals that were routinely used in the more traditional lab. Outcomes showed that annual savings

  4. Shear velocity model for the Kyrgyz Tien Shan from joint inversion of receiver function and surface wave data

    NASA Astrophysics Data System (ADS)

    Gilligan, Amy; Roecker, Steven W.; Priestley, Keith F.; Nunn, Ceri

    2014-10-01

    The Tien Shan is the largest active intracontinental orogenic belt on Earth. To better understand the processes causing mountains to form at great distances from a plate boundary, we analyse passive source seismic data collected on 40 broad-band stations of the MANAS project (2005-2007) and 12 stations of the permanent KRNET seismic network to determine variations in crustal thickness and shear wave speed across the range. We jointly invert P- and S-wave receiver functions with surface wave observations from both earthquakes and ambient noise to reduce the ambiguity inherent in the images obtained from the techniques applied individually. Inclusion of ambient noise data improves constraints on the upper crust by allowing dispersion measurements to be made at shorter periods. Joint inversion can also reduce the ambiguity in interpretation by revealing the extent to which various features in the receiver functions are amplified or eliminated by interference from multiples. The resulting wave speed model shows a variation in crustal thickness across the range. We find that crustal velocities extend to ˜75 km beneath the Kokshaal Range, which we attribute to underthrusting of the Tarim Basin beneath the southern Tien Shan. This result supports the plate model of intracontinental convergence. Crustal thickness elsewhere beneath the range is about 50 km, including beneath the Naryn Valley in the central Tien Shan where previous studies reported a shallow Moho. This difference apparently is the result of wave speed variations in the upper crust that were not previously taken into account. Finally, a high velocity lid appears in the upper mantle of the Central and Northern part of the Tien Shan, which we interpret as a remnant of material that may have delaminated elsewhere under the range.

  5. Evidence for an early nitrogen isotopic evolution in the solar nebula from volatile analyses of a CAI from the CV3 chondrite NWA 8616

    NASA Astrophysics Data System (ADS)

    Füri, Evelyn; Chaussidon, Marc; Marty, Bernard

    2015-03-01

    Nitrogen and noble gas (Ne-Ar) abundances and isotope ratios, determined by CO2 laser extraction static mass spectrometry analysis, as well as Al-Mg and O isotope data from secondary ion mass spectrometry (SIMS) analyses, are reported for a type B calcium-aluminum-rich inclusion (CAI) from the CV3 chondrite NWA 8616. The high (26Al/27Al)i ratio of (5.06 ± 0.50) × 10-5 dates the last melting event of the CAI at 39-99+109ka after "time zero", limiting the period during which high-temperature exchanges between the CAI and the nebular gas could have occurred to a very short time interval. Partial isotopic exchange with a 16O-poor reservoir resulted in Δ17O > -5‰ for melilite and anorthite, whereas spinel and Al-Ti-pyroxene retain the inferred original 16O-rich signature of the solar nebula (Δ17O ⩽ -20‰). The low 20Ne/22Ne (⩽0.83) and 36Ar/38Ar (⩽0.75) ratios of the CAI rule out the presence of any trapped planetary or solar noble gases. Cosmogenic 21Ne and 38Ar abundances are consistent with a cosmic ray exposure (CRE) age of ∼14 to 20 Ma, assuming CR fluxes similar to modern ones, without any evidence for pre-irradiation of the CAI before incorporation into the meteorite parent body. Strikingly, the CAI contains 1.4-3.4 ppm N with a δ15N value of +8‰ to +30‰. Even after correcting the measured δ15N values for cosmogenic 15N produced in situ, the CAI is highly enriched in 15N compared to the protosolar nebula (δ15NPSN = -383 ± 8‰; Marty et al., 2011), implying that the CAI-forming region was contaminated by 15N-rich material within the first 0.15 Ma of Solar System history, or, alternatively, that the CAI was ejected into the outer Solar System where it interacted with a 15N-rich reservoir.

  6. Hydrothermal origin of hexagonal CaAl2Si2O8 (dmisteinbergite) in a compact type A CAI from the Northwest Africa 2086 CV3 chondrite

    NASA Astrophysics Data System (ADS)

    Fintor, Krisztian; Park, Changkun; Nagy, Szabolcs; Pál-Molnár, Elemér; Krot, Alexander N.

    2014-05-01

    We report an occurrence of hexagonal CaAl2Si2O8 (dmisteinbergite) in a compact type A calcium-aluminum-rich inclusion (CAI) from the CV3 (Vigarano-like) carbonaceous chondrite Northwest Africa 2086. Dmisteinbergite occurs as approximately 10 μm long and few micrometer-thick lath-shaped crystal aggregates in altered parts of the CAI, and is associated with secondary nepheline, sodalite, Ti-poor Al-diopside, grossular, and Fe-rich spinel. Spinel is the only primary CAI mineral that retained its original O-isotope composition (Δ17O ~ -24‰); Δ17O values of melilite, perovskite, and Al,Ti-diopside range from -3 to -11‰, suggesting postcrystallization isotope exchange. Dmisteinbergite, anorthite, Ti-poor Al-diopside, and ferroan olivine have 16O-poor compositions (Δ17O ~ -3‰). We infer that dmisteinbergite, together with the other secondary minerals, formed by replacement of melilite as a result of fluid-assisted thermal metamorphism experienced by the CV chondrite parent asteroid. Based on the textural appearance of dmisteinbergite in NWA 2086 and petrographic observations of altered CAIs from the Allende meteorite, we suggest that dmisteinbergite is a common secondary mineral in CAIs from the oxidized Allende-like CV3 chondrites that has been previously misidentified as a secondary anorthite.

  7. 2.5D Full Waveform Inversion of Teleseismic Body and Surface Waves in the Tien Shan

    NASA Astrophysics Data System (ADS)

    Baker, B. I.; Roecker, S. W.

    2013-12-01

    The Tien Shan is the best contemporary example of intracontinental shortening resulting from continental collision, a process believed to have been significant in the evolution of a number of ancient orogens. Previous tomographic studies of the Tien Shan implicate structures in the crust and upper mantle as key to understanding the dynamics of the region. In this study we apply recently developed full waveform inversion (FWI) techniques to passive data collected by the linear dense MANAS array between 2005 to 2007 in order to obtain higher resolution images of lateral heterogeneity beneath the Tien Shan than have previously been available. Our technique is an extension of that proposed by Roecker et al (2010); specifically the forward problem can now account for topographic features with a new 2.5D p-adaptive finite element solver. We incorporate a method developed by Bielak et. al. (2003) to input an appropriate force distribution to accommodate sources external to our model. The p-adaptivity allows us to suit element size to expected resolution as a function of depth and reduce the number of variables in inversion. Consequently, we can now explicitly calculate Frechet derivatives and generate the corresponding Gauss-Newton form with a model covariance regularization matrix all for modest additional computational expense. In order to take advantage of the complimentary sensitivities of different kinds of observations, we simultaneously invert fundamental mode Rayleigh waves and teleseismic P-wave coda. Our strategy is a multiscale approach by which we fit the longer period surface waves first followed by inclusion of body wave data.

  8. Thermal maturity patterns (CAI and %R) in the Ordovician and Devonian rocks of the Appalachian basin in Pennsylvania

    USGS Publications Warehouse

    Repetski, John E.; Ryder, Robert T.; Harper, John A.; Trippi, Michael H.

    2002-01-01

    The objective of this study is to enhance existing thermal maturity maps in Pennsylvania by establishing: 1) new subsurface CAI data points for the Ordovician and Devonian and 2) new %Ro and Rock Eval subsurface data points for Middle and Upper Devonian black shale units. Thermal maturity values for the Ordovician and Devonian strata are of major interest because they contain the source rocks for most of the oil and natural gas resources in the basin. Thermal maturity patterns of the Middle Ordovician Trenton Group are evaluated here because they closely approximate those of the overlying Ordovician Utica Shale that is believed to be the source rock for the regional oil and gas accumulation in Lower Silurian sandstones (Ryder and others, 1998) and for natural gas fields in fractured dolomite reservoirs of the Ordovician Black River-Trenton Limestones. Improved CAI-based thermal maturity maps of the Ordovician are important to identify areas of optimum gas generation from the Utica Shale and to provide constraints for interpreting the origin of oil and gas in the Lower Silurian regional accumulation and Ordovician Black River-Trenton fields. Thermal maturity maps of the Devonian will better constrain burial history-petroleum generation models of the Utica Shale, as well as place limitations on the origin of regional oil and gas accumulations in Upper Devonian sandstone and Middle to Upper Devonian black shale.

  9. Thermal maturity patterns in the Ordovician and Devonian of Pennsylvania using conodont color alteration index (CAI) and vitrinite reflectance (%Ro)

    USGS Publications Warehouse

    Repetski, J.E.; Ryder, R.T.; Harper, J.A.; Trippi, M.H.

    2006-01-01

    This new series of maps enhances previous thermal maturity maps in Pennsylvania by establishing: 1) new subsurface CAI data points for the Ordovician and Devonian and 2) new %Ro and Rock Eval subsurface data points for Middle and Upper Devonian black shale units. Thermal maturity values for the Ordovician and Devonian strata are of major interest because they contain the source rocks for most of the oil and natural gas resources in the basin. Thermal maturity patterns of the Middle Ordovician Trenton Group are evaluated here because they closely approximate those of the overlying Ordovician Utica Shale that is believed to be the source rock for the regional oil and gas accumulation in Lower Silurian sandstones and for natural gas fields in fractured dolomite reservoirs of the Ordovician Black River-Trenton Limestones. Improved CAI-based thermal maturity maps of the Ordovician are important to identify areas of optimum gas generation from the Utica Shale and to provide constraints for interpreting the origin of oil and gas in the Lower Silurian regional accumulation and Ordovician Black River-Trenton fields. Thermal maturity maps of the Devonian will better constrain burial history-petroleum generation models of the Utica Shale, as well as place limitations on the origin of regional oil and gas accumulations in Upper Devonian sandstone and Middle to Upper Devonian black shale.

  10. Thermal maturity patterns (CAI and %R%) in the Ordovician and Devonian rocks of the Appalachian basin in New York State

    USGS Publications Warehouse

    Weary, David J.; Ryder, Robert T.; Nyahay, Richard

    2000-01-01

    The objective of this study is to enhance existing thermal maturity maps in New York State by establishing: 1) new subsurface CAI data points for the Ordovician and Devonian and 2) new %Ro and Rock Eval subsurface data points for Middle and Upper Devonian black shale units. The thermal maturity of the Ordovician and Devonian rocks is of major interest because they contain the source for most of the unconventional natural gas resources in the basin. Thermal maturity patterns of the Middle Ordovician Trenton Group are evaluated here because they closely approximate those of the overlying Ordovician Utica Shale that is believed to be the source rock for the regional oil and gas accumulation in Lower Silurian sandstones (Jenden and others, 1993; Ryder and others, 1998). Improved CAI-based thermal maturity maps of the Ordovician are important to identify areas of optimum gas generation from the Utica Shale and to provide constraints for interpreting the origin of oil and gas in the Lower Silurian regional accumulation, in particular, its basin-centered part (Ryder, 1998). Thermal maturity maps of the Devonian will better constrain burial history-petroleum generation models of the Utica Shale, as well as place limitations on the origin of regional oil and gas accumulation in Upper Devonian sandstone and Middle to Upper Devonian black shale.

  11. Thermal maturity patterns (CAI and %Ro) in the Ordovician and Devonian rocks of the Appalachian basin in West Virginia

    USGS Publications Warehouse

    Repetski, John E.; Ryder, Robert T.; Avary, Katharine Lee; Trippi, Michael H.

    2005-01-01

    The objective of this study is to enhance existing thermal maturity maps in West Virginia by establishing: 1) new subsurface CAI data points for the Ordovician and Devonian and 2) new %Ro and Rock Eval subsurface data points for Middle and Upper Devonian black shale units. Thermal maturity values for the Ordovician and Devonian strata are of major interest because they contain the source rocks for most of the oil and natural gas resources in the basin. Thermal maturity patterns of the Middle Ordovician Trenton Limestone are evaluated here because they closely approximate those of the overlying Ordovician Utica Shale that is believed to be the source rock for the regional oil and gas accumulation in Lower Silurian sandstones (Ryder and others, 1998) and for natural gas fields in fractured dolomite reservoirs of the Ordovician Black River-Trenton Limestones. Improved CAI-based thermal maturity maps of the Ordovician are important to identify areas of optimum gas generation from the Utica Shale and to provide constraints for interpreting the origin of oil and gas in the Lower Silurian regional accumulation and Ordovician Black River-Trenton fields. Thermal maturity maps of the Devonian will better constrain burial history-petroleum generation models of the Utica Shale, as well as place limitations on the origin of regional oil and gas accumulations in Upper Devonian sandstone and Middle to Upper Devonian black shale.

  12. Evaluation of the Experimental CAI Network (1973-1975) of the Lister Hill National Center for Biomedical Communications, National Library of Medicine. Final Report. No. ED-75-1.

    ERIC Educational Resources Information Center

    Rubin, Martin L.; And Others

    An evaluation was made of the biomedical Computer Assisted Instruction (CAI) Network Experiment, established by the National Library of Medicine in 1973 to test the feasibility of sharing CAI learning materials through a national computer network. The evaluation was designed to assist decision makers in planning a future mechanism for distributing…

  13. Folded Lithospheric Basins in Central Asia: Altai-Sayan and Tien Shan basins in a folding lithosphere

    NASA Astrophysics Data System (ADS)

    Delvaux, Damien; Cloetingh, Sierd; Beekman, Fred; Sokoutis, Dimitrios; Burov, Evguenii; Buslov, Misha; Abdrakhmatov, Kanatbeck

    2014-05-01

    Central Asia is a classic example for continental lithospheric folding. In particular, the Altay-Sayan belt in South-Siberia and the Kyrgyz Tien Shan display a special mode of lithospheric deformation, involving decoupled lithospheric mantle folding and upper crustal folding and faulting. A review of the paleostress data and tectono-stratigraphic evolution of the Kurai-Chuya basin in Siberian Altai, Zaisan basin in Kazakh South Altai and Issyk-Kul basin in Kyrgyz Tien Shan suggests that these basins were initiated in an extensional context and later inverted by a combination of fault-controlled deformation and flexural folding. They deformed by a combination of lithospheric buckling inducing surface tilting, uplift and subsidence, together with upper crustal fault-controlled deformation. They are good examples of Folded Lithospheric Basins (FLB) which typically form in a buckling lithosphere. Their characteristic basin fill and symmetry, inner structure, folding wavelength and amplitude, thermal regime and time frame are examined in relation to basement structure, stress field, strain rate, timing of deformation, and compared to existing modelling results. Both regions of active lithospheric folding have a heterogeneous crust with a long history of accretion-collision, subsequently reactivated as a far-field effect of the Indian-Eurasian collision. Thanks to the youthfulness of the tectonic deformation in this region (peak deformation in late Pliocene - early Pleistocene), the surface expression of lithospheric deformation is well documented by the surface topography and superficial tectonic structures.

  14. Calcium-aluminum-rich inclusions with fractionation and unidentified nuclear effects (FUN CAIs): II. Heterogeneities of magnesium isotopes and 26Al in the early Solar System inferred from in situ high-precision magnesium-isotope measurements

    NASA Astrophysics Data System (ADS)

    Park, Changkun; Nagashima, Kazuhide; Krot, Alexander N.; Huss, Gary R.; Davis, Andrew M.; Bizzarro, Martin

    2017-03-01

    Calcium-aluminum-rich inclusions with isotopic mass fractionation effects and unidentified nuclear isotopic anomalies (FUN CAIs) have been studied for more than 40 years, but their origins remain enigmatic. Here we report in situ high precision measurements of aluminum-magnesium isotope systematics of FUN CAIs by secondary ion mass spectrometry (SIMS). Individual minerals were analyzed in six FUN CAIs from the oxidized CV3 carbonaceous chondrites Axtell (compact Type A CAI Axtell 2271) and Allende (Type B CAIs C1 and EK1-4-1, and forsterite-bearing Type B CAIs BG82DH8, CG-14, and TE). Most of these CAIs show evidence for excess 26Mg due to the decay of 26Al. The inferred initial 26Al/27Al ratios [(26Al/27Al)0] and the initial magnesium isotopic compositions (δ26Mg0) calculated using an exponential law with an exponent β of 0.5128 are (3.1 ± 1.6) × 10-6 and 0.60 ± 0.10‰ (Axtell 2271), (3.7 ± 1.5) × 10-6 and -0.20 ± 0.05‰ (BG82DH8), (2.2 ± 1.1) × 10-6 and -0.18 ± 0.05‰ (C1), (2.3 ± 2.4) × 10-5 and -2.23 ± 0.37‰ (EK1-4-1), (1.5 ± 1.1) × 10-5 and -0.42 ± 0.08‰ (CG-14), and (5.3 ± 0.9) × 10-5 and -0.05 ± 0.08‰ (TE) with 2σ uncertainties. We infer that FUN CAIs recorded heterogeneities of magnesium isotopes and 26Al in the CAI-forming region(s). Comparison of 26Al-26Mg systematics, stable isotope (oxygen, magnesium, calcium, and titanium) and trace element studies of FUN and non-FUN igneous CAIs indicates that there is a continuum among these CAI types. Based on these observations and evaporation experiments on CAI-like melts, we propose a generic scenario for the origin of igneous (FUN and non-FUN) CAIs: (i) condensation of isotopically normal solids in an 16O-rich gas of approximately solar composition; (ii) formation of CAI precursors by aggregation of these solids together with variable abundances of isotopically anomalous grains-possible carriers of unidentified nuclear (UN) effects; and (iii) melt evaporation of these precursors

  15. The contribution of the androgen receptor (AR) in human spatial learning and memory: A study in women with complete androgen insensitivity syndrome (CAIS).

    PubMed

    Mueller, S C; Verwilst, T; Van Branteghem, A; T'Sjoen, G; Cools, M

    2016-02-01

    Few studies have examined the impact of androgen insensitivity on human spatial learning and memory. In the present study, we tested 11 women with complete androgen insensitivity syndrome (CAIS), a rare genetic disorder characterized by complete absence of AR activity, and compared their performance against 20 comparison males and 19 comparison females on a virtual analog of the Morris Water Maze task. The results replicated a main sex effect showing that men relative to women were faster in finding the hidden platform and had reduced heading error. Furthermore, findings indicated that mean performance of women with CAIS was between control women and control men, though the differences were not statistically significant. Effect size estimates (and corresponding confidence intervals) of spatial learning trials showed little difference between women with CAIS and control women but CAIS women differed from men, but not women, on two variables, latency to find the platform and first-move latency. No differences between groups were present during visible platform trials or the probe trial, a measure of spatial memory. Moreover, groups also did not differ on estimates of IQ and variability of performance. The findings are discussed in relation to androgen insensitivity in human spatial learning and memory.

  16. An Evaluation of the Cognitive and Affective Performance of an Integrated Set of CAI Materials in the Principles of Macroeconomics. Studies in Economic Education, No. 4.

    ERIC Educational Resources Information Center

    Daellenbach, Lawrence A.; And Others

    The purpose of this study was to determine the effect of computer assisted instruction (CAI) on the cognitive and affective development of college students enrolled in a principles of macroeconomics course. The hypotheses of the experiment were stated as follows: In relation to the traditional principles course, the experimental treatment will…

  17. Dynamics of intracontinental convergence between the western Tarim basin and central Tien Shan constrained by centroid moment tensors of regional earthquakes

    NASA Astrophysics Data System (ADS)

    Huang, Guo-chin Dino; Roecker, Steven W.; Levin, Vadim; Wang, Haitao; Li, Zhihai

    2017-01-01

    Among the outstanding tectonic questions regarding the convergence between the Tien Shan and Tarim basin in northwestern China are the manner in which deformation is accommodated within their lithospheres, and the extent that the Tarim lithosphere underthrusts the Tien Shan. In particular, the amount and type of deformation within the Tarim basin is poorly understood. It is also uncertain if the convergence between the Tarim and the Tien Shan takes place mainly along a discrete boundary, or if the Tarim lithosphere simply indents into the Kazach shield, forming the Tien Shan through crustal thickening accommodated by a distributed series of thrust faults. In this study we use hypocentres from published earthquake catalogues and waveforms recorded by regional seismic networks to determine earthquake source parameters through regional centroid moment tensor inversion. The entire dataset consists of 160 earthquakes that occurred between 1969 and 2009 and with moment magnitudes between 3.5 and 7 distributed throughout the central Tien Shan and northwestern Tarim Basin. The estimated focal depths of these earthquakes range from the near-surface to about 44 km. Focal mechanisms throughout much of the Tien Shan indicate active deformation accommodated by thrust faults from at least the upper crust to 30 km depth. South of the Tien Shan, the Jia-shi earthquake sequence within the Tarim basin suggests that both crustal shortening and localized flexure are part of a complicated process involving rotational convergence. Inside the Tarim basin, two earthquakes with thrust faulting mechanisms near the crust-mantle boundary beneath the Bachu uplift imply a brittle rheology of the lower crust. High-angle thrust events occur broadly across the Tien Shan, suggesting that the Tarim lithosphere as a whole is strong and indents into the Kazach shield to create the mountain range.

  18. Dynamics of Intra-Continental Convergence Between the Western Tarim Basin and Central Tien Shan Constrained by Centroid Moment Tensors of Regional Earthquakes

    NASA Astrophysics Data System (ADS)

    Huang, Guo-chin Dino; Roecker, Steven W.; Levin, Vadim; Wang, Haitao; Li, Zhihai

    2016-11-01

    Among the outstanding tectonic questions regarding the convergence between the Tien Shan and Tarim basin in northwestern China are the manner in which deformation is accommodated within their lithospheres, and the extent that the Tarim lithosphere underthrusts the Tien Shan. In particular, the amount and type of deformation within the Tarim basin is poorly understood. It is also uncertain if the convergence between the Tarim and the Tien Shan takes place mainly along a discrete boundary, or if the Tarim lithosphere simply indents into the Kazach shield, forming the Tien Shan through crustal thickening accommodated by a distributed series of thrust faults. In this study we use hypocenters from published earthquake catalogs and waveforms recorded by regional seismic networks to determine earthquake source parameters through regional centroid moment tensor inversion. The entire dataset consists of 160 earthquakes that occurred between 1969 and 2009 and with moment magnitudes between 3.5 and 7 distributed throughout the central Tien Shan and northwestern Tarim Basin. The estimated focal depths of these earthquakes range from the near-surface to about 44 km. Focal mechanisms throughout much of the Tien Shan indicate active deformation accommodated by thrust faults from at least the upper crust to 30 km depth. South of the Tien Shan, the Jia-shi earthquake sequence within the Tarim basin suggests that both crustal shortening and localized flexure are part of a complicated process involving rotational convergence. Inside the Tarim basin, two earthquakes with thrust faulting mechanisms near the crust-mantle boundary beneath the Bachu uplift imply a brittle rheology of the lower crust. High-angle thrust events occur broadly across the Tien Shan, suggesting that the Tarim lithosphere as a whole is strong and indents into the Kazach shield to create the mountain range.

  19. Chronological study of oxygen isotope composition for the solar protoplanetary disk recorded in a fluffy Type A CAI from Vigarano

    NASA Astrophysics Data System (ADS)

    Kawasaki, Noriyuki; Itoh, Shoichi; Sakamoto, Naoya; Yurimoto, Hisayoshi

    2017-03-01

    Fluffy Type A Ca-Al-rich inclusions (CAIs) containing reversely zoned melilite crystals are suggested to be aggregates of direct condensates from solar nebular gas. We conducted an investigation of 26Al-26Mg systematics of a fluffy Type A CAI from Vigarano, named V2-01, with known oxygen isotopic distributions of reversely zoned melilite crystals; we also conducted oxygen isotope measurements of coexisting minerals. Two of six reversely zoned melilite crystals show continuous variations in magnesium isotopic composition, with δ25Mg decreasing along the inferred direction of crystal growth, which supports the idea that they originated through condensation. Petrography suggests that the constituent minerals of V2-01 formed in the following order: first spinel and fassaite enclosed by melilite, then reversely zoned melilite crystals, and spinel and diopside in the Wark-Lovering rim. The spinel enclosed by melilite has 16O-rich compositions (Δ17O ∼ -24‰) and on an Al-Mg evolutionary diagram plots along model isochron with an initial value of (26Al/27Al)0 = (5.6 ± 0.2) × 10-5. The fassaite enclosed by melilite crystals shows variable oxygen isotopic compositions (Δ17O ∼ -12‰ and -17‰) and plots on an isochron with (26Al/27Al)0 = (5.6 ± 0.2) × 10-5. The oxygen isotopic compositions of reversely zoned melilite showed continuous variations in Δ17O along the inferred direction of crystal growth, suggesting that surrounding nebular gas, during the formation of the reversely zoned melilite, changed from 16O-poor (Δ17O values larger than -10‰) to 16O-rich (Δ17O ∼ -25‰). The six reversely zoned melilite crystals show indistinguishable initial 26Al/27Al values with an average (26Al/27Al)0 of (4.7 ± 0.3) × 10-5, which is clearly distinguishable from the value of enclosed spinel and fassaite, indicating a younger formation age than the enclosed spinel and fassaite. The spinel and diopside from the Wark-Lovering rim show 16O-rich compositions (Δ17O

  20. Constraints on the Origin of Chondrules and CAIs from Short-lived and Long-lived Radionuclides

    NASA Technical Reports Server (NTRS)

    Kita, N. T.; Huss, G. R.; Tachibana, S.; Amelin, Y.; Zinner, E.; Nyquist, L. E.; Hutcheon, I. D.

    2004-01-01

    In order to understand the timing of events in the early solar system, we rely on the radio-nuclide-based chronometers applied to materials in primitive meteorites. Because the time scale of early-solar system evolution was on the order of a few million years (Myr), we focus on so-called "short-lived radionuclides" with mean lives of less than 10 Myr (Table 1), as well as on the long-lived U-Pb system where high precision 207Pb-206Pb ages are applied. Note that the validity of some systems as chronometers (e.g., Be-B, Fe-Ni) has yet to be established. We summarize literature data for chondrules and CAIs and discuss how these chronometers constrain formation time scales in the early solar system.

  1. Spectral characteristics of total ozone and temperature vertical distribution over the Issyk Kul lake (Northern Tien Shan)

    NASA Astrophysics Data System (ADS)

    Aref'ev, Vladimir N.; Visheratin, Konstantin N.; Kashin, Felix V.; Kamenogradsky, Nikita Y.; Semyonov, Vladimir K.; Sinyakov, Valeriy P.

    2003-04-01

    The results of long-term measurements of total ozone (TO) obtained during 1979-2001 over Tien Shand at the Issyk Kul (IK) station have been analyzed by the Fourier transform and the wavelet method. The results of the spectral analysis for TO were compared with similar results for the ground surface temperatures. It has been found that the variability of the surface temperature behavior correlates with the TO variations. To study the temperature spectral harmonics variations with altitude the NCER/NCAR data on temperature vertical distributions were used. It was found that within the range of 850-10 mb the temperature spectra behaved differently mainly at the heights less than those of the surrounding mountains, below the polar tropopause and between the polar and tropical topopauses. The peculiarities of TO harmonics for the periods from 15 to 45 months are in higher correlation with the temperature spectral harmonics up to levels of 100-50 mbar.

  2. Repeated large-magnitude earthquakes in a tectonically active, low-strain continental interior: The northern Tien Shan, Kyrgyzstan

    NASA Astrophysics Data System (ADS)

    Landgraf, A.; Dzhumabaeva, A.; Abdrakhmatov, K. E.; Strecker, M. R.; Macaulay, E. A.; Arrowsmith, Jr.; Sudhaus, H.; Preusser, F.; Rugel, G.; Merchel, S.

    2016-05-01

    The northern Tien Shan of Kyrgyzstan and Kazakhstan has been affected by a series of major earthquakes in the late 19th and early 20th centuries. To assess the significance of such a pulse of strain release in a continental interior, it is important to analyze and quantify strain release over multiple time scales. We have undertaken paleoseismological investigations at two geomorphically distinct sites (Panfilovkoe and Rot Front) near the Kyrgyz capital Bishkek. Although located near the historic epicenters, both sites were not affected by these earthquakes. Trenching was accompanied by dating stratigraphy and offset surfaces using luminescence, radiocarbon, and 10Be terrestrial cosmogenic nuclide methods. At Rot Front, trenching of a small scarp did not reveal evidence for surface rupture during the last 5000 years. The scarp rather resembles an extensive debris-flow lobe. At Panfilovkoe, we estimate a Late Pleistocene minimum slip rate of 0.2 ± 0.1 mm/a, averaged over at least two, probably three earthquake cycles. Dip-slip reverse motion along segmented, moderately steep faults resulted in hanging wall collapse scarps during different events. The most recent earthquake occurred around 3.6 ± 1.3 kyr ago (1σ), with dip-slip offsets between 1.2 and 1.4 m. We calculate a probabilistic paleomagnitude to be between 6.7 and 7.2, which is in agreement with regional data from the Kyrgyz range. The morphotectonic signals in the northern Tien Shan are a prime example of deformation in a tectonically active intracontinental mountain belt and as such can help understand the longer-term coevolution of topography and seismogenic processes in similar structural settings worldwide.

  3. Models of fluid saturated zones according magnetotellurics and seismics data on Tien-Shan crust and mantle along transect MANAS

    NASA Astrophysics Data System (ADS)

    Bataleva, E.; Rybin, A.; Batalev, V.; Matyukov, V.

    2009-04-01

    Recognized as one of the highest, youngest, and most active orogenic systems on the Earth the Tien Shan is situated internal to the Eurasian continent. New deep seismic data acquired from 2004 to 2007 constitute an -400 km lithospheric transect located from the northwestern Tarim Basin in China to the northern Tien Shan in Kyrgyzstan. This seismic profile consists of 40 seismic stations "Quanterra" containing STS-2 (Streckeisen, Switzerland) and CMG - 3T (Güralp Systems Ltd) broadband seismic receivers. Registration of the seismic data in each station was conducted with sampling frequency of 40 Hz. Time service based on GPS clock was applied on each station. Average distance between the seismic stations along the profile is 10-15 km. Observations were held on 30 stations in Kyrgyzstan and on 10 of them in China. As a result of seismic investigations wave speeds cross-section was calculated. A 450 km long north-south magnetotelluric profile spanning the Tien Shan from Kazakhstan to western China reveals lateral variations in the resistivity of the Earth crust and mantle lithosphere to depths of 140 km. MT profile consisting of 19 long period MT soundings (20-20,000 s periods) were combined with 30 broadband stations (0.1-1600 s periods). Broadband measurements (0.001-100 s periods) were also acquired at the 14 long period sites in Kazakhstan and Kyrgyzstan. [Bielinski, et al 2003] Conductivity changes of up to one order of magnitude are a result from variations in temperature or composition, or both. Previous magneto telluric (MT) studies [Trapeznikov et al., 1997] partly show that some low velocity layers also have low resistivity, lending support to the fluid hypothesis. Studies of wave speeds reveal sections of the crust that have pronounced low velocity zones in the thicker portions of the crust which are attributed to crustal metasomatism [Ghose et al., 1998] or fluid filled fractures in pervasively deformed rocks [Vinnik et al., 2002]. Comparing an obtained

  4. Isotopic Measurements in CAIs with the Nanosims: Implications to the understanding of the Formation process of Ca, Al-Rich Inclusions

    NASA Technical Reports Server (NTRS)

    Ito, M.; Messenger, S.; Walker, Robert M.

    2007-01-01

    Ca, Al-rich Inclusions (CAIs) preserve evidence of thermal events that they experienced during their formation in the early solar system. Most CAIs from CV and CO chondrites are characterized by large variations in O-isotopic compositions of primary minerals, with spinel, hibonite, and pyroxene being more O-16-rich than melilite and anorthite, with delta 17, O-18 = approx. -40%o (DELTA O-17 = delta O-17 - 0.52 x delta O-18 = approx. - 20%o ). These anomalous compositions cannot be accounted for by standard mass dependent fractionation and diffusive process of those minerals. It requires the presence of an anomalous oxygen reservoir of nucleosynthetic origin or mass independent fractionations before the formation of CAIs in the early solar system. The CAMECA NanoSIMS is a new generation ion microprobe that offers high sensitivity isotopic measurements with sub 100 nm spatial resolution. The NanoSIMS has significantly improved abilities in the study of presolar grains in various kind of meteorites and the decay products of extinct nuclides in ancient solar system matter. This instrument promises significant improvements over other conventional ion probes in the precision isotopic characterization of sub-micron scales. We report the results of our first O isotopic measurements of various CAI minerals from EK1-6-3 and 7R19-1(a) utilizing the JSC NanoSIMS 50L ion microprobe. We evaluate the measurement conditions, the instrumental mass fractionation factor (IMF) for O isotopic measurement and the accuracy of the isotopic ratio through the analysis of a San Carlos olivine standard and CAI sample of 7R19-1(a).

  5. Thermal Maturity Patterns (CAI and %Ro) in Upper Ordovician and Devonian Rocks of the Appalachian Basin: A Major Revision of USGS Map I-917-E Using New Subsurface Collections

    USGS Publications Warehouse

    Repetski, John E.; Ryder, Robert T.; Weary, David J.; Harris, Anita G.; Trippi, Michael H.

    2008-01-01

    The conodont color alteration index (CAI) introduced by Epstein and others (1977) and Harris and others (1978) is an important criterion for estimating the thermal maturity of Ordovician to Mississippian rocks in the Appalachian basin. Consequently, the CAI isograd maps of Harris and others (1978) are commonly used by geologists to characterize the thermal and burial history of the Appalachian basin and to better understand the origin and distribution of oil and gas resources in the basin. The main objectives of our report are to present new CAI isograd maps for Ordovician and Devonian rocks in the Appalachian basin and to interpret the geologic and petroleum resource implications of these maps. The CAI isograd maps presented herein complement, and in some areas replace, the CAI-based isograd maps of Harris and others (1978) for the Appalachian basin. The CAI data presented in this report were derived almost entirely from subsurface samples, whereas the CAI data used by Harris and others (1978) were derived almost entirely from outcrop samples. Because of the different sampling methods, there is little geographic overlap of the two data sets. The new data set is mostly from the Allegheny Plateau structural province and most of the data set of Harris and others (1978) is from the Valley and Ridge structural province, east of the Allegheny structural front.

  6. Three-dimensional velocity structure and earthquake locations beneath the northern Tien Shan of Kyrgyzstan, central Asia

    NASA Astrophysics Data System (ADS)

    Ghose, Sujoy; Hamburger, Michael W.; Virieux, Jean

    1998-02-01

    We used the arrival times of local earthquakes and quarry blasts recorded by the Kyrgyzstan Broadband Network (KNET) to obtain three-dimensional (3-D) P and S wave velocity models of the upper crust beneath an actively deforming mountain front and its associated foreland in the Kyrgyz Tien Shan. The continuous velocity models, described by cubic B spline interpolation of the squared slowness over a regular 3-D grid, were computed by simultaneous inversion of hypocenter and medium parameters. Exact ray tracing was done in the smooth 3-D medium by shooting rays from the sources to the stations by an analytical perturbation method based on the paraxial ray theory. The deduced large, sparse, linear system was solved using the damped, iterative, least squares algorithm LSQR. The stability and resolution of the result was qualitatively tested by two synthetic tests: the spike test and the checkerboard resolution test. We found that the models are well resolved up to a depth of ˜27 km for most parts of our image domain. The P and S wave velocity models are consistent with each other and provide evidence for marked heterogeneity in the upper crustal structure beneath the northern Tien Shan. At shallower depths (<7 km) the sediment-filled foreland is imaged as a relatively lower velocity feature compared to the mountains, which are cored by crystalline basement rocks. In contrast, at midcrustal depths the mountains are underlain by relatively lower velocity materials compared to the foreland. A distinct contrast in velocity structure is also observed between the eastern and western parts of the Kyrgyz Range at midcrustal depths, with the presence of relatively higher velocities toward the east. The seismicity is concentrated near the traces of major active faults and extends deeper beneath the foreland compared to the mountains. The regional compression in the Tien Shan is accommodated along a series of high-angle reverse faults distributed throughout the orogenic system

  7. Upper Paleozoic tectonics in the Tien Shan (Central Asian Orogenic Belt): insight from new structural data (Kyrgyzstan)

    NASA Astrophysics Data System (ADS)

    Jourdon, Anthony; Petit, Carole; Rolland, Yann; Loury, Chloé; Bellahsen, Nicolas; Guillot, Stéphane; Ganino, Clément

    2016-04-01

    Due to successive block accretions, the polarity of structures and tectonic evolution of the Central Asian Orogenic Belt (CAOB) are still a matter of debate. There are several conflicting models about the polarity of subduction during the Paleozoic, the number of microplates and oceanic basins and the timing of tectonic events in Kyrgyz and Chinese Tien Shan. In this study, we propose new structural maps and cross-sections of Middle and South Kyrgyz Tien Shan (MTS and STS respectively). These cross-sections highlight an overall dextral strike-slip shear zone in the MTS and a north verging structure related to south-dipping subduction in the STS. These structures are Carboniferous in age and sealed by Mesozoic and Cenozoic deposits. In detail, the STS exhibits two deformation phases. The first one is characterized by coeval top-to-the north thrusting and top-to-the-South normal shearing at the boundaries of large continental unit that underwent High-Pressure (Eclogite facies) metamorphism. We ascribe this phase to the exhumation of underthrusted passive margin units of the MTS. The second one corresponds to a top to the North nappe stacking that we link to the last collisional events between the MTS and the Tarim block. Later on, during the Late Carboniferous, a major deformation stage is characterized by the deformation of the MTS and its thrusting over the NTS. This deformation occurred on a large dextral shear zone between the NTS and the MTS known as Song-Kul Zone or Nikolaiev Line as a "side effect" of the Tarim/MTS collision. Based on these observations, we propose a new interpretation of the tectonic evolution of the CAOB. The resulting model comprises the underthrusting of the MTS-Kazakh platform beneath the Tarim and its exhumation followed by the folding, shortening and thickening of the internal metamorphic units during the last collisional events which partitioned the deformation between the STS and the MTS. Finally, the docking of the large Tarim Craton

  8. A New Type of Foreign Clast in A Polymict Ureilite: A CAI or AL-Rich Chondrule

    NASA Technical Reports Server (NTRS)

    Goodrich, C. A.; Ross, D. K.; Treiman, A. H.

    2017-01-01

    Introduction: Polymict ureilites are breccias interpreted to represent regolith formed on a ureilitic asteroid [1-3]. They consist of approximately 90-95% clasts of various ureilite types (olivine-pyroxene rocks with Fo 75-95), a few % indigenous feldspathic clasts, and a few % foreign clasts [4-20]. The foreign clasts are diverse, including fragments of H, L, LL and R chondrites, angrites, other achondrites, and dark clasts similar to CC [6,7,9-19]. We report a new type of foreign clast in polymict ureilite DaG 999. Methods: Clast 8 in Dar al Gani (DaG) 999/1 (Museum fur Naturkunde) was discovered during a survey of feldspathic clasts in polymict ureilites [19,20]. It was studied by BEI, EMPA, and X-ray mapping on the JEOL 8530F electron microprobe at ARES, JSC. Petrography and Mineral Compositions: Clast 8 is sub-rounded to irregular in shape, approximately 85 micrometers in diameter, and consists of approximately 68% pyroxene and 32% mesostasis (by area). Part of the pyroxene (top half of clast in Fig. 1a and 2) shows a coarse dendritic morphology; the rest appears massive. Mesostasis may be glassy and contains fine needles/grains of pyroxene. The pyroxene has very high CaO (23.5 wt.%) and Al2O3 (19.7 wt.%), with the formula: (Ca(0.91)Mg(0.63)Fe(0.01)Al(sup VI) (0.38)Cr(0.01)Ti(0.05)1.99 Si2O6. The bulk mesostasis also has very high Al2O3 (approximately 26 wt.%). A bulk composition for the clast was obtained by combining modal abundances with phase compositions (Table 1, Fig. 3). Discussion: The pyroxene in clast 8 has a Ca-Al-(Ti)- rich (fassaitic) composition that is clearly distinct from compositions of pyroxenes in main group ureilites [22] or indigenous feldspathic clasts in polymict ureilites [4-8]. It also has significantly higher Al than fassaite in angrites (up to approximately 12 wt.% [23]), which occur as xenoliths in polymict ureilites. Ca-Al-Ti rich pyroxenes are most commonly found in CAIs, Al-rich chondrules and other types of refractory

  9. Seasonal deuterium excess in a Tien Shan ice core: Influence of moisture transport and recycling in Central Asia

    USGS Publications Warehouse

    Kreutz, K.J.; Wake, C.P.; Aizen, V.B.; DeWayne, Cecil L.; Synal, H.-A.

    2003-01-01

    Stable water isotope (??18O, ??D) data from a high elevation (5100 masl) ice core recovered from the Tien Shan Mountains, Kyrgyzstan, display a seasonal cycle in deuterium excess (d = ??D - 8*??18O) related to changes in the regional hydrologic cycle during 1994-2000. While there is a strong correlation (r2 = 0.98) between ??18O and ??D in the ice core samples, the regression slope (6.9) and mean d value (23.0) are significantly different than the global meteoric water line values. The resulting time-series ice core d profile contains distinct winter maxima and summer minima, with a yearly d amplitude of ???15-20???. Local-scale processes that may affect d values preserved in the ice core are not consistent with the observed seasonal variability. Data from Central Asian monitoring sites in the Global Network of Isotopes in Precipitation (GNIP) have similar seasonal d changes. We suggest that regional-scale hydrological conditions, including seasonal changes in moisture source, transport, and recycling in the Caspian/Aral Sea region, are responsible for the observed spatial and temporal d variability.

  10. A unique astigmatic nodal property in misaligned Ritchey-Chrétien telescopes with misalignment coma removed.

    PubMed

    Schmid, Tobias; Thompson, Kevin P; Rolland, Jannick P

    2010-03-01

    We present the aberration field response of Ritchey-Chrétien telescopes, with the aperture stop on the primary mirror, to secondary mirror misalignments. More specifically, we derive a general condition for the geometry of the binodal astigmatic aberration field for a telescope that has been aligned to remove field-constant coma. It has been observed that when the coma caused by secondary mirror misalignments is removed the astigmatic field is typically not symmetric around the periphery, but, significantly, it is always effectively zero on-axis. This observation is a manifestation of binodal astigmatism where one of the astigmatic nodes remains near the field center. Here, we show how the condition to remove field-constant coma simultaneously creates a constraint whereby one of the astigmatic nodes must remain effectively on-axis. This result points to why the alignment of a large telescope based on axial imagery is insufficient and demonstrates exactly the geometry of the remaining misalignment aberration field, which dominates the performance of the telescope, providing insights into more complete alignment approaches.

  11. The disappearance of glaciers in the Tien Shan Mountains in Central Asia at the end of Pleistocene

    NASA Astrophysics Data System (ADS)

    Takeuchi, Nozomu; Fujita, Koji; Aizen, Vladimir B.; Narama, Chiyuki; Yokoyama, Yusuke; Okamoto, Sachiko; Naoki, Kazuhiro; Kubota, Jumpei

    2014-11-01

    Glaciers in Central Asia are among the largest ice masses in the Eurasian continent and have supplied vital water to local inhabitants for thousands of years. The glaciers in this region are generally believed to be remnants of the last deglaciation, however, glacier variability in the central Asian mountains since the Last Glacial Maximum (LGM) has not been well documented. Here, we report an 86.87 m-deep ice core record drilled on an ice cap in the Tien Shan Mountains of Central Asia. Radiocarbon dating of organic soil from the bottom of the ice-core borehole showed that the age of the soil was 12,656 - 12,434 cal years before present, coincident with the beginning of the Younger Dryas cold period (YD). This result indicates that the ice cap did not exist in the Bølling-Allerød period (BA), which was the warm period before the YD, and that the BA climate was significantly warmer than at present. It also indicates that the ice cap has never entirely disappeared in any warm periods throughout the Holocene. We estimated that during the BA its extent was 43% or less of the present glacier coverage in the mountains. Our results suggest that this region at the end of Pleistocene was considerably warmer than at present, and that most of the present glaciers in this region are not relics of the Last Glacial period, but are composed of ice formed during the YD and Holocene.

  12. Source parameters of the major historical earthquakes in the Tien-Shan region from the late 19th to the early 20th century.

    NASA Astrophysics Data System (ADS)

    Kulikova, Galina; Krüger, Frank

    2016-04-01

    The Tien-Shan is one of the largest mountain belts in the world. Its deformation is dominated by intermontane basins bounded by active thrust and reverse faulting. The Tien-Shan mountain belt is characterized by a very high rate of seismicity along its margins as well as within the Tien-Shan interior. The study area of the here presented work, the western part of the Tien-Shan region, is currently seismically active with small and moderate sized earthquakes. However, at the end of 19th beginning of 20th century, this region was struck by a remarkable series of large magnitude (M>7) earthquakes, two of them reached magnitude 8. These large earthquakes occurred before the global digital seismic network was installed and therefore were recorded only by analog seismic instruments. The processing of the analog is complicated especially due to the digitization of the records - a very time-consuming and delicate part. Therefore a special set of techniques is developed and modern methods are adapted for the digitized instrumental data analysis. Here presented study evaluates the impact of large magnitude M>7.0 earthquakes, in the Tien-Shan region, on the overall regional tectonics. It also investigates the accuracy of previously estimated source parameters for those earthquakes, which were mainly based on macroseismic observations, and re-estimate them based on the instrumental data. Ten strongest and most interesting historical earthquakes in Tien-Shan region are analyzed with in presented work. With the developed techniques, the source parameters of these major earthquakes are determined and their impact on the regional tectonics was investigated. The large magnitudes of the earthquakes are confirmed by instrumental data. The focal mechanisms of these earthquakes were determined providing evidence for responsible faults or fault systems.

  13. Underthrusting of Tarim beneath the Tien Shan and deep structure of their junction zone: Main results of seismic experiment along MANAS Profile Kashgar-Song-Köl

    NASA Astrophysics Data System (ADS)

    Makarov, V. I.; Alekseev, D. V.; Batalev, V. Yu.; Bataleva, E. A.; Belyaev, I. V.; Bragin, V. D.; Dergunov, N. T.; Efimova, N. N.; Leonov, M. G.; Munirova, L. M.; Pavlenkin, A. D.; Roecker, S.; Roslov, Yu. V.; Rybin, A. K.; Shchelochkov, G. G.

    2010-03-01

    The results of reflection CMP seismic profiling of the Central Tien Shan in the meridional tract 75-76° E from Lake Song-Köl in Kyrgyzstan to the town of Kashgar in China are considered. The seismic section demonstrating complex heterogeneous structure of the Earth’s crust and reflecting its near-horizontal delamination with vertical and inclined zones of compositional and structural differentiation was constructed from processing of initial data of reflection CMP seismic profiling, earthquake converted-wave method (ECWM), and seismic tomography. The most important is the large zone of underthrusting of the Tarim Massif beneath the Tien Shan.

  14. Tectonically controlled relief evolution in the Northern Tien Shan and Junggar Alatau from the Eocene to the Present

    NASA Astrophysics Data System (ADS)

    Seib, N.; Kley, J.; Voigt, T.; Kober, M.

    2012-04-01

    The Cenozoic Tien Shan and Junggar Alatau mountains developed on the southern part of the Paleozoic Altaid orogen as a far-field effect of the collision of the Indian and Eurasian plates. Highland terrain, active seismicity, and fast GPS-derived motions are evidence of rapid ongoing mountain growth today. Variations in relief energy, hight-to-width ratio of ranges and apatite fission track (AFT) exhumation ages suggest they rose at different times. The strong dissection of the higher ridges (heights of up to 2km), indicates an earlier onset and higher rates of uplift. At the other end of the spectrum are low, little dissected ridges. According to AFT ages, exhumation in the Junggar Range began at 9 Ma (Jolivet et al., 2010), circa 11 Ma in the central Kyrgyz Range (Sobel et al., 2006) and 10 Ma in the Terskey Alatau. An AFT age of the low Sogety range is 77 Ma, suggesting that the Cenozic exhumation of the ridge was insufficient to expose rocks from below c.3 km depth. The synclinal lows between the basement highs preserve Cenozoic strata of Eocene to Quaternary age, probably deposited in a once continuous basin (the Ili Basin) and recording the entire history of Tien Shan uplift. Facies pattern of proximal alluvial fans are strictly related to the recent higher mountain areas in the north and in the south. During Middle Miocene, a large lake developed in the basin center. Up to the Middle Miocene sedimentation was accompanied by normal faulting of small magnitude. The main Cenozoic folding and thrusting occurred after that time and before deposition of the Chorgos formation. Shortening was accommodated by reactivation of inherited basement structures, by a switch to reverse or strike-slip motion on normal faults, and the nucleation of new thrusts. The majority of faults which emplace basement rocks over upper Cenozoic sediments dip steeply at angles of 60-70˚, and some have throws of more than 200 m. They are marked by topographic steps and contrasting morphology

  15. Regional based modeling approach for rainfall-induced debris flows in the continental-climatic Northern Tien Shan (SE Kazakhstan)

    NASA Astrophysics Data System (ADS)

    Fischer, Thomas; Küfmann, Carola; Haas, Florian; Baume, Otfried; Becht, Michael

    2013-04-01

    The high mountain systems of Central Asia (Hindukush, Pamir and Tien Shan) are dominated by continental-climatic conditions. Nevertheless, westerly maritime air circulation and convective rainfalls during the summer season result in high rainfall intensities. In combination with a high availability of unconsolidated material rainfall triggered debris flows are prominent and intensive geomorphologic processes in these mountain areas. The presented study aims to figure out a regional based modeling approach for rainfall-induced debris flow processes based on combination of a disposition model for debris flow starting zones with process-flow models. The investigation area has a size of about 700 square kilometers and is situated in the Northern Tien Shan mountains in SE Kazakhstan (investigation areas: valleys of Prochadnaja, Big Almatinka, Little Almatinka and Left Talgar). The area is characterized by mountain forest zone, alpine meadows and high-alpine glaciated areas with the highest peaks at 4500m. In a first step the disposition (point of process triggering) of actual debris flows was analyzed. Due to different triggering mechanisms, the processes were divided into channel-type and slope-type debris flows. Detailed mapping of actual debris flows initiation areas and a GIS-based geostatistical disposition analysis are used to identify the main geofactor-variables and geofactor combinations which enhance the triggering of rainfall-induced debris flows. It can be shown that both, longtime variable geofactors (such as local geomorphology and hydrology) plays a significant role for triggering debris flows, as well as mid- and short time variable geofactors. Especially actual permafrost distribution and degradation plus glacier retreat comes into the focus of interest. This is most notably for rainfall induced slope-type debris flows which primarily are triggered in the discontinuous and continuous permafrost areas eroding younger unconsolidated material from actual

  16. Active Seismicity and Tectonics in Central Asia from Seismological Data Recorded in the Pamir and Tien Shan Mountain Ranges

    NASA Astrophysics Data System (ADS)

    Sippl, Christian; Schurr, Bernd; Schneider, Felix M.; Yuan, Xiaohui; Mechie, James; Minaev, Vladislav; Abdybachaev, Ulan A.; Gadoev, Mustafo; Oimahmadov, Ilhomjon

    2010-05-01

    Active tectonics in the Pamir mountains in central Asia, the westernmost part of the India-Eurasia collision zone, are controlled by ongoing convergence (about 20 mm/yr), causing substantial crustal shortening and compressional deformation. This leads to high seismicity rates throughout the region. Whereas seismic activity along the rim of the Pamir plateau is mostly compressional and concentrated along the Main Pamir Thrust, the distribution and focal mechanisms of earthquakes in its interior are more diffuse, with extensional events occurring along North-South trending rift zones (Kara Kul, Wachan). Seismicity in the south-western Pamir and in the Hindu Kush features frequent intermediate-depth earthquakes, reaching hypocentral depths of 300 km, which is rare for regions not obviously related to active subduction of oceanic lithosphere. These mantle earthquakes, which are not observed beneath the Himalayas and Tibet further east, form a rather well-defined Wadati-Benioff zone that was readily interpreted as subducted lithosphere present below the current collisional orogen. Earlier seismological studies showed the presence of a northward-dipping lithospheric slab under the Hindu Kush and a southward-dipping one beneath the Pamirs, with a small seismic gap in-between. Different hypotheses concerning the nature of these slabs (oceanic or continental lithosphere) and tectonic geometry in general (two slabs subducting in opposite directions or a single, hugely contorted slab) have been proposed in literature. Political instability in the region in the last two decades hampered on-site studies and field work, leaving many key issues poorly understood. In the framework of the multidisciplinary project TIPAGE (Tien Shan Pamir Geodynamic Programme), for the first time, new field campaigns collecting high quality data have been made possible. Local seismicity in the Pamir and Tien Shan mountain ranges (Tajikistan and Kyrgyzstan) is currently being recorded by a temporary

  17. Seasonal Deuterium Excess in a Tien Shan Ice Core: Influence of Moisture Transport and Recycling in Central Asia

    NASA Astrophysics Data System (ADS)

    Kreutz, K. J.; Wake, C. P.; Aizen, V. B.; Cecil, D.; Green, J.; Synal, H.; Introne, D. S.

    2002-12-01

    Stable water isotope (δ18O, δD) data from a high elevation (5100 masl) ice core recovered from the Tien Shan Mountains, Kyrgyzstan, display a seasonal cycle in deuterium excess (d = δD - 8*δ18O) related to changes in the regional hydrologic cycle during 1994-2000. While there is a strong correlation (r2 = 0.98) between δ18O and δD in the ice core samples, the regression slope (6.9) and mean d value (23.0) are significantly different than the global meteoric water line slope of 8 and global d value of 10. The resulting time-series ice core d profile contains distinct winter maxima and summer minima, with a yearly d amplitude of ~15-20 \\permil. Local-scale processes (i.e., sublimation, partial summer melting, snow formation temperature) that may affect d values preserved in the ice core are not consistent with the observed seasonal variability. Rather, we suggest that regional-scale hydrological conditions, including seasonal changes in moisture source, transport, and recycling in the Caspian/Aral Sea region, are responsible for the observed d variability. Examination of data from the Global Network of Isotopes in Precipitation (GNIP) indicates similar seasonal changes in southwestern Central Asian (Afghanistan and Tajikistan), likely related to moisture supply from the Mediterranean Sea during summer. The two years with the highest d values in the ice core record are 1997 and 1998, suggesting a possible link to ENSO ocean/atmosphere variability. The isotope data presented here provide a basis for interpreting centennial-scale ice core d records currently being developed from the region, and highlight the complexity of time-series isotope records from mid-latitude ice cores.

  18. A twentieth century major soluble ion record of dust and anthropogenic pollutants from Inilchek Glacier, Tien Shan

    NASA Astrophysics Data System (ADS)

    Grigholm, B.; Mayewski, P. A.; Aizen, V.; Kreutz, K.; Aizen, E.; Kang, S.; Maasch, K. A.; Sneed, S. B.

    2017-02-01

    Using a high-resolution ( 18 samples/year) major soluble ion record (Na+, K+, Mg2+, Ca2+, Cl-, NO3-, and SO42-) covering the period 1908-1995 A.D. from the Inilchek Glacier, Tien Shan, Kyrgyzstan, we provide a detailed climate and environmental proxy record for the region. Chemical concentrations, empirical orthogonal function analyses, and noncrustal excess calculations are used to identify natural and potential anthropogenic depositional trends. Dominant dust proxy species (i.e., Ca2+) reveal highest concentrations during the 1950s-1970s, with declining decadal trends through the end of the record. These trends likely reflect decreases in central Asian dust storm activity post-1950, which has been associated with coupled atmospheric circulation variability and anthropogenic activities. Comparison between Ca2+ and ERA-Interim (1979-1995) climate reanalysis data indicates a strong relationship to spring (March-May) geopotential height patterns in northwest China and southern Siberia associated with the Siberian High. Noncrustal contribution (excess) estimates of NO3-, K+, SO42-, and Cl- concentrations suggest discernable anthropogenic inputs began between the 1950s and 1970s, increased into the middle/late 1980s, and declined in the 1990s. Excess trends coincide with Former Soviet Union consumption, production, and emission of fossil fuels and fertilizers, reflecting the rapid growth of agriculture and industry, as well as economic declines in the middle to late 1980s/early 1990s. Excess-Cl- trends reflect timings that coincide with the construction of the Pavlodar Chemical Plant and the military production of Cl2 in Kazakhstan. NOAA Hybrid Single-Particle Lagrangian Integrated Trajectory back trajectory frequency analysis suggests eastern Uzbekistan (e.g., Fergana Valley), Kyrgyzstan, and southern Kazakhstan as the primary pollutant sources to the study region.

  19. New Petrology, Mineral Chemistry and Stable MG Isotope Compositions of an Allende CAI: EK-459-7-2

    NASA Technical Reports Server (NTRS)

    Jeffcoat, C. R.; Kerekgyarto, A. G.; Lapen, T. J.; Righter, M.; Simon, J. I.; Ross, D. K.

    2016-01-01

    Calcium-aluminum-rich inclusions (CAIs) are the key to understanding physical and chemical conditions in the nascent solar nebula. These inclusions have the oldest radiometric ages of solar system materials and are composed of phases that are predicted to condense early from a gas of solar composition. Thus, their chemistry and textures record conditions and processes in the earliest stages of development of the solar nebula. Type B inclusions are typically larger and more coarse grained than other types with substantial evidence that many of them were at least partially molten. Type B inclusions are further subdivided into Type B1 (possess thick melilite mantle) and Type B2 (lack melilite mantle). Despite being extensively studied, the origin of the melilite mantles of Type B1 inclusions remains uncertain. We present petrologic and chemical data for a Type B inclusion, EK-459-7-2, that bears features found in both Type B1 and B2 inclusions and likely represents an intermediate between the two types. Detailed studies of more of these intermediate objects may help to constrain models for Type B1 rim formation.

  20. Lithospheric structure across the central Tien Shan constrained by gravity anomalies and joint inversions of receiver function and Rayleigh wave dispersion

    NASA Astrophysics Data System (ADS)

    Li, Yonghua; Shi, Lei; Gao, Jiayi

    2016-07-01

    Shear wave velocity structure across the central Tien Shan orogeny was generated by jointly inverting Rayleigh wave phase and group velocity with teleseismic P-wave receiver functions at 40 broadband seismic stations. The inferred seismic structure was validated by forward modeling of the complete Bouguer anomaly data. The joint inversion result reveals larger crust thicknesses beneath the Kokshaal (∼68-72 km) and Kyrgyz ranges (∼62-64 km), while other units have crustal thicknesses between 48 and 58 km. A fast velocity layer (Vs = 3.6-3.9 km/s) in the upper crust is found in some seismic stations within the Kazakh Shield. Our models show the presence of high velocity and density layers in the lowermost crust throughout the region, consistent with the presence of mafic/ultramafic lithologies. The large crustal thickness is associated with a thickened mafic layer in the lower crust, indicating that the thickened crust may be partly caused by magmatic underplating. The low velocity and density anomaly in the middle crust, and low upper mantle velocity observed in our model beneath the middle Tien Shan reflect the presence of partial melt in the crust due to the intrusion of hot mantle material. The lack of correlation between Moho depth and topography, together with the gravity results, suggests that the topographic compensation in the central Tien Shan is not confined to the crust. This requires significant support from the mantle to account for the relative high elevation of the middle Tien Shan.

  1. Active thrusting and folding along the northern Tien Shan and Late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan

    NASA Astrophysics Data System (ADS)

    Avouac, Jean-Philippe; Tapponnier, P.; Bai, M.; You, H.; Wang, G.

    1993-04-01

    Geometries and rates of Late Cenozoic thrust faulting and folding along the northern piedmont of the Tien Shan mountain belt, which was the location of the 1906 Manas earthquake, are studied. A flexural foredeep of the Dzungarian basement, filled with up to 11,000 m of sediment, is overthrusted by the 5,000 m northern range of the Tien Shan. The active thrust is found to reach the surface 30 km north of the front range, within a 200-km-long zone of Neogene-Quaternary anticlines. Cenozoic shortening of the folded Dzungarian sediments is estimated to be on the order of 30 km, and the Cenozoic shortening rate is found to have been 3.0 +/- 1.5 mm/yr. Reactivation of the Tien Shan by the collision of India and Asia is determined to have taken place in the early to middle Miocene. This is consistent with the existence of thick late Neogene and Quaternary deposits. Reactivation of the Tien Shan roughly coincides with the great mid-Miocene changes in tectonic regimes, denudation, and sedimentation rates seen in southeast Asia.

  2. Efremovka 101.1: A Primitive CAI with Superrefractory REE Patterns and Enormous Enrichments of Sc, Zr, and Y in Fassaite and Perovskite

    NASA Astrophysics Data System (ADS)

    El Goresy, A.; Zinner, E. K.; Matsunami, S.; Palme, H.; Spettel, B.; Lin, Y.; Nazarov, M.

    1993-07-01

    A fragment (30 mg) consisting of two inclusions (101.1 and 101.2) was separated from the Efremovka (CV3) meteorite. 101.1 is an unusual Type A CAI, whereas 101.2 consists of Cr-spinel and fassaite. INAA of the whole fragment revealed 16% MgO reflecting significant contributions from 101.2. Refractory lithophile elements in the bulk fragment have CI-enrichment factors of ~14 with two times enrichment factors for Ca, Eu, and Yb. CAI 101.1 (1.6 mm) contains more than 90% gehlenitic melilite (Ak(sub)1- Ak(sub)32) in its core. It is surrounded by a 5 layer rim sequence (~40 micrometers thick) consisting of spinel -->Al- diopside + fassaite (<= 0.7% Sc2O3) -->forsterite (Fo(sub)97- Fo(sub)100) --> diopside --> forsterite. Two small complete CAIs with a two layer sequence (diopside + anorthite) are contained within the core. Numerous layered sinuous inclusions presumably rim sequence fragments also consisting of diopside + anorthite, are locally crowded in the core. The melilite core is sprinkled with fassaite, perovskite, FeNi, and OsRu-rich metal blebs. Fassaite grains (<= 30 micrometers) contain enormous concentrations in Sc (up to 12.9% Sc2O3) and Zr (up to 5.4% ZrO2). Fassaite rims around FeNi blebs are rich in V (up to 5.4% V2O3) and are zoned with decreasing Sc-, Zr-, and V-concents from the metal cores to the outer fassaite rims. Sc2O3 and ZrO2 concentrations in fassaite display a positive correlation with a correlation coeffient of 0.88. This coherent behavior is a result of a complex cation substitution involving Mg, Ti, Sc, Zr, and V. A coupled substitution is demonstrated by the excellent linear correlation between Mg^2++Ti^4+(y) and Sc^3++Zr^4++Ti^3++V^3+(x) satisfying the equation y = 0.70-0.66x and having a linear regression coefficient of 0.84. Ti^3+/Ti^tot varies between 0.27 and 1. In contrast to fassaites, perovskites are generally depleted in Sc and Zr and enriched in Y (<=1.4% Y2O3). The assemblage andradite+wollastonite+ Fe^degree/or FeNi metal was

  3. Digestibility and nitrogen retention of diets containing different levels of fibre in local (Mong Cai), F1 (Mong Cai x Yorkshire) and exotic (Landrace x Yorkshire) growing pigs in Vietnam.

    PubMed

    Len, N T; Lindberg, J E; Ogle, B

    2007-08-01

    Total tract digestibility and nitrogen retention of three diets containing different levels of fibre [200, 260 and 320 g/kg neutral detergent fibre (NDF) in dry matter] were determined in three breeds of growing pig at an initial age of approximately 3.5 months. The breeds were local (Mong Cai, MC), F1 crossbred (MC x Yorkshire) and exotic (Landrace x Yorkshire, LY), allocated at random within breed (block) to double 3 x 3 Latin squares. The main fibrous ingredients of the experimental diets were rice bran, cassava residue meal and non-dehulled groundnut cake meal. Digestibility of organic matter (OM), crude protein (CP), NDF, crude fibre, gross energy (GE) and ether extract (EE) decreased as the level of dietary NDF increased (p < 0.001). The r(2) values for the relationship between NDF level and digestibility of OM, CP, GE and EE were 83%, 83%, 80% and 82% respectively. On average, an increase in NDF content of 1% unit resulted in a decrease in OM, CP, GE and EE digestibility of 0.67%, 0.75%, 0.50% and 0.42% units respectively. Digestibility of energy and nutrients was the highest for MC and the lowest for LY (p < 0.01), with intermediate values for F1. There was a negative effect of NDF level on nitrogen (N) retained as a proportion of intake (p < 0.05). Nitrogen retention and utilization were significantly higher (p < 0.001) for LY than for MC and F1 pigs.

  4. Crustal structure of the northern margin of the eastern Tien Shan, China, and its tectonic implications for the 1906 M~7.7 Manas earthquake

    USGS Publications Warehouse

    Wang, Chun-Yong; Yang, Zhu-En; Luo, Hai; Mooney, W.D.

    2004-01-01

    The Tien Shan orogenic belt is the most active intracontinental mountain belt in the world. We describe an 86-km-long N–S-trending deep seismic reflection profile (which passes through the southern Junggar basin) located on the northeastern Tien Shan piedmont. Two distinct anticlines beneath the northern margin of the Tien Shan are clearly imaged in the seismic section. In addition, we have imaged two detachment surfaces at depths of ∼7 and ∼16 km. The detachment surface at 16-km depth corresponds to the main detachment that converges with the steep angle reverse fault (the Junggar Southern Marginal Fault) on which the 1906 M~7.7 Manas earthquake occurred. A 12–14-km-thick sedimentary basin is imaged beneath the southern Junggar basin near Shihezi. The crust beneath the northern margin of the Tien Shan is 50–55-km thick, and decreases beneath the Junggar basin to 40–45-km thick. The crustal image of the deep seismic reflection profile is consistent with models derived from nearby seismic refraction data and Bouguer gravity anomalies in the same region. The faulting associated with the 1906 Manas earthquake also fits within the structural framework imaged by the seismic reflection profile. Present-day micro-seismicity shows a hypocentral depth-distribution between 5 and 35 km, with a peak at 20 km. We hypothesize that the 1906 Manas earthquake initiated at a depth of ∼20 km and propagated upwards, causing northward slip on the sub-horizontal detachments beneath the southern Junggar basin. Thus, in accord with regional geological mapping, the current shortening within the eastern Tien Shan is accommodated both by high-angle reverse faulting and detachment faulting that can be clearly imaged at depth in seismic reflection data.

  5. Crustal structure of the northern margin of the eastern Tien Shan, China, and its tectonic implications for the 1906 M~7.7 Manas earthquake

    NASA Astrophysics Data System (ADS)

    Wang, Chun-Yong; Yang, Zhu-En; Luo, Hai; Mooney, W. D.

    2004-06-01

    The Tien Shan orogenic belt is the most active intracontinental mountain belt in the world. We describe an 86-km-long N-S-trending deep seismic reflection profile (which passes through the southern Junggar basin) located on the northeastern Tien Shan piedmont. Two distinct anticlines beneath the northern margin of the Tien Shan are clearly imaged in the seismic section. In addition, we have imaged two detachment surfaces at depths of ˜7 and ˜16 km. The detachment surface at 16-km depth corresponds to the main detachment that converges with the steep angle reverse fault (the Junggar Southern Marginal Fault) on which the 1906 M~7.7 Manas earthquake occurred. A 12-14-km-thick sedimentary basin is imaged beneath the southern Junggar basin near Shihezi. The crust beneath the northern margin of the Tien Shan is 50-55-km thick, and decreases beneath the Junggar basin to 40-45-km thick. The crustal image of the deep seismic reflection profile is consistent with models derived from nearby seismic refraction data and Bouguer gravity anomalies in the same region. The faulting associated with the 1906 Manas earthquake also fits within the structural framework imaged by the seismic reflection profile. Present-day micro-seismicity shows a hypocentral depth-distribution between 5 and 35 km, with a peak at 20 km. We hypothesize that the 1906 Manas earthquake initiated at a depth of ˜20 km and propagated upwards, causing northward slip on the sub-horizontal detachments beneath the southern Junggar basin. Thus, in accord with regional geological mapping, the current shortening within the eastern Tien Shan is accommodated both by high-angle reverse faulting and detachment faulting that can be clearly imaged at depth in seismic reflection data.

  6. Role of Lithosphere structural inheritance in the localization of intraplate deformation: the example of the Tien Shan (Central Asian Orogenic Belt)

    NASA Astrophysics Data System (ADS)

    Jourdon, Anthony; Le Pourhiet, Laetitia; Petit, Carole; Rolland, Yann

    2016-04-01

    Due to the India-Asia collision, the deformation of the Eurasian continent extends over several thousand kilometers, far away from the Himalayan belt. However, some areas like the Tarim craton are poorly deformed while others, as the Tien Shan belt or Tibet plateau, display large deformation rates. These actively deforming areas correspond to ancient plate boundaries which were previously involved in the construction of large orogenic belts. The Tien Shan is a relevant example to study the role of structural inheritance in the localization of recent deformation because of its Paleozoic tectonic history. Indeed, the Tien Shan has been built during two consecutive orogenies (Caledonian and Variscan) which formed large scale structures (as suture zones) clearly identifiable on the field. These structures are now reworked as active deformation zones where large earthquakes can occur. In order to improve our understanding of the role of this strong structural inheritance on the Cenozoic deformation, this study couples two approaches: 1-A field study which allowed us to identify the major Paleozoic structures, their geometry and the main lithologies involved. Our new findings include the reconnaissance of a transcurrent system in Middle Tien Shan, and a south-dipping structure of the major suture zone of the South Tien Shan/ North Tarim. 2-Based on a reconstruction of the pre-Cenozoic structure geometries, we use the thermomechanical modeling code Ptatin to simulate the lithospheric deformation of the belt depending on the geometry and rheology of inherited structures. Our results show that inherited structures first localize the deformation before that antithetic neoformed structures develop on the outer parts of the belt. This result is consistent with seismologic, seismic and GPS data, which show that the deformation is now localized on the borders of the belt, and especially propagates in the South Tien Shan/ North Tarim boundary along a N-dipping top-to-the South

  7. The Middle AsiaN Active Source (MANAS) Profile: Preliminary Results From A Deep Seismic Transect in the Tien Shan of Kyrgyzstan and China

    NASA Astrophysics Data System (ADS)

    Knapp, J. H.; Roecker, S. W.; Park, S. K.; Schelochkov, G.; He, R.

    2007-12-01

    New near-vertical deep seismic reflection data, acquired during the summer of 2007, constitute an ~350 km lithospheric transect from the northwestern Tarim Basin in China to the central Tien Shan of Kyrgyzstan. Recognized as one of the highest, youngest, and most active orogenic systems on Earth, the Tien Shan are situated internal to the Eurasian continent, removed up to 3000 km from the former plate boundary with the Indian subcontinent. Existing geologic constraints imply that up to 200 km of shortening may have occurred in Late Tertiary to Recent time. Additionally, geologic, topographic, and gravimetric data suggest that continental lithosphere of the Tarim basin may presently be subducting beneath the southern margin of the Tien Shan, in the absence of an oceanic slab. While geodetic measurements document that the Tien Shan currently record about half of the shortening between India and Eurasia, geologic data dictate that active faults are restricted to only several of the individual ranges that make up the mountain belt. Passive-source seismological studies have shown the surprising result that the orogenic crust is thickest (65-70 km) at both the southern and northern margins of the Tien Shan, and thins dramatically to ~35 km within the internal part of the orogen. Key targets of the MANAS (Middle AsiaN Active Source) Profile include (1) the top of the Tarim crust as it descends beneath the southern Tien Shan, (2) an inferred crustal-scale frontal ramp, representing where the continental plate may have broken and is now descending into the upper mantle, (3) the geometry of demonstrably active faults below the shallow depths to which they can be inferred from surface geologic constraints, (4) the topography and seismic reflection signature of the Moho, especially given the unexpected variations in crustal thickness across the orogen, and (5) the significance of both crustal and upper mantle conductivity anomalies previously identified through magnetotelluric

  8. Lithospheric structure across the central Tien Shan constrained by gravity anomalies and joint inversions of receiver function and Rayleigh group velocity data

    NASA Astrophysics Data System (ADS)

    Li, Yonghua; Shi, Lei; Gao, Jiayi

    2016-04-01

    Shear wave velocity structure across the central Tien Shan orogeny was generated by jointly inverting Rayleigh wave phase and group velocity with teleseismic P-wave receiver functions at 40 broad band seismic stations of the MANAS project. The inferred seismic structure was validated by forward modeling of the complete Bouguer anomaly data. The joint inversion result reveals larger crust thicknesses beneath the Kokshaal (~68-72 km) and Kyrgyz ranges (~62-64 km), while other units have crustal thicknesses between 48 and 58 km. A fast velocity layer (Vs = 3.6-3.9 km/s) in the upper crust is found in some seismic stations within the Kazakh Shield. Our models show the presence of high velocity and density layers in the lowermost crust throughout the region, consistent with the presence of mafic/ultramafic lithologies. The large crustal thickness is associated with a thickened mafic layer in the lower crust, indicating that the thickened crust may be partly caused by magmatic underplating. The low velocity and density anomaly in the middle crust, and low upper mantle velocity observed in our model beneath the middle Tien Shan reflects the presence of partial melt in the crust due to the intrusion of hot mantle material. The lack of correlation between Moho depth and topography, together with the gravity results, suggests that the topographic compensation in the central Tien Shan is not confined to the crust. This requires significant support from the mantle to account for the relative high elevation of the middle Tien Shan.

  9. Tomographic image of the crust and upper mantle beneath the western Tien Shan from the MANAS broadband deployment: Possible evidence for lithospheric delamination

    NASA Astrophysics Data System (ADS)

    Zhiwei, Li; Roecker, Steve; Zhihai, Li; Bin, Wei; Haitao, Wang; Schelochkov, Gennady; Bragin, Vitaly

    2009-11-01

    We combine teleseismic P arrival times from the recent MANAS deployment of broadband sensors with P and S arrival times from local events recorded by the GENGHIS deployment and analog observations from the Kyrgyz Institute of Seismology to generate a high resolution (~ 20 km) image of elastic wavespeeds in the crust and upper mantle beneath the western Tien Shan. The total data set consists of 29,006 P and 21,491 S arrivals from 2176 local events recorded at 144 stations along with 5202 P arrivals from 263 teleseismic events recorded at 40 stations. The most significant feature in our image of the mantle beneath the Tien Shan is a pair of large, elongated high wavespeed regions dipping in opposite directions from the near surface to depths of at least 400 km. These regions appear to be continuous and extend upwards to bounding range fronts where the Tarim Basin is being overthrust by the Kokshal range on the south side, and the Kazach shield underthrusts the Kyrgyz range on the north side. While it is tempting to interpret these high wavespeed anomalies as evidence for contemporary subduction of continental lithosphere, such a scenario is difficult to reconcile with both the timing of the orogen and the size of the wavespeed anomaly. We suggest instead that they represent downwelling side-limbs of a lithospheric delamination beneath the central part of the Tien Shan, possibly by siphoning of the bordering continental lithosphere as the central part descends.

  10. CAI Invention Strategies.

    ERIC Educational Resources Information Center

    Rodrigues, Raymond J.; Rodrigues, Dawn

    Prewriting programs using computers fall into two broad categories: interactive and noninteractive. An early example of a noninteractive program is that of Ellen Nold, called "Cinnamon." Its purpose was to present the student with a series of content questions. In answering such questions, the student would be accumulating a set of data…

  11. CAI Applications in Statics.

    ERIC Educational Resources Information Center

    Nelson, Clayton C.; And Others

    1986-01-01

    Describes a statics course developed at Texas A&M University in the engineering curriculum which utilizes computer-assisted instruction. Discusses the organization and management of the team that developed the course, the selection of the hardware and software used, and the implementation model and lesson prototype developed for the course.…

  12. Conodont color alteration index (CAI) map and conodont-based age determinations for the Winchester 30' x 60' Quadrangle and adjacent area, Virginia, West Virginia, and Maryland

    USGS Publications Warehouse

    Harris, Anita G.; Stamm, Nancy R.; Weary, David J.; Repetski, John E.; Stamm, Robert G.; Parker, Ronald A.

    1994-01-01

    Most of the conodont data presented in this report (table 1) were acquired to support 1:100,000-scale geologic mapping of the Winchester 30' X 60' quadrangle by the U.S. Geological Survey (USGS). Conodonts were chosen to provide a biostratigraphic framework for the Upper Cambrian to Mississippian marine carbonate rocks that make up about 25 percent of the Paleozoic strata exposed in the quadrangle (~2,130 m of the approximately 9,450 m) of Paleozoic strata exposed in the quadrangle). Thickness of stratigraphic units are from McDowell (1991), our own measurements, and from many of the stratigraphic reports and geologic maps listed in the references cited. Conodont biostratigraphic and color alteration index (CAI) analyses help identify stratigraphic units and structural discontinuities, particularly in the Upper Cambrian to Middle Ordovician chiefly carbonate rocks of the Shenandoah Valley and North Mountain fault zone. Conodont biofacies analyses provide additional information about the provincial affinities of the conodonts and the depositional environment of the rocks that contain them. Lithostratigraphic, biostratigraphic, paleoenvironmental, and CAI data for all conodont samples are given in table 1.

  13. A link between oxygen, calcium and titanium isotopes in 26Al-poor hibonite-rich CAIs from Murchison and implications for the heterogeneity of dust reservoirs in the solar nebula

    NASA Astrophysics Data System (ADS)

    Kööp, Levke; Davis, Andrew M.; Nakashima, Daisuke; Park, Changkun; Krot, Alexander N.; Nagashima, Kazuhide; Tenner, Travis J.; Heck, Philipp R.; Kita, Noriko T.

    2016-09-01

    PLACs (platy hibonite crystals) and related hibonite-rich calcium-, aluminum-rich inclusions (CAIs; hereafter collectively referred to as PLAC-like CAIs) have the largest nucleosynthetic isotope anomalies of all materials believed to have formed in the solar system. Most PLAC-like CAIs have low inferred initial 26Al/27Al ratios and could have formed prior to injection or widespread distribution of 26Al in the solar nebula. In this study, we report 26Al-26Mg systematics combined with oxygen, calcium, and titanium isotopic compositions for a large number of newly separated PLAC-like CAIs from the Murchison CM2 chondrite (32 CAIs studied for oxygen, 26 of these also for 26Al-26Mg, calcium and titanium). Our results confirm (1) the large range of nucleosynthetic anomalies in 50Ti and 48Ca (our data range from -70‰ to +170‰ and -60‰ to +80‰, respectively), (2) the substantial range of Δ17O values (-28‰ to -17‰, with Δ17O = δ17O - 0.52 × δ18O), and (3) general 26Al-depletion in PLAC-like CAIs. The multielement approach reveals a relationship between Δ17O and the degree of variability in 50Ti and 48Ca: PLAC-like CAIs with the highest Δ17O (∼-17‰) show large positive and negative 50Ti and 48Ca anomalies, while those with the lowest Δ17O (∼-28‰) have small to no anomalies in 50Ti and 48Ca. These observations could suggest a physical link between anomalous 48Ca and 50Ti carriers and an 16O-poor reservoir. We suggest that the solar nebula was isotopically heterogeneous shortly after collapse of the protosolar molecular cloud, and that the primordial dust reservoir, in which anomalous carrier phases were heterogeneously distributed, was 16O-poor (Δ17O ⩾ -17‰) relative to the primordial gaseous (CO + H2O) reservoir (Δ17O < -35‰). However, other models such as CO self-shielding in the protoplanetary disk are also considered to explain the link between oxygen and calcium and titanium isotopes in PLAC-like CAIs.

  14. Spatial variability of recent glacier area changes in the Tien Shan Mountains, Central Asia, using Corona (~ 1970), Landsat (~ 2000), and ALOS (~ 2007) satellite data

    NASA Astrophysics Data System (ADS)

    Narama, Chiyuki; Kääb, Andreas; Duishonakunov, Murataly; Abdrakhmatov, Kanatbek

    2010-03-01

    Geographic variability of the recent changes of glacier coverage in the Tien Shan Mountains, Central Asia, is assessed using Corona KH-4B satellite photographs for 1968-1971, Landsat 7 ETM+data for 1999-2002, and ALOS/PRISM and AVNIR data for 2006-2008. The four mountain regions investigated (Pskem, Ili-Kungöy, At-Bashy, and SE-Fergana) cover several distributed glacierized areas in the Tien Shan Mountain system, a region that is affected by highly variable local precipitation regimes. Over the 30 years investigated between ~ 1970 and ~ 2000, glacier area decreased by 19% in the Pskem region, 12% in the Ili-Kungöy region, 12% in the At-Bashy region, and 9% in the SE-Fergana region. In the last 7 years (~ 2000 to ~ 2007), glacier area shrank by 5% in the Pskem region, 4% in the Ili-Kungöy region, 4% in the At-Bashy region, and 0% in the SE-Fergana region. Glacier behavior has varied markedly in these regions. The most dramatic glacier shrinkage has occurred in the outer ranges of the Tien Shan Mountains. Recent glacier area loss has resulted from rising summer temperatures. Regional differences of glacier-area changes related to local climate conditions, to the altitudinal distribution of glacier areas, and to the relative proportion of glaciers in different size classes. The observed accelerated glacier shrinkage is expected to have two impacts on the more populated outer ranges: 1) water shortages during summer and 2) increased threat from glacier hazards such as glacier lake outburst floods (GLOFs) and ice avalanches.

  15. Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite

    NASA Astrophysics Data System (ADS)

    Han, Jangmi; Brearley, Adrian J.

    2016-06-01

    We have carried out a FIB/TEM study of refractory CAI-like objects in one AOA from the ALHA77307 CO3.0 chondrite. The CAI-like objects in the AOA consist of a zoned sequence with a spinel-rich core through an intergrowth layer of spinel and Al-Ti-rich diopside to a diopside rim. The spinel-rich core consists of polycrystalline aggregates of spinel and ±minor melilite showing equilibrated grain boundary textures. The intergrowth layer contains fine-grained diopside and spinel with minor anorthite with highly curved and embayed grain boundaries. The diopside rim consists of polycrystalline aggregates of diopside. The compositions of pyroxene change significantly outward from Al-Ti-rich diopside in contact with the spinel-rich core to Al-Ti-poor diopside next to the surrounding olivine of the AOA. Overall microstructural and chemical characteristics suggest that the spinel-rich core formed under equilibrium conditions whereas the intergrowth layer is the result of reactions that occurred under conditions that departed significantly from equilibrium. The remarkable changes in formation conditions of the CAI-like objects may have been achieved by transport and injection of refractory objects into a region of a partially-condensed, Ca,Ti-saturated gas which reacted with spinel and melilite to form Al-Ti-rich diopside. Crystallographically-oriented TiO2 nanoparticles decorate the grain boundaries between spinel grains and between spinel and Al-Ti-rich diopside grains. During the disequilibrium back-reaction of spinel with a partially-condensed, Ca,Ti-saturated gas, metastable TiO2 nanoparticles may have condensed by an epitaxial nucleation mechanism and grown on the surface of spinel. These TiO2 nanoparticles are disordered intergrowths of the two TiO2 polymorphs, anatase and rutile. These nanoparticles are inferred to have nucleated as anatase that underwent partial transformation into rutile. The local presence of the TiO2 nanoparticles and intergrowth of anatase and

  16. Paleo-Climate and Glaciological Reconstruction in Central Asia through the Collection and Analysis of Ice Cores and Instrumental Data from the Tien Shan

    SciTech Connect

    Vladimir Aizen; Donald Bren; Karl Kreutz; Cameron Wake

    2001-05-30

    While the majority of ice core investigations have been undertaken in the polar regions, a few ice cores recovered from carefully selected high altitude/mid-to-low latitude glaciers have also provided valuable records of climate variability in these regions. A regional array of high resolution, multi-parameter ice core records developed from temperate and tropical regions of the globe can be used to document regional climate and environmental change in the latitudes which are home to the vase majority of the Earth's human population. In addition, these records can be directly compared with ice core records available from the polar regions and can therefore expand our understanding of inter-hemispheric dynamics of past climate changes. The main objectives of our paleoclimate research in the Tien Shan mountains of middle Asia combine the development of detailed paleoenvironmental records via the physical and chemical analysis of ice cores with the analysis of modern meteorological and hydrological data. The first step in this research was the collection of ice cores from the accumulation zone of the Inylchek Glacier and the collection of meteorological data from a variety of stations throughout the Tien Shan. The research effort described in this report was part of a collaborative effort with the United State Geological Survey's (USGS) Global Environmental Research Program which began studying radionuclide deposition in mid-latitude glaciers in 1995.

  17. Combining Computer Assisted Instruction (CAI) and a Live TV Teacher To Extend Learning Opportunities into the Home. A Learning Productivity Research and Developmental Project of the Research Foundation of the State University of New York and Instructional Systems Inc.

    ERIC Educational Resources Information Center

    Benson, Gregory M., Jr.

    The State University of New York and Instructional Systems, Inc., (ISI) developed a project to combine computer assisted instruction (CAI) and live, interactive videoconferencing with a television teacher, conducted via cable. The project is being pursued by the Syracuse (New York) City School District in conjunction with the State University of…

  18. Cost-Benefit Analysis for ECIA Chapter 1 and State DPPF Programs Comparing Groups Receiving Regular Program Instruction and Groups Receiving Computer Assisted Instruction/Computer Management System (CAI/CMS). 1986-87.

    ERIC Educational Resources Information Center

    Chamberlain, Ed

    A cost benefit study was conducted to determine the effectiveness of a computer assisted instruction/computer management system (CAI/CMS) as an alternative to conventional methods of teaching reading within Chapter 1 and DPPF funded programs of the Columbus (Ohio) Public Schools. The Chapter 1 funded Compensatory Language Experiences and Reading…

  19. An Iron Microprobe Study of Be-B Isotope Systematic in Melilite-Rich CAIs Based on Newly Determined Be/B Relative Sensitivity Factors for Melilitic Glass Standards

    NASA Astrophysics Data System (ADS)

    Fukuda, K.; Fujiya, W.; Hiyagon, H.; Sugiura, N.; Takahata, N.; Sano, Y.

    2016-08-01

    We report relative sensitivity factors for melilitic glasses and Be-B systematics of melilite-rich CAIs in CO, CH and ungrouped C chondrites. The variable 10Be/9Be ratios observed in this study supports 10Be production by local irradiation processes.

  20. JPH-2 INTERACTS WITH Cai-HANDLING PROTEINS AND ION CHANNELS IN DYADS: CONTRIBUTION TO PREMATURE VENTRICULAR CONTRACTION-INDUCED CARDIOMYOPATHY

    PubMed Central

    Jiang, Min; Zhang, Mei; Howren, Maureen; Wang, Yuhong; Tan, Alex; Balijepalli, Ravi C.; Huizar, Jose F.; Tseng, Gea-Ny

    2015-01-01

    Background In a canine model of premature ventricular contraction-induced cardiomyopathy (PVC-CM), Cav1.2 is downregulated and misplaced from t-tubules. Junctophilin-2 (JPH-2) is also downregulated. Objective To understand the role of JPH-2 in PVC-CM, and to probe changes in other proteins involved in dyad structure and function. Methods We quantify t-tubule contents (di-8-ANEPPS fluorescence in live myocytes), examine myocyte ultra-structures (electron microscopy), probe JPH-2 interacting proteins (co-immunoprecipitation), quantify dyad and non-dyad protein levels (immunoblotting), and examine subcellular distributions of dyad proteins (immunofluorescence/confocal microscopy). We also test direct JPH-2 modulation of channel function (vs indirect modulation through dyad formation) using heterologous expression. Results PVC myocytes have reduced t-tubule contents but otherwise normal ultra-structures. Among nineteen proteins examined, only JPH-2, bridging-integrator-1 (BIN-1) and Cav1.2 are highly downregulated in PVC hearts. However, statistical analysis indicates a general reduction of dyad protein levels when JPH-2 is downregulated. Furthermore, several dyad proteins, including Na/Ca exchanger, are missing or shifted from dyads to peripheral surface in PVC myocytes. JPH-2 directly or indirectly interacts with Cai-handling proteins, Cav1.2 and KCNQ1, although not BIN-1 or other scaffolding proteins tested. Expression in mammalian cells, that do not have dyads, confirms direct JPH-2 modulation of ICaL (Cav1.2/Cavβ2) and IKs (KCNQ1/KCNE1). Conclusion JPH-2 is more than a ‘dyad glue’: it can modulate Cai-handling and ion channel function in the dyad region. Downregulation of JPH-2, BIN-1 and Cav1.2 plays a deterministic role in PVC-CM. Dissecting the hierarchical relationship among the three is necessary for the design of therapeutic interventions to prevent the progression of PVC-CM. PMID:26538326

  1. Paleozoic structure of Middle Tien Shan (Kyrgyzstan Central Asian Orogenic Belt): Insights on the polarity and timing of tectonic motions, subductions, and lateral correlations

    NASA Astrophysics Data System (ADS)

    Jourdon, Anthony; Loury, Chloé; Rolland, Yann; Petit, Carole; Bellahsen, Nicolas

    2015-04-01

    The structure and Palaeozoic tectonic evolution in Kyrgyz and Chinese Tien Shan Central Asian Orogenic Belt (CAOB) are still a matter of debate. There are numerous and conflicting models about the polarity of tectonic motions in the Paleozoic, the number of continental blocks and oceanic basins involved and the timing of tectonic events. In this study we propose new maps and structural cross-sections of Middle and South Kyrgyz Tien Shan (TS). These cross-sections allow us to highlight an overall South-verging structure in the Middle TS, with a thick-skin style involving the crystalline basement. This deformation occurred during the Early Carboniferous, and is sealed by an Upper Carboniferous unconformity. We ascribe this structure to an Upper Plate deformation linked to north-dipping subduction below Middle TS. In contrast, the South TS exhibits a north-verging structure, linked to south-dipping subduction, which is evidenced by an accretionary prism, a volcanic arc, and high-pressure rocks (Loury et al., 2015), and is correlated to similar structures in the Chinese TS (e.g., Charvet et al., 2011). Based on these observations, we propose a new interpretation of the tectonic evolution of the Middle and South TS CAOB. The resulting model comprises a long-lived north-dipping subduction of the Turkestan Ocean below the Middle TS-Karazakh Platform and a short-lived south-dipping subduction of a marginal back-arc basin below the Tarim. Consequently, the South TS is interpreted as a rifted block from the Tarim. Finally, the docking of the large Tarim Craton to the CAOB corresponds to a rapid collision phase (320-300 Ma). This put an end to the long-lived Paleozoic subduction history in the CAOB. Charvet, J., Shu, L., et al., 2011. Palaeozoic tectonic evolution of the Tianshan belt, NW China. Science China Earth Sciences, 54, 166-184. Loury, C. , Rolland, Y., Guillot S., Mikolaichuk, A.V., Lanari, P., Bruguier, O., D.Bosch, 2015. Crustal-scale structure of South Tien Shan

  2. Joint Inversion of Receiver Functions and Surface Wave Group Velocities from the MANAS data set to Determine Custal Thickness Variations in theTien Shan

    NASA Astrophysics Data System (ADS)

    Gilligan, A.; Priestley, K. F.; Roecker, S. W.

    2012-12-01

    The Tien Shan is the largest active intracontinental orgogenic belt on the Earth. To better understand the processes causing mountains to form in this location distant from a plate boundary, we analyze passive source seismic data collected on 40 broad band stations of the MANAS project (2005-2007) to determine variations in crustal thickness and wavespeed across the range. The linear MANAS array transects the Tien Shan just to the east of the Talas Fergana fault and extends from the Tarim Basin north over the Kokshal Range and across the Naryn Valley to the Kyrgyz Range and the Kazakh Shield. This data set has a denser station spacing (~10 km) than that available in previous studies. We combine P- and S-wave receiver functions with surface wave observations from both earthquakes and ambient noise analysis to reduce the ambiguity inherent in the images obtained from the techniques applied individually. In particular, fundamental-mode surface-wave dispersion observations are sensitive to absolute wavespeed averages rather than contrasts, while receiver functions are primarily sensitive to wavespeed contrasts and vertically integrated travel times rather than absolute wavespeeds. Moreover, analysis of the ambient noise allows dispersion measurements at shorter periods which improves constraints for the upper crust. We jointly invert P- and S-wave receiver functions, fundamental mode Rayleigh wave group velocity determined from 1.75 years of continuous seismic ambient noise for periods 4-28s, and group velocity data for periods 10-70s from the surface wave study of Acton et al. (2010). The resulting crustal model show a strong variation in the Moho depth across the range. We find the thickest crust (~60 km) beneath the Kokshal range, while that beneath the Naryn Valley, in the middle of the Tien Shan is thin (~45 km) and is of similar thickness to that beneath the Tarim Basin and Kazakh shield. This suggests a lack of crustal shortening, or shortening of a previously

  3. A 'college of astrology and medicine'? Charles V, Gervais Chrétien, and the scientific manuscripts of Maître Gervais's College.

    PubMed

    Boudet, Jean-Patrice

    2010-06-01

    Considered an institution mainly devoted to astrology and medicine by Simon de Phares and by some historians who believe that he was reliable, the college founded in 1371 by Charles V's first physician, Gervais Chrétien, was in fact primarily dedicated to theological students. It was not before 1377 that there were created there two bursaries for scholares regis, specialising in 'licit mathematical sciences', and two medical fellowships. Yet the influence of the activity of these fellows seems to have been rather moderate and-as far as we can learn from the material still extant, notably from manuscripts that belonged to Maître Gervais' College and to some of its members-this institution was devoted much more to theological studies than to medicine and the quadrivium.

  4. Multisegment rupture in the 11 July 1889 Chilik earthquake (Mw 8.0-8.3), Kazakh Tien Shan, interpreted from remote sensing, field survey, and paleoseismic trenching

    NASA Astrophysics Data System (ADS)

    Abdrakhmatov, K. E.; Walker, R. T.; Campbell, G. E.; Carr, A. S.; Elliott, A.; Hillemann, C.; Hollingsworth, J.; Landgraf, A.; Mackenzie, D.; Mukambayev, A.; Rizza, M.; Sloan, R. A.

    2016-06-01

    The 11 July 1889 Chilik earthquake (Mw 8.0-8.3) forms part of a remarkable sequence of large earthquakes in the late nineteenth and early twentieth centuries in the northern Tien Shan. Despite its importance, the source of the 1889 earthquake remains unknown, though the macroseismic epicenter is sited in the Chilik valley, ~100 km southeast of Almaty, Kazakhstan (~2 million population). Several short fault segments that have been inferred to have ruptured in 1889 are too short on their own to account for the estimated magnitude. In this paper we perform detailed surveying and trenching of the ~30 km long Saty fault, one of the previously inferred sources, and find that it was formed in a single earthquake within the last 700 years, involving surface slip of up to 10 m. The scarp-forming event, likely to be the 1889 earthquake, was the only surface-rupturing event for at least 5000 years and potentially for much longer. From satellite imagery we extend the mapped length of fresh scarps within the 1889 epicentral zone to a total of ~175 km, which we also suggest as candidate ruptures from the 1889 earthquake. The 175 km of rupture involves conjugate oblique left-lateral and right-lateral slip on three separate faults, with step overs of several kilometers between them. All three faults were essentially invisible in the Holocene geomorphology prior to the last slip. The recurrence interval between large earthquakes on any of these faults, and presumably on other faults of the Tien Shan, may be longer than the timescale over which the landscape is reset, providing a challenge for delineating sources of future hazard.

  5. Geomorphology and Ice Content of Glacier - Rock Glacier &ndash; Moraine Complexes in Ak-Shiirak Range (Inner Tien Shan, Kyrgyzstan)

    NASA Astrophysics Data System (ADS)

    Bolch, Tobias; Kutuzov, Stanislav; Rohrbach, Nico; Fischer, Andrea; Osmonov, Azamat

    2015-04-01

    Meltwater originating from the Tien Shan is of high importance for the runoff to the arid and semi-arid region of Central Asia. Previous studies estimate a glaciers' contribution of about 40% for the Aksu-Tarim Catchment, a transboundary watershed between Kyrgyzstan and China. Large parts of the Ak-Shiirak Range drain into this watershed. Glaciers in Central and Inner Tien Shan are typically polythermal or even cold and surrounded by permafrost. Several glaciers terminate into large moraine complexes which show geomorphological indicators of ice content such as thermo-karst like depressions, and further downvalley signs of creep such as ridges and furrows and a fresh, steep rock front which are typical indicators for permafrost creep ("rock glacier"). Hence, glaciers and permafrost co-exist in this region and their interactions are important to consider, e.g. for the understanding of glacial and periglacial processes. It can also be assumed that the ice stored in these relatively large dead-ice/moraine-complexes is a significant amount of the total ice storage. However, no detailed investigations exist so far. In an initial study, we investigated the structure and ice content of two typical glacier-moraine complexes in the Ak-Shiirak-Range using different ground penetrating radar (GPR) devices. In addition, the geomorphology was mapped using high resolution satellite imagery. The structure of the moraine-rock glacier complex is in general heterogeneous. Several dead ice bodies with different thicknesses and moraine-derived rock glaciers with different stages of activities could be identified. Few parts of these "rock glaciers" contain also massive ice but the largest parts are likely characterised by rock-ice layers of different thickness and ice contents. In one glacier forefield, the thickness of the rock-ice mixture is partly more than 300 m. This is only slightly lower than the maximum thickness of the glacier ice. Our measurements revealed that up to 20% of

  6. Intraplate mountain building in response to continent continent collision—the Ancestral Rocky Mountains (North America) and inferences drawn from the Tien Shan (Central Asia)

    NASA Astrophysics Data System (ADS)

    Dickerson, Patricia Wood

    2003-04-01

    The intraplate Ancestral Rocky Mountains of western North America extend from British Columbia, Canada, to Chihuahua, Mexico, and formed during Early Carboniferous through Early Permian time in response to continent-continent collision of Laurentia with Gondwana—the conjoined masses of Africa and South America, including Yucatán and Florida. Uplifts and flanking basins also formed within the Laurentian Midcontinent. On the Gondwanan continent, well inboard from the marginal fold belts, a counterpart structural array developed during the same period. Intraplate deformation began when full collisional plate coupling had been achieved along the continental margin; the intervening ocean had been closed and subduction had ceased—that is, the distinction between upper versus lower plates became moot. Ancestral Rockies deformation was not accompanied by volcanism. Basement shear zones that formed during Mesoproterozoic rifting of Laurentia were reactivated and exerted significant control on the locations, orientations, and modes of displacement on late Paleozoic faults. Ancestral Rocky Mountain uplifts extend as far south as Chihuahua and west Texas (28° to 33°N, 102° to 109°W) and include the Florida-Moyotes, Placer de Guadalupe-Carrizalillo, Ojinaga-Tascotal and Hueco Mountain blocks, as well as the Diablo and Central Basin Platforms. All are cored with Laurentian Proterozoic crystalline basement rocks and host correlative Paleozoic stratigraphic successions. Pre-late Paleozoic deformational, thermal, and metamorphic histories are similar as well. Southern Ancestral Rocky Mountain structures terminate along a line that trends approximately N 40°E (present coordinates), a common orientation for Mesoproterozoic extensional structures throughout southern to central North America. Continuing Tien Shan intraplate deformation (Central Asia) has created an analogous array of uplifts and basins in response to the collision of India with Eurasia, beginning in late

  7. Title of abstract - Different approaches to the determining of 3-d P and S wave velocity structures of the crust beneath Northern Tien Shan

    NASA Astrophysics Data System (ADS)

    Kryukova, O.

    2003-04-01

    The seismic images of the crust beneath Northern Tien Shan (NTS) are obtained with using of different sets of data and several algorithms for solution of local earthquake tomography problem. The NTS is a very interesting region from geophysical point if view due to high seismic activity caused by interplate collision: Tien Shan and Kazakh. A rectangular region under investigation is constrained by lines 41.90o N - 43.40o N and 73.50o E- 76.50o E. 14661 P and 14436 S wave arrival times recorded 12 seismic stations of the Kyrgyzstan Broadband Network (KNET) from local earthquake in 1991-1999 years are used. In addition, data from 267 local earthquake recorded over a period of about 20 years by a regional arrays of 93 seismographs in NTS are involved in inversions. 1-d optimal velocity models and stations delays are estimated with help of program VELEST (E.Kissling, 1995). Block parameterization of model and ray tracing described by Thurber and Ellsworth (1980) are used for determination of 3-d velocity structure and relocation of events as one of the approaches (programs S.Roecker Sphypit90 and Sphrel3d). Other approach consists in application linear or cubic B spline interpolation of velocity function and ray tracing Um and Thurber (1987) for the solution of forward problem (program C.Thurber et al. Simulps and own program). The data resolution analysis and statistical analysis of models was carried out. Calculated P wave tomographic models were compared with tomographic models S.Roecker et al. (1993), S.Ghose et al. (1998) and T.Sabitova (1996). The main result is the confirmation of existence of different seismic velocity structure beneath Kyrgyz Range and Chu Basin. Using various sets of date and methods for reconstruction velocity model is effective in reveal of more reliable velocity heterogeneities in the domain of research. The author is grateful to dr. I. Kitov for help and to dr. I.Sanina for useful discussion.

  8. Targeting PML-RARα and Oncogenic Signaling Pathways by Chinese Herbal Mixture Tien-Hsien Liquid in Acute Promyelocytic Leukemia NB4 Cells

    PubMed Central

    Yao, Chih-Jung; Yang, Chia-Ming; Chuang, Shuang-En; Yan, Jiann-Long; Liu, Chun-Yen; Chen, Suz-Wen; Yan, Kun-Huang; Lai, Tung-Yuan; Lai, Gi-Ming

    2011-01-01

    Tien-Hsien Liquid (THL) is a Chinese herbal mixture that has been used worldwide as complementary treatment for cancer patients in the past decade. Recently, THL has been shown to induce apoptosis in various types of solid tumor cells in vitro. However, the underlying molecular mechanisms have not yet been well elucidated. In this study, we explored the effects of THL on acute promyelocytic leukemia (APL) NB4 cells, which could be effectively treated by some traditional Chinese remedies containing arsenic trioxide. The results showed THL could induce G2/M arrest and apoptosis in NB4 cells. Accordingly, the decrease of cyclin A and B1 were observed in THL-treated cells. The THL-induced apoptosis was accompanied with caspase-3 activation and decrease of PML-RARα fusion protein. Moreover, DNA methyltransferase 1 and oncogenic signaling pathways such as Akt/mTOR, Stat3 and ERK were also down-regulated by THL. By using ethyl acetate extraction and silica gel chromatography, an active fraction of THL named as EAS5 was isolated. At about 0.5–1% of the dose of THL, EAS5 appeared to have most of THL-induced multiple molecular targeting effects in NB4 cells. Based on the findings of these multi-targeting effects, THL might be regarding as a complementary and alternative therapeutic agent for refractory APL. PMID:19897545

  9. [Soil microarthropods and macrofauna in monsoon tropical forests of Cat Tien and Bi Dup-Nui Ba National Parks, Southern Vietnam].

    PubMed

    Anichkin, A E; Beliaeva, N V; Dovgobrod, I G; Shveenkova, Iu B; Tiunov, A V

    2007-01-01

    The abundance, biomass, vertical distribution, and taxonomic composition of soil invertebrates (springtails, macrofauna, and termites) were studied in forest formations differing in edaphic and climatic conditions: lowland forests dominated by Lagerstroeomia spp. or Dipterocarpus spp. in the Cat Tien National Park and in a mountain pine (Pinus kesiya) forest on the Da Lat Plateau, southern Vietnam. In the lowland forests, springtails had a relatively low density (10000-12000 ind./m2), but their diversity was high (41-43 species in each forest). The density of large soil invertebrates (without ants and termites) reached 500-700 ind./m2 at a biomass of approximately 30 g/m2 (with earthworms accounting for up to 230 ind./m2 and 19-28 g/m2). Among termites, species of the genera Macrotermes and Odontotermes were dominant. Their total biomass in some areas exceeded 15-20 g/m2. In the mountain pine forest, the total biomass of soil macrofauna was approximately 11 g/m2, the abundance and diversity of springtails were low (7500 ind./m2, 28 species), and wood-destroying species of the genera Schedorhinotermes sp. and Coptotermes sp. dominated among termites.

  10. A Medical Research and Evaluation Facility Defense and Studies Supporting the Medical Chemical Defense Program. Task 95-38: Evaluation of the Vesicating Properties of Neutralized Chemical Agent Identification Set (CAIS) Components.

    DTIC Science & Technology

    1997-06-01

    total of 11 hairless guinea pigs ( HGPs ) were used in this phase with seven or eight sites dosed on each animal. All animals were examined 24 hr...A total of 24 HGPs were used, dosing six to eight sites per animal with a 1 hr duration of exposure. All animals were examined 24 hr following...Change: The "blue" wastestream, that CAIS component containing neat HD neutralized with DCDMH, has been found to cause microvesication in HGPs at

  11. Dietary exposure to aflatoxin B1, ochratoxin A and fuminisins of adults in Lao Cai province, Viet Nam: A total dietary study approach.

    PubMed

    Huong, Bui Thi Mai; Tuyen, Le Danh; Tuan, Do Huu; Brimer, Leon; Dalsgaard, Anders

    2016-12-01

    Aflatoxins, fumonisins and ochratoxin A that contaminate various agricultural commodities are considered of significant toxicity and potent human carcinogens. This study took a total dietary study approach and estimated the dietary exposure of these mycotoxins for adults living in Lao Cai province, Vietnam. A total of 42 composite food samples representing 1134 individual food samples were prepared according to normal household practices and analysed for the three mycotoxins. Results showed that the dietary exposure to aflatoxin B1 (39.4 ng/kg bw/day) and ochratoxin A (18.7 ng/kg bw/day) were much higher than recommended provisional tolerable daily intake (PTDI) values mainly due to contaminated cereals and meat. The exposure to total fumonisins (1400 ng/kg bw/day) was typically lower than the PTDI value (2000 ng/kg bw/day). The estimated risk of liver cancer associated with exposure to aflatoxin B1 was 2.7 cases/100,000 person/year. Margin of exposure (MOE) of renal cancer linked to ochratoxin A and liver cancer associated with fumonisins were 1124 and 1954, respectively indicating risk levels of public health concern. Further studies are needed to evaluate the efficiency of technical solutions which could reduce mycotoxin contamination as well as to determine the health effects of the co-exposure to different types of mycotoxins.

  12. Holocene River Dynamics, Climate Change and Floodwater Farming in the Watersheds of the Pamir and Tien Shan Mountains of Inner Asia

    NASA Astrophysics Data System (ADS)

    Macklin, M. G.; Panyushkina, I. P.; Toonen, W. H. J.

    2014-12-01

    The Ili, Syr Dayra and Amu Dayra rivers of Inner Asia are emerging as critical areas for the development of irrigation-based agriculture in the ancient world. Following research by Russian archaeologists in the 1970s it is evident that these watersheds had flourishing riverine civilizations comparable to those in Mesopotamia and the Indus Valley. But unlike these areas where the relationship between Holocene river dynamics, climate change and floodwater farming is increasingly underpinned by radiometric dating, the alluvial archaeology of Inner Asia is significantly under researched. To address this, a major multi-disciplinary research program was begun in 2011 centred on the Talgar catchment, a south-bank tributary of the Ili river, southeast Kazakhstan. Building on archaeological excavations and surveys conducted over the past 20 years, we have undertaken one of the most detailed investigations of Holocene people-river environment interactions in Inner Asia. River development has been reconstructed over the last 20,000 years and human settlement histories from the Eneolithic to the Medieval period documented. Periods of Holocene river aggradation and high water levels in Lake Balkhash and Aral Sea correspond with cooler and wetter neoglacial episodes while river entrenchment and floodplain soil development are associated with warmer and drier conditions. Floodwater farming in the Talgar river reached its acme in the late Iron Age (400-200 cal. BC) with more than 60 settlement sites and 550 burial mounds. This corresponds to a period of reduced flood flows, river stability and glacier retreat in the Tien Shan headwaters. A new hydroclimatic-based model for the spatial and temporal dynamics of floodwater farming in the Ili, Syr Dayra and Amu Dayra watersheds is proposed, which explains the large scale expansion (down-river) and contraction (up-river) of settlements since the first use of irrigation in the Neolithic through to the late Medieval period.

  13. Mid-twentieth century increases in anthropogenic Pb, Cd and Cu in central Asia set in hemispheric perspective using Tien Shan ice core

    NASA Astrophysics Data System (ADS)

    Grigholm, B.; Mayewski, P. A.; Aizen, V.; Kreutz, K.; Wake, C. P.; Aizen, E.; Kang, S.; Maasch, K. A.; Handley, M. J.; Sneed, S. B.

    2016-04-01

    High-resolution major and trace element (Al, As, Ca, Cd, Co, Cr, Cu, Fe, Li, Mn, Na, Pb, S, Ti, and V) ice core records from Inilchek glacier (5120 m above sea level) on the northwestern margin of the Tibetan Plateau provide the first multi-decadal ice core record spanning the period 1908-1995 AD in central Tien Shan. The trace element records reveal pronounced temporal baseline trends and concentration maxima characteristic of post-1950 anthropogenic emissions. Examination of Pb, Cd and Cu concentrations, along with non-crustal calculation estimates (i.e. excess (ex) and enrichment factor (EF)), reveal that discernable anthropogenic inputs began during the 1950s and rapidly increased to the late-1970s and early 1980s, by factors up to of 5, 6 and 3, respectively, relative to a 1910-1950 means. Pb, Cd and Cu concentrations between the 1950s-1980s are reflective of large-scale Soviet industrial and agricultural development, including the growth of production and/or consumption of the non-ferrous metals, coal and phosphate fertilizers. NOAA HYSPLIT back-trajectory frequency analysis suggests pollutant sources originating primarily from southern Kazakhstan (e.g. Shymkent and Balkhash) and the Fergana Valley (located in Kazakhstan, Uzbekistan and Kyrgyzstan). Inilchek ice core Pb, Cd and Cu reveals declines during the 1980s concurrent with Soviet economic declines, however, due to the rapid industrial and agricultural growth of western China, Pb, Cd and Cu trends increase during the 1990s reflecting a transition from primarily central Asian sources to emission sources from western China (e.g. Xinjiang Province).

  14. Thermal and chemical evolution in the early Solar System as recorded by FUN CAIs: Part II - Laboratory evaporation of potential CMS-1 precursor material

    NASA Astrophysics Data System (ADS)

    Mendybaev, Ruslan A.; Williams, Curtis D.; Spicuzza, Michael J.; Richter, Frank M.; Valley, John W.; Fedkin, Alexei V.; Wadhwa, Meenakshi

    2017-03-01

    We present the results of laboratory experiments in which a forsterite-rich melt estimated to be a potential precursor of Allende CMS-1 FUN CAI was evaporated into vacuum for different lengths of time at 1900 °C. The evaporation of this melt resulted in residues that define trajectories in chemical as well as magnesium, silicon and oxygen isotopic composition space and come very close to the measured properties of CMS-1. The isotopic composition of the evaporation residues was also used to determine the kinetic isotopic fractionation factors [α2,1 (vapor-melt) defined as the ratio of isotopes 2 and 1 of a given element in the evaporating gas divided by their ratio in the evaporating source] for evaporation of magnesium (α25,24 for 25Mg/24Mg), silicon (α29,28 for 29Si/28Si) and oxygen (α18,16 for 18O/16O) from the forsterite-rich melt at 1900 °C. The values of α25,24 = 0.98383 ± 0.00033 and α29,28 = 0.99010 ± 0.00038 are essentially independent of change in the melt composition as evaporation proceeds. In contrast, α18,16 changes from 0.9815 ± 0.0016 to ∼0.9911 when the residual melt composition changes from forsteritic to melilitic. Using the determined values of α25,24 and α29,28 and present-day bulk chemical composition of the CMS-1, the composition of the precursor of the inclusion was estimated to be close to the clinopyroxene + spinel + forsterite assemblage condensed from a solar composition gas. The correspondence between the chemical composition and isotopic fractionation of experimental evaporation residues and the present-day bulk chemical and isotopic compositions of CMS-1 is evidence that evaporation played a major role in the chemical evolution of CMS-1.

  15. Geology, mineralization, and fluid inclusion characteristics of the Kumbel oxidized W-Cu-Mo skarn and Au-W stockwork deposit in Kyrgyzstan, Tien Shan

    NASA Astrophysics Data System (ADS)

    Soloviev, Serguei G.

    2015-02-01

    The Kumbel deposit is located within a metallogenic belt of W-Mo, Cu-Mo, Au-W, and Au deposits along the Late Paleozoic active continental margin of Tien Shan. The deposit is related to a Late Carboniferous multiphase pluton, with successive intrusive phases from early olivine monzogabbro through monzonite-quartz monzonite to granodiorite and granite, with the latest monzogabbro-porphyry dikes. The deposit represents an example of a complex W-Cu-Mo-Au magmatic-hydrothermal system related to magnetite-series high-K calc-alkaline to shoshonitic igneous suite. It contains large bodies of W-Cu-Mo oxidized prograde and retrograde skarns, with abundant andradite garnet, magnetite, and especially hematite, as well as K-feldspar, molybdoscheelite, chalcopyrite, and molybdenite, with transitions to zones of intense quartz-K-feldspar (with minor andradite and hematite) veining. The skarns are cut by quartz-carbonate ± adularia ± sericite veins (locally sheeted) and stockworks bearing scheelite and minor Cu, Zn, Pb sulfides, as well as Au, Bi, Te, and As mineralization. The association of these veins with the oxidized skarns and magnetite-series intrusion is consistent with the general oxidized, intrusion-related W-Mo-Cu-Au type of deposit, with an affinity to the alkalic (silica-saturated) Cu-Au ± Mo porphyry deposits. The fluid inclusion data show the predominance of magmatic-hydrothermal aqueous chloride fluid during the formation of skarns and quartz-carbonate-scheelite-sulfide veins. The high fluid pressures (˜1,750 bars), together with their high temperature (up to 600 °C) and high salinity (˜50-60 wt% NaCl-equiv.), suggest the formation of skarns and quartz-K-feldspar-andradite-hematite veins under conditions typical of magmatic-hydrothermal transition (depth of ≥4-5 km) of intrusion-related mineralized system, possibly by exsolution of the fluids from crystallizing magma. The auriferous quartz-carbonate-scheelite-sulfide veins formed from high to moderate

  16. Atmospheric circulation patterns and geochemistry time series from ice/firn cores and snow samples of central Asian glaciers (Pamir, Tien Shan and Altai).

    NASA Astrophysics Data System (ADS)

    Aizen, E. M.; Aizen, V. B.; Joswiak, D. R.; Mayewski, P. A.

    2008-12-01

    from Aral region are for the Tien Shan; 3. Western and central Gobi and Kazakhstan dust are for the Altai. The Aral region is the source of dust aerosol for Altai also. Based on in-situ data in the western Central Asia and Altai ice core records of particle number content there is tendency on decrease of dust storms frequency from the 30th in central and eastern Asia.

  17. Assembly of the Pamirs: Age and origin of magmatic belts from the southern Tien Shan to the southern Pamirs and their relation to Tibet

    USGS Publications Warehouse

    Schwab, M.; Ratschbacher, L.; Siebel, W.; McWilliams, M.; Minaev, V.; Lutkov, V.; Chen, F.; Stanek, K.; Nelson, B.; Frisch, W.; Wooden, J.L.

    2004-01-01

    Magmatic rocks and depositional setting of associated volcaniclastic strata along a north-south traverse spanning the southern Tien Shan and eastern Pamirs of Kyrgyzstan and Tajikistan constrain the tectonics of the Pamirs and Tibet. The northern Pamirs and northwestern Tibet contain the north facing Kunlun suture, the south facing Jinsha suture, and the intervening Carboniferous to Triassic Karakul-Mazar subduction accretion system; the latter is correlated with the Songpan-Garze-Hoh Xi system of Tibet. The Kunlun arc is a composite early Paleozoic to late Paleozoic-Triassic arc. Arc formation in the Pamirs is characterized by ???370-320 Ma volcanism that probably continued until the Triassic. The cryptic Tanymas suture of the southern northern Pamirs is part of the Jinsha suture. A massive ??????227 Ma batholith stitches the Karakul-Mazar complex in the Pamirs. There are striking similarities between the Qiangtang block in the Pamirs and Tibet. Like Tibet, the regional structure of the Pamirs is an anticlinorium that includes the Muskol and Sares domes. Like Tibet, the metamorphic rocks in these domes are equivalents to the Karakul-Mazar-Songpan-Garze system. Granitoids intruding the Qiangtang block yield ???200-230 Ma ages in the Pamirs and in central Tibet. The stratigraphy of the eastern Pshart area in the Pamirs is similar to the Bangong-Nujiang suture zone in the Amdo region of eastern central Tibet, but a Triassic ocean basin sequence is preserved in the Pamirs. Arc-type granitoids that intruded into the eastern Pshart oceanic-basin-arc sequence (???190-160 Ma) and granitoids that cut the southern Qiangtang block (???170-160 Ma) constitute the Rushan-Pshart arc. Cretaceous plutons that intruded the central and southern Pamirs record a long-lasting magmatic history. Their zircons and those from late Miocene xenoliths show that the most distinct magmatic events were Cambro-Ordovician (???410-575 Ma), Triassic (???210-250 Ma; likely due to subduction along the

  18. Assessment of Glacial Area and Volume Change in Tien Shan (Central Asia) During the Last 60 years Using Geodetic, Aerial Photo, ASTER and STRM Data

    NASA Astrophysics Data System (ADS)

    Kuzmichenok, V.; Aizen, V.; Surazakov, A.; Aizen, E.

    2004-12-01

    The water-issue problems that occur during times of persistent drought are extremely important for central Asia. Despite the presence of large deserts and prairies with very low precipitation and extremely dry climates, central Asian mountains hold one of the greatest concentrations of perennial snow and ice in the mid-latitudes and constitute a vital source of water for more then 100,000,000 people living in this region. This research aims to evaluate glacial area and ice volume changes using aerial photographs from 1943, 1977, and Satellite Remote Sensing data from 2000/2003 over the Akshiirak ice-fields and Ala Archa glacierized basin in the central and northern Tien Shan to understand changes in the glacier water resources of central Asia during the last 60 years. These data were converted from WGS-84 to STRM and then to the Pulkovo 1942 (Russian) coordinate system using a 7-parameter Helmert transformation method. For vertical validation, the STRM DEM was compared to a DEM constructed with additional 5 m and 10 m contour lines digitized from 1:25000 topographic maps for low-relief, non-glacial areas. Glacier boundaries were digitized from an ASTER L1A image acquired on August 18, 2003 and orthorectified using Orthobase digital photogrammetric package with 9.5 m RMSE of 28 ground control points. To delineate glaciers in problem areas, resulting from debris-covered termini and shadows, thermal bands and true hardware-enabled stereo viewing with nadir 3N and backward-looking 3B bands was used. Digitizing accuracy of the 2003 glacier boundaries was verified from GPS field measurements of 7 glacier termini in 2002. For surface elevation comparison, a second DEM was generated from 10 m contour lines for all glaciers (424 km2) using 16 topographic maps of 1:25000 scale that were created using the aerial photographs of 1977. In 1943, the glaciers of the Akshiirak massif covered 424.7 km2 and 42.8 km2 in the Ala Archa glacierized basin. From 1943 to 1977, the glacial

  19. Effect of Fibre Level and Fibre Source on Gut Morphology and Micro-environment in Local (Mong Cai) and Exotic (Landrace×Yorkshire) Pigs.

    PubMed

    Ngoc, T T B; Hong, T T T; Len, N T; Lindberg, J E

    2012-12-01

    The effect of genotype, fibre level and fibre source on gut morphology, environment and microflora was studied using 18 Mong Cai (MC) and 18 Landrace×Yorkshire (LY) pigs, aged around 60 d. The diets were based on maize, rice bran, soybean meal, fish meal and soybean oil, and cassava residue (CR) or brewer's grain (BG) as fibrous ingredient sources in the high-fibre diets (HF). A low-fibre diet (LF), containing around 200 g NDF/kg dry matter (DM), was formulated without CR and BG as feed ingredients. The HF diets (HF-CR and HF-BG) were formulated to contain around 270 g NDF/kg DM. The experiment was arranged according to a 2×3 factorial completely randomized design with six replications, and lasted 30 d. Crypt density in ileum was lowest (p<0.05) and villus height in jejunum and ileum were the greatest (p<0.05) in pigs fed diet HF-BG. Villus width in ileum was greatest in pigs fed diets HF-CR and HF-BG (p<0.05). Lactic acid bacteria (LAB) counts in stomach were greatest (p<0.05) and E. coli counts in ileum and colon were lowest (p<0.05) in pigs fed diet HF-CR. The concentration of total organic acids in ileum, caecum and colon were greatest (p<0.05), and pH in ileum and colon were lowest (p<0.05) in pigs fed diet HF-CR. Crypt density in ileum was lowest, and villus height in ileum and villus width in jejunum and ileum was greatest in LY pigs (p<0.05). LAB counts in stomach and ileum were greatest, and E. coli counts in ileum were lowest in MC pigs (p<0.05). The concentration of total organic acids in ileum, caecum and colon were greatest (p<0.05) and pH lowest (p<0.05) in MC pigs.

  20. Human Factors in CAI Design.

    ERIC Educational Resources Information Center

    Rambally, Gerard K.; Rambally, Rodney S.

    1987-01-01

    Identifies human factor issues involved in the student-computer interface in computer assisted instruction and makes specific recommendations for screen design. Factors considered include simplicity, spaciousness, relevance, standardization, changing display screen contents, color coding, shape and size coding, and brightness coding. (Author/LRW)

  1. A New Direction for CAI

    ERIC Educational Resources Information Center

    Dyer, Charles A.

    1976-01-01

    Author contends that the future of computer assisted instruction lies in the wealth of concepts, analytical tools and practical techniques which computer scientists have accumulated in the process of learning to build and program various kinds of systems and hardware. (Author/HB)

  2. Generative CAI in Analytical Geometry.

    ERIC Educational Resources Information Center

    Uttal, William R.; And Others

    A generative computer-assisted instruction system is being developed to tutor students in analytical geometry. The basis of this development is the thesis that a generative teaching system can be developed by establishing and then stimulating a simplified, explicit model of the human tutor. The goal attempted is that of a computer environment…

  3. CAI on a Programmable Calculator

    ERIC Educational Resources Information Center

    Schlaphoff, Carl W.

    1975-01-01

    This article describes a procedure for presenting routine practice problems on a programable calculator with attached teletype. The program uses a random number generator to write problems, gives feedback and assigns grades according to the procedures outlined (and flow-charted) by the author. (SD)

  4. Dermal toxicity evaluation of neutralized Chemical Agent Identification Sets (CAIS) with an overview of the dermal toxicity of vesicant agents and their degradation products. Final report, January-September 1995

    SciTech Connect

    Olajos, E.J.; Cameron, K.P.; Way, R.A.; Manthei, J.H.; Heitkamp, D.H.

    1996-10-01

    Acute dermal toxicity (limit test) and skin irritation studies were conducted in New Zealand white rabbits to ascertain the systemic toxicity and skin-injury potential of chemically-neutralized Chemical Agent Identification Sets (CAIS). Studies also included the assessment of oxidant/solvent systems and solvent induced toxicity. The toxicity limit test consisted of a 24-hr occluded exposure to 1.0 ml/kg of `test article.` Dermal irritation studies were based on a 4-hr occluded exposure to 0.5 ml of `test article.` Chemical neutralization of CAIS resulted in complex product solutions (wastestreams) containing ppm levels of agent and an array of degradation products. Findings from the skin irritation testing of wastestreams and oxidant/solvent systems indicate that wastestream-induced skin effects (edema and erythema) were equivalent to or less in severity than the skin effects produced by exposure to oxidant/solvent systems. Systemic effects were not observed in 4/5 wastestream-exposed groups; however, 2/5 wastestream-treated groups exhibited systemic effects. Lethality was noted in only 1/5 wastestream-treated groups. Limit test data indicate that agents (HD, HN, or L) were destroyed by reaction with oxidant to less toxic materials.

  5. Field evaluation of spatial repellency of metofluthrin-impregnated latticework plastic strips against Aedes aegypti (L.) and analysis of environmental factors affecting its efficacy in My Tho City, Tien Giang, Vietnam.

    PubMed

    Kawada, Hitoshi; Iwasaki, Tomonori; LE Loan, Luu; Tien, Tran Khanh; Mai, Nguyen Thi Nhu; Shono, Yoshinori; Katayama, Yasuyuki; Takagi, Masahiro

    2006-12-01

    Spatial repellency of metofluthrin-impregnated polyethylene latticework plastic strips against Aedes aegypti mosquitoes was evaluated. Analysis of environmental factors affecting the efficacy of these strips, such as room temperature, humidity, and house structure, was performed in a residential area in My Tho City, Tien Giang Province, Vietnam. Treatment with the strips at the rate of 1 strip per 2.6-5.52 m(2) (approximately 600 mg per 2.6-5.52 m(2)) reduced the collection of Ae. aegypti resting inside the houses for at least eight weeks. Multiple regression analysis indicated that both increase in the average room temperature and decrease in the area of openings in the rooms that were treated with the strips positively affected the spatial repellency of metofluthrin.

  6. Significant efficiency findings while controlling for the frequent confounders of CAI research in the PlanAlyzer project's computer-based, self-paced, case-based programs in anemia and chest pain diagnosis.

    PubMed

    Lyon, H C; Healy, J C; Bell, J R; O'Donnell, J F; Shultz, E K; Wigton, R S; Hirai, F; Beck, J R

    1991-04-01

    Richard E. Clark in his widely published comprehensive studies and meta-analyses of the literature on computer assisted instruction (CAI) has decried the lack of carefully controlled research, challenging almost every study which shows the computer-based intervention to result in significant post-test proficiency gains over a non-computer-based intervention. We report on a randomized study in a medical school setting where the usual confounders found by Clark to plague most research, were carefully controlled. PlanAlyzer is a microcomputer-based, self-paced, case-based, event-driven system for medical education which was developed and used in carefully controlled trials in a second year medical school curriculum to test the hypothesis that students with access to the interactive programs could integrate their didactic knowledge more effectively and/or efficiently than with access only to traditional textual "nonintelligent" materials. PlanAlyzer presents cases, elicits and critiques a student's approach to the diagnosis of two common medical disorders: anemias and chest pain. PlanAlyzer uses text, hypertext, images and critiquing theory. Students were randomized, one half becoming the experimental group who received the interactive PlanAlyzer cases in anemia, the other half becoming the controls who received the exact same content material in a text format. Later in each year there was a crossover, the controls becoming the experimentals for a similar intervention with the cardiology PlanAlyzer cases. Preliminary results at the end of the first two full trials shows that the programs have achieved most of the proposed instructional objectives, plus some significant efficiency and economy gains. 96 faculty hours of classroom time were saved by using PlanAlyzer in their place, while maintaining high student achievement. In terms of student proficiency and efficiency, the 328 students in the trials over two years were able to accomplish the project's instructional

  7. Response to the Comment by S.B. Simon, L. Grossman, and S.R. Sutton on "Valence state of titanium in the Wark-Lovering rim of a Leoville CAI as a record of progressive oxidation in the early Solar Nebula"

    NASA Astrophysics Data System (ADS)

    Young, Edward D.; Dyl, Kathryn A.; Simon, Justin I.

    2012-05-01

    S. Simon et al. incorrectly suggest that in earlier work we claimed there was no Ti3+ in Wark-Lovering rim pyroxenes. In neither the paper by Simon et al. (2005) nor the subsequent paper by Dyl et al. (2011) did we assert that there was no Ti3+ in rim pyroxenes. Rather, we found that many pyroxenes have Ti3+ below detection while others have lower Ti3+/Ti4+ than is typical of CAI interiors, indicating rim formation in a relatively oxidizing environment. Dyl et al. (2011) showed through exhaustive testing that the suggestion by Simon et al. (2007) that EMPA data in the paper by Simon et al. (2005) were flawed is incorrect. Here we consider each point raised in the comment by S. Simon et al. and reiterate that our electron microprobe data and the XANES data of Simon et al. (2007) agree and demonstrate a statistically significant (˜2σ) or greater difference between rim and interior pyroxene Ti3+/Ti4+. We show that the oxidation states of Ti in Wark-Lovering rim pyroxenes, the chemistry of rim pyroxenes, and the modal abundances of rim minerals are best explained by reaction between the CAI and gas that was orders of magnitude more oxidizing than the solar-like gas from which the CAIs originally formed.

  8. Chinese Herbal Mixture, Tien-Hsien Liquid, Induces G2/M Cycle Arrest and Radiosensitivity in MCF-7 Human Breast Cancer Cells through Mechanisms Involving DNMT1 and Rad51 Downregulation

    PubMed Central

    Chow, Jyh-Ming; Yang, Chia-Ming; Kuo, Hui-Ching; Chang, Chia-Lun; Lee, Hsin-Lun; Lai, I-Chun; Chuang, Shuang-En

    2016-01-01

    The Chinese herbal mixture, Tien-Hsien Liquid (THL), has been proven to suppress the growth and invasiveness of cancer cells and is currently regarded as a complementary medicine for the treatment of cancer. Our previous study using acute promyelocytic leukemia cells uncovered its effect on the downregulation of DNA methyltransferase 1 (DNMT1) which is often overexpressed in cancer cells resulting in the repression of tumor suppressors via hypermethylation. Herein, we explored the effects of THL in MCF-7 breast cancer cells that also demonstrate elevated DNMT1. The results show that THL dose-dependently downregulated DNMT1 accompanied by the induction of tumor suppressors such as p21 and p15. THL arrested cell cycle in G2/M phase and decreased the protein levels of cyclin A, cyclin B1, phospho-pRb, and AKT. DNMT1 inhibition was previously reported to exert a radiosensitizing effect in cancer cells through the repression of DNA repair. We found that THL enhanced radiation-induced clonogenic cell death in MCF-7 cells and decreased the level of DNA double-strand break repair protein, Rad51. Our observations may be the result of DNMT1 downregulation. Due to the fact that DNMT1 inhibition is now a mainstream strategy for anticancer therapy, further clinical trials of THL to confirm its clinical efficacy are warranted. PMID:27525019

  9. Seasonal variability of ionic concentrations in surface snow and elution processes in snow-firn packs at the PGPI site on Ürümqi glacier No. 1, eastern Tien Shan, China

    NASA Astrophysics Data System (ADS)

    Li, Zhongqin; Edwards, Ross; Mosley-Thompson, E.; Wang, Feiteng; Dong, Zhibao; You, Xiaoni; Li, Huilin; Li, Chuanjin; Zhu, Yuman

    To investigate the effects of both non-meltwater and meltwater-related post-depositional processes on chemical species within the snow-firn pack, a research program, the Program for Glacier Processes Investigation, was initiated in July 2002 by the Tien Shan Glaciological Station, Chinese Academy of Sciences. The seasonal variability of the ionic concentrations in surface snow samples and ion elution behavior in the snow-firn pack were assessed from surface samples collected year-round and 1011 samples collected from a snow pit at weekly intervals from September 2003 through September 2004. The results indicate that elevated ionic concentrations in spring and summer result from Asian dust-storm-derived aerosol input and other aerosols entrained in precipitation. Potential sources of these chemical species are explored using correlation and factor analyses. The elution sequence through the snow-firn pack was determined to be SO42- > Ca2+ > Na+ > NO3- > Cl- > K+ > Mg2+ > NH4+. The elution of ions at the sampling site was found to be driven primarily by air temperature and became evident when a diurnal mean temperature of -3.6°C was attained. At 0.3°C all of the year-round new ionic input was leached from the snow.

  10. Authoring a CAI Lesson in Nutrition Education.

    ERIC Educational Resources Information Center

    Ries, Carol P.; And Others

    1984-01-01

    A nutrition lesson on vegetarianism (focusing on vegetarian types, complementary protein, special-care nutrients, and diet planning) that uses a pre-developed plan which concentrates on lesson content and design has been developed. Initial planning and procedures involved in developing the unit (selecting teaching modes, text writing, formatting,…

  11. Design Guidelines for CAI Authoring Systems.

    ERIC Educational Resources Information Center

    Hunka, S.

    1989-01-01

    Discussion of the use of authoring systems for courseware development focuses on guidelines to be considered when designing authoring systems. Topics discussed include allowing a variety of instructional strategies; interaction with peripheral processes such as student records; the editing process; and human factors in computer interface design,…

  12. New Study Says CAI May Favor Introverts.

    ERIC Educational Resources Information Center

    Hopmeier, George

    1981-01-01

    A personality research study using the Myers-Briggs Type Indicator indicates that computer-assisted instruction programs favor introverts, i.e., those learners who can concentrate on details, memorize facts, and stay with a task until it is completed. (JJD)

  13. Learning German: A CAI Program Catalogue.

    ERIC Educational Resources Information Center

    Coombs, Virginia M.

    1984-01-01

    Presents a catalogue of microcomputer courseware specifically designed for use in learning German. Covers four types of software: (1) authoring systems for drill and practice, (2) drill and practice programs that are self-contained, (3) authoring systems that create game-like materials, and (4) game programs. Includes a listing of publishers and…

  14. Introducing the Docile Technology Inmemoriam of CAI.

    ERIC Educational Resources Information Center

    Bushnell, Don D.

    The most common mode for the use of computers in education is for the student to be directed by the programed stimulus of the computer. This method has failed to solve the long-standing problems of education. The author suggests that the time-shared computer assisted instruction console should be used as a problem-solving tool for the student. He…

  15. Compupoem: CAI for Writing and Studying Poetry.

    ERIC Educational Resources Information Center

    Marcus, Stephen

    1982-01-01

    Describes a computer program that prompts the user for different parts of speech and formats the words in a haiku-like poetic structure. (Available from "The Computing Teacher," Department of Computer and Information Science, University of Oregon, Eugene, OR 97403.) (AEA)

  16. Improving Early Reading Comprehension Using Embodied CAI

    ERIC Educational Resources Information Center

    Glenberg, Arthur M.; Goldberg, Andrew B.; Zhu, Xiaojin

    2011-01-01

    An embodied approach to reading comprehension suggests that emerging readers must learn to map words and phrases onto their remembered experiences, but this is made difficult by the necessity of focusing attention on decoding. Having children manipulate toys to correspond to what they are reading overcomes this problem, but introduces its own…

  17. No High School Diploma? You've Got Options! = No tienes un diploma de la escuela preparatoria? Tienes opciones!

    ERIC Educational Resources Information Center

    EdSource, 2006

    2006-01-01

    If a student completes high school but is unable to graduate, there are still options. The student can still get a high school diploma whether he or she dropped out, failed the California High School Exit Exam, or did not have enough course credits. As many know, a high school diploma is a passport to a more interesting and better paying job.…

  18. CAI versus Paper and Pencil--Discrepancies in Students' Performance.

    ERIC Educational Resources Information Center

    Hativa, Nira

    1988-01-01

    This study identified differences in elementary school students' performance of arithmetic tasks using paper and pencil and computer-assisted instruction. Many were found to perform more poorly using the computer, while others showed the opposite tendency. These findings challenge the validity of decisions made by the computer-based management…

  19. Computer Assisted Instruction (CAI): A Partner for PI?

    ERIC Educational Resources Information Center

    Edwards, John S.; Tillman, Murray

    1982-01-01

    Discusses differences between computer-delivered instruction and print-delivered instruction and the importance of the role of the instructional design process when adapting traditional teaching materials to newer media. The use of authoring systems for preparing materials and computer-managed instruction as a support for programed instruction are…

  20. CAI Programs and Macros for Formative Curriculum Evaluation.

    ERIC Educational Resources Information Center

    Dasenbrock, David; Teates, Thomas

    This technical memo is designed for persons who are interested in research with and development of curriculum material. Detailed information regarding computer programs, and program documentation used in the development and evaluation of ISCS curriculum materials is provided. The memo includes supplemental information to ISCS Technical Report I…

  1. CAI and Its Application in Rural Junior English Class

    ERIC Educational Resources Information Center

    He, Xiaojun

    2015-01-01

    Superiority in developing students' listening, speaking, etc. This thesis explores how to provide a better environment for English teaching in rural junior school with the aid of multimedia and find some ways to improve teaching efficiency. In recent years, using multimedia is the direction of reform and mainstream in English teaching. Compared…

  2. A Microprocessor Based CAI System with Graphic Capabilities.

    ERIC Educational Resources Information Center

    Mabry, Frank J.; And Others

    This paper describes a system which operates on an independent basis as well as connected to communications network, e.g., PLATO and ASCII based communication systems. The system also has facilities for local production and use of PILOT lessons, for support of a generalized programming language (NSBASIC), and for development of graphic sequences.…

  3. Future Review of CAI and the Coming of Videodisk Technology.

    ERIC Educational Resources Information Center

    Hirschbuhl, John J.; Seeman, Robert

    This paper describes the continuing development of a computer assisted instruction system that will connect the computer and a video storage device so as to allow the computer to regulate the delivery of instruction to individual television terminals. The video storage device consists of a videodisc player which feeds television signals from 60…

  4. The Formation of Igneous CAIs and Chondrules by Impacts?

    NASA Technical Reports Server (NTRS)

    Connolly, Harold C., Jr.; Love, Stanley G.

    2001-01-01

    Numerous challenges exist with forming the igneous spheres found within chondrites via collision events in the early solar nebula. We explore these challenges and discuss potential methods to overcome them. Collision models should be received cautiously. Additional information is contained in the original extended abstract.

  5. Presenting Questions, Processing Responses, and Providing Feedback in CAI.

    ERIC Educational Resources Information Center

    Wager, Walter; Wager, Susan

    1985-01-01

    Surveys research on programmed instruction, questions, and feedback in instruction to identify guidelines for developing computer assisted instruction. The most important guidelines identified are those related to use of questions as attention, coding, and rehearsal devices, and those related to corrective feedback. (MBR)

  6. A CAI System for Simulation of Enzymes Kinetics.

    ERIC Educational Resources Information Center

    Amorim, G. G.; Leao, F. S.; Martins, M. R.; Santos, J. D.; Novaes, M. A.; Filho, J. L. Lima

    1999-01-01

    Describes a computer software program that simulates each step of the glycolytic enzyme pathway. Serves as a means of providing interactive learning for undergraduate biochemistry students with the aim of better preparing them for laboratory work. (Author/CCM)

  7. OASIS-V: A Data-Base Driven CAI System.

    ERIC Educational Resources Information Center

    Dever, Michael K.; Spencer, Judson

    1979-01-01

    The system consists of a single program with data bases containing the material to be displayed. Editing, loading, and other support programs were written to transfer the burden of material and maintenance tasks from the user to the computer. (Author/IRT)

  8. Matching Feedback and Cognitive Style in Visual CAI Tasks.

    ERIC Educational Resources Information Center

    Hedberg, John G.; McNamara, Suzanne E.

    The effects of different types of feedback in computer assisted instruction were studied in 30 college students with different cognitive styles. The program, written in Apple Pilot and administered on an Apple IIE microcomputer, consisted of 16 problem solving tasks; for each, a graphic display and a textual question were presented. Two feedback…

  9. An investigation of CAI teaching methods in an electronics course

    NASA Astrophysics Data System (ADS)

    Wood, Kenneth W.

    1982-08-01

    Computers are increasingly being used in the classroom. An investigation of several educational techniques in a computer-based version of an electronics course is reported. We found that, with a lesson for teaching virtual equality, students learned faster when using a general to specific approach. Students using a simulation of a Schmitt trigger before a qualitative analysis of the circuit performed the analysis faster and with less difficulty than the group performing the analysis first and then exploring the circuit with the simulation. Given a sizable amount of optional material in a computer lesson, most of the electronics students used all of the optional material.

  10. Intelligent CAI: An Author Aid for a Natural Language Interface.

    ERIC Educational Resources Information Center

    Burton, Richard R.; Brown, John Seely

    This report addresses the problems of using natural language (English) as the communication language for advanced computer-based instructional systems. The instructional environment places requirements on a natural language understanding system that exceed the capabilities of all existing systems, including: (1) efficiency, (2) habitability, (3)…

  11. OE-CAI: Computer-Assisted Instruction of Old English.

    ERIC Educational Resources Information Center

    Alcaraz, Alejandro

    2002-01-01

    Provides a survey of computer assisted instruction as applied to the Old English language from the work of the late 1980's pioneers to December 2001. Each instructional item--whether a website, java exercise, or an online course--is reviewed and URLs are provided in footnotes. Reviews are accompanied by pertinent background and practical advice.…

  12. Multimedia Cai Program for Students with Mathematics Difficulties

    ERIC Educational Resources Information Center

    Seo, You-Jin; Bryant, Diane

    2012-01-01

    This study investigated the effectiveness of "Math Explorer" at enhancing the word problem-solving skills of students with mathematics difficulties (MD). The study, which had a multiple-probe-across-subjects design, was conducted over 18 weeks. Four students with MD in Grades 2 and 3 participated. All students were able to use the four-step…

  13. Major unresolved issues in the formation of chondrules and CAIs

    NASA Technical Reports Server (NTRS)

    Wood, J. A.

    1994-01-01

    So much has been learned and published about chondrites and so many models have been floated (but neither proven nor refuted) that the subject has become extremely diffuse and amorphous. It is impossible to remain simultaneously aware of all the many constraints, from many different subdisciplines, that bear on nebular processes. This paper attempts to impose some structure on the situation and loosen the interpretational logjam by breaking the chondrite problem into a series of well-defined questions. Most are open questions; those that some might consider closed by now may deserve formal reexamination.

  14. The Mn-53-Cr-53 System in CAIs: An Update

    NASA Technical Reports Server (NTRS)

    Papanastassiou, D. A.; Wasserburg, G. J.; Bogdanovski, O.

    2005-01-01

    High precision techniques have been developed for the measurement of Cr isotopes on the Triton mass spectrometer, at JPL. It is clear that multiple Faraday cup, simultaneous ion collection may reduce the uncertainty of isotope ratios relative to single Faraday cup ion collection, by the elimination of uncertainties from ion beam instabilities (since ion beam intensities for single cup collection are interpolated in time to calculate isotope ratios), and due to a greatly increased data collection duty cycle, for simultaneous ion collection. Efforts to measure Cr by simultaneous ion collection have not been successful in the past. Determinations on Cr-50-54Cr, by simultaneous ion collection on the Finnigan/ MAT 262 instrument at Caltech, resulted in large variations in extrinsic precision, for normal Cr, of up to 1% in Cr-53/Cr-52 (data corrected for mass fractionation, using Cr-50/Cr-52).

  15. Formation of chondrules and CAIs by nebular processes

    NASA Technical Reports Server (NTRS)

    Palme, H.

    1994-01-01

    Chondrules are essential components of most chondritic meteorites. Carbonaceous chondrites, with the exception of CI chondrites, contain 30-50% chondrules, ordinary and enstatite chondrites even more. A better understanding of chondrule formation will therefore lead to an improved understanding of the origin of meteorites. Most studies of chondrules are, however, concerned with their texture and mineralogy. As chondrules, by definition, passed through a molten stage, their present texture and mineralogy can only provide information on conditions of crystallization from a melt and the subsequent solid-state cooling history. Information concerning chondrule formation is contained in their chemical and isotopic composition. The two most important observations relevant to the chemistry of the chondrules are their generally low Fe content and the large compositional variability of chondrules from a single meteorite, reflected in major variations of Mg/Si ratios, of Al and other refractory element abundances, total Fe, metal (Fe, Ni), and sulfide. This large compositional variability is surprising considering the uniform and nearly solar composition of bulk chondrites, which, in some cases, consist of more than 90% of chondrules.

  16. "Intelligent" Computer Assisted Instruction (CAI) Applications. Interim Report.

    ERIC Educational Resources Information Center

    Brown, John Seely; And Others

    Interim work is documented describing efforts to modify computer techniques used to recognize and process English language requests to an instructional simulator. The conversion from a hand-coded to a table driven technique are described in detail. Other modifications to a simulation based computer assisted instruction program to allow a gaming…

  17. The Development of Visual Materials for CAI. Technical Memo 5.

    ERIC Educational Resources Information Center

    Best, Elowese

    User-originated 16mm filmstrips for use with an IBM 1512 computer-controlled rear screen projector can be made at half the commercial cost. This report describes the procedures necessary for preparing, photographing, and processing either a black-and-white or color filmstrip for a computer-assisted instruction program. Master preparation,…

  18. Interactive Graphics in CAD/CAI in Chemical Engineering.

    ERIC Educational Resources Information Center

    Lewin, D. R.

    This paper describes the development of a software program which incorporates interactive graphics techniques into a teaching and research environment at the Department of Chemical Engineering, Technion, Israel, and the experience of transferring the software from mainframe to personal computer (PC) operating systems at the California Institute of…

  19. El Que No Tiene Dingo, Tiene Mandingo: The Inadequacy of the "Mestizo" as a Theoretical Construct in the Field of Latin American Studies--The Problem and Solution.

    ERIC Educational Resources Information Center

    Rosa, Andrew Juan

    1996-01-01

    Argues that the "mestizo" paradigm as a theoretical construct used in Latin American studies denies the historical and cultural contributions of Africans to Latin American society and that it is fundamentally inaccurate and racist. Discusses ways of correcting these misconceptions. (GR)

  20. "El coronel no tiene quien le escriba," Gabriel Garcia Marquez. Performance Guides to Spanish Texts.

    ERIC Educational Resources Information Center

    Gies, David Thatcher, Comp.

    This performance guide is the result of work conducted at the University of Virginia's National Endowment for the Humanities Summer Institute, 1989, on "Spanish Literature in Performance," in which 25 secondary school Spanish teachers studied Spanish texts from the perspective of classroom performance to deepen knowledge of the texts and…

  1. Observations of high-energy radiation during thunderstorms at Tien-Shan

    NASA Astrophysics Data System (ADS)

    Gurevich, A. V.; Almenova, A. M.; Antonova, V. P.; Chubenko, A. P.; Karashtin, A. N.; Kryakunova, O. N.; Lutsenko, V. Yu.; Mitko, G. G.; Ptitsyn, M. O.; Piscal, V. V.; Ryabov, V. A.; Salikhov, N. M.; Sadykov, T. Kh.; Shepetov, A. L.; Shlyugaev, Yu. V.; Thu, W. M.; Vil'danova, L. I.; Zastrozhnova, N. N.; Zybin, K. P.

    2016-07-01

    Energetic radiation during thunderstorms is studied. The possibility to identify the high-energy lightning emission in the 10 s monitoring mode is demonstrated. Simultaneous measurements of gamma-ray emission, high-energy electrons, and neutron radiation in the triggering mode are fulfilled. Energy spectra of gamma emission and electrons are obtained. The intensity both of electrons and gamma rays in lightning discharge prevail the background emission by 1.5 to 2 orders of magnitude.

  2. Saving Energy around the House = Tien Tan Trong Viec Tieu Thu Nang Luc Trong Nha.

    ERIC Educational Resources Information Center

    Noyes, Marilyn; Jarrett, Von

    This bilingual booklet is intended to help Vietnamese refugees learn basic energy conservation skills. Included in the booklet are Vietnamese and English translations of basic energy conservation practices related to the following areas: heating, cooling, cooking, using refrigerators and freezers, lighting, water heating, doing laundry, pursuing…

  3. Tiene Arte Valor Afuera Del Barrio: The Murals of East Los Angeles and Boyle Heights

    ERIC Educational Resources Information Center

    Holscher, Louis M.

    1976-01-01

    Discusses the themes of the murals and explores the possible uses that the murals in Los Angeles have for the outsider, the non-Chicano, for those who have only a little understanding or awareness of the Chicano community. (Author/AM)

  4. "Todo Tiene que ver con lo que se Habla." It's All About the Talk

    ERIC Educational Resources Information Center

    Frey, Nancy; Fisher, Douglas; Nelson, John

    2013-01-01

    Chula Vista Elementary School District, the largest in California, dramatically raised its student achievement while taking on increasing proportions of English learners by focusing on what it calls teacher talk--the way lessons are developed, delivered, and executed.

  5. Palaeogegraphic and palaeotopography evolution of the chinese Tien Shan during the Mesozoic : a sedimentological synthesis

    NASA Astrophysics Data System (ADS)

    Heilbronn, Gloria; Jolivet, Marc; Robin, Cécile; Barrier, Laurie; Bourquin, Sylvie; Jia, Yingying; Fu, Bihong

    2014-05-01

    The Tian Shan is one of the main ranges of Central Asia Orogenic Belt. The Tertiary deformation is driven by the India-Asia collision stress field. However, the deformation appears localised along inherited tectonic structures formed during the Palaeozoic - Early Mesozoic history of the range (e.g. Jolivet et al., 2010). Our aim is to reconstruct the pre-Tertiary history of relief building in the Chinese Tian Shan. We use the sedimentary facies, sediment provenances and paleocurrent directions of the exposed Mesozoic sections in the northern and southern piedmonts and inside the range. This will be used to understand the long-term reactivation pattern of the main inherited structures and to assess their influence on the localisation and propagation of the deformation. We first established 6 complete reference sections spanning from the Upper Triassic to the Palaeogene. These sections are interpreted in terms of sedimentary facies, palaeoenvironments and prograding-retrograding sequences. The correlation of these 6 sections allows us to propose some palaeogeographic maps for the middle Jurassic, the upper Jurassic - lower Cretaceous transition, the upper Cretaceous and the late Cretaceous - Paleogene transition. The dismantling of reliefs associated to the late-paleozoic range stops in the upper Trias. The Jurassic is characterised by a low tectonic activity and results in a general planation phase of the Tian Shan area. The supposed low relief is possibly associated to local activity of normal faults : this is attested by alluvial fan deposits on the internal sections, as well as paleocurrent directions to the North in the northern foothills and to the south in the southern foothills. These faults could belong to pull apart basins opening in a transtensive tectonic régime, under a humid climate, what is testified by numerous organic matter layers. The upper Jurassic - lower Cretaceous transition is characterized by a huge conglomeratic event at the scale of all the northern foothills, associated with some eolian deposits certified a arid climat at this period. We propose that alluvial fans are the result of the erosion of relatively small and local reliefs, caused by normal faults. This interpretation is in contradiction with all hypothesis of the literature supporting compressional tectonic and reactivation of the range during the Upper Jurassic. Nevertheless it fits to the interpretation of low thermochronology data. During the Upper Cretaceous, the widespread occurrence of alluvial fans indicates the ongoing erosion of a local positive topography in the Tian Shan area. A significant late Lower - early Upper Cretaceous unconformity is observable in the S-Junggar, N-Tarim and Turfan Basins (Hendrix et al., 1992). It is confirmed by low temperature thermochronology data that show a "major" late Lower Cretaceous unroofing event near Kuqa on the southern foothills (Dumitru et al., 2001) and some late Lower to early Upper Cretaceous exhumation ages within the range (Jolivet et al., 2010). This marks the onset of a new exhumation phase that goes on during the Upper Cretaceous and seems to stop after a peak in the late Upper Cretaceous. Following the Upper Cretaceous inversion episode, a tectonic quiet period characterises the late Upper Cretaceous - Early Paleogene and enables the formation of a widespread calcrete.

  6. Training Corrective Maintenance Performance on Electronic Equipment with CAI Terminals: I. A Feasibility Study.

    ERIC Educational Resources Information Center

    Rigney, Joseph W.

    A report is given of a feasibility study in which several possible relationships between student, computer terminal, and electronic equipment were considered. The simplest of these configurations was set up and examined in terms of its feasibility for teaching the performance of fault localization on a Navy transceiver. An instructional program…

  7. Low-cost Computer-Aided Instruction/Computer-Managed Instruction (CAI/ CMI) System: Feasibility Study

    DTIC Science & Technology

    1979-12-01

    F3101I5-78-C-OOS I proiect I1121,. with Technical Training D~ivision. Air Force IHuman Resources Laboi at orv (A lS (’ V Iow rv Air Voice Base. Colorado...8217 , iil tlut to the cttl,1putter, full lld ple\\ t.rallsilissic’n should be usled . In u11u du1 lx, e,1h ch tor IV\\r Code is sent to Ole compu tet’l" IS...Tinopl x 02up to ’xxQO Tele-Dynamics 7294T OPp to 1.1111 Svntech TT- ZW Op to 1l8O100 Novation 20 6O Penri 1 lS . ’~t "i 4.4.2 Transmni ssicn to mul

  8. CAI in Learning Voice in English Grammar among Eighth Standard Students--An Experimental Study

    ERIC Educational Resources Information Center

    Ramesh, R.; Sumathi, B.

    2010-01-01

    English is a language, which is spoken by numerous people across the world. It has acquired a prominent place in meeting the communicational needs of the people. Grammar is a set of rules that helps the people to use the language better. In schools, the teachers of English are considered as the most important factor in making the study of English…

  9. Military Standard Common APSE (Ada Programming Support Environment) Interface Set (CAIS).

    DTIC Science & Technology

    1985-01-01

    QUEUEASE. LAST-KEY (QUEENAME) . LASTREI.TIONI(QUEUE-NAME). FILE-NODE. PORN . ATTRIBUTTES. ACCESSCONTROL. LEVEL); CLOSE (QUEUE BASE); CLOSE(FILE NODE...PROPOSED XIIT-STD-C.4 31 J NNUAfY logs procedure zTERT (ITERATOR: out NODE ITERATON; MAMIE: NAME STRING.KIND: NODE KID : KEY : RELATIONSHIP KEY PA1TTE1 :R

  10. A Novel CAI System for Space Conceptualization Training in Perspective Sketching

    ERIC Educational Resources Information Center

    Luh, Ding-Bang; Chen, Shao-Nung

    2013-01-01

    For many designers, freehand sketching is the primary tool for conceptualization in the early stage of the design process. However, current education on concept presentation techniques rarely emphasizes the construction of the most fundamental spatial unit, the cube. Incorrect construction of spatial units leads to disproportions that deviate from…

  11. Differential Characteristics and Methods of Operation Underlying CAI/CMI Drill and Practice Systems.

    ERIC Educational Resources Information Center

    Hativa, Nira

    1988-01-01

    Describes computer systems that combine drill and practice instruction with computer-managed instruction (CMI) and identifies system characteristics in four categories: (1) hardware, (2) software, (3) management systems, and (4) methods of daily operation. Topics discussed include microcomputer networks, graphics, feedback, degree of learner…

  12. In Defense of CAI: Is Drill-and-Practice a Dirty Word?

    ERIC Educational Resources Information Center

    Yates, Daniel S.

    1983-01-01

    Discussion of microcomputers to provide drill-and-practice in mathematics highlights educational research, early instructional software and its bad reputation, and the current trend toward the production of higher quality software. (MBR)

  13. 77 FR 9625 - Presentation of Final Conventional Conformance Test Criteria and Common Air Interface (CAI...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-02-17

    ...The U.S. Department of Commerce's (DOC) National Institute of Standards and Technology (NIST), Law Enforcement Standards Office (OLES), in partnership with the U.S. Department of Homeland Security (DHS) Office for Interoperability and Compatibility (OIC), will hold a public meeting on Thursday, March 15, 2012 at 1 p.m. Mountain Time, via teleconference. The purpose of the meeting is to present......

  14. Can U.S. Developed CAI Work Effectively in a Developing Country?

    ERIC Educational Resources Information Center

    Royer, James M.; And Others

    1994-01-01

    Describes a study that examined the impact of computer-assisted instruction developed in the United States on the reading and math performance of students in Grenada. Results were compared with students receiving conventional instruction for high and low ability students and for gender differences. (Contains seven references.) (LRW)

  15. Rejoinder to MacCallum, Edwards, and Cai (2012) and Rindskopf (2012): Mastering a New Method

    ERIC Educational Resources Information Center

    Muthen, Bengt; Asparouhov, Tihomir

    2012-01-01

    This rejoinder discusses the general comments on how to use Bayesian structural equation modeling (BSEM) wisely and how to get more people better trained in using Bayesian methods. Responses to specific comments cover how to handle sign switching, nonconvergence and nonidentification, and prior choices in latent variable models. Two new…

  16. CAI--Socratic Dialogue and Laboratory Simulation in Pathology. Technical Report Number Three.

    ERIC Educational Resources Information Center

    Hellerstein, Earl E.; And Others

    The report describes work accomplished in the development of instructional materials for second-year medical students taking a histopathology laboratory course. The objectives and methods are described and several examples of techniques are illustrated with short segments of dialogue. These segments also illustrate the branching characteristics of…

  17. Conodont color alteration (CAI) as an aid to structural interpretation in the Black Pine Mountains, Idaho

    USGS Publications Warehouse

    Smith, Fred J.; Wardlaw, Bruce R.

    2012-01-01

    The Black Pine Mountains, southeastern Cassia County, Idaho, consist of southern and northern blocks separated by a northeast-trending, high-angle fault. Differences in conodont color alteration values distinguish the two blocks. The southern block has significantly higher organic maturation levels than the northern block and is interpreted to have been thrust northeastward adjacent to the northern block.

  18. Results of a Follow-Up Survey of CAI Development in Selected Institutions of Higher Education.

    ERIC Educational Resources Information Center

    Karrer, Urs

    Designed to test the premise that the production system for courseware has a strong impact on the quality of the courseware developed, a survey of 14 U.S. institutions of higher education was conducted in 1986 to investigate the production systems used by these schools. Many of the questions used and the list of institutions surveyed were…

  19. Materials Data on Ba2CaI6 (SG:117) by Materials Project

    SciTech Connect

    Kristin Persson

    2016-02-04

    Computed materials data using density functional theory calculations. These calculations determine the electronic structure of bulk materials by solving approximations to the Schrodinger equation. For more information, see https://materialsproject.org/docs/calculations

  20. Materials Data on Sr2CaI6 (SG:117) by Materials Project

    DOE Data Explorer

    Kristin Persson

    2016-02-04

    Computed materials data using density functional theory calculations. These calculations determine the electronic structure of bulk materials by solving approximations to the Schrodinger equation. For more information, see https://materialsproject.org/docs/calculations

  1. Evaluation of C.A.I. as Used by Various Handicaps.

    ERIC Educational Resources Information Center

    St. Aubin, Raymond

    This paper summarizes a project undertaken by South Metropolitan Association for Low-Incidence Handicapped (SMA) in 1975 to provide handicapped children in the south suburban area of metropolitan Chicago with learning opportunities via computer assisted instruction. Students exhibiting hearing, visual mental, or other learning disabilities were…

  2. CASIP--A Novel Authoring Tool for Open Ended Natural Language CAI.

    ERIC Educational Resources Information Center

    Anbar, Michael

    Computer-assisted instruction that uses open ended questions and calls for answers in natural language is the preferred method of instruction in many training situations. A novel authoring tool has been developed to meet the specific needs of open ended computerized instruction. This program, named CASIP, is essentially a single purpose…

  3. A General-Purpose ASCII Decoder for Control of Peripheral Devices for CAI Terminals.

    ERIC Educational Resources Information Center

    Rigney, Joseph W.; Williams, Louis A.

    The ASCII (American Standard Code for Information Interchange) decoder described here accepts inputs from an acoustic coupler, or Modem, in a remote time-sharing system. On receipt of a special command character the decoder recognizes, stores, and decodes the next two decimal digits. The output can be used to access any one of 100 items. For…

  4. Cai-Beneficial Teaching Tool at Texas School for the Deaf

    ERIC Educational Resources Information Center

    Culberton, Lynda B.

    1974-01-01

    Described are efforts of 15 schools for the deaf to continue for their 2000 students (after federal project funding termination) the computer assisted instruction program transmitted through telephone lines between 1971 and 1973 from the Institute for Mathematical Studies in Social Sciences, Stanford University. (Author/MC)

  5. Integration of CAI into a Freshmen Liberal Arts Math Course in the Community College.

    ERIC Educational Resources Information Center

    McCall, Michael B.; Holton, Jean L.

    1982-01-01

    Discusses four computer-assisted-instruction programs used in a college-level mathematics course to introduce computer literacy and improve mathematical skills. The BASIC programs include polynomial functions, trigonometric functions, matrix algebra, and differential calculus. Each program discusses mathematics theory and introduces programming…

  6. The Formation of Boundary Clinopyroxenes and Associated Glass Veins in Type B1 CAIs

    SciTech Connect

    Paque, J M; Beckett, J R; Ishii, H A; Toppani, A; Burnett, D S; Teslich, N; Dai, Z R; Bradley, J P

    2008-05-18

    We used focused ion beam thin section preparation and scanning transmission electron microscopy (FIB/STEM) to examine the interfacial region between spinel and host melilite for three spinel grains, two from the mantle and one from the core of an Allende type B1 inclusion, and a second pair of spinel grains from a type B1 inclusion from the Leoville carbonaceous chondrite. The compositions of boundary clinopyroxenes decorating spinel surfaces are generally consistent with those of coarser clinopyroxenes from the same region of the inclusion, suggesting little movement of spinels between mantle and core regions after the formation of boundary clinopyroxenes. The host melilite displays no anomalous compositions near the interface, and anorthite or other late-stage minerals are not observed, suggesting that crystallization of residual liquid was not responsible for the formation of boundary clinopyroxenes. Allende spinels display either direct spinel-melilite contact or an intervening boundary clinopyroxene between the two phases. In the core, boundary clinopyroxene is mantled by a thin (1-2 {micro}m thick) layer of normally zoned (X{sub Ak} increasing away from the melilite-clinopyroxene contact) melilite with X{sub Ak} matching that of the host melilite at the melilite-melilite contact. In the mantle, X{sub Ak} near boundary spinels is constant. Spinels in a Leoville type B1 inclusion are more complex with boundary clinopyroxene, as observed in Allende, but also variable amounts of glass ({approx}1 {micro}m width), secondary calcite, perovskite, and an unknown Mg-, Al-, OH-rich and Ca-, Si-poor crystalline phase that may be a layered double hydrate. Glass compositions are consistent to first order with a precursor consisting mostly of Mg-carpholite or sudoite with some aluminous diopside. One possible scenario of formation for the glass veins is that open system alteration of melilite produced a porous, hydrated aggregate of Mg-carpholite or sudoite + aluminous diopside that was shock melted and quenched to a glass. The unknown crystalline phase may be a shocked remnant of the precursor phase assemblage but is more likely to have formed later by alteration of the glass. Calcite appears to be an opportunistic fracture filling that postdated all major shock events. Boundary clinopyroxenes probably share a common origin with coarser-grained pyroxenes from the same region of the inclusion. In the mantle, these crystals may represent clinopyroxene crystallized in Ti-rich liquids caused by the direct dissolution of perovskite and an associated Sc-Zr-rich phase or as a reaction product between dissolving perovskite and liquid (i.e., indirect dissolution of perovskite). In the core, any perovskite and associated Ti-enriched liquids that may have originally been present disappeared before the growth of boundary clinopyroxene.

  7. Hyper InterActive CAI: Using HyperCard To Develop Computer-Assisted Instruction.

    ERIC Educational Resources Information Center

    Desberg, Peter

    This hands-on guide shows readers how to use HyperCard software to create instructional programs on the Macintosh computer. The book describes how to choose subject matter, design a program, and determine the method of presentation, including the type of interaction and guiding metaphors that will be used. It explains how to make programs easy for…

  8. CAI: A Model for the Comparison and Selection of Integrated Learning Systems in Large School Districts.

    ERIC Educational Resources Information Center

    Resta, Paul E.; Rost, Paul

    The Albuquerque (New Mexico) Public Schools conducted a three-year study of integrated computer-based learning systems, including WICAT, Dolphin, PLATO, CCC, and DEGEM. Through cooperation with the Education Consolidation Improvement Act Chapter 1 program, four large integrated learning systems (ILS) were purchased and studied. They were installed…

  9. The Coast Guard's CAI Approach to Basic Math and Reading Skills.

    ERIC Educational Resources Information Center

    Glidden, William C.; And Others

    To meet the remedial-instructional needs of its recruits, the Coast Guard developed a basic skills program, entitled the Basic Educational Enrichment Program (BEEP), at its recruit training center in Cape May, New Jersey. Objectives of the program were to ensure that all graduates of Coast Guard recruit training possess at least eighth-grade…

  10. Disorders of sexual differentiation: surgical challenges of vaginal reconstruction in complete androgen insensitivity syndrome (CAIS).

    PubMed

    Munoz, Jose A; Swan, Kenneth G

    2010-02-01

    Disorders of sexual differentiation have proven difficult to treat not only because of physicians' lack of understanding regarding the determinants of sexual orientation, but also because of the psychological impact associated with sexual dysfunction. Patients with complete androgen insensitivity syndrome not only must undergo gonadectomy after puberty, requiring post-gonadectomy hormonal replacement, but also can suffer from underdeveloped, blind vaginal pouches. As a result, sexual intercourse is compromised. Many attempts have been made throughout medical history to correct the vaginal defect, including surgical and nonsurgical approaches, each with its own technical difficulties and complications. Presently, consensus regarding the optimal time for intervention is when the patient is ready to begin sexual life. However, the optimal surgical approach has not been established. In general, nonsurgical vaginal dilatation, like the Frank and Ingram methods, should be followed by surgical interventions, such as described by McIndoe, Vecchietti, and intestinal transplantation, in case of failure of the more conservative procedures.

  11. ONR Conference on CAI Languages Held at Cambridge, Massachusetts, 2-3 March 1966.

    ERIC Educational Resources Information Center

    Entelek, Inc., Newburyport, MA.

    An invitational meeting was held to consider computer-assisted instruction. Topics discussed included the BBM (Bolt, Beranek, Newman, Inc.) Mathematics program and programing languages, such as, Coursewriter, AUTHOR (Automatically Translating Heuristically Organized Routines), and PLATO/CATO (Programed Logic for Automatic Teaching Operations/PLATO…

  12. Conventional CBI versus Intelligent CAI: Suggestions for the Development of Future systems.

    ERIC Educational Resources Information Center

    Park, Ok-choon; Seidel, Robert J.

    1987-01-01

    Designed to promote cooperative efforts between researchers in artificial intelligence and instruction for the development of future computer-delivered instructional systems, this article contrasts intelligent computer-assisted instruction (ICAI) and traditional computer-based instruction (CBI) in terms of the basic philosophies underlying their…

  13. CAI and Imagery: Interactive Computer Graphics for Teaching About Invisible Process. Technical Report No. 74.

    ERIC Educational Resources Information Center

    Rigney, Joseph W.; Lutz, Kathy A.

    In preparation for a study of using interactive computer graphics for training, some current theorizing about internal and external, digital and analog representational systems are reviewed. The possibility is considered that there are two, overlapping, internal, analog representational systems, one for organismic states and the other for external…

  14. Using CAI To Improve Participation and Achievement in Science Research Projects in Middle School Science.

    ERIC Educational Resources Information Center

    Price, Suzanne M.

    The high percentage of students not participating in or completing a science research project has been a recurring problem for science teachers. In this project, three variables influencing the problem are identified: (1) students' failure to engage in an active search for science research topics; (2) inadequate resource materials at the middle…

  15. Development of nursing CAI in the administration: nursing daily hospital problems.

    PubMed

    Carmagnani, M I; Cunha, I C; Marin, H F

    1995-01-01

    Since the nurse emerged as a qualified professional to attend human beings, the role which always characterized his/her action was assistance. Already since the foundation of the first nursing school, teaching aimed at developing the student to dispense nursing care necessary for the patient's assistance. When the nurse started to perform their activities in nosocomial and community institutions, the need for someone who would be responsible for the organization, coordination and control of nursing personnel and the Nursing Unit itself, in short, someone who would head the services became apparent. At present, the professional role of the nurse is changing regarding his/her overall assistance to the patient, caring directly, determining and/or carrying out nursing assistance necessary for the patient's health, maintenance or recovery. In this manner, it is necessary for nurses to use tools of administration science such as planning, decision making, and planned changes in order to be able to provide the nursing assistance with quality. Thus, this study aims at helping the development of the nurse's interest in computer during the teaching-learning process, motivating the search for knowledge in computerized sources. We intended to offer the opportunity for discussion and reflection on problems of nosocomial nursing practice, favoring interchange of theory and practice. The system is being developing using ToolBook Live Software to be run in Windows environment. The content of the subject allow the user (student or professional nursing) to choose the most correct answers to questions in the knowledge area. In this case, to discuss nursing administration issues through the study of practical situations is possible, such as the opportunity the verify the performance in tests.

  16. A CAI (Computer-Assisted Instruction) Course on Constructing PLANIT lessons: Development, Content, and Evaluation

    DTIC Science & Technology

    1980-06-01

    PLANIT lesson records for each student after the student signed off from each online session. 44 pa-BECKMG LOG-INFA1~ INTER- T" ACTION PLANI ARfCOPYj FPu ...answers (11) Same action for several tags e.g. BCD F: LET’S REVIEW B:2 (12) Actions extending to a second line 3. THE (M)ULTIPLE CHOICE FRAE 3.0

  17. ENIGMA, CAI-CMI for Introductory Logic: Some of Its Abilities with English Sentences.

    ERIC Educational Resources Information Center

    Laymon, Ronald

    The philosophy department of the Ohio State University began development of a computer-tutorial program, called ENIGMA, in 1972. The aim of the course was to help students to use various logical tools in the analysis of everyday arguments by giving drill-and-practice sessions, testing, and grading examinations. Part of ENIGMA is the propositional…

  18. Presentación del estudio “Links” de hombres que tienes sexo con hombres en Buenos Aires, Argentina

    PubMed Central

    Carballo-Diéguez, Alex; Ávila, María M; Balán, Iván C.; Marone, Rubén; Pando, María A.; Barreda, Victoria

    2011-01-01

    Resumen Estudios previos en Buenos Aires reportaron altas prevalencias de HIV entre HSH, con valores que oscilan entre 9 y 14% durante casi 10 años de continuo testeo. El objetivo principal de este estudio fue la evaluación de factores relacionados al comportamiento de alto riesgo para transmisión del HIV entre HSH entre los que se incluyen el conocimiento y factores emocionales, socioculturales y ambientales. Por otro lado se realizó la estimación de prevalencia e incidencia de HIV utilizando RDS (Respondent Driven Sampling), así como la presencia de otras infecciones de transmisión sexual. Por último se evaluaron los hábitos de testeo para HIV indagando que factores facilitan o impiden su realización. El estudio constó de dos fases, en primer lugar una fase cualitativa y posteriormente una fase cuantitativa con una duración total de 4 años y medio. Durante la fase cualitativa se realizaron 44 entrevistas individuales en profundidad, 8 grupos focales y 10 observaciones etnográficas (hoteles, baños públicos (“teteras”), cines pornográficos, fiestas privadas, dark rooms y discotecas). Durante la fase cuantitativa del estudio se realizó el reclutamiento de 500 participantes que provinieron de la Ciudad Autónoma de Buenos Aires, así como del Gran Buenos Aires. El reclutamiento se comenzó con 16 participantes llamados semillas. Se realizó el diagnóstico de infección por HIV, hepatitis B y C (HBV y HCV), Treponema pallidum, Virus Papiloma Humano (HPV) y Chlamidias. La colaboración establecida entre los grupos de trabajo enfocados en áreas diversas posibilitó el abordaje conjunto de nuevas estrategias de investigación antes no exploradas en nuestro país. Los resultados más relevantes de esta investigación serán progresivamente publicados en sucesivos números de Actualizaciones en SIDA. PMID:25264397

  19. Streamflow variability for the Aksu River on the southern slopes of the Tien Shan inferred from tree ring records

    NASA Astrophysics Data System (ADS)

    Zhang, Ruibo; Yuan, Yujiang; Gou, Xiaohua; Yang, Qing; Wei, Wenshou; Yu, Shulong; Zhang, Tongwen; Shang, Huaming; Chen, Feng; Fan, Ziang; Qin, Li

    2016-05-01

    Gauged river flow records from China generally span only a few decades, which hampers the detection of long-term, decadal- to centennial-scale cycles and trends in streamflow variability. New and updated tree-ring chronologies help reconstructed the water-year (October-September) streamflow for the Aksu River, which is an important river at the edge of the Taklimakan Desert that drains into the Tarim Basin. The reconstruction dates back to 1692 and has an adjusted r2 of 0.61 (1957-2006). Based on frequency, intensity and duration of droughts and pluvial events, the lowest streamflows occurred in the 1920s. Since then streamflow has continuously increased, and was exceptionally rapidly after the 1960s, until today. The start and end of the 20th century to the present were the highest streamflow periods. The mid-20th century was the longest and driest period over the past 300 yr. The reconstructed streamflow series has a strong positive correlation with the North Atlantic Oscillation Index. Changes in mid-latitude circulation patterns influencing precipitation may have indirectly resulted in streamflow variations along the Aksu River over the past 300 yr. The rapid increase and the exceptional streamflows of the 1960s are likely linked with global warming and mid-latitude atmospheric circulation changes.

  20. Presentación del estudio "Links" de hombres que tienes sexo con hombres en Buenos Aires, Argentina.

    PubMed

    Carballo-Diéguez, Alex; Avila, María M; Balán, Iván C; Marone, Rubén; Pando, María A; Barreda, Victoria

    2011-03-01

    Estudios previos en Buenos Aires reportaron altas prevalencias de HIV entre HSH, con valores que oscilan entre 9 y 14% durante casi 10 años de continuo testeo. El objetivo principal de este estudio fue la evaluación de factores relacionados al comportamiento de alto riesgo para transmisión del HIV entre HSH entre los que se incluyen el conocimiento y factores emocionales, socioculturales y ambientales. Por otro lado se realizó la estimación de prevalencia e incidencia de HIV utilizando RDS (Respondent Driven Sampling), así como la presencia de otras infecciones de transmisión sexual. Por último se evaluaron los hábitos de testeo para HIV indagando que factores facilitan o impiden su realización. El estudio constó de dos fases, en primer lugar una fase cualitativa y posteriormente una fase cuantitativa con una duración total de 4 años y medio. Durante la fase cualitativa se realizaron 44 entrevistas individuales en profundidad, 8 grupos focales y 10 observaciones etnográficas (hoteles, baños públicos ("teteras"), cines pornográficos, fiestas privadas, dark rooms y discotecas). Durante la fase cuantitativa del estudio se realizó el reclutamiento de 500 participantes que provinieron de la Ciudad Autónoma de Buenos Aires, así como del Gran Buenos Aires. El reclutamiento se comenzó con 16 participantes llamados semillas. Se realizó el diagnóstico de infección por HIV, hepatitis B y C (HBV y HCV), Treponema pallidum, Virus Papiloma Humano (HPV) y Chlamidias. La colaboración establecida entre los grupos de trabajo enfocados en áreas diversas posibilitó el abordaje conjunto de nuevas estrategias de investigación antes no exploradas en nuestro país. Los resultados más relevantes de esta investigación serán progresivamente publicados en sucesivos números de Actualizaciones en SIDA.

  1. Distribution of seismicity in the Pamir-Tien Shan-Hindu Kush region, central Asia, from TIPAGE seismic data

    NASA Astrophysics Data System (ADS)

    Sippl, C.; Schurr, B.; Schneider, F.; Yuan, X.; Mechie, J.; Haberland, C. A.; Orunbaev, S.; Gadoev, M.; Negmatullaev, S.; Rui, H.; Pingren, L.

    2011-12-01

    The Pamir-Hindu Kush region in central Asia is unique as it hosts vigorous intermediate-depth (80-300 km) seismicity in the continental interior far away from oceanic plate subduction. The earthquakes occur within an S-shaped seismic zone extending from north-western Afghanistan into the Eastern Pamir plateau. This zone shows an intriguing geometry, with earthquake hypocenter locations resembling a Wadati-Benioff zone with significant change in its dip along strike, from sub-vertically northward in the Hindu Kush to shallower southward dipping in the Eastern Pamir. The interpretation of these observations and the nature of the seismic zone are still debated. Proposed models include two-sided subduction of Indian and Asian lithosphere, an overturned slab of exclusively Indian material as well as scenarios involving delamination of mantle lithosphere. Another unsolved question is whether the subducted material is of continental or oceanic nature. Plate reconstructions provide no ocean of fitting age, yet absence of hydrated oceanic lithosphere also takes away the mechanism to generate earthquakes at the pressure and temperature regime of the upper mantle. Analyzing two years of data (2008-2010) from a number of new temporary deployments as well as permanent stations in the region, we detected more than 15,000 earthquakes. The sheer number of events prohibits a manual determination of phase onsets. We therefore implemented an automatic scheme that uses state-of-the-art picking algorithms for both P and S phases including a quality assessment of the phase arrivals. The scheme involves several stages of picking, relocation, re-picking and weeding out spurious arrivals. We will demonstrate the robustness of the scheme by comparison with several hand-picked sub sets of the catalogue. We further refined the earthquake locations by determining differential travel times for clustered events using cross correlation and the double-difference relocation algorithm. Our results reveal some new details about the structure and geometry of the seismic zone: in the Eastern Pamir, intermediate-depth seismicity is confined to depths between 90 and 180 km and thus clearly separated from shallow seismicity along the Main Pamir Thrust, which does not reach depths in excess of 30 km. The lower crust throughout the Pamir appears to be completely aseismic. The gap between crustal and mantle seismicity persists along-strike, but becomes smaller towards the west. The mantle seismic zone appears continuous along its shallowest level (~90-100 km depth) all the way from the Hindu Kush to the eastern Pamir. On this "rack" hang three "curtains" with high seismic activity and increasing steepness and larger maximum depths from east to west.

  2. Ozone Variations over Central Tien-Shan in Central Asia and Implications for Regional Emissions Reduction Strategies

    EPA Science Inventory

    The variability of total column ozone (TCO) and tropospheric column ozone (TrCO) was examined in Central Asia. Measurements were conducted at the Lidar Station Teplokluchenka in eastern Kyrgyzstan for one year, July 2008–July 2009. TCO was obtained using a handheld Microtops II ...

  3. Remote-sensing-based analysis of the 1996 surge of Northern Inylchek Glacier, central Tien Shan, Kyrgyzstan

    NASA Astrophysics Data System (ADS)

    Häusler, Hermann; Ng, Felix; Kopecny, Alexander; Leber, Diethard

    2016-11-01

    The evolution of Northern Inylchek Glacier and its proglacial lake - Upper Lake Merzbacher - during its 1996 surge and the surrounding decades is analyzed with remote sensing imagery. Overall retreat of the glacier from 1943 to 1996 enlarged the lake to 4 km long and ≈ 100 m deep. The surge in 1996 initiated between 12 September and 7 October and advanced the glacier by 3.7 km to override most of Upper Lake Merzbacher. The surge phase probably ended in December 1996 and involved mean flow velocities across the lower trunk of the glacier that reached 50 m d- 1 over a 32-day period. Water displaced by the surge from Upper Lake Merzbacher, totalling 1.5 × 108 m3 in volume, accelerated filling of Lower Lake Merzbacher downvalley and helped trigger this marginal ice-dammed lake to outburst in a jökulhlaup around late November/early December. The characteristics and duration of the surge render it as similar to temperate glacier surges elsewhere. It may have been facilitated by low basal friction caused by water-saturated sediments in the upper lake bed. Furthermore, bathymetric measurements show that the surge evacuated much sediment into the upper lake, causing its depth to reduce from 20 to 30 m in 1996 to 8 m by 2005 and 2 m by 2011; the corresponding deposition rates imply glacier-catchment specific mean sediment yields of 1.4 to 3.4 × 103 Mg km- 2 a- 1 in the years after the surge. Our study documents novel interactions within a cascade system of glaciers and lakes that exhibits surging and outburst-flood behavior.

  4. COMPUTER-ASSISTED INSTRUCTION, A SURVEY OF THE LITERATURE. SECOND EDITION

    DTIC Science & Technology

    A selective review of 242 documents related to computer-assisted instruction (CAI). Principal headings: CAI Reviews and Bibliographies, Applications...of CAI, Major CAI Centers, CAI Systems Studies, CAI Languages, Instructional Theory, and Program Preparation and Evaluation. An appendix lists 140 CAI programs. The review will be updated semiannually.

  5. Topics in CAI: Information Transfers and Review. Paper I; Control and Feedback in the Environment of a Computer Tutor. Paper II; Review in CAI: The Problem and an Implemented Solution.

    ERIC Educational Resources Information Center

    Siklossy, Laurent

    Two papers are included in this report. "Control and Feedback in the Environment of a Computer Tutor" investigates some control and feedback properties of a tutorial environment comprised of a student, his computer tutor, and the designer of the computer tutor. Three classes of computer tutor are described: rigid, generative, and knowledgeable.…

  6. The Development of an On-Line Laboratory for CAI and Behavioral Research (1964-1968). Technical Report.

    ERIC Educational Resources Information Center

    Judd, Wilson A.

    Psychologists and educational researchers who may be interested in installing a computer system in a behavioral science laboratory may learn from the experience gained in the development and operation of the Computer Facility at the Learning and Research Development Center of the University of Pittsburgh. Built around a PDP-7 computer, using a…

  7. Problem-Solving Behaviors as a Function of Instructional Mode, Conceptual Systems, and Field Independence in a CAI Environment.

    ERIC Educational Resources Information Center

    Lazzaro, Anthony; Szabo, Michael

    This study investigated the problem-solving performance of education undergraduates while engaged in the solution of complex, data-rich, real problems in a computer environment. The problem used was the riddle of the frozen wooly mammoths. Two instructional programs were used: the problem mode (I) engages the problem-solver in the data base with…

  8. Lessons Learned in Systemic District Reform: A Cross-District Analysis from the Comprehensive Aligned Instructional System (CAIS) Benchmarking Study

    ERIC Educational Resources Information Center

    Waters, Louise Bay; Vargo, Merrill

    2008-01-01

    Urban district reform has been hampered by the challenge of understanding and supporting the tremendous complexity of district change. Improving this understanding through actionable, practice-based research is the purpose of this study. The authors began the study with the hypothesis that achieving districts both align their instructional systems…

  9. Draft Specification of the Common APSE (Ada Programming Support Environments) Interface Set (CAIS). Version 1.1.

    DTIC Science & Technology

    1983-09-30

    Ideally, all APSE tools DD, vLAm 147 COTON or I NOv 66is oSwLEtEaUCASII SN )02 IF St. 06,SECURITY CLASSIFICATION Of THIS 1PAG9 (ft;..Data X-014 I.N...has finished all the modifications/entries that are desired, the user presses a special key (function key or enter key) which causes the modified

  10. Vegetation and climate history in arid western China during MIS2: New insights from pollen and grain-size data of the Balikun Lake, eastern Tien Shan

    NASA Astrophysics Data System (ADS)

    Zhao, Yongtao; An, Cheng-Bang; Mao, Limi; Zhao, Jiaju; Tang, Lingyu; Zhou, Aifeng; Li, Hu; Dong, Weimiao; Duan, Futao; Chen, Fahu

    2015-10-01

    Marine Isotope Stage (MIS) 2 is mostly a cold period encompassing the Last Glacial Maximum (LGM), but the regional expression of MIS2 in arid areas of China is not well known. In this paper, we use high-resolution lacustrine pollen and grain-size records from Balikun Lake to infer vegetation, lake evolution, and climate in arid western China during MIS2. Our results suggest that: 1) the regional vegetation around Balikun was mainly dominated by desert and/or desert-steppe, and Balikun Lake was relatively shallow and experienced high aeolian input during MIS2; 2) distinctive runoff from mountain glacial meltwater in the eastern parts of the Balikun basin caused a high relative abundance of Artemisia pollen during the LGM (26.5-19.2 cal kyr BP), while simultaneously the desert areas expanded as indicated by the high abundance of desert shrubs (e.g., Elaeagnaceae, Rhamnaceae, Hippophae). This cold and dry LGM climate triggered a substantial lowering of lake level; 3) an extremely cold and dry climate prevailing from 17.0 to 15.2 cal kyr BP, correlated with Heinrich event 1 (H1), would explain the low vegetation cover found then; and 4) the warm and humid Bølling/Allerød interstadial (BA: ca. 15-ca. 13 cal kyr BP) is clearly recorded in the Balikun region by the development of wetland herb communities (e.g., Poaceae, Cyperaceae, Typha), and the lake level rose due to increased runoff. Our results challenge the traditional view of cold and wet climatic conditions and high lake levels in arid western China during the LGM, and we propose that changes in local temperature modulated by July insolation was an indispensable factor in triggering vegetation evolution in the Balikun region during MIS2.

  11. Constraints on timing and rates of strath terrace formation on actively uplifting anticlines in the foreland of the Chinese Tien Shan.

    NASA Astrophysics Data System (ADS)

    Bufe, A.; Burbank, D. W.; Chen, J.; Liu, L.; Li, T.; Thompson, J. A.

    2014-12-01

    The formation of strath surfaces (fluvially created, sub-horizontal erosion surfaces) requires that the rate of lateral erosion outpaces the rate of incision of a river. The change from incision to strath cutting has commonly been linked to a decrease of incision rates due to shielding of the river bed by a thick sediment cover1. Straths are abandoned when the bed cover is reduced and incision resumes. A more recent study suggests that strath terrace formation might be linked to a change between a braided and a single-thread river2. Finally, several models have explored strath formation due to inherent dynamics of meandering systems3,4. In the foreland of the Tian Shan in northwest China, weakly consolidated Pliocene sand and siltstones are being actively uplifted at rates of 1 - 3 mm/y by a series of detachment anticlines. A number of elevated, several-kilometer-wide planation surfaces bear witness to a history of multiple strath cutting events by braided streams. In contrast, modern rivers incise into the uplifting folds creating 10 - 200 m deep canyons while the up- and downstream alluvial fans remain unincised. We use GIS analysis, field mapping, and OSL dating to describe incision and beveling of the folds. Our chronologic data reveal at least 2 - 3 beveling events over the last 40 ky on the Mutule fold. We find that lateral erosion of the bedrock during beveling events occurs at rates that are more than an order of magnitude higher than average incision rates. During times of incision (which can be tens of thousands of years long), lateral erosion rates need to be considerably lower in order to explain the formation of narrow canyons. Thus, our observations of scale, rate, and intermittency of strath cutting, seem difficult to reconcile with models that explain strath formation by variations of the incision rate1 or intrinsic meandering dynamics under steady forcing3,4. The critical requirement to explain our observations appears to be repeated changes in the rate of lateral erosion, for example, by climatically modulated changes in river lateral mobility. 1 Hancock, G. S. & Anderson, R. S. (2002), GSA Bulletin 114, 1131-1142. 2 Finnegan, N. J. & Balco, G. (2013), GSA Bulletin 125, 1114-1124. 3 Finnegan, N. J. & Dietrich, W. E. (2011), Geology 39, 143-146. 4 Limaye, A. B. S. & Lamb, M. P. (2014), JGR: Earth Surface 119, 927-950.

  12. Evaluation of Streptomyces strains isolated from herbal vermicompost for their plant growth-promotion traits in rice.

    PubMed

    Gopalakrishnan, Subramaniam; Vadlamudi, Srinivas; Bandikinda, Prakash; Sathya, Arumugam; Vijayabharathi, Rajendran; Rupela, Om; Kudapa, Himabindu; Katta, Krishnamohan; Varshney, Rajeev Kumar

    2014-01-20

    Six actinomycetes, CAI-13, CAI-85, CAI-93, CAI-140, CAI-155 and KAI-180, isolated from six different herbal vermi-composts were characterized for in vitro plant growth-promoting (PGP) properties and further evaluated in the field for PGP activity in rice. Of the six actinomycetes, CAI-13, CAI-85, CAI-93, CAI-140 and CAI-155 produced siderophores; CAI-13, CAI-93, CAI-155 and KAI-180 produced chitinase; CAI-13, CAI-140, CAI-155 and KAI-180 produced lipase; CAI-13, CAI-93, CAI-155 and KAI-180 produced protease; and CAI-13, CAI-85, CAI-140 and CAI-155 produced ß-1-3-glucanase whereas all the six actinomycetes produced cellulase, hydrocyanic acid and indole acetic acid (IAA). The actinomycetes were able to grow in NaCl concentrations of up to 8%, at pH values between 7 and 11, temperatures between 20 and 40 °C and compatible with fungicide bavistin at field application levels. In the rice field, the actinomycetes significantly enhanced tiller numbers, panicle numbers, filled grain numbers and weight, stover yield, grain yield, total dry matter, root length, volume and dry weight over the un-inoculated control. In the rhizosphere, the actinomycetes also significantly enhanced total nitrogen, available phosphorous, % organic carbon, microbial biomass carbon and nitrogen and dehydrogenase activity over the un-inoculated control. Sequences of 16S rDNA gene of the actinomycetes matched with different Streptomyces species in BLAST analysis. Of the six actinomycetes, CAI-85 and CAI-93 were found superior over other actinomycetes in terms of PGP properties, root development and crop productivity. qRT-PCR analysis on selected plant growth promoting genes of actinomycetes revealed the up-regulation of IAA genes only in CAI-85 and CAI-93.

  13. Dermal Toxicity Evaluation of Neutralized Chemical Agent Identification Sets (CAIS) with an Overview of the Dermal Toxicity of Vesicant Agents and their Degradation Products.

    DTIC Science & Technology

    1996-10-01

    100 Aquatic Toxicity: LC 5. (rainbow trout): 43,800 yg/L (96 hr) LC5 0 (blue gill): 100,000 ug/L (96 hr) LC50 ( Daphnia magna ): 28,900 ug/L (48 hr...on Foods, Drugs , and Cosmetics", In: Dermal Toxicity, pp 49-52, Assoc. of Food and Drug Officers of the U.S., Topeka, KS (1965). Draize, J.H...ingredient of powder laundry bleaches. DCDMH contains about 66% "available chlorine". Other uses of DCDYIH are: (1) as an intermediate drug and

  14. Design and Synthesis of Novel Nonsteroidal Anti-Inflammatory Drugs and Carbonic Anhydrase Inhibitors Hybrids (NSAIDs-CAIs) for the Treatment of Rheumatoid Arthritis.

    PubMed

    Bua, Silvia; Di Cesare Mannelli, Lorenzo; Vullo, Daniela; Ghelardini, Carla; Bartolucci, Gianluca; Scozzafava, Andrea; Supuran, Claudiu T; Carta, Fabrizio

    2017-02-09

    We report the synthesis of a series of hybrid compounds incorporating 6- and 7-substituted coumarins (carbonic anhydrase, CA inhibitors) derivatized with clinically used NSAIDs (indomethacin, sulindac, ketoprofen, ibuprofen, diclofenac, ketorolac, etc., cyclooxygenase inhibitors) as agents for the management of rheumatoid arthritis (RA). Most compounds were effective in inhibiting the RA overexpressed hCA IX and XII, with KI values in the low nanomolar-subnanomolar ranges. The antihyperalgesic activity of such compounds was assessed by means of the paw-pressure and incapacitance tests using an in vivo RA model. Among all tested compounds, the 7-coumarine hybrid with ibuprofen showed potent and persistent antihyperalgesic effect up to 60 min after administration.

  15. Requirements for IV&V of NATO (North Atlantic Treaty Organization) Common Ada Programming Support Environment (APSE) Interface Set (CAIS) implementation

    DTIC Science & Technology

    1988-10-01

    kernel calls ( Pesch et al. 1985), In the original specification of the kernel calls, the syntax of each system function was formally defined. However, the...26-27 August 1985. Pesch . Ilerbvi-t. Schnupp, Perter, Schaller, Hans, and Spirk, Anton Paul, "Test Case Generation U.ing Prolog." in Proceedings of the

  16. Petrological Characteristics of the Fine-Grained CAIs from the Reduced CV Chondrites Thiel Mountains 07003 and 07007, and Origin of Anorthite

    NASA Astrophysics Data System (ADS)

    Kim, H.; Choi, B.-G.

    2016-08-01

    We classified nodules of FGIs into three types; melilite-bearing without anorthite, anorthite-bearing without melilite, and both melilite- and anorthite-bearing. The former two types are dominant while the latter is relatively rare.

  17. Beyond Argumentation and Comparison/Contrast: Extending the Socrates CAI Design Principles to Classroom Teaching and the Interpretation and Production of Other Forms of Discourse.

    ERIC Educational Resources Information Center

    Bacig, Thomas D.; And Others

    1990-01-01

    Examines relationships between critical thinking and writing. Compares a pencil-and-paper and computer-assisted versions of a process/model program to a traditional composition program. Reports experimental groups showed greater argumentative powers. Extends approach to poetry and technical writing. Suggests collaborative learning potential.…

  18. Iron Isotope Systematics of Refractory Inclusions

    NASA Astrophysics Data System (ADS)

    Shollenberger, Q. R.; Brennecka, G. A.; Schuth, S.; Weyer, S.

    2016-08-01

    CAIs from CV3 and CK meteorites are investigated for their Fe isotopic compositions. Some CAIs show correlated mass-dependent and mass-independent Fe isotopic variations, indicating possible mixing between the original CAI Fe and the host rock.

  19. Effectiveness of Cognitive Skills-Based Computer-Assisted Instruction for Students with Disabilities: A Synthesis

    ERIC Educational Resources Information Center

    Weng, Pei-Lin; Maeda, Yukiko; Bouck, Emily C.

    2014-01-01

    Computer-assisted instruction (CAI) for students with disabilities can be categorized into the following categories: visual, auditory, mobile, and cognitive skills-based CAI. Cognitive-skills based CAI differs from other types of CAI largely in terms of an emphasis on instructional design features. We conducted both systematic review of…

  20. Design, Build and Validation of a Small-Scale Combustion Chamber Testing Facility

    DTIC Science & Technology

    2006-03-01

    Page Figure 1 CAI Model 300- NDIR Analyzer .......................................................................... 8 Figure 2 Signal Versus...CAI Model 300- NDIR Analyzer. Figure 1 CAI Model 300- NDIR Analyzer Using a curved reflecting surface, all of the light from an infrared source is...minimizes the contribution by interference gasses. The differential pressure system of the CAI Model 300- NDIR reduces the effect of the extra

  1. The Effect of an Intelligent Tutoring System (ITS) on Student Achievement in Algebraic Expression

    ERIC Educational Resources Information Center

    Chien, Tsai Chen; Md. Yunus, Aida Suraya; Ali, Wan Zah Wan; Bakar, Ab. Rahim

    2008-01-01

    In this experimental study, use of Computer Assisted Instruction (CAI) followed by use of an Intelligent Tutoring System (CAI+ITS) was compared to the use of CAI (CAI only) in tutoring students on the topic of Algebraic Expression. Two groups of students participated in the study. One group of 32 students studied algebraic expression in a CAI…

  2. Evaluation of Computer-Aided Instruction in a Gross Anatomy Course: A Six-Year Study

    ERIC Educational Resources Information Center

    McNulty, John A.; Sonntag, Beth; Sinacore, James M.

    2009-01-01

    Web-based computer-aided instruction (CAI) has become increasingly important to medical curricula. This multi-year study investigated the effectiveness of CAI and the factors affecting level of individual use. Three CAI were tested that differed in specificity of applicability to the curriculum and in the level of student interaction with the CAI.…

  3. Computer-Aided Instruction and Communication Skills.

    ERIC Educational Resources Information Center

    Euler, Dieter

    1990-01-01

    Investigates effect of computer-aided instruction (CAI) on acquisition of communication skills. Sketches a tutorial of the basic communication structure. Recommends confining CAI to cognitive learning because CAI cannot advance communication skills. Maintains that integrating CAI in social arrangements will allow the computer to remain an…

  4. Computer-Assisted Instruction in Debate: Possibilities and Problems.

    ERIC Educational Resources Information Center

    Sheckels, Theodore F., Jr.

    1983-01-01

    Presents justifications for computer-assisted instruction (CAI) in debate. Suggests programs that could be written. Discusses one CAI application: the use of CAI drills to train negative team members and to instruct in cross-examination skills. Includes the "Listing of CAI Drill for 1st Negative Debater." (PD)

  5. The 24 July 2008 outburst flood at the western Zyndan glacier lake and recent regional changes in glacier lakes of the Teskey Ala-Too range, Tien Shan, Kyrgyzstan

    NASA Astrophysics Data System (ADS)

    Narama, C.; Duishonakunov, M.; Kääb, A.; Daiyrov, M.; Abdrakhmatov, K.

    2010-04-01

    On 24 July 2008, a glacier lake outburst flood (GLOF) occurred at the western (w-) Zyndan glacier lake in the Tong District of Ysyk-Köl Oblast, Kyrgyzstan. The flood killed three people and numerous livestock, destroyed infrastructure, and devastated potato and barley crops as well as pastures. Tuurasuu village and a downstream reservoir on the Zyndan river escaped heavy damage because the main flood was diverted toward the Tong river. RTK-GPS and satellite data (Landsat 7 ETM+, ALOS/PRISM, and ALOS/AVNIR-2) reveal that the flood reduced the lake area from 0.0422 km2 to 0.0083 km2, discharging 437 000 m3 of water. This glacier lake was not present in a Landsat 7 ETM+ image taken on 26 April 2008. It formed rapidly over just two and half months from early May to the late July, when large amounts of snow and glacier melt water became trapped in a basin in the glacier terminus area, blocked by temporary closure of the drainage channel through the terminal moraine that included much dead-ice. In the same mountain region, most other glacier-lake expansions were not particularly large during the period from 1999-2008. Although events like the w-Zyndan glacier lake outburst occur infrequently in the high Central Asian mountains, such fast developing, short-lived lakes are particularly dangerous and not easy to monitor using satellite data. Appropriate measures to protect against such lake outburst hazards in this region include educating residents on glacier hazards and monitoring techniques, providing frequently updated maps of glacier lakes, and planning and monitoring land-use, including house locations.

  6. Review of the Parasa undulata (Cai, 1983) species group with the first conifer-feeding larva for Limacodidae and descriptions of two new species from China and Taiwan (Lepidoptera, Limacodidae)

    PubMed Central

    Wu, Shipher; Chang, Weichun

    2013-01-01

    Abstract Although the caterpillars are well-known for the stings and magnificent coloration, the systematics of Limacodidae is historically neglected and chaotic due to the difficulty in matching the larval with adult stages as well as the very conservative and convergent adult morphology. One of the biggest taxonomic problems surrounds a collective group from Southeastern Asia, termed the “green limacodid moths”, which harbours at least 90 species placed in the genus Parasa Walker, 1859 and 14 “subunits”. The P. undulata group was previously composed of 3 species from China and Taiwan, and characterized only by wing pattern. This species group is extensively studied herein with two new species described, i.e. P. viridiflamma sp. n. (Taiwan) and P. minwangi sp. n. (S. China), and discovery of female genitalia of three species, presenting new phylogenetic insights in this potentially paraphyletic genus. In addition, one limacodid larva was found to be feeding exclusively on Picea (Pinaceae) in Taiwan. Its identity, Parasa pygmy Solovyev, 2010 in P. undulata group, is confirmed through matching its COI sequence to the adult. This discovery is also biologically significant because the previous known host breadth of Parasa was of polyphagy on various angiosperm plant families. This case, therefore, represents the first record of conifer-feeding behavior in this family as well as the first of specialized herbivory in the genus. Meanwhile, the background match between Picea leaves and larval coloration is shared with other Picea-feeding insects. This phenomenon is worth of further investigation in the aspect of convergent evolution of crypsis associated with a particular plant. PMID:24194663

  7. Evaluation of computer-aided instruction in a gross anatomy course: a six-year study.

    PubMed

    McNulty, John A; Sonntag, Beth; Sinacore, James M

    2009-01-01

    Web-based computer-aided instruction (CAI) has become increasingly important to medical curricula. This multi-year study investigated the effectiveness of CAI and the factors affecting level of individual use. Three CAI were tested that differed in specificity of applicability to the curriculum and in the level of student interaction with the CAI. Student personality preferences and learning styles were measured using the Meyers Briggs Type Indicator (MBTI) and Kolb's Learning Style Inventory (LSI). Information on "computer literacy" and use of CAI was collected from student surveys. Server logs were used to quantify individual use of respective CAI. There was considerable variability in the level of utilization of each CAI by individual students. Individual use of each CAI differed and was associated with gender, MBTI preferences and learning style, but not with "computer literacy." The majority of students found the CAI useful for learning and used the CAI by themselves. Students who accessed the CAI resources most frequently scored significantly higher on exams compared with students who never accessed the resources. Our results show that medical students do not uniformly use CAI developed for their curriculum and this variability is associated with various attributes of individual students. Our data also provide evidence of the importance of understanding student preferences and learning styles when implementing CAI into the curriculum.

  8. Renewed Search for FUN (Fractionated and Unidentified Nuclear Effects) in Primitive Chondrites

    NASA Astrophysics Data System (ADS)

    Tollstrup, D. T.; Wimpenny, J. B.; Yin, Q.-Z.; Ebel, D. S.; Jacobsen, B.; Hutcheon, I. D.

    2011-03-01

    We have developed and are actively applying a method for rapidly searching for FUN CAIs in meteorite slabs of almost any dimension that does not require the removal of CAI inclusions from museum slab specimens.

  9. The Successive Contributions of Computers to Education: A Survey.

    ERIC Educational Resources Information Center

    Lelouche, Ruddy

    1998-01-01

    Shows how education has successively benefited from traditional information processing through programmed instruction and computer-assisted instruction (CAI), artificial intelligence, intelligent CAI, intelligent tutoring systems, and hypermedia techniques. Contains 29 references. (DDR)

  10. Research on the Use of Computer-Assisted Instruction.

    ERIC Educational Resources Information Center

    Craft, C. O.

    1982-01-01

    Reviews recent research studies related to computer assisted instruction (CAI). The studies concerned program effectiveness, teaching of psychomotor skills, tool availability, and factors affecting the adoption of CAI. (CT)

  11. Effectiveness of Computer-Assisted Instruction in Technical Education: A Meta-Analysis.

    ERIC Educational Resources Information Center

    Yaakub, Mohammad Naim; Finch, Curtis R.

    2001-01-01

    A meta-analysis of 21 studies compared the effectiveness of computer-assisted instruction (CAI) with traditional instruction. Results showed that CAI focusing on higher-order learning in technical education was more effective. (Contains 38 references.) (JOW)

  12. Strategies in Computer-Assisted Instruction: A Selective Overview.

    ERIC Educational Resources Information Center

    Block, Karen K.

    The history of some computer-assisted instruction (CAI) strategies is traced. A number of components of computerized instruction systems are described and explanations provided on the influence these components have in the development and production of a CAI system. A description of the interaction between a student and a CAI system is presented…

  13. Computer-Assisted Instruction: Potential for College Level Instruction and Review of Research.

    ERIC Educational Resources Information Center

    Dwyer, Francis M.

    Some basic concepts and types of computer assisted instruction (CAI) are presented, and their application in college and university settings is considered. CAI literature of the late 1960's--including descriptions of specific CAI systems together with studies of instructional effectiveness, learning time, and student attitudes--is then summarized.…

  14. Computer-Assisted Instruction In Dental Diagnosis; A Systematic Product Development.

    ERIC Educational Resources Information Center

    Barber, Thomas K.; Sokolow, Sonya

    A developmental project created and field tested a computer-assisted instructional (CAI) unit in dental diagnosis. The main objectives were to determine 1) if, after having received CAI, the dental student could determine whether a patient had a clinical need for space management and 2) if the dental student's attitude toward CAI and space…

  15. Improving Computer-Assisted Instruction in Teaching Higher-Order Skills

    ERIC Educational Resources Information Center

    Sinclair, Kelsey J.; Renshaw, Carl E.; Taylor, Holly A.

    2004-01-01

    Computer-assisted instruction (CAI) has been shown to enhance rote memory skills and improve higher order critical thinking skills. The challenge now is to identify what aspects of CAI improve which specific higher-order skills. This study focuses on the effectiveness of using CAI to teach logarithmic graphing and dimensional analysis. Two groups…

  16. Effectiveness of Using Computer-Assisted Supplementary Instruction for Teaching the Mole Concept.

    ERIC Educational Resources Information Center

    Yalcinalp, Serpil; And Others

    1995-01-01

    Examines the effect of computer-assisted instruction (CAI) on students' understanding of chemical formulas and mole concept, and their attitudes toward chemistry and CAI. Reports that students who used the CAI accompanied with lectures scored significantly higher and demonstrated significant improvement in attitudes compared to the control group…

  17. Computer Assisted Instruction. Education Automation Monograph Series, [Number One].

    ERIC Educational Resources Information Center

    Stolurow, Lawrence M.

    Computer-assisted instruction (CAI) attacks one of the greatest problems of education--how to get sufficient variety in educational materials to teach each individual without requiring a group of trained personnel to prepare all possible variations. CAI permits individualization electronically. CAI can be used to train problem solving, for drill…

  18. Student Achievement and the Use of the Program "Study Island"

    ERIC Educational Resources Information Center

    Bernard, Benjamin Thomas

    2013-01-01

    Computer Aided Instruction (CAI) has been used for many years in an attempt to increase student achievement. Districts have spent millions of dollars implementing different forms of CAI that may or may not be working. This study was an attempt to describe one such district and its CAI implementation. The study sought to complete three tasks. The…

  19. Teaching Law with Computers: A Collection of Essays.

    ERIC Educational Resources Information Center

    Burris, Russell; And Others

    The use of the computer in teaching law is examined in this collection of essays. Discussed are the development of law-related programmed workbooks, predecessors to computer aided instruction (CAI); research findings and their implications for the design of law-related CAI exercises; advantages and limitations of CAI programs in law; and attempts…

  20. Effects of Computer-Assisted Instruction on Correct Responding and Procedural Integrity during Early Intensive Behavioral Intervention

    ERIC Educational Resources Information Center

    Kodak, Tiffany; Fisher, Wayne W.; Clements, Andrea; Bouxsein, Kelly J.

    2011-01-01

    Computer-assisted instruction (CAI) is used to teach a variety of skills to children with developmental disabilities. However, it remains unclear whether CAI or direct instruction from a therapist produces better learning outcomes. In addition, no studies have evaluated the ease of training therapists to implement CAI versus direct instruction. In…

  1. The Effects of Computer-Assisted Instruction on Number Combination Skill in At-Risk First Graders

    ERIC Educational Resources Information Center

    Fuchs, Lynn S.; Fuchs, Douglas; Hamlet, Carol L.; Powell, Sarah R.; Capizzi, Andrea M.; Seethaler, Pamela M.

    2006-01-01

    The purpose of this pilot study was to assess the potential for computer-assisted instruction (CAI) to enhance number combination skill among children with concurrent risk for math disability and reading disability. A secondary purpose was to examine the effects of CAI on spelling. At-risk students were assigned randomly to math or spelling CAI,…

  2. Efficacy of Computer-Assisted Instruction for the Development of Early Literacy Skills in Young Children

    ERIC Educational Resources Information Center

    Macaruso, Paul; Rodman, Alyson

    2011-01-01

    Two studies examined the efficacy of using computer-assisted instruction (CAI) to supplement a phonics-based reading curriculum for preschoolers and kindergartners in an urban public school system. The CAI programs provided exercises in phonological awareness and basic phonics skills. We compared treatment classes using CAI with control classes…

  3. Computer-Assisted Instruction, Media Richness, and College Student Performance

    ERIC Educational Resources Information Center

    Timmerman, C. Erik; Kruepke, Kristine A.

    2006-01-01

    This meta analysis examines the effect of computer-assisted instruction (CAI) upon college student performance, addresses the impact of various study characteristics upon effects, and explores how media richness theory may predict CAI performance gains. Findings indicate that student performance gains are larger for CAI than traditional…

  4. Analysis of Studies of the Effects of Computer-Assisted Instruction on the Mathematics Performance of Students with Learning Disabilities

    ERIC Educational Resources Information Center

    Seo, You-Jin; Bryant, Diane Pedrotty

    2009-01-01

    The purpose of this study was to conduct a meta-study of computer-assisted instruction (CAI) studies in mathematics for students with learning disabilities (LD) focusing on examining the effects of CAI on the mathematics performance of students with LD. This study examined a total of 11 mathematics CAI studies, which met the study selection…

  5. "It's High-Tech, but Is It Better?": Applications of Technology in Psychiatry Education

    ERIC Educational Resources Information Center

    Krain, Lewis P.; Bostwick, J. Michael; Sampson, Shirlene

    2007-01-01

    Objective: This article reviews the existing literature on the use of computer assisted instruction (CAI) in the field of psychiatry to answer the questions, 1) Is CAI an effective tool for teaching psychiatry? and 2) What are the best methods for studying CAI in a real-world training environment? Method: A Medline search was conducted for…

  6. Computer-Aided Instruction for Adult Professionals: A Research Report.

    ERIC Educational Resources Information Center

    Shaw, Doris Smith

    1992-01-01

    Discusses computer-aided instruction (CAI) for adult learners and describes research conducted at the U.S. Army Construction Engineering Research Laboratory to study the impact of CAI on design professionals, i.e., architects and engineers. Attitudes of adult professionals are examined, and design requirements for a CAI system for professionals…

  7. A Computer-Based Instructional Simulation for Teacher Training and Evaluation in Special Education. Report No. R-65.

    ERIC Educational Resources Information Center

    Cantrell, William H.; Edwards, Agnes M.

    The development of a computer-assisted instruction simulation (CARE-S) in the Computer-Assisted Instruction (CAI) Center at the University of Texas in Austin is documented. The work is an outgrowth of the CARE 1 CAI program entitled "Early Identification of Handicapping Conditions in Children" which was developed in the CAI laboratory at…

  8. Drills vs. Games--Any Differences? A Pilot Study.

    ERIC Educational Resources Information Center

    McMullen, David W.

    This study investigated the effect of informational, drill, and game format computer-assisted instruction (CAI) on the achievement, retention, and attitude toward instruction of sixth-grade science students (N=37). An informational CAI lesson on Halley's Comet was administered to three randomly selected groups of sixth-grade students. A CAI drill…

  9. User Interface Improvements in Computer-Assisted Instruction, the Challenge.

    ERIC Educational Resources Information Center

    Chalmers, P. A.

    2000-01-01

    Identifies user interface problems as they relate to computer-assisted instruction (CAI); reviews the learning theories and instructional theories related to CAI user interface; and presents potential CAI user interface improvements for research and development based on learning and instructional theory. Focuses on screen design improvements.…

  10. Oxygen isotopic abundances in calcium- aluminum-rich inclusions from ordinary chondrites: implications for nebular heterogeneity.

    PubMed

    McKeegan, K D; Leshin, L A; Russell, S S; MacPherson, G J

    1998-04-17

    The oxygen isotopic compositions of two calcium-aluminum-rich inclusions (CAIs) from the unequilibrated ordinary chondrite meteorites Quinyambie and Semarkona are enriched in 16O by an amount similar to that in CAIs from carbonaceous chondrites. This may indicate that most CAIs formed in a restricted region of the solar nebula and were then unevenly distributed throughout the various chondrite accretion regions. The Semarkona CAI is isotopically homogeneous and contains highly 16O-enriched melilite, supporting the hypothesis that all CAI minerals were originally 16O-rich, but that in most carbonaceous chondrite inclusions some minerals exchanged oxygen isotopes with an external reservoir following crystallization.

  11. Complete Androgen Insensitivity Syndrome in Three Sisters

    PubMed Central

    Verim, Levent

    2014-01-01

    Disorders of sexual development (DSD) are congenital anomalies due to atypical development of chromosomes, gonads and anatomy. Complete androgen insensitivity syndrome (CAIS), also known as testicular feminization (TF) is a rare DSD disease. The majority of CAIS patients apply to hospital with the complaint of primary amenorrhea or infertility. Given that CAIS patients are all phenotypically female while having 46, XY karyotypes, CAIS diagnosis should be disclosed in an age-appropriate manner preferably by a mental health professional. Cases are reported here for three 46XY siblings consistent with CAIS. PMID:24520507

  12. Cytoplasmic pH influences cytoplasmic calcium in MC3T3-E1 osteoblast cells

    NASA Technical Reports Server (NTRS)

    Lin, H. S.; Hughes-Fulford, M.; Kumegawa, M.; Pitts, A. C.; Snowdowne, K. W.

    1993-01-01

    We found that the cytoplasmic concentration of calcium (Cai) of MC3T3-E1 osteoblasts was influenced by the type of pH buffer we used in the perfusing medium, suggesting that intracellular pH (pHi) might influence Cai. To study this effect, the Cai and pHi were monitored as we applied various experimental conditions known to change pHi. Exposure to NH4Cl caused a transient increase in both pHi and Cai without a change in extracellular pH (pHo). Decreasing pHo and pHi by lowering the bicarbonate concentration of the medium decreased Cai, and increasing pHi by the removal of 5% CO2 increased Cai. Clamping pHi to known values with 10 microM nigericin, a potassium proton ionophore, also influenced Cai: acid pHi lowered Cai, whereas alkaline pHi increased it. The rise in Cai appears to be very sensitive to the extracellular concentration of calcium, suggesting the existence of a pH-sensitive calcium influx mechanism. We conclude that physiologic changes in pH could modulate Cai by controlling the influx of calcium ions and could change the time course of the Cai transient associated with hormonal activation.

  13. Application of Polarimetric-Interferometric Phase Coherence Optimization (PIPCO) Procedure to SIR-C/X-SAR Tien-Shan Tracks 122.20(94 Oct. 08)/154.20(94 Oct. 09) Repeat-Orbit C/L-Band Pol-D-InSAR Imag

    NASA Technical Reports Server (NTRS)

    Boerner, W. M.; Mott, H.; Verdi, J.; Darizhapov, D.; Dorjiev, B.; Tsybjito, T.; Korsunov, V.; Tatchkov, G.; Bashkuyev, Y.; Cloude, S.; Papathanassiou, K.; Pottier, E.; Lee, J.; Ainsworth, T.; Schuler, D.; Grandi, G.; Rosen, P.; Peltzer, G.

    1998-01-01

    During the past decade, Radar Polarimetry has established itself as a mature science and advanced technology in high resolution POL-SAR imaging, image target characterization and selective image feature extraction.

  14. EVIDENCE FOR MULTIPLE SOURCES OF {sup 10}Be IN THE EARLY SOLAR SYSTEM

    SciTech Connect

    Wielandt, Daniel; Krot, Alexander N.; Bizzarro, Martin; Nagashima, Kazuhide; Huss, Gary R.; Ivanova, Marina A.

    2012-04-01

    Beryllium-10 is a short-lived radionuclide (t{sub 1/2} = 1.4 Myr) uniquely synthesized by spallation reactions and inferred to have been present when the solar system's oldest solids (calcium-aluminum-rich inclusions, CAIs) formed. Yet, the astrophysical site of {sup 10}Be nucleosynthesis is uncertain. We report Li-Be-B isotope measurements of CAIs from CV chondrites, including CAIs that formed with the canonical {sup 26}Al/{sup 27}Al ratio of {approx}5 Multiplication-Sign 10{sup -5} (canonical CAIs) and CAIs with Fractionation and Unidentified Nuclear isotope effects (FUN-CAIs) characterized by {sup 26}Al/{sup 27}Al ratios much lower than the canonical value. Our measurements demonstrate the presence of four distinct fossil {sup 10}Be/{sup 9}Be isochrons, lower in the FUN-CAIs than in the canonical CAIs, and variable within these classes. Given that FUN-CAI precursors escaped evaporation-recondensation prior to evaporative melting, we suggest that the {sup 10}Be/{sup 9}Be ratio recorded by FUN-CAIs represents a baseline level present in presolar material inherited from the protosolar molecular cloud, generated via enhanced trapping of galactic cosmic rays. The higher and possibly variable apparent {sup 10}Be/{sup 9}Be ratios of canonical CAIs reflect additional spallogenesis, either in the gaseous CAI-forming reservoir, or in the inclusions themselves: this indicates at least two nucleosynthetic sources of {sup 10}Be in the early solar system. The most promising locale for {sup 10}Be synthesis is close to the proto-Sun during its early mass-accreting stages, as these are thought to coincide with periods of intense particle irradiation occurring on timescales significantly shorter than the formation interval of canonical CAIs.

  15. Arrhythmogenic consequences of intracellular calcium waves.

    PubMed

    Xie, Lai-Hua; Weiss, James N

    2009-09-01

    Intracellular Ca(2+) (Ca(i)(2+)) waves are known to cause delayed afterdepolarizations (DADs), which have been associated with arrhythmias in cardiac disease states such as heart failure, catecholaminergic polymorphic ventricular tachycardia, and digitalis toxicity. Here we show that, in addition to DADs, Ca(i)(2+) waves also have other consequences relevant to arrhythmogenesis, including subcellular spatially discordant alternans (SDA, in which the amplitude of the local Ca(i)(2+) transient alternates out of phase in different regions of the same cell), sudden repolarization changes promoting the dispersion of refractoriness, and early afterdepolarizations (EADs). Ca(i)(2+) was imaged using a charge-coupled device-based system in fluo-4 AM-loaded isolated rabbit ventricular myocytes paced at constant or incrementally increasing rates, using either field stimulation, current clamp, or action potential (AP) clamp. Ca(i)(2+) waves were induced by Bay K 8644 (50 nM) + isoproterenol (100 nM), or low temperature. When pacing was initiated during a spontaneous Ca(i)(2+) wave, SDA occurred abruptly and persisted during pacing. Similarly, during rapid pacing, SDA typically arose suddenly from spatially concordant alternans, due to an abrupt phase reversal of the subcellular Ca(i)(2+) transient in a region of the myocyte. Ca(i)(2+) waves could be visualized interspersed with AP-triggered Ca(i)(2+) transients, producing a rich variety of subcellular Ca(i)(2+) transient patterns. With free-running APs, complex Ca(i)(2+) release patterns were associated with DADs, EADs, and sudden changes in AP duration. These findings link Ca(i)(2+) waves directly to a variety of arrhythmogenic phenomena relevant to the intact heart.

  16. Comment on "ancient asteroids enriched in refractory inclusions".

    PubMed

    Hezel, Dominik C; Russell, Sara S

    2008-11-14

    Sunshine et al. (Reports, 25 April 2008, p. 514) reported that certain asteroids contain 30 +/- 10 volume percent calcium- and aluminum-rich inclusions (CAIs). We contend that the amount of CAIs in CV chondrites is two to three times as low as the 10 volume percent assumed by the authors; thus, we question whether the CAI-rich bodies they studied are indeed older than known asteroids or formed before the injection of (26)Al into the solar nebula.

  17. A Study of Knowledge-Based Systems for Photo Interpretation.

    DTIC Science & Technology

    1980-06-01

    OIL (15] CAI Electronics SOPHIE (10] Medicine GUIDON [14] Learning Chemistry Meta-DENDRAL (i] Agriculture INDUCE [19] Mathematics AM [40] Intelligent...16 6. Computer-Aided Instruction: GUIDON Three types of traditional computer-aided instruction (CAI) are often distinguished: frame-oriented drill-and...systems have an obvious contribution to make to CAI. The GUIDON system developed by Clancey at Stanford exploits the MYCIN knowledge base about

  18. Growth of calcium-aluminum-rich inclusions by coagulation and fragmentation in a turbulent protoplanetary disk: Observations and simulations

    NASA Astrophysics Data System (ADS)

    Charnoz, Sébastien; Aléon, Jérôme; Chaumard, Noël; Baillié, Kévin; Taillifet, Esther

    2015-05-01

    Whereas it is generally accepted that calcium-aluminum-rich inclusions (CAIs) from chondritic meteorites formed in a hot environment in the solar protoplanetary disk, the conditions of their formation remain debated. Recent laboratory studies of CAIs have provided new kind of data: their size distributions. We report that size distributions of CAIs measured in laboratory from sections of carbonaceous chondrites have a power law size distribution with cumulative size exponent between -1.7 and -1.9, which translates into cumulative size exponent between -2.5 and -2.8 after correction for sectioning. To explain these observations, numerical simulations were run to explore the growth of CAIs from micrometer to centimeter sizes, in a hot and turbulent protoplanetary disk through the competition of coagulation and fragmentation. We show that the size distributions obtained in growth simulations are in agreement with CAIs size distributions in meteorites. We explain the CAI sharp cut-off of their size distribution at centimeter sizes as the direct result from the famous fragmentation barrier, provided that CAI fragment for impact velocities larger than 10 m/s. The growth/destruction timescales of millimeter- and centimeter-sized CAIs is inversely proportional to the local dust/gas ratio and is about 10 years at 1300 K and up to 104 years at 1670 K. This implies that the most refractory CAIs are expected to be smaller in size owing to their long growth timescale compared to less refractory CAIs. Conversely, the least refractory CAIs could have been recycled many times during the CAI production era which may have profound consequences for their radiometric age.

  19. Acta Aeronautica et Astronautica Sinica.

    DTIC Science & Technology

    1981-12-29

    SPECIMENS 68 WITH SINGLE EDGE NOTCH Liu Ligeng, Chen Xianxi and Cai Qigong (Central Iron and Steel Research Institute) ON THE DESIGN OF TRANSONIC TURBINE...et al, Mechanism of Overload Effect on Fatigue Crack Propagation in Aluminum Alloy. Eng. Fract. Mech. 1978 No. 2. (13) Chen Hu, Cai Qigong et al...this paper. 67b J-INTEGRAL EXPERIMENTAL CALIBRATION OF SHEET SPECIMENS WITH SINGLE EDGE NOTCH Lui Ligeng, Chen Xianxi and Cai Qigong (Central Iron and

  20. Medical Treatment for Acromegaly does not Increase the Risk of Central Adrenal Insufficiency: A Long-Term Follow-Up Study.

    PubMed

    Ceccato, F; Lizzul, L; Zilio, M; Barbot, M; Denaro, L; Emanuelli, E; Alessio, L; Rolma, G; Manara, R; Saller, A; Boscaro, M; Scaroni, C

    2016-08-01

    Central adrenal insufficiency (CAI) in acromegaly may be related to pituitary adenoma or induced by various medical treatments, transsphenoidal neurosurgery (TNS) or radiotherapy (RT), alone or combined. We assessed the role of all available treatments for acromegaly in inducing CAI. We retrospectively studied 97 patients. CAI was diagnosed if morning serum cortisol was <138 nmol/l, or if its response was inadequate in the low-dose short synacthen test. Seventy-four subjects underwent TNS (and 17 of whom also underwent RT), and 23 were on primary medical therapy: overall we diagnosed 21 cases of CAI. Duration of acromegaly, invasion of cavernous sinus, disease control, and type of medical treatment were much the same for patients with and without CAI, which was identified in 18% of patients (10/57) after one TNS, and in 53% (9/17) after RT (p=0.01); repeat surgery increased the risk of CAI (p=0.02). The risk of CAI onset during the follow-up was lower among patients treated with TNS or medical therapy than after RT (p=0.035). Medical treatment did not raise the risk of CAI, whereas a 5- and 4-fold higher risk of CAI was associated with repeat TNS and RT, respectively. Basal or stimulated cortisol levels were similar among acromegalic patients without CAI and matched controls with nonsecreting pituitary lesions. A significant proportion of patients with acromegaly developed CAI over time. While primary or secondary medical treatment did not contribute to the risk of CAI, repeat TNS and RT correlated with pituitary-adrenal axis impairment.

  1. Chirped Airy-Gaussian beam in a medium with a parabolic potential

    NASA Astrophysics Data System (ADS)

    Zhang, Liping; Deng, Fu; Peng, Yulian; Chen, Bo; Peng, Xi; Li, Dongdong; Deng, Dongmei

    2017-01-01

    By solving the normalized dimensionless linear parabolic (Schrödinger-like) equations in the paraxial approximation, we can obtain the analytic solutions of the chirped Airy-Gaussian (CAiG) beam in a medium with a parabolic potential. We study the propagation properties of the finite energy CAiG beam in a parabolic potential and the influence of the distribution factor and the chirped factor on the CAiG beam. The propagation of the CAiG beam changes drastically with the distribution factor increasing: the CAiG beam tends to the chirped Airy beam when the distribution factor is very small; while as the distribution factor increases further, the CAiG beam tends to the chirped Gaussian beam. At the same time, the CAiG beam with a chirp has big changes when the chirped factor is increasing: the multi-peak structure is not obvious, the accelerated velocity and the peak intensity are larger, but the period does not change; when the CAiG beam has a quadratic chirp, the maximum intensity of the CAiG beam becomes smaller and the envelope is gradually smoother with the increasing of the chirped factor.

  2. Novel androgen receptor gene mutation in patient with complete androgen insensitivity syndrome.

    PubMed

    Ning, Ye; Zhang, Feng; Zhu, Yong; Chen, Huixing; Lu, Jianqi; Li, Zheng

    2012-07-01

    To present a rare case of a patient probably with complete androgen insensitivity syndrome (CAIS) and studied its potential genetic cause. A 24-year-old woman with a normal-appearing vulva and vagina presented to us because of primary amenorrhea. Imaging studies showed no uterus or ovary development but inguinal cryptorchism. Histopathologic examination revealed normal testicular structures. Sequencing the CAIS-associated androgen receptor gene revealed a novel missense mutation of T to G (F698L). A novel androgen receptor gene mutation in the ligand binding domain was detected in the present patient with CAIS, supporting the important role of an androgen receptor defect in the etiology of CAIS.

  3. Effect of computer-aided instruction versus traditional modes on student PT's learning musculoskeletal special tests

    NASA Astrophysics Data System (ADS)

    Ford, Gregory Scott

    2007-12-01

    Title. Effect of computer-aided instruction versus traditional modes on student PT's learning musculoskeletal special tests. Problem. Lack of quantitative evidence to support the use of computer-aided instruction (CAI) in PT education for both the cognitive and psychomotor domains and lack of qualitative support as to an understanding why CAI may or may not be effective. Design. 3 group single-blind pre-test, immediate post-test, final post-test repeated measures with qualitative survey for the CAI group. Methods. Subjects were randomly assigned to CAI, live demonstration or textbook learning groups. Three novel special tests were instructed. Analysis of performance on written and practical examinations was conducted across the 3 repeated measures. A qualitative survey was completed by the CAI group post intervention. Results. CAI is equally as effective as live demonstration and textbook learning of musculoskeletal special tests in the cognitive domain, however, CAI was superior to live demonstration and textbook instruction at final post-testing. Significance. The significance of this research is that a gap in the literature of PT education needs to be bridged as it pertains to the effect of CAI on learning in both the cognitive and psychomotor domains as well as attempt to understand why CAI results in certain student performance. The methods of this study allowed for a wide range of generalizability to any and all PT programs across the country.

  4. Trace element and petrologic clues to the formation of forsterite-bearing Ca-Al-rich inclusions in the Allende meteorite

    NASA Technical Reports Server (NTRS)

    Wark, D. A.; Boynton, W. V.; Keays, R. R.; Palme, H.

    1987-01-01

    New trace element and petrographic data are presented for the TE, 818a, 110-A forsterite-bearing Ca-Al-rich inclusions (CAIs) from the Allende meteorite; these form a continuum with type B1 and B2 CAIs, and are here accordingly designated 'type B3'. Evidence is adduced to the effect that 818a was strongly reheated and modified in the nebula after its initial crystallization. A three-stage formation process is required for 818a, involving crystallization of the primary CAI, reheating and partial volatilization of Mg and Si from the outer portion of the CAI, and a metasomatic alteration of the melilite-rich mantle.

  5. 182Hf-182W age dating of a 26Al-poor inclusion and implications for the origin of short-lived radioisotopes in the early Solar System.

    PubMed

    Holst, Jesper C; Olsen, Mia B; Paton, Chad; Nagashima, Kazuhide; Schiller, Martin; Wielandt, Daniel; Larsen, Kirsten K; Connelly, James N; Jørgensen, Jes K; Krot, Alexander N; Nordlund, Ake; Bizzarro, Martin

    2013-05-28

    Refractory inclusions [calcium-aluminum-rich inclusions, (CAIs)] represent the oldest Solar System solids and provide information regarding the formation of the Sun and its protoplanetary disk. CAIs contain evidence of now extinct short-lived radioisotopes (e.g., (26)Al, (41)Ca, and (182)Hf) synthesized in one or multiple stars and added to the protosolar molecular cloud before or during its collapse. Understanding how and when short-lived radioisotopes were added to the Solar System is necessary to assess their validity as chronometers and constrain the birthplace of the Sun. Whereas most CAIs formed with the canonical abundance of (26)Al corresponding to (26)Al/(27)Al of ∼5 × 10(-5), rare CAIs with fractionation and unidentified nuclear isotope effects (FUN CAIs) record nucleosynthetic isotopic heterogeneity and (26)Al/(27)Al of <5 × 10(-6), possibly reflecting their formation before canonical CAIs. Thus, FUN CAIs may provide a unique window into the earliest Solar System, including the origin of short-lived radioisotopes. However, their chronology is unknown. Using the (182)Hf-(182)W chronometer, we show that a FUN CAI recording a condensation origin from a solar gas formed coevally with canonical CAIs, but with (26)Al/(27)Al of ∼3 × 10(-6). The decoupling between (182)Hf and (26)Al requires distinct stellar origins: steady-state galactic stellar nucleosynthesis for (182)Hf and late-stage contamination of the protosolar molecular cloud by a massive star(s) for (26)Al. Admixing of stellar-derived (26)Al to the protoplanetary disk occurred during the epoch of CAI formation and, therefore, the (26)Al-(26)Mg systematics of CAIs cannot be used to define their formation interval. In contrast, our results support (182)Hf homogeneity and chronological significance of the (182)Hf-(182)W clock.

  6. 182Hf–182W age dating of a 26Al-poor inclusion and implications for the origin of short-lived radioisotopes in the early Solar System

    PubMed Central

    Holst, Jesper C.; Olsen, Mia B.; Paton, Chad; Nagashima, Kazuhide; Schiller, Martin; Wielandt, Daniel; Larsen, Kirsten K.; Connelly, James N.; Jørgensen, Jes K.; Krot, Alexander N.; Nordlund, Åke; Bizzarro, Martin

    2013-01-01

    Refractory inclusions [calcium–aluminum-rich inclusions, (CAIs)] represent the oldest Solar System solids and provide information regarding the formation of the Sun and its protoplanetary disk. CAIs contain evidence of now extinct short-lived radioisotopes (e.g., 26Al, 41Ca, and 182Hf) synthesized in one or multiple stars and added to the protosolar molecular cloud before or during its collapse. Understanding how and when short-lived radioisotopes were added to the Solar System is necessary to assess their validity as chronometers and constrain the birthplace of the Sun. Whereas most CAIs formed with the canonical abundance of 26Al corresponding to 26Al/27Al of ∼5 × 10−5, rare CAIs with fractionation and unidentified nuclear isotope effects (FUN CAIs) record nucleosynthetic isotopic heterogeneity and 26Al/27Al of <5 × 10−6, possibly reflecting their formation before canonical CAIs. Thus, FUN CAIs may provide a unique window into the earliest Solar System, including the origin of short-lived radioisotopes. However, their chronology is unknown. Using the 182Hf–182W chronometer, we show that a FUN CAI recording a condensation origin from a solar gas formed coevally with canonical CAIs, but with 26Al/27Al of ∼3 × 10−6. The decoupling between 182Hf and 26Al requires distinct stellar origins: steady-state galactic stellar nucleosynthesis for 182Hf and late-stage contamination of the protosolar molecular cloud by a massive star(s) for 26Al. Admixing of stellar-derived 26Al to the protoplanetary disk occurred during the epoch of CAI formation and, therefore, the 26Al–26Mg systematics of CAIs cannot be used to define their formation interval. In contrast, our results support 182Hf homogeneity and chronological significance of the 182Hf–182W clock. PMID:23671077

  7. A Method for Evaluating Competency in Assessment and Management of Suicide Risk

    ERIC Educational Resources Information Center

    Hung, Erick K.; Binder, Renee L.; Fordwood, Samantha R.; Hall, Stephen E.; Cramer, Robert J.; McNiel, Dale E.

    2012-01-01

    Objective: Although health professionals increasingly are expected to be able to assess and manage patients' risk for suicide, few methods are available to evaluate this competency. This report describes development of a competency-assessment instrument for suicide risk-assessment (CAI-S), and evaluates its use in an objective structured clinical…

  8. Using Dynamic Software in Mathematics: The Case of Reflection Symmetry

    ERIC Educational Resources Information Center

    Tatar, Enver; Akkaya, Adnan; Kagizmanli, Türkan Berrin

    2014-01-01

    This study was carried out to examine the effects of computer-assisted instruction (CAI) using dynamic software on the achievement of students in mathematics in the topic of reflection symmetry. The study also aimed to ascertain the pre-service mathematics teachers' opinions on the use of CAI in mathematics lessons. In the study, a mixed research…

  9. Computer-Assisted Instruction at Stanford.

    ERIC Educational Resources Information Center

    Suppes, Patrick

    Programs for computer-assisted instruction (CAI) which were developed at Stanford University from 1963-70 are described, and prospects for CAI in the 1970's are considered briefly. The programs include ones in arithmetic, logic, and reading for elementary grades and in basic Russian and remedial algebra for college students. Of these, the logic…

  10. Computer-Assisted Instruction: Stanford's 1965-66 Arithmetic Program.

    ERIC Educational Resources Information Center

    Suppes, Patrick; And Others

    A review of the possibilities and challenges of computer-assisted instruction (CAI), and a brief history of CAI projects at Stanford serve to give the reader the context of the particular program described and analyzed in this book. The 1965-66 arithmetic drill-and-practice program is described, summarizing the curriculum and project operation. An…

  11. B. F. Skinner's Technology of Teaching.

    ERIC Educational Resources Information Center

    Green, John O.

    1984-01-01

    B. F. Skinner provides advice for educators on several issues related to computer-assisted instruction (CAI). Some pitfalls of programed instruction in the 1960s which CAI may also face today, aversive control, courseware design, and use of computer graphics are among the areas explored. (JN)

  12. A Comparison of Computer-Assisted Instruction and Tutorials in Hematology and Oncology.

    ERIC Educational Resources Information Center

    Garrett, T. J.; And Others

    1987-01-01

    A study comparing the effectiveness of computer-assisted instruction (CAI) and small group instruction found no significant difference in medical student achievement in oncology but higher achievement through small-group instruction in hematology. Students did not view CAI as more effective, but saw it as a supplement to traditional methods. (MSE)

  13. Renal Diet Therapy--A Computer-Assisted Instruction Model.

    ERIC Educational Resources Information Center

    Schroeder, Lois; Thiele, Victoria F.

    1981-01-01

    A computer-assisted instruction (CAI) unit was designed to teach renal diet therapy. Utilizing this unit, differences in performance and attitudes between traditionally taught and CAI taught students (N=34), and differences in achievement between students in two nutrition fields were assessed. (DS)

  14. Computer Assisted Instruction in Mathematics Can Improve Students' Test Scores: A Study.

    ERIC Educational Resources Information Center

    Brown, Frank

    This research assessed the academic impact of a computer-assisted instructional (CAI) software program to teach mathematics. The research hypothesis states that the use of the CAI program will produce superior academic achievement in mathematics for students who use the program compared to students instructed in mathematics without the program.…

  15. An Overview of the Computer as Teacher: A Progress Report of a Research Project to Introduce Diagnostic Testing and Computerized Instruction into the Composition Program at Northeast Missouri State University.

    ERIC Educational Resources Information Center

    Cottey, Patricia

    Suspecting that computer assisted instruction (CAI) could help teach grammar to freshman composition students at Northeast Missouri State University (NMSU), three instructors received a research grant to begin a program of testing basic writing skills and to initiate CAI instruction for those students who needed help in the tested areas. A survey…

  16. Sigal's Ineffective Computer-Based Practice of Arithmetic: A Case Study.

    ERIC Educational Resources Information Center

    Hativa, Nira

    1988-01-01

    A student was observed practicing arithmetic with a computer-assisted instruction (CAI) system. She enjoyed practice and believed that it helped. However, she consistently failed to solve problems on the computer that she could do with pencil and paper. This paper suggests reasons for her problems and draws implications for CAI. (Author/PK)

  17. Individual Differences and Learner Control I: Program Development and Investigation of Control Over Mnemonics in Computer-Assisted Instruction. AFHRL-TR-74-3. Interim Report.

    ERIC Educational Resources Information Center

    Judd, Wilson A.; And Others

    The reported research was designed to investigate the impact of learner control on performance and anxiety in a computer-assisted instruction (CAI) task. The first phase entailed the development of a two-hour CAI program on the identification of edible plants. The second phase was experimentation to determine the effectiveness of learner control.…

  18. Learning with Computers in Small Groups: Cognitive and Affective Outcomes.

    ERIC Educational Resources Information Center

    Mevarech, Zemira R.; And Others

    1991-01-01

    Examines the effects of cooperative and individualistic computer-assisted instruction (CAI) programs on cognitive and affective variables in Israeli grade six mathematics classes. Analyses of the data indicate that students who used CAI for drill and practice in pairs performed better than students who used the same program individually. (30…

  19. The Application and Evaluation of PLATO IV in AF Technical Training.

    ERIC Educational Resources Information Center

    Mockovak, William P.; And Others

    The Air Force has been plagued with the rising cost of technical training and has increasingly turned to computer-assisted instruction (CAI) for better cost effectiveness. Toward this aim a trial of PLATO IV, a CAI system utilizing a graphic display and centered at the University of Illinois, was initiated at the Chanute and Sheppard training…

  20. Some Conceptual Issues in Computer-Assisted Instruction.

    ERIC Educational Resources Information Center

    Kearsley, Greg P.

    1977-01-01

    The design of CAI for individualization of instruction and its relationship to broader educational systems is detailed. Effectiveness of CAI in various student populations and subject matter is presented, as well as design methods, and research studies in cognitive psychology and artificial intelligence are reviewed. (RAO)

  1. Inhibition of pro-inflammatory cytokines in tumour associated macrophages is a potential anti-cancer mechanism of carboxyamidotriazole.

    PubMed

    Ju, Rui; Wu, Danwei; Guo, Lei; Li, Juan; Ye, Caiying; Zhang, Dechang

    2012-05-01

    Carboxyamidotriazole (CAI) has not only direct anti-cancer activities, but also anti-inflammation effects in a variety of inflammatory animal models. In the present study, we investigated whether macrophages, which are important both in cancer and inflammation, could be regulated by CAI. The results showed that CAI could inhibit tumour necrosis factor-α (TNF-α) production in macrophages in various environments, including those isolated from peritoneal cavity of adjuvant-induced arthritis (AA) rats, from Lewis lung carcinoma (LLC) transplanted tumours and those induced by LLC cells in vitro. Dexamethasone (DEX), one of the pro-inflammatory cytokines inhibitors, could enhance CAI's inhibition of LLC cells proliferation and invasion in macrophages and LLC cells co-culture systems, as well as the tumour growth in vivo. However, DEX failed to enhance CAI's inhibition of LLC cells proliferation when LLC cells were cultured alone, suggesting that the combination of CAI and DEX exerted great anti-tumour effects probably by acting on macrophages in the tumour environment. Over all, we found CAI could act on macrophages and regulate the production of TNF-α not only in inflammatory diseases but also in tumour microenvironment, which might be another anti-tumour mechanism of CAI.

  2. Using the Computer to Teach Methods and Interpretative Skills in the Humanities: Implementing a Project.

    ERIC Educational Resources Information Center

    Jones, Bruce William

    The results of implementing computer-assisted instruction (CAI) in two religion courses and a logic course at California State College, Bakersfield, are examined along with student responses. The main purpose of the CAI project was to teach interpretive skills. The most positive results came in the logic course. The programs in the New Testament…

  3. Design Considerations in Development of Minicomputer-Based Computer Aided Instructional Hardware Systems.

    ERIC Educational Resources Information Center

    Wells, C. H.

    A minicomputer-based computer-assisted instructional (CAI) system was designed at the University of Texas Medical Branch in an attempt to lower both the excessive hardware costs and the inordinate amount of time required for the preparation of each hour of instructional material associated with traditional CAI systems. A prototype system with an…

  4. Effect of isosmotic removal of extracellular Ca2+ and of membrane potential on cell volume in muscle cells.

    PubMed

    Peña-Rasgado, C; McGruder, K D; Summers, J C; Rasgado-Flores, H

    1994-09-01

    Isosmotic removal of extracellular Ca2+ (Cao) and changes in membrane potential (Vm) are frequently performed manipulations. Using isolated voltage-clamped barnacle muscle cells, we studied the effect of these manipulations on isosmotic cell volume. Replacing Cao by Mg2+ induced 1) verapamil-sensitive extracellular Na(+)-dependent membrane depolarization, 2) membrane depolarization-dependent cell volume reduction in cells whose sarcoplasmic reticulum (SR) was presumably loaded with Ca2+ [intracellular Ca2+ (Cai)-loaded cells], and 3) cell volume increase in cells whose SR was presumably depleted of Ca2+ (Cai-depleted cells) or in Cai-loaded cells whose Vm was held constant. Membrane depolarization induced 1) volume reduction in Cai-loaded cells or 2) verapamil-sensitive volume increase in Cai-depleted cells. This suggests tha, in Cai-loaded cells, membrane depolarization induces SR Ca2+ release, which in turn promotes volume reduction. Conversely, in Cai-depleted cells, the depolarization activates Na+ influx through a verapamil-sensitive pathway leading to the volume increase. This pathway is also revealed when Cao is removed in either Cai-depleted cells or in cells whose Vm is held constant.

  5. Computer-Assisted Instruction: A Survey of the Literature, Third Edition.

    ERIC Educational Resources Information Center

    Hickey, Albert E., Ed.

    References to literature published before July 1968 on computer-assisted instruction (CAI) are presented in this survey. Nine subject area chapters, providing the framework for the references, deal with general statements on CAI (including benefits, state of the art, problems, roles in society, financial support, and trends); applications of CAI…

  6. Reasoning from Incomplete Knowledge.

    ERIC Educational Resources Information Center

    Collins, Allan M.; And Others

    People use a variety of plausible, but uncertain inferences to answer questions about which their knowledge is incomplete. Such inferential thinking and reasoning is being incorporated into the SCHOLAR computer-assisted instruction (CAI) system. Socratic tutorial techniques in CAI systems such as SCHOLAR are described, and examples of their…

  7. Intelligent Computer-Assisted Instruction: A Review and Assessment of ICAI Research and Its Potential for Education.

    ERIC Educational Resources Information Center

    Dede, Christopher J.; And Others

    The first of five sections in this report places intelligent computer-assisted instruction (ICAI) in its historical context through discussions of traditional computer-assisted instruction (CAI) linear and branching programs; TICCIT and PLATO IV, two CAI demonstration projects funded by the National Science Foundation; generative programs, the…

  8. Is Computer-Aided Instruction an Effective Tier-One Intervention for Kindergarten Students at Risk for Reading Failure in an Applied Setting?

    ERIC Educational Resources Information Center

    Kreskey, Donna DeVaughn; Truscott, Stephen D.

    2016-01-01

    This study investigated the use of computer-aided instruction (CAI) as an intervention for kindergarten students at risk for reading failure. Headsprout Early Reading (Headsprout 2005), a type of CAI, provides internet-based, reading instruction incorporating the critical components of reading instruction cited by the National Reading Panel (NRP…

  9. Evaluation of Imagine Learning English, a Computer-Assisted Instruction of Language and Literacy for Kindergarten Students

    ERIC Educational Resources Information Center

    Longberg, Pauline Oliphant

    2012-01-01

    As computer assisted instruction (CAI) becomes increasingly sophisticated, its appeal as a viable method of literacy intervention with young children continues despite limited evidence of effectiveness. The present study sought to assess the impact of one such CAI program, "Imagine Learning English" (ILE), on both the receptive…

  10. Computer-Assisted Instruction in the N.W.T.

    ERIC Educational Resources Information Center

    Garraway, Tom

    For the past seven years, the Division of Educational Research Services at the University of Alberta has been operating an IBM 1500 CAI system. This paper describes demonstration projects set up in anticipation of the establishment of remote CAI in the North West Territories. These include a moon landing simulation program; a diagnostic program in…

  11. The Application of Computer Technology to the Instruction of Undereducated Adults. Final Report.

    ERIC Educational Resources Information Center

    Cole, James L.

    Two different uses of computers in instruction are Computer Assisted Instruction (CAI) and Computer Managed Instruction (CMI). CMI is primarily concerned with data management in the instructional process, and CAI is the use of computers to control the instructional process itself. The uses of computers in instruction can be described in four main…

  12. Computer-Assisted Instruction of Early Academic Skills.

    ERIC Educational Resources Information Center

    Hitchcock, Caryl H.; Noonan, Mary Jo

    2000-01-01

    Five preschool students with disabilities received direct instruction on matching shapes, colors, and numbers or letters, followed by guided practice using constant time delay under two conditions: computer-assisted instruction (CAI) with interactive software and teacher-assisted instruction (TAI). CAI was either equal or superior to TAI across…

  13. Religious Studies as a Test-Case For Computer-Assisted Instruction In The Humanities.

    ERIC Educational Resources Information Center

    Jones, Bruce William

    Experiences with computer-assisted instructional (CAI) programs written for religious studies indicate that CAI has contributions to offer the humanities and social sciences. The usefulness of the computer for presentation, drill and review of factual material and its applicability to quantifiable data is well accepted. There now exist…

  14. RASCAL: A Rudimentary Adaptive System for Computer-Aided Learning.

    ERIC Educational Resources Information Center

    Stewart, John Christopher

    Both the background of computer-assisted instruction (CAI) systems in general and the requirements of a computer-aided learning system which would be a reasonable assistant to a teacher are discussed. RASCAL (Rudimentary Adaptive System for Computer-Aided Learning) is a first attempt at defining a CAI system which would individualize the learning…

  15. Gross Anatomy Videos: Student Satisfaction, Usage, and Effect on Student Performance in a Condensed Curriculum

    ERIC Educational Resources Information Center

    Topping, Daniel B.

    2014-01-01

    Anatomy educators are being tasked with delivering the same quantity and quality of material in the face of fewer classroom and laboratory hours. As a result they have turned to computer-aided instruction (CAI) to supplement and augment curriculum delivery. Research on the satisfaction and use of anatomy videos, a form of CAI, on examination…

  16. Brain responses to sexual images in 46,XY women with complete androgen insensitivity syndrome are female-typical.

    PubMed

    Hamann, Stephan; Stevens, Jennifer; Vick, Janice Hassett; Bryk, Kristina; Quigley, Charmian A; Berenbaum, Sheri A; Wallen, Kim

    2014-11-01

    Androgens, estrogens, and sex chromosomes are the major influences guiding sex differences in brain development, yet their relative roles and importance remain unclear. Individuals with complete androgen insensitivity syndrome (CAIS) offer a unique opportunity to address these issues. Although women with CAIS have a Y chromosome, testes, and produce male-typical levels of androgens, they lack functional androgen receptors preventing responding to their androgens. Thus, they develop a female physical phenotype, are reared as girls, and develop into women. Because sexually differentiated brain development in primates is determined primarily by androgens, but may be affected by sex chromosome complement, it is currently unknown whether brain structure and function in women with CAIS is more like that of women or men. In the first functional neuroimaging study of (46,XY) women with CAIS, typical (46,XX) women, and typical (46, XY) men, we found that men showed greater amygdala activation to sexual images than did either typical women or women with CAIS. Typical women and women with CAIS had highly similar patterns of brain activation, indicating that a Y chromosome is insufficient for male-typical human brain responses. Because women with CAIS produce male-typical or elevated levels of testosterone which is aromatized to estradiol these results rule out aromatization of testosterone to estradiol as a determinate of sex differences in patterns of brain activation to sexual images. We cannot, however, rule out an effect of social experience on the brain responses of women with CAIS as all were raised as girls.

  17. Mathematics and At-Risk Adult Learners: Would Technology Help?

    ERIC Educational Resources Information Center

    Li, Qing; Edmonds, K. A.

    2005-01-01

    In this paper, we examine the effects of computer-assisted instruction (CAI) on adult at-risk learners in fundamental mathematics education. This examination includes comparing the results of adult learners experiencing learning with CAI with those who do not. Further, we explore and present viable teaching and learning strategies for at-risk…

  18. Teacher Use of Computer-Assisted Instruction for Young Inattentive Students: Implications for Implementation and Teacher Preparation

    ERIC Educational Resources Information Center

    Murray, Desiree W.; Rabiner, David L.

    2014-01-01

    Teacher preparation and training appear limited in the area of computer-assisted instruction (CAI) as well as more general instruction and management for students with disabilities including those with attention problems. Research suggests that CAI is a promising intervention for young inattentive students, with several inherent advantages;…

  19. Benefits of Computer-Assisted Instruction to Support Reading Acquisition in English Language Learners

    ERIC Educational Resources Information Center

    Macaruso, Paul; Rodman, Alyson

    2011-01-01

    Young children who are English language learners (ELLs) face major challenges in learning to read English. This study examined whether computer-assisted instruction (CAI) can be beneficial to ELL kindergartners enrolled in bilingual classes. The CAI programs provided systematic and structured exercises in developing phonological awareness and…

  20. Secondary School Students' Attitudes towards Mathematics Computer--Assisted Instruction Environment in Kenya

    ERIC Educational Resources Information Center

    Mwei, Philip K.; Wando, Dave; Too, Jackson K.

    2012-01-01

    This paper reports the results of research conducted in six classes (Form IV) with 205 students with a sample of 94 respondents. Data represent students' statements that describe (a) the role of Mathematics teachers in a computer-assisted instruction (CAI) environment and (b) effectiveness of CAI in Mathematics instruction. The results indicated…

  1. Community College Psychology Faculty Uses and Attitudes toward Computer-Assisted Instruction

    ERIC Educational Resources Information Center

    Glasgow, Yvette; Keim, Marybelle C.

    2005-01-01

    Full-time and part-time psychology faculty at 100 publicly-supported community colleges in 4 midwestern states were surveyed to determine their use of computer-assisted instruction (CAI). Attitudes about CAI and faculty access and availability of computers for classroom and personal use were also determined. Of the respondents, 97% had computers…

  2. Using Computer Assisted Instruction to Teach Science Facts to Students with Moderate to Severe Disabilities

    ERIC Educational Resources Information Center

    Berrong, Amy Ketterer

    2011-01-01

    Previous research has found the use of computer-assisted instruction (CAI) to be effective in teaching skills to a variety of populations. Students with and without disabilities have been taught a variety of skills including social skills and core academic content using CAI. Students with moderate to severe disabilities (MSD) have been taught a…

  3. Effects of Computer-Assisted Comprehension Training in Less Skilled Comprehenders in Second Grade: A One-Year Follow-Up Study

    ERIC Educational Resources Information Center

    Potocki, Anna; Ecalle, Jean; Magnan, Annie

    2013-01-01

    This study examines the effects of a new CAI program designed to remediate text comprehension difficulties in less skilled comprehenders at the beginning of learning to read. In a randomized control trial design, two groups of second grade children experiencing comprehension difficulties were selected and trained using two CAI programs. One of…

  4. Examining the Impact of Teacher-Generated Feedback in Online Math Courses Where Computer-Assisted Instruction Is Embedded

    ERIC Educational Resources Information Center

    Hoey, Rebecca Simon

    2012-01-01

    Teacher feedback and interaction are factors of success and satisfaction in online courses, but courses designed for computer-assisted instruction (CAI) require less communication between a teacher and student. The goal of this research was to examine the impact of teachers' feedback in online self-paced secondary math courses where CAI was…

  5. The Efficacy of Computer-Assisted Instruction for Advancing Literacy Skills in Kindergarten Children

    ERIC Educational Resources Information Center

    Macaruso, Paul; Walker, Adelaide

    2008-01-01

    We examined the benefits of computer-assisted instruction (CAI) as a supplement to a phonics-based reading curriculum for kindergartners in an urban public school system. The CAI program provides systematic exercises in phonological awareness and letter-sound correspondences. Comparisons were made between children in classes receiving a sufficient…

  6. Efficacy of Teachtown: Basics Computer-Assisted Intervention for the Intensive Comprehensive Autism Program in Los Angeles Unified School District

    ERIC Educational Resources Information Center

    Whalen, Christina; Moss, Debbie; Ilan, Aaron B.; Vaupel, Manya; Fielding, Paul; MacDonald, Kevin; Cernich, Shannon; Symon, Jennifer

    2010-01-01

    Computer Assisted Instruction (CAI) has shown increased popularity recently and there are many studies showing promise for this approach for children with Autism Spectrum Disorders (ASD). However, there are no between-subject studies to date assessing the efficacy of CAI with this population. In this study, 47 preschool and K-1 students in ASD…

  7. A note on cement in asteroids

    NASA Astrophysics Data System (ADS)

    Bilalbegović, G.

    2016-09-01

    Cement mineral tobermorite was formed in hydrothermal experiments on alternation of calcium-aluminum-rich inclusions (CAIs) in carbonaceous chondrite meteorites. Unidentified bands at 14 μm were measured for CAIs and the matrix of the Allende meteorite sample, as well as for Hektor and Agamemnon asteroids. The presence of cement nanoparticles may explain the feature at 14 μm.

  8. Effects of Computer-Assisted Instruction for Struggling Elementary Readers with Disabilities

    ERIC Educational Resources Information Center

    Regan, Kelley; Berkeley, Sheri; Hughes, Melissa; Kirby, Suzanne

    2014-01-01

    Despite a lack of conclusive evidence, many researchers in the field view computer-assisted instruction (CAI) as an opportunity for improved instruction for students with disabilities. This study examined the effects of a CAI program, Lexia Strategies for Older Students (SOS)™ on the word recognition skills of four, upper elementary students with…

  9. Curriculum Alignment Initiative Report to the Coordinating Board for Higher Education

    ERIC Educational Resources Information Center

    Missouri Department of Higher Education, 2008

    2008-01-01

    It is recommended that the Coordinating Board for Higher Education approve the Curriculum Alignment Initiative (CAI) report, with recognition of the dynamic nature of competencies. It is further recommended that the board direct the Commissioner of Higher Education to make the CAI Report available online to interested government agencies and…

  10. Benefits of Computer-Assisted Instruction for Struggling Readers in Middle School

    ERIC Educational Resources Information Center

    Macaruso, Paul; Rodman, Alyson

    2009-01-01

    This study investigated the benefits of computer-assisted instruction (CAI) for middle-school students attending remedial reading classes. As a supplement to a strong language-based reading curriculum, a CAI programme that works on strengthening phonics word identification skills was provided to students in the treatment group. These students were…

  11. Using Computer-Assisted Interviewing to Consult with Children with Autism Spectrum Disorders: An Exploratory Study

    ERIC Educational Resources Information Center

    Barrow, Wilma; Hannah, Elizabeth F.

    2012-01-01

    This article explores the use of computer-assisted interviewing (CAI) as a tool for consulting with children with autism spectrum disorders (ASD). This is considered within the context of a research study which utilized one CAI programme, "In My Shoes", to investigate children and young people's views of provision, support, and participation in…

  12. Comparative Effects of Two Modes of Computer-Assisted Instructional Package on Solid Geometry Achievement

    ERIC Educational Resources Information Center

    Gambari, Isiaka Amosa; Ezenwa, Victoria Ifeoma; Anyanwu, Romanus Chogozie

    2014-01-01

    The study examined the effects of two modes of computer-assisted instructional package on solid geometry achievement amongst senior secondary school students in Minna, Niger State, Nigeria. Also, the influence of gender on the performance of students exposed to CAI(AT) and CAI(AN) packages were examined. This study adopted a pretest-posttest…

  13. Complete androgen insensitivity syndrome--a review.

    PubMed

    Oakes, Meghan B; Eyvazzadeh, Aimee D; Quint, Elisabeth; Smith, Yolanda R

    2008-12-01

    This review paper highlights important diagnostic and therapeutic concerns for girls with Complete Androgen Insensitivity Syndrome (CAIS). CAIS is an androgen receptor defect disorder associated with vaginal and uterine agenesis in women with a 46,XY karyotype. The major clinical issues surrounding this syndrome include timing of gonadectomy, hormone replacement, vaginal dilation, and attention to psychological issues.

  14. The Effectiveness of Computer-Assisted Instruction in Teaching Introductory Statistics

    ERIC Educational Resources Information Center

    Basturk, Ramazan

    2005-01-01

    The focus of this study is to demonstrate and discuss the educational advantages of Computer Assisted Instruction (CAI). A quasi-experimental design compared learning outcomes of participants in an introductory statistics course that integrated CAI to participants in a Lecture-only introductory statistics course. Reviews of participants' identical…

  15. A Comparative Evaluation of Computer Based and Non-Computer Based Instructional Strategies.

    ERIC Educational Resources Information Center

    Emerson, Ian

    1988-01-01

    Compares the computer assisted instruction (CAI) tutorial with its non-computerized pedagogical roots: the Socratic Dialog with Skinner's Programmed Instruction. Tests the effectiveness of a CAI tutorial on diffusion and osmosis against four other interactive and non-interactive instructional strategies. Notes computer based strategies were…

  16. Framework for Computer Assisted Instruction Courseware: A Case Study.

    ERIC Educational Resources Information Center

    Betlach, Judith A.

    1987-01-01

    Systematically investigates, defines, and organizes variables related to production of internally designed and implemented computer assisted instruction (CAI) courseware: special needs of users; costs; identification and definition of realistic training needs; CAI definition and design methodology; hardware and software requirements; and general…

  17. An Overview of Computer-Assisted Instruction for Adult Educators.

    ERIC Educational Resources Information Center

    Dick, Walter

    After a detailed history and definition of Computer-Assisted Instruction (which identifies drill and practice, tutorial, and problem-solving activities as comprising CAI), the development and implementation of a college level computer based multimedia physics course is described as an example of tutorial activities in CAI for those interested in…

  18. Computer Aided Instruction: A Study of Student Evaluations and Academic Performance

    ERIC Educational Resources Information Center

    Collins, David; Deck, Alan; McCrickard, Myra

    2008-01-01

    Computer aided instruction (CAI) encompasses a broad range of computer technologies that supplement the classroom learning environment and can dramatically increase a student's access to information. Criticism of CAI generally focuses on two issues: it lacks an adequate foundation in educational theory and the software is difficult to implement…

  19. Computer Assisted Instruction Remediation Program for Credit Course in Bibliographic Instruction.

    ERIC Educational Resources Information Center

    Sugranes, Maria R.; And Others

    1986-01-01

    Describes and evaluates computer assisted instruction (CAI) remedial program used for credit course in bibliographic instruction, noting need, requirements, development, planning, and implementation. Statistics are presented to support principle that CAI can be valuable instructional methodology for bibliographic instruction programs. Test-retake…

  20. In Search of New Ideas, Research Findings, and Emerging Technologies? Here's Where To Find Them.

    ERIC Educational Resources Information Center

    Powell, Gary C.

    There are many avenues available to computer-assisted instruction (CAI) practitioners and developers in search of access to new ideas, research findings, and emerging technologies that will assist them in developing CAI products. Seven such avenues are described in detail: (1) graduate student interns, who bring unique insights, theory, and…