Sample records for chisels
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Penetration tests to study the mechanical tribological properties of chisel type knife
NASA Astrophysics Data System (ADS)
Vlăduţoiu, L.; Chişiu, G.; Andrei, T.; Predescu, A.; Muraru, C.; Vlăduţ, V.
2017-02-01
The goal of this study was to analyze the behaviour of chisel knife type penetration in a certain type of sand. A series of penetration tests were carried out with chisel knife type, the answer to penetration depending mainly on nature, shape, size of knife and operating parameters such as speed, depth and working conditions. Tests were conducted in work conditions with wet sand and dry sand and determined force of resistance to penetration of the chisel knife type to a certain depth.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Bachan, John
Chisel is a new open-source hardware construction language developed at UC Berkeley that supports advanced hardware design using highly parameterized generators and layered domain-specific hardware languages. Chisel is embedded in the Scala programming language, which raises the level of hardware design abstraction by providing concepts including object orientation, functional programming, parameterized types, and type inference. From the same source, Chisel can generate a high-speed C++-based cycle-accurate software simulator, or low-level Verilog designed to pass on to standard ASIC or FPGA tools for synthesis and place and route.
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RUNNER BOX MAINTENANCE. FRANK FEHER USES A COMPRESSED AIRPOWERED CHISEL ...
RUNNER BOX MAINTENANCE. FRANK FEHER USES A COMPRESSED AIR-POWERED CHISEL TO CHIP OUT CONGEALED METAL IN PREPARATION FOR ANOTHER HEAT. - American Brass Foundry, 70 Sayre Street, Buffalo, Erie County, NY
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Terpitz, Ulrich; Zimmermann, Dirk
2010-01-01
The Eppendorf Piezo-Power Microdissection (PPMD) system uses a tungsten needle (MicroChisel) oscillating in a forward-backward (vertical) mode to cut cells from surrounding tissue. This technology competes with laser-based dissection systems, which offer high accuracy and precision, but are more expensive and require fixed tissue. In contrast, PPMD systems can dissect freshly prepared tissue, but their accuracy and precision is lower due to unwanted lateral vibrations of the MicroChisel. Especially in tissues where elasticity is high, these vibrations can limit the cutting resolution or hamper the dissection. Here we describe a cost-efficient and simple glass capillary-encapsulation modification of MicroChisels for effective attenuation of lateral vibrations. The use of modified MicroChisels enables accurate and precise tissue dissection from highly elastic material.
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Determining the coating thickness of tablets by chiseling and image analysis.
Sasić, Slobodan
2010-09-15
Several tablets are chiseled and imaged in order to determine the variation in the coating thickness with the addition of the coating material (weight-gain). Chiseling is carried out with an ultrasonic chisel. The chiseled tablets are imaged in full and these images are exported into programming language Matlab in order to numerically analyze all the pixels along one side of the tablet. The coating thickness is statistically assessed at four cutting depths for three tablets obtained from four weight-gain experiments, a total of 48 images. The coating layer is clearly visible and determinable in the 'white-light' images even for the smallest weight gain of 1% but with sizeable errors due to the diffused boundaries between the coating and the core on one, and the coating and the background on the other side. Addition of the coating material clearly increases the coating thickness which is found to be somewhat higher at the top of the tablets than at the edges. Two approaches for assessment of the coating thickness are tested and are found to be in a very good agreement except for the thinnest coating layer. Copyright 2010 Elsevier B.V. All rights reserved.
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The impact of digging on craniodental morphology and integration.
McIntosh, A F; Cox, P G
2016-12-01
The relationship between the form and function of the skull has been the subject of a great deal of research, much of which has concentrated on the impact of feeding on skull shape. However, there are a number of other behaviours that can influence craniodental morphology. Previous work has shown that subterranean rodents that use their incisors to dig (chisel-tooth digging) have a constrained cranial shape, which is probably driven by a necessity to create high bite forces at wide gapes. Chisel-tooth-digging rodents also have an upper incisor root that is displaced further back into the cranium compared with other rodents. This study quantified cranial shape and upper incisors of a phylogenetically diverse sample of rodents to determine if chisel-tooth-digging rodents differ in craniodental morphology. The study showed that the crania of chisel-tooth-digging rodents shared a similar place in morphospace, but a strong phylogenetic signal within the sample meant that this grouping was nonsignificant. It was also found that the curvature of the upper incisor in chisel-tooth diggers was significantly larger than in other rodents. Interestingly, most subterranean rodents in the sample (both chisel-tooth and scratch diggers) had upper incisors that were better able to resist bending than those of terrestrial rodents, presumably due to their similar diets of tough plant materials. Finally, the incisor variables and cranial shape were not found to covary consistently in this sample, highlighting the complex relationship between a species' evolutionary history and functional morphology. © 2016 European Society For Evolutionary Biology. Journal of Evolutionary Biology © 2016 European Society For Evolutionary Biology.
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Comparison of Piezosurgery and Hammer-Chisel in Endoscopic Dacryocystorhinostomy.
Çukurova, Ibrahim; Bulğurcu, Suphi; Arslan, Ilker Burak; Dikilitaş, Bünyamin
2018-05-08
In this study, we compared the advantages and disadvantages of piezosurgery and hammer-chisel used in endoscopic dacryocystorhinostomy (EDCR). Between January 2012 and January 2016, 10 women and 8 men in whom piezosurgery was used (group 1) and 11 women and 7 men in whom hammer-chisel was used (group 2) during EDCR operations were compared retrospectively. Recurrence, operation time, postoperative bleeding, and operative cost were evaluated in patients who were followed for an average of 11.8 months. In addition, visual analogue scale (VAS) was used to assess pain at 6 hours postoperatively. No recurrence was observed in group 1, but recurrence was observed in 2 patients in group 2 (P = 0.685). There was no postoperative bleeding in both groups. The mean duration of operation was 30.6 ± 8.2 minutes in group 1 and 46.8 ± 9.5 minutes in group 2 (P = 0.038). The VAS score in group 1 was 2.7 ± 1.4 and the VAS score in group 2 was 5.8 ± 2.2 (P = 0.01). Piezosurgery costs an additional $325 for each patient while the use of the hammer-chisel does not incur additional costs. Piezosurgery causes shorter operation time, less recurrence, and less pain when compared with hammer-chisel.
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Objective analysis of impressed chisel toolmarks
Spotts, Ryan; Chumbley, L. Scott
2015-08-06
Historical and recent challenges to the practice of comparative forensic examination have created a driving force for the formation of objective methods for toolmark identification. In this study, fifty sequentially manufactured chisels were used to create impression toolmarks in lead (500 toolmarks total). An algorithm previously used to statistically separate known matching and nonmatching striated screwdriver marks and quasi-striated plier marks was used to evaluate the chisel marks. Impression toolmarks, a more complex form of toolmark, pose a more difficult test for the algorithm that was originally designed for striated toolmarks. Lastly, results show in this instance that the algorithmmore » can separate matching and nonmatching impression marks, providing further validation of the assumption that toolmarks are identifiably unique.« less
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Manzano-Moreno, Francisco J; Herrera-Briones, Francisco J; Linares-Recatala, Macarena; Ocaña-Peinado, Francisco M; Reyes-Botella, Candela; Vallecillo-Capilla, Manuel F
2015-03-01
The aim of this study was to compare levels of bacterial contamination of autogenous bone collected when using low-speed drilling, a back-action chisel, and a bone filter. Bone tissue samples were taken from 31 patients who underwent surgical extraction of their third lower molars. Before surgical removal of the molar, bone particles were collected by a low-speed drill or a back-action chisel. Then, a stringent aspiration protocol was applied during the ostectomy to collect particulate bone by a bone filter. Processing of samples commenced immediately by incubation in an anaerobic or a CO2-rich atmosphere. The number of colony-forming units (CFUs) was determined at 48 hours of culture. No significant difference in the number of CFUs per milliliter was observed between the low-speed drilling group and the back-action chisel group in the anaerobic or CO2-rich condition (P = .34). However, significantly more micro-organisms were found in the bone filter group than in the low-speed drilling group or the back-action chisel group in the anaerobic and CO2-rich conditions (P < .001). Particulate bone harvested with low-speed drilling or a back-action chisel is safer for use as an autograft than are bone particles collected with a bone filter. These results suggest that bone obtained from low-speed drilling is safe and straightforward to harvest and could be the method of choice for collecting particulate bone. Further research is needed to lower the bacterial contamination levels of autogenous bone particles used as graft material. Copyright © 2015 American Association of Oral and Maxillofacial Surgeons. Published by Elsevier Inc. All rights reserved.
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McIntosh, Andrew F; Cox, Philip G
2016-10-01
The African mole-rats (Bathyergidae) are a family of rodents highly adapted for life underground. Previous research has shown that chisel-tooth digging mole-rats (which use their incisors to dig burrows) are clearly distinguishable from scratch diggers (which only use the forelimbs to tunnel) on the basis of morphology of the skull, and that the differences are linked to the production of high bite forces and wide gapes. We hypothesized that the skull of a chisel-tooth digging mole-rat would perform better at wider gapes than that of a scratch digging mole-rat during incisor biting. To test this hypothesis, we created finite-element models of the cranium of the scratch digging Bathyergus suillus and the chisel-tooth digging Fukomys mechowii , and loaded them to simulate incisor bites at different gapes. Muscle loads were scaled such that the ratio of force to surface area was the same in both models. We measured three performance variables: overall stress across the cranium, mechanical efficiency of biting and degree of deformation across the skull. The Fukomys model had a more efficient incisor bite at all gapes, despite having greater average stress across the skull. In addition, the Fukomys model deformed less at wider gapes, whereas the Bathyergus model deformed less at narrower gapes. These properties of the cranial morphology of Fukomys and Bathyergus are congruent with their respective chisel-tooth and scratch digging behaviours and, all other factors being equal, would enable the more efficient production of bite force at wider gapes in Fukomys . However, in vivo measurements of muscle forces and activation patterns are needed to fully understand the complex biomechanics of tooth digging.
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NASA Astrophysics Data System (ADS)
McIntosh, Andrew F.; Cox, Philip G.
2016-10-01
The African mole-rats (Bathyergidae) are a family of rodents highly adapted for life underground. Previous research has shown that chisel-tooth digging mole-rats (which use their incisors to dig burrows) are clearly distinguishable from scratch diggers (which only use the forelimbs to tunnel) on the basis of morphology of the skull, and that the differences are linked to the production of high bite forces and wide gapes. We hypothesized that the skull of a chisel-tooth digging mole-rat would perform better at wider gapes than that of a scratch digging mole-rat during incisor biting. To test this hypothesis, we created finite-element models of the cranium of the scratch digging Bathyergus suillus and the chisel-tooth digging Fukomys mechowii, and loaded them to simulate incisor bites at different gapes. Muscle loads were scaled such that the ratio of force to surface area was the same in both models. We measured three performance variables: overall stress across the cranium, mechanical efficiency of biting and degree of deformation across the skull. The Fukomys model had a more efficient incisor bite at all gapes, despite having greater average stress across the skull. In addition, the Fukomys model deformed less at wider gapes, whereas the Bathyergus model deformed less at narrower gapes. These properties of the cranial morphology of Fukomys and Bathyergus are congruent with their respective chisel-tooth and scratch digging behaviours and, all other factors being equal, would enable the more efficient production of bite force at wider gapes in Fukomys. However, in vivo measurements of muscle forces and activation patterns are needed to fully understand the complex biomechanics of tooth digging.
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Gao, Yongbo; Jiang, Ai; Li, Boyou; Yang, Liming
2011-08-01
To study the effect of piezosurgery in the extraction of mandibular impacted third molars. 228 mandibular impacted third molars with relative difficulty for extraction according to the scheme of degree of difficulty for extraction were included in the study, and were divided into two groups (114 teeth each group): Test group (treated by piezosurgery), control group (treated by traditional chisel osteotomy). The surgery time and pain, restriction of mouth opening and facial swelling after surgery, were evaluated in both groups. The average surgery time was (16 +/- 5.2) min in test group and (30 +/- 8.7) min in control group. The surgery time, pain, facial swelling rate, and restriction of mouth opening were lower than control group (P<0.05). Compared with traditional chisel osteotomy, the average surgery time with piezosurgery was significantly shorter and the complications are obviously reduced.
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Sculpting Computational-Level Models.
Blokpoel, Mark
2017-06-27
In this commentary, I advocate for strict relations between Marr's levels of analysis. Under a strict relationship, each level is exactly implemented by the subordinate level. This yields two benefits. First, it brings consistency for multilevel explanations. Second, similar to how a sculptor chisels away superfluous marble, a modeler can chisel a computational-level model by applying constraints. By sculpting the model, one restricts the (potentially infinitely large) set of possible algorithmic- and implementational-level theories. Copyright © 2017 Cognitive Science Society, Inc.
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Investigation into the Effects of Textural Properties on Cuttability Performance of a Chisel Tool
NASA Astrophysics Data System (ADS)
Tumac, Deniz; Copur, Hanifi; Balci, Cemal; Er, Selman; Avunduk, Emre
2018-04-01
The main objective of this study is to investigate the effect of textural properties of stones on cutting performance of a standard chisel tool. Therewithal, the relationships between textural properties and cutting performance parameters and physical and mechanical properties were statistically analyzed. For this purpose, physical and mechanical property tests and mineralogical and petrographic analyses were carried out on eighteen natural stone samples, which can be grouped into three fundamentally different geological origins, i.e., metamorphic, igneous, and sedimentary. Then, texture coefficient analyses were performed on the samples. To determine the cuttability of the stones; the samples were cut with a portable linear cutting machine using a standard chisel tool at different depths of cut in unrelieved (non-interactive) cutting mode. The average and maximum forces (normal and cutting) and specific energy were measured, and the obtained values were correlated with texture coefficient, packing weighting, and grain size. With reference to the relation between depth of cut and cutting performance of the chisel tool for three types of natural stone groups, specific energy decreases with increasing depth of cut, and cutting forces increase in proportion to the depth of cut. The same is observed for the relationship between packing weighting and both of specific energy and cutter forces. On the other hand, specific energy and the forces decrease while grain size increases. Based on the findings of the present study, texture coefficient has strong correlation with specific energy. Generally, the lower depth of cut values in cutting tests shows higher and more reliable correlations with texture coefficient than the increased depth of cut. The results of cutting tests show also that, at a lower depth of cut (less than 1.5 mm), even stronger correlations can be observed between texture coefficient and cutting performance. Experimental studies indicate that cutting performance of chisel tools can be predicted based on texture coefficients of the natural stones.
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Morphology of bone particles after harvesting with 4 different devices.
Papadimitriou, Dimitrios E V; Schmidt, Erich C; Caton, Jack G; Romanos, Georgios E
2013-04-01
Autogenous bone is routinely used for regeneration of osseous defects around teeth and implants, and different instruments are available for bone harvesting. The purpose of this study was to describe the morphology of bone particles after harvesting with 4 different instruments. Bone particles were harvested from fresh cow ribs with 2 different types of back action chisels, a safescraper and a sonic device. The samples were examined morphologically using light microscopy and scanning electron microscopy. The bone particles after the back action chisel I had an appearance similar to "pencil shavings." With the back action chisel II, they were like thin paper with an "accordion bellows" appearance. After removal with the safescraper, they had an irregular shape (with an irregular surface) resembling "crushed stone." Finally, the appearance of the bone particles obtained with the sonic device was homogenous, condensed and continuous, and had a "seaweed" appearance. Harvesting of bone particles with 4 different devices produce distinctly difference sizes and shapes, which may influence the results of grafting procedures.
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Runoff losses of sediment and phosphorus from no-till and cultivated soils receiving dairy manure.
Verbree, David A; Duiker, Sjoerd W; Kleinman, Peter J A
2010-01-01
Managing manure in no-till systems is a water quality concern because surface application of manure can enrich runoff with dissolved phosphorus (P), and incorporation by tillage increases particulate P loss. This study compared runoff from well-drained and somewhat poorly drained soils under corn (Zea mays, L.) production that had been in no-till for more than 10 yr. Dairy cattle (Bos taurus L.) manure was broadcast into a fall planted cover crop before no-till corn planting or incorporated by chisel/disk tillage in the absence of a cover crop. Rainfall simulations (60 mm h(-1)) were performed after planting, mid-season, and post-harvest in 2007 and 2008. In both years and on both soils, no-till yielded significantly less sediment than did chisel/disking. Relative effects of tillage on runoff and P loss differed with soil. On the well-drained soil, runoff depths from no-till were much lower than with chisel/disking, producing significantly lower total P loads (22-50% less). On the somewhat poorly drained soil, there was little to no reduction in runoff depth with no-till, and total P loads were significantly greater than with chisel/disking (40-47% greater). Particulate P losses outweighed dissolved P losses as the major concern on the well-drained soil, whereas dissolved P from surface applied manure was more important on the somewhat poorly drained soil. This study confirms the benefit of no-till to erosion and total P runoff control on well-drained soils but highlights trade-offs in no-till management on somewhat poorly drained soils where the absence of manure incorporation can exacerbate total P losses.
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Turhan, Semra Akkaya; Toker, Ebru
2015-01-01
To evaluate the lens edge interaction with the ocular surface with different edge designs using optical coherence tomography and to examine the effect of lens power on the lens edge interactions. Four types of silicone hydrogel lenses with different edge designs (round-, semi-round-, chisel-, and knife-edged) at six different powers (+5.0, +3.0, +1.0, -1.0, -3.0, and -5.0 diopters) were fitted to both eyes of 20 healthy volunteers. Optical coherence tomography images were taken at the corneal center and at the limbus within 15-30 minutes after insertion. The images were evaluated with respect to two parameters: conjunctival indentation exerted by the lens edge; and the tear film gaps between the posterior surface of the lens and the ocular surface. The amount of conjunctival indentation was measured with the distortion angle of the conjunctiva at the lens edge. The degree of conjunctival indentation was highest with the chisel-edged design followed by the semi-round design (P<0.0001). Knife- and round-edged lenses exerted similar levels of conjunctival indentation that was significantly lower compared to chisel-edged lens (P<0.001). For each one of the tested lens edge designs, no significant difference was observed in the conjunctival indentation with respect to lens power. The chisel-edged lens produced the highest amount of conjunctival indentation for each one of the six lens powers (P<0.0001). Post-lens tear film gaps at the limbus were observed at most in the round-edge design (P=0.001). The fitting properties of contact lenses may be influenced by their edge design but not by their lens power.
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Turhan, Semra Akkaya; Toker, Ebru
2015-01-01
Purpose To evaluate the lens edge interaction with the ocular surface with different edge designs using optical coherence tomography and to examine the effect of lens power on the lens edge interactions. Methods Four types of silicone hydrogel lenses with different edge designs (round-, semi-round-, chisel-, and knife-edged) at six different powers (+5.0, +3.0, +1.0, −1.0, −3.0, and −5.0 diopters) were fitted to both eyes of 20 healthy volunteers. Optical coherence tomography images were taken at the corneal center and at the limbus within 15–30 minutes after insertion. The images were evaluated with respect to two parameters: conjunctival indentation exerted by the lens edge; and the tear film gaps between the posterior surface of the lens and the ocular surface. The amount of conjunctival indentation was measured with the distortion angle of the conjunctiva at the lens edge. Results The degree of conjunctival indentation was highest with the chisel-edged design followed by the semi-round design (P<0.0001). Knife- and round-edged lenses exerted similar levels of conjunctival indentation that was significantly lower compared to chisel-edged lens (P<0.001). For each one of the tested lens edge designs, no significant difference was observed in the conjunctival indentation with respect to lens power. The chisel-edged lens produced the highest amount of conjunctival indentation for each one of the six lens powers (P<0.0001). Post-lens tear film gaps at the limbus were observed at most in the round-edge design (P=0.001). Conclusion The fitting properties of contact lenses may be influenced by their edge design but not by their lens power. PMID:26045658
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[The influence of tobacco-smoke toxic components on glucosaminoglycans in biologic tissues].
Zurabashvili, D Z; Chanturiia, I R; Kapanadze, L R; Kikalishvili, B Iu; Daneliia, G G
2010-04-01
The aim of the work is detailed analysis of glucosaminoglikans and glukuronic acid in chisel tooth and molars of tobacco-smokers and non-smokers. The total number of 140 patients (tobacco-smokers - 60) by acute serous pulpit is investigated. The conducted quantative and qualitative analyzes show that tobacco-smokers tooth contains les glucosaminoglikans (chondroitinsulfats A and C) and more glucuronic acid than non-smokers individuals. The chisel tooth pulp contained considerably more glucuronic acid as compared with molars. These studies support the hypothesis of important role of cigarette smoke toxical components in the tooth support mechanisms. The studies are necessary to be held in different directions.
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Strip-tillage: A conservation alternative to full-width tillage systems
NASA Astrophysics Data System (ADS)
Wolkowski, Richard
2015-04-01
Historically no-till management has been a challenge for maize production in the Midwestern USA because crop residue slows the warming of the soil in the spring and can physically impair planting by plugging the planter. After trying no-till, producers often return to more aggressive tillage operations to address residue concerns; however these systems can cause soil erosion and can increase the cost of production. An alternative system known as strip-tillage has been suggested as a compromise between no-till and full-width tillage. This practice utilizes implements that loosen the soil and allow warming in the row area, yet maintain nearly as much residue as no-till. Strip-tillage is generally understood to be a single pass with a separate implement in the fall, although spring strip-tillage is possible if soil moisture and conditions permit. Strip-tillage can be accomplished in a shorter time, with lower energy and equipment inputs compared to full-width tillage. The first of two studies that examined the merits of strip-tillage was conducted the University of Wisconsin Lancaster Agricultural Research Station (42.84, -90.80). Natural runoff collectors were installed in a field having a silt loam soil with an 8% slope in fall chisel and fall strip-tillage system. The measured soil loss in a year that experienced substantial rainfall prior to canopy closure was 10.6 Mg ha-1 in chisel vs. 0.64 Mg ha-1 in strip-tillage. Soil loss was much less for both systems in the second year when early season rainfall was minimal. A second, ten year study was conducted at the University of Wisconsin Arlington Agricultural Research Station (43.30, -89.36) that compared fall strip-tillage with fall chisel/spring field cultivator and no-till systems in both a continuous maize and soybean-maize rotation. This work showed equal maize grain yield in maize after soybean when comparing chisel and strip-tillage. No-till yield was about 5 % lower. Yield in continuous maize was highest in the chisel system, being about 4 % greater than strip-tillage and 8 % greater than no-till. An economic analysis of this data showed that the benefit to strip-tillage is greatest in maize following soybean. Strip-tillage is a system that can optimize both economic and environmental return for maize production and should be implemented more widely, especially on erosive soils.
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The earliest herbivorous marine reptile and its remarkable jaw apparatus.
Chun, Li; Rieppel, Olivier; Long, Cheng; Fraser, Nicholas C
2016-05-01
Newly discovered fossils of the Middle Triassic reptile Atopodentatus unicus call for a radical reassessment of its feeding behavior. The skull displays a pronounced hammerhead shape that was hitherto unknown. The long, straight anterior edges of both upper and lower jaws were lined with batteries of chisel-shaped teeth, whereas the remaining parts of the jaw rami supported densely packed needle-shaped teeth forming a mesh. The evidence indicates a novel feeding mechanism wherein the chisel-shaped teeth were used to scrape algae off the substrate, and the plant matter that was loosened was filtered from the water column through the more posteriorly positioned tooth mesh. This is the oldest record of herbivory within marine reptiles.
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NASA Astrophysics Data System (ADS)
Bolobov, V. I.; BinhLe, Thanh
2018-03-01
It is shown that shallow cryogenic treatment at -75°C (SCT) of the materials of hydraulic breaker chisels - P20, 1080 and D2 steels leads to a decrease (44 ÷ 82%) in the amount of retained austenite and an increase (26 ÷ 99%) in the amount of carbides in the structure of hardened steel, which is accompanied by an increase in its hardness (1.4 ÷ 2.1%) and abrasive wear resistance (10 ÷ 31%) with a simultaneous decrease in impact toughness (19 ÷ 24%). Deep cryogenic treatment at -196°C (DCT) and subsequent low-temperature tempering of D2 steel leads to a significant increase in its wear resistance (98%) and impact toughness (32%).
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The earliest herbivorous marine reptile and its remarkable jaw apparatus
Chun, Li; Rieppel, Olivier; Long, Cheng; Fraser, Nicholas C.
2016-01-01
Newly discovered fossils of the Middle Triassic reptile Atopodentatus unicus call for a radical reassessment of its feeding behavior. The skull displays a pronounced hammerhead shape that was hitherto unknown. The long, straight anterior edges of both upper and lower jaws were lined with batteries of chisel-shaped teeth, whereas the remaining parts of the jaw rami supported densely packed needle-shaped teeth forming a mesh. The evidence indicates a novel feeding mechanism wherein the chisel-shaped teeth were used to scrape algae off the substrate, and the plant matter that was loosened was filtered from the water column through the more posteriorly positioned tooth mesh. This is the oldest record of herbivory within marine reptiles. PMID:27386529
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Wi, Jaemin; Seo, Hyejin; Lee, Jong Yeon; Nam, Dong Heun
2016-01-01
To evaluate the efficacy and outcomes of intracameral illuminator-assisted nucleofractis technique in cataract surgery. Since June 2012, this novel technique has been performed in all cataract cases by one surgeon (approximately 300 cases of various densities). Trenching continues until the posterior plate white reflex between an endonucleus and an epinucleus is identified (enhanced depth trench). After trenching, cracking is initiated with minimal separation force, and completion of cracking is confirmed by posterior capsule reflex (one-shot crack). With followability enhanced by an elliptical phaco mode, the divided nucleus is efficiently cut into small fragments by a chisel-shaped illuminator (phaco cut). We have not experienced any capsular bag or zonular complications, and the effective phacoemulsification time seemed to be shorter than that with the conventional technique. This technique simplifies the complete division of the nucleus, which is the most challenging step in safe and efficient phacoemulsification.
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DETAIL VIEW OF LARGE BORE HOLE, SHOWING TRIANGULAR SHAPE FORMED ...
DETAIL VIEW OF LARGE BORE HOLE, SHOWING TRIANGULAR SHAPE FORMED BY CHISEL METHOD OF DRILLING - Granite Hill Plantation, Quarry No. 3, South side of State Route 16, 1.3 miles northeast east of Sparta, Sparta, Hancock County, GA
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NASA Astrophysics Data System (ADS)
Prasetyo, T.; Amar, S.; Arendra, A.; Zam Zami, M. K.
2018-01-01
This study develops an on-line detection system to predict the wear of DCMT070204 tool tip during the cutting process of the workpiece. The machine used in this research is CNC ProTurn 9000 to cut ST42 steel cylinder. The audio signal has been captured using the microphone placed in the tool post and recorded in Matlab. The signal is recorded at the sampling rate of 44.1 kHz, and the sampling size of 1024. The recorded signal is 110 data derived from the audio signal while cutting using a normal chisel and a worn chisel. And then perform signal feature extraction in the frequency domain using Fast Fourier Transform. Feature selection is done based on correlation analysis. And tool wear classification was performed using artificial neural networks with 33 input features selected. This artificial neural network is trained with back propagation method. Classification performance testing yields an accuracy of 74%.
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Annual Research Review: Parenting and Children's Brain Development--The End of the Beginning
ERIC Educational Resources Information Center
Belsky, Jay; de Haan, Michelle
2011-01-01
After questioning the practical significance of evidence that parenting influences brain development--while highlighting the scientific importance of such work for understanding "how" family experience shapes human development--this paper reviews evidence suggesting that brain structure and function are "chiselled" by parenting. Although the…
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A New Model of Teaching Pedagogy in CHISEL for the 21th Century.
ERIC Educational Resources Information Center
Huang, Li-yi
This paper describes and compares six models for teaching second languages developed and adopted since 1840 (grammar-translation, direct, structural, situational, audiolingual, and communicative methods), and proposes a seventh, the cognitive-linguistic method, incorporating Noam Chomsky's theory of learning. The model takes both extralinguistic…
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USDA-ARS?s Scientific Manuscript database
Agricultural and soil management practices have been reported to affect alachlor sorption-desorption and degradation rates. The objectives of this study were to: (a) assess differences in alachlor sorption due to tillage treatments (chisel plow and ridge tillage) on soils from three Midwestern U.S. ...
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Code of Federal Regulations, 2011 CFR
2011-07-01
... Relating to Labor (Continued) OCCUPATIONAL SAFETY AND HEALTH ADMINISTRATION, DEPARTMENT OF LABOR... work operations. In some cases a chin strap may be necessary to keep the helmet on an employee's head..., grinding machining, masonry work, woodworking, sawing, drilling, chiseling, powered fastening, riveting...
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Code of Federal Regulations, 2014 CFR
2014-07-01
... Relating to Labor (Continued) OCCUPATIONAL SAFETY AND HEALTH ADMINISTRATION, DEPARTMENT OF LABOR... work operations. In some cases a chin strap may be necessary to keep the helmet on an employee's head..., grinding machining, masonry work, woodworking, sawing, drilling, chiseling, powered fastening, riveting...
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Code of Federal Regulations, 2012 CFR
2012-07-01
... Relating to Labor (Continued) OCCUPATIONAL SAFETY AND HEALTH ADMINISTRATION, DEPARTMENT OF LABOR... work operations. In some cases a chin strap may be necessary to keep the helmet on an employee's head..., grinding machining, masonry work, woodworking, sawing, drilling, chiseling, powered fastening, riveting...
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Code of Federal Regulations, 2013 CFR
2013-07-01
... Relating to Labor (Continued) OCCUPATIONAL SAFETY AND HEALTH ADMINISTRATION, DEPARTMENT OF LABOR... work operations. In some cases a chin strap may be necessary to keep the helmet on an employee's head..., grinding machining, masonry work, woodworking, sawing, drilling, chiseling, powered fastening, riveting...
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Fire effects on rock images and similar cultural resources [Chapter 5
Roger E. Kelly; Daniel F. McCarthy
2012-01-01
Throughout human global history, people have purposely altered natural rock surfaces by drilling, drawing, painting, incising, pecking, abrading and chiseling images into stone. Some rock types that present suitable media surfaces for these activities are fine-grained sandstones and granites, basalts, volcanic tuff, dolomites, and limestones. Commonly called rock...
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Translations on Eastern Europe Political, Sociological, and Military Affairs, Number 1354
1977-02-16
sheets, embroidery and uncomplicated items for en- terprises. The 8-year schools do not have production plans but they can boast about quite...well they handle the file and the chisel and how, from the skillful fingers of the girls, rich embroidery emerges; I look at the pretty little
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Tillage and Water Deficit Stress Effects on Corn (Zea mays, L.) Root Distribution
USDA-ARS?s Scientific Manuscript database
One goal of soil management is to provide optimum conditions for root growth. Corn root distributions were measured in 2004 from a crop rotation – tillage experiment that was started in 2000. Corn was grown either following corn or following sunflower with either no till or deep chisel tillage. Wate...
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Testing methods to mitigate Caribbean yellow-band disease on Orbicella faveolata
Whitcher, Elizabeth M.; Code, Tessa; Pollock, Clayton; Lundgren, Ian; Hillis-Starr, Zandy
2018-01-01
Outbreaks of coral diseases continue to reduce global coral populations. In the Caribbean, yellow band is a severe and wide-spread disease that commonly affects corals of the Orbicella spp. complex, significantly impeding coral reproduction, and hindering the natural recovery of Orbicella spp. populations. Caribbean yellow-band disease (CYBD) lesions may be severe, and often result in the complete loss of coral tissue. The slow spread of CYBD, however, provides an opportunity to test methods to mitigate the disease. Here we report the results of in situ experiments, conducted within Buck Island Reef National Monument in St. Croix, USVI, to test the effectiveness of three techniques to minimize disease impact on Orbicella faveolata: (1) shading, (2) aspirating, and (3) chiseling a “firebreak” to isolate the lesion. Neither shading nor aspirating the diseased tissue significantly reduced CYBD tissue loss. However, chiseling reduced the rate and amount of tissue lost by 31%. While 30–40% of the chiseled lesions appeared to be free of disease signs 12–16 months after treatment, success significantly and steadily declined over 23 months, indicating a possible lack of long-term viability of the technique. The results of this study demonstrate that creating a “firebreak” between diseased and healthy-appearing tissue slows the spread of the disease and may prolong the life of O. faveolata colonies. The firebreak method yielded the best results of all the techniques tested, and also required the least amount of effort and resources. However, we do not recommend that this treatment alone be used for long-term disease mitigation. Rather, we propose that modifications of this and other treatment options be sought. The results also highlight the need for extended monitoring of CYBD after any treatment, due to the slow but variable rate and pattern of tissue loss in this disease. PMID:29770279
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Basic Hand Tools for Bricklaying and Cement Masonry [and] Basic Hand Tools of the Carpenter.
ERIC Educational Resources Information Center
Texas A and M Univ., College Station. Vocational Instructional Services.
Intended for student use, this unit discusses and illustrates the tools used in brick and masonry and carpentry. Contents of the brick and masonry section include informative materials on bricklaying tools (brick trowels, joint tools, levels, squares, line and accessories, rules, hammers and chisels, tool kits) and cement masonry tools (tampers,…
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USDA-ARS?s Scientific Manuscript database
Land application of manure from tylosin-treated swine introduces tylosin-resistant enterococci, erm genes, which confer resistance to tylosin, and tylosin. This study documents the occurrence and transport of tylosin-resistant enterococci, erm genes, and tylosin in tile-drained chisel plow and no-ti...
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AmeriFlux US-Ro5 Rosemount I18_South
Baker, John [USDA-ARS; Griffis, Tim [University of Minnesota
2018-01-01
This is the AmeriFlux version of the carbon flux data for the site US-Ro5 Rosemount I18_South. Site Description - This tower is located in a farm field farmed in accordance with the dominant farming practice in the region: a corn/soybean rotation with chisel plow tillage in the fall following corn harvest and in the spring following soybeans.
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AmeriFlux US-Ro3 Rosemount- G19
Baker, John [USDA-ARS; Griffis, Tim [University of Minnesota
2016-01-01
This is the AmeriFlux version of the carbon flux data for the site US-Ro3 Rosemount- G19. Site Description - This tower is located in a farm field farmed in accordance with the cominant farming practice in the region: a corn/soybean rotation with chisel plow tillage in the fall following corn harvest and in the spring following soybeans.
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AmeriFlux US-Ro1 Rosemount- G21
Baker, John [USDA-ARS; Griffis, Tim [University of Minnesota; Griffis, Timothy [University of Minnesota
2016-01-01
This is the AmeriFlux version of the carbon flux data for the site US-Ro1 Rosemount- G21. Site Description - This tower is located in a farm field farmed in accordance with the dominant farming practice in the region: a corn/soybean rotation with chisel plow tillage in the fall following corn harvest and in the spring following soybeans.
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AmeriFlux US-Ro2 Rosemount- C7
Baker, John [USDA-ARS; Griffis, Tim [University of Minnesota
2018-01-01
This is the AmeriFlux version of the carbon flux data for the site US-Ro2 Rosemount- C7. Site Description - This tower is located in a farm field farmed in accordance with the dominant farming practice in the region: a corn/soybean/clover rotation with chisel plow tillage in the fall following corn harvest and in the spring following soybeans.
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ERIC Educational Resources Information Center
Milne, David H.; Schafersman, Steven D.
1983-01-01
Creationists claim that human footprints coexist with those of dinosaurs in Cretaceous limestone exposed in the Paluxy riverbed near Glen Rose, Texas. Analysis of photos shows that the features in question are not human footprints and that creationist documentation/analysis of the prints is riddled with omissions, misrepresentations,…
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Powder-Collection System for Ultrasonic/Sonic Drill/Corer
NASA Technical Reports Server (NTRS)
Sherrit, Stewart; Bar-Cohen, Yoseph; Bao, Xiaoqi; Chang, Zensheu; Blake, David; Bryson, Charles
2005-01-01
A system for collecting samples of powdered rock has been devised for use in conjunction with an ultrasonic/sonic drill/corer (USDC) -- a lightweight, lowpower apparatus designed to cut into, and acquire samples of, rock or other hard material for scientific analysis. The USDC includes a drill bit, corer, or other tool bit, in which ultrasonic and sonic vibrations are excited by an electronically driven piezoelectric actuator. The USDC advances into the rock or other material of interest by means of a hammering action and a resulting chiseling action at the tip of the tool bit. The hammering and chiseling actions are so effective that unlike in conventional twist drilling, a negligible amount of axial force is needed to make the USDC advance into the material. Also unlike a conventional twist drill, the USDC operates without need for torsional restraint, lubricant, or a sharp bit. The USDC generates powder as a byproduct of the drilling or coring process. The purpose served by the present samplecollection system is to remove the powder from the tool-bit/rock interface and deliver the powder to one or more designated location(s) for analysis or storage
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Hinck, Jo E.; Linder, Greg L.; Otton, James K.; Finger, Susan E.; Little, Edward E.; Tillitt, Donald E.
2013-01-01
Chemical data from soil and weathered waste material samples collected from five uranium mines north of the Grand Canyon (three reclaimed, one mined but not reclaimed, and one never mined) were used in a screening-level risk analysis for the Arizona chisel-toothed kangaroo rat (Dipodomys microps leucotis); risks from radiation exposure were not evaluated. Dietary toxicity reference values were used to estimate soil-screening thresholds presenting risk to kangaroo rats. Sensitivity analyses indicated that body weight critically affected outcomes of exposed-dose calculations; juvenile kangaroo rats were more sensitive to the inorganic constituent toxicities than adult kangaroo rats. Species-specific soil-screening thresholds were derived for arsenic (137 mg/kg), cadmium (16 mg/kg), copper (1,461 mg/kg), lead (1,143 mg/kg), nickel (771 mg/kg), thallium (1.3 mg/kg), uranium (1,513 mg/kg), and zinc (731 mg/kg) using toxicity reference values that incorporate expected chronic field exposures. Inorganic contaminants in soils within and near the mine areas generally posed minimal risk to kangaroo rats. Most exceedances of soil thresholds were for arsenic and thallium and were associated with weathered mine wastes.
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Fabrication Development and Flow Testing of Underwater Superhydrophobic Films for Drag Reduction
2017-03-21
form a large area Sidewall improved by using a chisel-edge blade 3/20/17 9 17/52 Task 3: Flow testing and characterization 18/52 Task 3.1 Develop shear...Before data collection for each run , the water tunnel was run at Re= 1.45x107 for a 3-5 minutes to de-wet SHPo sample, but improvement was not
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Nitrous oxide emissions from corn-soybean systems in the midwest.
Parkin, Timothy B; Kaspar, Thomas C
2006-01-01
Soil N2O emissions from three corn (Zea mays L.)-soybean [Glycine max (L.) Merr.] systems in central Iowa were measured from the spring of 2003 through February 2005. The three managements systems evaluated were full-width tillage (fall chisel plow, spring disk), no-till, and no-till with a rye (Secale cereale L. 'Rymin') winter cover crop. Four replicate plots of each treatment were established within each crop of the rotation and both crops were present in each of the two growing seasons. Nitrous oxide fluxes were measured weekly during the periods of April through October, biweekly during March and November, and monthly in December, January, and February. Two polyvinyl chloride rings (30-cm diameter) were installed in each plot (in and between plant rows) and were used to support soil chambers during the gas flux measurements. Flux measurements were performed by placing vented chambers on the rings and collecting gas samples 0, 15, 30, and 45 min following chamber deployment. Nitrous oxide fluxes were computed from the change in N2O concentration with time, after accounting for diffusional constraints. We observed no significant tillage or cover crop effects on N2O flux in either year. In 2003 mean N2O fluxes were 2.7, 2.2, and 2.3 kg N2O-N ha(-1) yr(-1) from the soybean plots under chisel plow, no-till, and no-till + cover crop, respectively. Emissions from the chisel plow, no-till, and no-till + cover crop plots planted to corn averaged 10.2, 7.9, and 7.6 kg N2O-N ha(-1) yr(-1), respectively. In 2004 fluxes from both crops were higher than in 2003, but fluxes did not differ among the management systems. Fluxes from the corn plots were significantly higher than from the soybean plots in both years. Comparison of our results with estimates calculated using the Intergovernmental Panel on Climate Change default emission factor of 0.0125 indicate that the estimated fluxes underestimate measured emissions by a factor of 3 at our sites.
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1989-08-14
peel the cover skins using a wood chisel, tin snips, pliars, etc. to remove the skin without damaging the wires or the heating elements. O.5T-.3...called " Banana Boxes" because they are about the same shape and construction as the boxes used to ship bananas . These boxes would be similar to the ones
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Fort Leonard Wood German POW Stonework: Maintenance and Repair
2017-07-01
powered chisels, scaler (power chipper), and thin diamond- bladed grinders should be approved by architect or project manager. All work should be...Figure 5. Deteriorated mortar and plant growth on the patio of Garlington House. Photo NCPTT 8 • Raising mower blades to avoid low-ly- ing features...protective perimeter around features, attaching protective bumpers to the lawn mower, raising mower blades to avoid low-lying features, and using smaller
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AmeriFlux US-Ro6 Rosemount I18_North
Baker, John [USDA-ARS; Griffis, Tim [University of Minnesota
2018-01-01
This is the AmeriFlux version of the carbon flux data for the site US-Ro6 Rosemount I18_North. Site Description - This tower is located in a farm field farmed in accordance with a conservation type agricultural practice in the region: a corn/soybean/clover (living mulch/cover crop) rotation with chisel plow tillage in the fall following corn harvest and in the spring following soybeans.
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Mensink, Gertjan; Verweij, Jop P; Frank, Michael D; Eelco Bergsma, J; Richard van Merkesteyn, J P
2013-09-01
An unfavourable fracture, known as a bad split, is a common operative complication in bilateral sagittal split osteotomy (BSSO). The reported incidence ranges from 0.5 to 5.5%/site. Since 1994 we have used sagittal splitters and separators instead of chisels for BSSO in our clinic in an attempt to prevent postoperative hypoaesthesia. Theoretically an increased percentage of bad splits could be expected with this technique. In this retrospective study we aimed to find out the incidence of bad splits associated with BSSO done with splitters and separators. We also assessed the risk factors for bad splits. The study group comprised 427 consecutive patients among whom the incidence of bad splits was 2.0%/site, which is well within the reported range. The only predictive factor for a bad split was the removal of third molars at the same time as BSSO. There was no significant association between bad splits and age, sex, class of occlusion, or the experience of the surgeon. We think that doing a BSSO with splitters and separators instead of chisels does not increase the risk of a bad split, and is therefore safe with predictable results. Copyright © 2012 The British Association of Oral and Maxillofacial Surgeons. Published by Elsevier Ltd. All rights reserved.
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NASA Astrophysics Data System (ADS)
Hamrick, Joseph L., II
Thin rectangular samples of Ti-6Al-4V were damaged by four methods to represent foreign object damage found in turbine engine blades: (1) impact with 2 mm. and 5 mm diameter glass spheres at 305 m/s, (2) impact with 2 mm and 4 mm diameter steel spheres at 305 m/s, (3) quasi-static displacement controlled indentation using steel chisels with 1 mm, 2 nun and 5 mm diameter tips and (4) shearing notches with a 2 mm. diameter chisel point under a quasi-static loading condition. Finite element analysis was used to study the relationship between the stress state created by the plastic damage and the fatigue strength. A new method of quantifying the amount of plastic damage from multiple methods was developed. The fatigue strength required for crack initiation at 10E7 cycles was found to be a function of the total depth from the edge of the undeformed specimen up to the end of the plastically deformed zone. For damage depths less than 1750 mum, the reduction in fatigue strength is proportional to the depth of total damage. For depths > 1750 mum, there appears to be a threshold value of fatigue strength.
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Benchmark Design and Installation: A synthesis of Existing Information.
1987-07-01
casings (15 ft deep) drilled to rock and filled with concrete. Disks - 1 . Set on vertically stable structures (e.g., dam monoliths). 2 . Set in rock ...Structural movement survey 1 . Rock outcrops (first choice) -- chiseled square on high point. 2 . Massive concrete structure (second choice) - cut square on...bolt marker (type 2 ). 58,. % %--"% %I 1 ± 4 -I,.- Table Cl. Recomnded benchmarks. Type of condition or terrain Type of markert Bedrock, rock outcrops
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1991-07-15
frying pan 3.51 0.57 102 garbage can 3.31 0.44 103 giraffe 2.83 0.12 104 glass 2.26 -0.26 105 glasses 2.27 -0.25 106 glove 2.97 0.21 107 goat 3.44 0.52 108...50 caterpillar 2.14 -0.33 51 celery 2.84 0.13 52 chain 2.72 0.05 53 chair 0.88 -1.17 54 cherry 3.71 0.70 55 chicken 3.70 0.70 56 chisel 1.12 -1.01 57
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Desaeger, Johan A; Seebold, Kenneth W; Csinos, Alex S
2008-03-01
Metam-sodium, 1,3-dichloropropene (1,3-D) and chloropicrin are widely used soil fumigants. Combined application of metam-sodium and 1,3-D + chloropicrin is intended to improve efficacy and broaden spectrum of control, but little is known about the effect on crop safety. This study aimed to evaluate the effects of application timing of fumigant combinations on soilborne pest and disease control (nematodes, soil fungi and weeds) and growth of squash. Two separate tests with chisel-injected and drip-applied fumigant combinations and plant-back times ranging from 1 to 4 weeks were conducted in Tifton, GA, USA, in spring and fall 2002. Fumigant combinations using 1,3-D, chloropicrin and metam-sodium were as effective as methyl bromide in controlling Meloidogyne incognita (Kofoid & White) Chitwood, Pythium irregulare Buis., Rhizoctonia solani Kühn and Cyperus esculentus L. Chisel-applied combinations were more effective in terms of root-knot nematode control than drip-applied combinations. Root-knot nematode reduced squash yields by up to 60%. Phytotoxicity problems and lower yields were observed during spring, especially following 1,3-D + chloropicrin and when plant-back periods were shorter. The main problem with fumigant alternatives to methyl bromide may not be reduced efficacy but, in particular for 1,3-D products, loss of flexibility in terms of longer plant-back periods. (c) 2008 Society of Chemical Industry.
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Influence of the axial rotation angle on tool mark striations.
Garcia, Derrel Louis; Pieterman, René; Baiker, Martin
2017-10-01
A tool's axial rotation influences the geometric properties of a tool mark. The larger the axial rotation angle, the larger the compression of structural details like striations. This complicates comparing tool marks at different axial rotations. Using chisels, tool marks were made from 0° to 75° axial rotation and compared using an automated approach Baiker et al. [10]. In addition, a 3D topographic surface of a chisel was obtained to generate virtual tool marks and to test whether the axial rotation angle of a mark could be predicted. After examination of the tool mark and chisel data-sets it was observed that marks lose information with increasing rotation due to the change in relative distance between geometrical details on the tool and the disappearance of smaller details. The similarity and repeatability were high for comparisons between marks with no difference in axial rotation, but decreasing with increased rotation angle from 0° to 75°. With an increasing difference in the rotation angles, the tool marks had to be corrected to account for the different compression factors between them. For compression up to 7.5%, this was obtained automatically by the tool mark alignment method. For larger compression, manually re-sizing the marks to the uncompressed widths at 0° rotation before the alignment was found suitable for successfully comparing even large differences in axial rotation. The similarity and repeatability were decreasing however, with increasing degree of re-sizing. The quality was assessed by determining the similarity at different detail levels within a tool mark. With an axial rotation up to 75°, tool marks were found to reliably represent structural details down to 100μm. The similarity of structural details below 100μm was dependent on the angle, with the highest similarity at small rotation angles and the lowest similarity at large rotation angles. Filtering to remove the details below 100μm lead to consistently higher similarity between tool marks at all angles and allowed for a comparison of marks up to 75° axial rotation. Finally, generated virtual tool mark profiles with an axial rotation were compared to experimental tool marks. The similarity between virtual and experimental tool marks remained high up to 60° rotation after which it decreased due to the loss in quality in both marks. Predicting the rotation angle is possible under certain conditions up to 45° rotation with an accuracy of 2.667±0.577° rotation. Copyright © 2017 Elsevier B.V. All rights reserved.
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NASA Technical Reports Server (NTRS)
Bar-Cohen, Yoseph; Sherrit, Stewart; Herz, Jack
2005-01-01
An ultrasonic/sonic jackhammer (USJ) is the latest in a series of related devices. Each of these devices cuts into a brittle material by means of hammering and chiseling actions of a tool bit excited with a combination of ultrasonic and sonic vibrations. A small-scale prototype of the USJ has been demonstrated. A fully developed, full-scale version of the USJ would be used for cutting through concrete, rocks, hard asphalt, and other materials to which conventional pneumatic jackhammers are applied, but the USJ would offer several advantages over conventional pneumatic jackhammers.
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Daverede, I C; Kravchenko, A N; Hoeft, R G; Nafziger, E D; Bullock, D G; Warren, J J; Gonzini, L C
2004-01-01
Excessive fertilization with organic and/or inorganic P amendments to cropland increases the potential risk of P loss to surface waters. The objective of this study was to evaluate the effects of soil test P level, source, and application method of P amendments on P in runoff following soybean [Glycine max (L.) Merr.]. The treatments consisted of two rates of swine (Sus scrofa domestica) liquid manure surface-applied and injected, 54 kg P ha(-1) triple superphosphate (TSP) surface-applied and incorporated, and a control with and without chisel-plowing. Rainfall simulations were conducted one month (1MO) and six months (6MO) after P amendment application for 2 yr. Soil injection of swine manure compared with surface application resulted in runoff P concentration decreases of 93, 82, and 94%, and P load decreases of 99, 94, and 99% for dissolved reactive phosphorus (DRP), total phosphorus (TP), and algal-available phosphorus (AAP), respectively. Incorporation of TSP also reduced P concentration in runoff significantly. Runoff P concentration and load from incorporated amendments did not differ from the control. Factors most strongly related to P in runoff from the incorporated treatments included Bray P1 soil extraction value for DRP concentration, and Bray P1 and sediment content in runoff for AAP and TP concentration and load. Injecting manure and chisel-plowing inorganic fertilizer reduced runoff P losses, decreased runoff volumes, and increased the time to runoff, thus minimizing the potential risk of surface water contamination. After incorporating the P amendments, controlling erosion is the main target to minimize TP losses from agricultural soils.
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Antibiotic losses in leaching and surface runoff from manure-amended agricultural land.
Dolliver, Holly; Gupta, Satish
2008-01-01
A 3-yr field study quantified leaching and runoff losses of antibiotics from land application of liquid hog (chlortetracycline and tylosin) and solid beef (chlortetracycline, monensin, and tylosin) manures under chisel plowing and no-tillage systems. The study was conducted in southwestern Wisconsin, a karst area with steep, shallow, macroporous soils. Relative mass losses of chlortetracycline, monensin, and tylosin were <5% of the total amount applied with manure. Chlortetracycline was only detected in runoff, whereas monensin and tylosin were detected in leachate and runoff. Highest concentrations of monensin and tylosin in the leachate were 40.9 and 1.2 microg L(-1), respectively. Highest chlortetracycline, monensin, and tylosin concentrations in runoff were 0.5, 57.5, and 6.0 microg L(-1), respectively. For all three antibiotics, >90% of detections and 99% of losses occurred during the non-growing season due to fall manure application and slow degradation of antibiotics at cold temperatures. During years of high snowmelt, runoff accounted for nearly 100% of antibiotic losses, whereas during years of minimal snowmelt, runoff accounted for approximately 40% of antibiotic losses. Antibiotic losses were generally higher from the no-tillage compared with chisel plow treatment due to greater water percolation as a result of macroporosity and greater runoff due to lack of surface roughness in the no-tillage plots during the non-growing season. The results from this study suggest that small quantities of dissolved antibiotics could potentially reach surface and ground waters in the Upper Midwestern USA from manure-amended shallow macroporous soils underlain with fractured bedrock.
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Technical Modifications for Intraoral Quadrangular Le Fort II Osteotomy.
Klug, Clemens; Cede, Julia
2017-02-01
The intraoral quadrangular Le Fort II osteotomy (IQLFIIO) represents a reliable surgical method in cases of midfacial deficiency with good functional, esthetic, and stable long-term results. In this technical note, we present 3 surgical modifications to previous reports: 1) inferior orbital rim osteotomy by angulated piezosurgical instruments, thereby avoiding the use of chisels in the orbital region; 2) osteosynthetic fixation only laterally at the zygomatic buttress with 2 L-shaped miniplates, thus avoiding paranasal osteosynthesis; and 3) advancement step camouflage in the lateral infraorbital region with a compound mass of autologous bone chips and fibrin glue with the intention to reduce bone block-associated side effects. Thirteen consecutive patients presenting with midfacial deficiency and Class III malocclusion were treated by IQLFIIO and mandibular osteotomy. In all cases, osteotomy and consecutive down fracture could be conducted as planned using the piezotome. No atypical fractures were encountered. No cases of infraorbital nerve anesthesia developed. Midfacial hypesthesia was found in 54% of the operated sides after 3 months, in 23% after 6 months, and in 13% after 12 months. The 5-month postoperative 3-dimensional scans revealed osseous healing at the infraorbital advancement step. Our results suggest that IQLFIIO can be conducted fully without chisels in the orbital region. Implementation of piezosurgery in IQLFIIO allows for safe bone cutting in the orbital region. Two miniplates and step camouflage with fibrin glue-stabilized bone chips were sufficient for osseous healing. Future studies will focus on quantitative soft to hard tissue changes that occur with IQLFIIO advancement. Copyright © 2016 American Association of Oral and Maxillofacial Surgeons. Published by Elsevier Inc. All rights reserved.
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Cranial suture complexity in caviomorph rodents (Rodentia; Ctenohystrica).
Buezas, Guido; Becerra, Federico; Vassallo, Aldo
2017-08-01
Due to their flexibility, sutures are regions that experience greater strains than the surrounding rigid cranial bones. Cranial sutures differ in their degree of interdigitation or complexity. There is evidence indicating that a more convoluted suture better enables the absorption of high stresses coming from dynamic masticatory forces, and other functions. The Order Rodentia is an interesting clade to study this because of its taxa with diverse chewing modes. Due to repeated loading resulting from gnawing and grinding, energy absorption by the sutures might be a crucial factor in these mammals. Species within the infraorder Caviomorpha were chosen as a case study because of their ecomorphological and dietary diversity. This study compared five sutures from the rostrum and cranial vault across seven caviomorph families, and assessed their complexity by means of the relative length and fractal dimension. Across these rodents, cranial sutures are morphologically quite diverse. We found that the sutures connecting the rostrum with the vault were relatively more interdigitated than those in the cranial vault itself, especially premaxillofrontal sutures. Suture interdigitation was higher in species that display chisel-tooth digging and burrowing behaviors, especially in the families Ctenomyidae and Octodontidae, than those in families Dasyproctidae and Cuniculidae, which have more gracile masticatory systems. The reconstruction of the ancestral character state, on family and species phylogeny, points toward low suture interdigitation (i.e., low length ratio) as a likely ancestral state for interfrontal, premaxillofrontal and maxillofrontal sutures. Interspecific differences in suture morphology shown here might represent adaptations to different mechanical demands (i.e., soft vs. tough foods) or behaviors (e.g., chisel-tooth digging), which evolved in close association with the diverse environments occupied by caviomorph rodents. © 2017 Wiley Periodicals, Inc.
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NASA Astrophysics Data System (ADS)
Vidal Vázquez, E.; Miranda, J. G. V.; Mirás-Avalos, J. M.; Díaz, M. C.; Paz-Ferreiro, J.
2009-04-01
Mathematical description of the spatial characteristics of soil surface microrelief still remains a challenge. Soil surface roughness parameters are required for modelling overland flow and erosion. The objective of this work was to evaluate the potential of multifractal for analyzing the decay of initial surface roughness induced by natural rainfall under different soil tillage systems. Field experiments were performed on an Oxisol at Campinas, São Paulo State (Brazil). Six tillage treatments, namely, disc harrow, disc plow, chisel plow, disc harrow + disc level, disc plow + disc level and chisel plow + disc level were tested. In each plot soil surface microrelief was measured for times, with increasing amounts of natural rainfall using a pinmeter. The sampling scheme was a square grid with 25 x 25 mm point spacing and the plot size was 1350 x 1350 mm, so that each data set consisted of 3025 individual elevation points. Duplicated measurements were taken per treatment and date, yielding a total of 48 experimental data sets. All the investigated microrelief data sets exhibited, in general, scale properties, and the degree of multifractality showed wide differences between them. Multifractal analysis distinguishes two different patterns of soil surface microrelief, the first one has features close to monofractal spectra and the second clearly indicates multifractal behavior. Both, singularity spectra and generalized dimension spectra allow differentiating between soil tillage systems. In general, changes in values of multifractal parameters under simulated rainfall showed no or little correspondence with the evolution of the vertical microrelief component described by indices such as the standard deviation of the point height measurements. Multifractal parameters provided valuable information for chararacterizing the spatial features of soil surface microrelief as they were able to discriminate data sets with similar values for the vertical component of roughness.
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2003-08-01
laminate . The thickness of this unit ranges from 10 to more than 250 feet in the Westover ARB area. A glacial till layer of poorly sorted gravel, sand...trucks, concrete trucks, and flatbed trucks. The backhoe would be used with a percussion chisel as well as a lift bucket. Estimates were also...36.00 3.80 83.40 9.00 5.20 Concrete Truck 5 8 2 1.80 0.19 4.17 0.45 0.26 Emissions (lbs) 144.00 15.20 333.60 36.00 20.80 Flatbed Truck 10 8 1
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Effects of various debonding and adhesive clearance methods on enamel surface: an in vitro study.
Fan, Xiao-Chuan; Chen, Li; Huang, Xiao-Feng
2017-02-27
The purpose of this study was to evaluate orthodontic debonding methods by comparing the surface roughness and enamel morphology of teeth after applying two different debonding methods and three different polishing techniques. Forty eight human maxillary premolars, extracted for orthodontic reasons, were randomly divided into three groups. Brackets were bonded to teeth with RMGIC (Fuji Ortho LC, GC, Tokyo, Japan) (two groups, n = 18 each) after acid etching (30s), light cured for 40 s, exposed to thermocycling, then underwent 2 different bracket debonding methods: debonding pliers (Shinye, Hangzhou, China) or enamel chisel (Jinzhong, Shanghai, China); the third group (n = 12) comprised of untreated controls, with normal enamel surface roughness. In each debonded group, three cleanup techniques (n = 6 each) were tested, including (I) diamond bur (TC11EF, MANI, Tochigi, Japan) and One-Gloss (Midi, Shofu, Kyoto, Japan), (II) a Super-Snap disk (Shofu, Kyoto, Japan), and (III) One-Gloss polisher. The debonding methods were compared using the modified adhesive remnant index (ARI, 1-5). Cleanup efficiencies were assessed by recording operating times. Enamel surfaces were qualitatively and quantitatively evaluated with scanning electron microscopy (SEM) and surface roughness tester, respectively. Two surface roughness variables were evaluated: Ra (average roughness) and Rz (10-point height of irregularities). The ARI scores of debonded teeth were similar with debonding pliers and enamel chisel (Chi-square = 2.19, P > 0.05). There were significant differences between mean operating time in each group (F = 52.615, P < 0.01). The diamond bur + One-Gloss took the shortest operating time (37.92 ± 3.82 s), followed by the Super-Snap disk (56.67 ± 7.52 s), and the One-Gloss polisher (63.50 ± 6.99 s). SEM appearance provided by the One-Gloss polisher was the closest to the intact enamel surface, and surface roughness (Ra: 0.082 ± 0.046 μm; Rz: 0.499 ± 0.200 μm) was closest to the original enamel (Ra: 0.073 ± 0.048 μm; Rz: 0.438 ± 0.213 μm); the next best was the Super-Snap disk (Ra: 0.141 ± 0.073 μm; Rz: 1.156 ± 0.755 μm); then, the diamond bur + One-Gloss (Ra: 0.443 ± 0.172 μm; Rz: 2.202 ± 0.791 μm). Debonding pliers were safer than enamel chisels for removing brackets. Cleanup with One-Gloss polisher provided enamel surfaces closest to the intact enamel, but took more time, and Super-Snap disks provided acceptable enamel surfaces and efficiencies. The diamond bur was not suitable for removing adhesive remnant.
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NASA Astrophysics Data System (ADS)
García-Gil, Juan Carlos; Soler-Rovira, Pedro Angel; García López de Sa, Esther; Polo, Alfredo
2013-04-01
Soil tillage practices exert a significant influence on the dynamic of soluble organic C and N pools, affecting nutrient cycling in agricultural systems by enhancing its mineralization through microbial activities or stabilization in soil microaggregates, which contribute to mitigate greenhouse gases emissions. The objective of the present research was to determine the influence of three different soil management systems (moldboard plowing, chisel and no-tillage) and the application of composted sludge (CS) and thermally-dried sewage sludge (TSS) obtained from wastewater treatment processes on dissolved organic C (water-soluble organic C -WSOC-, carbohydrates, phenolic compounds) and soluble N (total-N, NH4+, NO3-) pools in a long-term field experiment (27 years) conducted on a sandy-loam soil at the experimental station "La Higueruela" (40° 03'N, 4° 24'W) under semi-arid conditions. Both organic amendments were applied at a rate of 30 tonnes per hectare prior to tillage practices. Unamended soils were used as control for each tillage system. Soil sampling was performed two months after tillage practices at the following depths for each treatment: 0-10 cm, 10-20 cm and 20-30 cm. Results obtained for unamended soils showed that no-tillage management increased total-N, NH4+ and NO3- contents at the 0-10 cm depth samples, meanwhile WSC and carbohydrates contents were larger at 20-30 cm depth samples in both moldboard and no-tillage plots. CS and TSS-amended soils presented a general increase in soluble C and N compounds, being significantly higher in TSS-amended soils, as TSS contains a great amount of labile organic C and N substrates due to the lack of stabilization treatment. TSS-amended soils under no-tillage and chisel plowing showed larger N, NH4+ and NO3- content at the 0-10 cm samples, meanwhile moldboard management exhibited larger NH4+ and NO3- content at 10-20 and 20-30 cm samples, possibly due to the incorporation of TSS at deeper depths (20-40 cm). CS and TSS-amended soils in no-tillage system showed the largest content of organic C pools at 0-10 cm depth samples due to less soil disturbance and the input of organic substrates with CS and TSS on soil surface. CS and TSS-amended soils under chisel plowing exhibited similar contents of soluble organic C pools at 10-20 and 20-30 cm depth samples and only TSS-amended soils increased significantly WSOC content at 0-10 cm samples. Similarly, contents of WSOC and carbohydrates in moldboard plowing were distributed more uniformly throughout the soil profile due to the turnover of soil and CS and TSS amendments into the plow layer. Acknowledgements: this research was supported by the Spanish CICYT, Project no. CTM2011-25557.
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NASA Astrophysics Data System (ADS)
García-Gil, Juan Carlos; Soler-Rovira, Pedro; López-de-Sa, Esther G.; Polo, Alfredo
2014-05-01
In semi-arid agricultural soils, seasonal dynamic of soil CO2 efflux (SCE) is highly variable. Based on soil respiration measurements the effects of different management systems (moldboard plowing, chisel and no-tillage) and the application of composted sludge (CS) and thermally-dried sewage sludge (TSS) was investigated in a long-term field experiment (28 years) conducted on a sandy-loam soil at the experimental station 'La Higueruela' (40o 03'N, 4o 24'W). Both organic amendments were applied at a rate of 30 Mg ha-1 prior to tillage practices. Unamended soils were used as control for each tillage system. SCE was moderate in late spring (2.2-11.8 μmol CO2 m-2 s-1) when amendments were applied and tillage was performed, markedly decreased in summer (0.4-3.2 μmol CO2 m-2 s-1), following a moderate increase in autumn (3.4-14.1 μmol CO2 m-2 s-1), rising sharply in October (5.6-39.8 μmol CO2 m-2 s-1 ). In winter, SCE was low (0.6-6.5 μmol CO2 m-2 s-1). In general, SCE was greater in chisel and moldboard tilled soils, and in CS and particularly TSS-amended soils, due to the addition of labile C with these amendments, meanwhile no-tillage soils exhibited smaller increases in C efflux throughout the seasons. Soil temperature controlled the seasonal variations of SCE. In summer, when drought occurs, a general decrease of SCE was observed due to a deficit in soil water content. After drought period SCE jumped to high values in response to rain events ('Birch effect') that changed soil moisture conditions. Soil drying in summer and rewetting in autumn may promotes some changes on the structure of soil microbial community, affecting associated metabolic processes, and enhancing a rapid mineralization of water-soluble organic C compounds and/or dead microbial biomass that acts as an energy source for soil microorganisms. To assess the effects of tillage and amendments on SCE, Q10 values were calculated. Data were grouped into three groups according to soil moisture (0.03-0.10 m3m-3, 0-11-0.21 m3m-3, 0.22-0.30 m3m-3). In general, Q10 values were lower at elevated temperatures when soil moisture contents decreased, confirming that SCE is less sensitive to soil temperature during drought periods. Q10 values were higher in moldboard and chisel tilled soils, possibly due to the incorporation of residues into soil and the increase of soil C substrate, meanwhile in no-tillage part of the organic C pools are likely protected from microorganisms by physico-chemical mechanisms. TSS-amended soils exhibited higher Q10 values than CS, pointing that the biochemical lability of the organic C added with amendments exerts an influence on SCE. Acknowledgements: this research was supported by the Spanish CICYT, Project no. CTM2011-25557.
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Implementation Analysis of Cutting Tool Carbide with Cast Iron Material S45 C on Universal Lathe
NASA Astrophysics Data System (ADS)
Junaidi; hestukoro, Soni; yanie, Ahmad; Jumadi; Eddy
2017-12-01
Cutting tool is the tools lathe. Cutting process tool CARBIDE with Cast Iron Material Universal Lathe which is commonly found at Analysiscutting Process by some aspects numely Cutting force, Cutting Speed, Cutting Power, Cutting Indication Power, Temperature Zone 1 and Temperatur Zone 2. Purpose of this Study was to determine how big the cutting Speed, Cutting Power, electromotor Power,Temperatur Zone 1 and Temperatur Zone 2 that drives the chisel cutting CARBIDE in the Process of tur ning Cast Iron Material. Cutting force obtained from image analysis relationship between the recommended Component Cuting Force with plane of the cut and Cutting Speed obtained from image analysis of relationships between the recommended Cutting Speed Feed rate.
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Recent developments in hydrologic instrumentation
Latkovich, Vito J.; Futrell, James C.; Kane, Douglas L.
1986-01-01
The programs of the U.S. Geological Survey require instrumentation for collecting and monitoring hydrologic data in cold regions. The availability of space-age materials and implementation of modern electronics and mechanics is making possible the recent developments of hydrologic instrumentation, especially in the area of measuring streamflow under ice cover. Material developments include: synthetic-fiber sounding and tag lines; polymer (plastic) sheaves, pulleys, and sampler components; and polymer (plastic) current-meter bucket wheels. Electronic and mechanical developments include: a current-meter digitizer; a fiber-optic closure system for current-meters; non-contact water-level sensors; an adaptable hydrologic data acquisition system; a minimum data recorder; an ice rod; an ice foot; a handled sediment sampler; a light weight ice auger with improved cutter head and blades; and an ice chisel.
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Hansson, J E; Eklund, L; Kihlberg, S; Ostergren, C E
1987-03-01
The main objective of the study was to find efficient hand tools which caused only minor vibration loading. Vibration measurements were carried out under standardised working conditions. The time during which car body repairers in seven companies were exposed to vibration was determined. Chisel hammers, impact wrenches, sanders and saws were the types of tools which generated the highest vibration accelerations. The average daily exposure at the different garages ranged from 22 to 70 min. The risk of vibration injury is currently rated as high. The difference between the highest and lowest levels of vibration was considerable in most tool categories. Therefore the choice of tool has a major impact on the magnitude of vibration exposure. The importance of choosing the right tools and working methods is discussed and a counselling service on vibration is proposed.
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[Chromatography analysis of tobacco smoke condensate in biology tissue].
Zurabashvili, D Z; Chanturia, I R; Kapanadze, L R
2010-01-01
Specialized analytical instrumentation for detailed analysis of nicotine, benz(alpha)pyrene, pyridine and benzene in tooth enamel and pulp of inveterate tobacco smokers is created. A Waters PPY-24 liquid chromatograph is equipped with Model M660 solvent programmer and a Model U6K sample injector is used. A Model 440 dual-wavelength detector is used to obtain absorbance ratios on dual-pen recorder. Our data show that concentration of tobacco smoke components in tooth cavity of inveterate tobacco smokers is different. The chisel tooth pulp contained considerably more nicotine and pyridine as compared with molars. The level of benzene does not change analyzed structures. The assumption of linearity between calculation of predicted retention times and concentration has been shown to be valid up to about 8,0% for all studied compounds.
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NASA Astrophysics Data System (ADS)
Iturria, Iban; Zubieta, Elena; Giménez, Rafael; Ángel Campo-Bescós, Miguel
2017-04-01
To address studies on soil erosion and water quality it is essential to understand and quantify water movements through the soil. The estimation of this movement is usually based on soil texture and structure since it is assumed that the water moves across soil matrix. However, soils prone to the formation of cracks or macropores could trigger rapid flow paths, capable of drastically changing the movement of the water and, therefore, its connectivity across the soil. This would have important consequences both for runoff -and thus for erosion- and for groundwater quality. Local preliminary studies have shown that in many agrarian soils in Navarre (Spain), infiltration rate was mainly determined by this type of preferential flow. On the other hand, the formation of these cracks basically responded to expansion/contraction processes of clays due to changes in soil moisture content caused by rainfall. The aim of this work was to quantify in agricultural soil the presence of cracks/macropores responsible for preferential flow and their temporal variation compared to different soil moisture contents. The work was carried out in experimental plots (150 m2) of the UPNA with different type of conventional tillage: (i) mouldboard plough: (ii) chisel and (iii) mouldboard+Molon rake. Each plot was divided into two halves or subplots. On half was submitted to the action of 4 simulated rainfall (5 days passing between each event); whereas in the other half, no rain was applied. Six subplots were thus defined. After each of the 4 rainfall, and once the 5 days had passed, the following experiments were conducted in each of the 6 subplots. In microplots (0.5 m2) a colourant (aqueous solution of bromide) was applied (Lu and Wu, 2003). To be specific, 8 mm of this solution was applied as intense rain with a sprinkler, but avoiding any waterlogging. Then, vertical cuts of 50-60 cm were made where the cracks/macropores were evidenced by the colourant. Photographs of the profiles were obtained. From these, binary images were obtained: soil matrix vs macropores/cracks. Statistical analysis was performed to characterize the macropore/crack distribution pattern. First results indicated clear differences between the different tillage in the crack/macropores distribution. For example, in treatments in which the mouldboard plough was used, (i and iii), a greater presence of macropores was observed in the upper 20 cm. However, with the treatment with chisel (ii), macropores were evident in the whole soil profile; this was due to the chisel making cracks in the plow sole thus promoting water flow. Also, this pattern was affected by rainfall (and therefore in soil moisture) but information is still scarce for any greater precisions. The extrapolation of these results would serve, for instance to (i) gain a better understanding of water movement and its connectivity in the soil and, thus, of the hydrological behaviour of typical agrarian catchments in Navarre; (ii) to improve the performance of hydrological models for land management, and (iii) optimize irrigation design and soil management practices. Reference Lu, J., Wu, L. 2003. Visualizing bromide and iodide water tracer in soil profiles by spray methods. Journal of Environmental Quality 32(1): 363-367
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Soil Carbon Changes in Transitional Grain Crop Production Systems in South Dakota
NASA Astrophysics Data System (ADS)
Woodard, H. J.
2004-12-01
Corn-C (Zea Mays L.), soybean-S (Glycine max L.) and spring wheat-W (Triticum aestivum L.) crops were seeded as a component of either a C-S, S-W, or C-S-W crop rotation on silt-loam textured soils ranging from 3.0-5.0% organic matter. Conservation tillage(chisel plow-field cultivator) was applied to half of the plots. The other plots were direct seeded as a no-till (zero-tillage) treatment. Grain yield and surface crop residues were weighed from each treatment plot. Crop residue (stover and straw) was removed from half of the plots. After four years, soil samples were removed at various increments of depth and soil organic carbon (C) and nitrogen (N) was measured. The ranking of crop residue weights occurred by the order corn>>soybean>wheat. Surface residue accumulation was also greatest with residue treatments that were returned to the plots, those rotations in which maize was a component, and those without tillage. Mean soil organic carbon levels in the 0-7.5cm depth decreased from 3.41% to 3.19% (- 0.22%) with conventional tillage (chisel plow/field cultivator) as compared to a decrease from 3.19% to 3.05% (-0.14%) in plots without tillage over a four year period. Organic carbon in the 0-7.5cm depth decreased from 3.21% to 3.01% (- 0.20%) after residue removed as compared to a decrease from 3.39% to 3.23% (-0.17%) in plots without tillage applied after four years. The soil C:N ratio (0-7.5cm) decreased from 10.63 to 10.37 (-0.26 (unitless)) in the tilled plots over a four-year period. Soil C:N ratio at the 0-7.5cm depth decreased from 10.72 to 10.04 (-0.68) in the no-till plots over a four year period. Differences in the soil C:N ratio comparing residue removed and residue returned were similar (-0.51 vs. -0.43 respectively). These soils are highly buffered for organic carbon changes. Many cropping cycles are required to determine how soil carbon storage is significantly impacted by production systems.
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Can short-term pasture management increase C balance in the Atlantic Rainforest?
da Rocha Junior, Paulo Roberto; Andrade, Felipe Vaz; Santos Satiro, Lucas; Donagemma, Guilherme Kangussú; de Sá Mendonça, Eduardo
2018-05-11
Few studies have shown the importance of different pasture management practices on C storage and the reduction of CO 2 -C emissions in tropical conditions. The objective of the present study was to determine short-term changes in C pools and C balance from different pasture management practices established in the Atlantic Rainforest. A field study was carried out in Alegre, ES, Brazil from September 2013 to August 2014 to investigate the first-year effect of pasture management practices on a Udult clayey soil. The different pasture management practices studied included the following: control (CON), chiseled (CHI), fertilized (FER), burned (BUR), integrated with crop-livestock (iCL) systems, and plowed and harrowed (PH). Monthly disturbed and undisturbed soil samples were taken at two different layers (0.00-0.05 and 0.05-0.20 m) for chemical, physical, and organic matter characterization. C inputs monitored in aboveground pools included plant aerial parts and litter, and belowground pools included roots and soil C stocks. C outputs monitored were CO 2 -C emissions, erosion water, and sediment. C balance was considered the difference between inputs and outputs in each treatment during four seasons. The spring and summer seasons had a strong influence on C inputs and outputs where there is significant difference between spring and summer, while the autumn and winter seasons had less influence. All pasture management practices exhibited positive C balance after 1 year. High values of C balance were verified in pastures fertilized (FER) (53.04 Mg ha -1 year -1 . Intermediate C balance was found in the burned (BUR) (40.84 Mg ha -1 year -1 ), traditional control (CON) (40.31 Mg ha -1 year -1 ), and in the plowing and harrowing (PH) (40.02 Mg ha -1 year -1 ) management practices. The practices of chiseled (40.00 Mg ha -1 year -1 ) and integrated crop-livestock systems (iCL) (59.06 Mg ha -1 year -1 ) resulted in low C balance.
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Zurabashvili, D; Chanturia, I; Kapanadze, L; Danelia, G
2010-02-01
The composition of cigarette-smoke is relatively well known in spite of its tremendous complexity. But the analysis of cigarette smoke toxicological influence on biochemical components of tooth enamel, dentine and pulpe is not completely study. The present study was designed to characterize the pulpe biochemical component (alpha-ketopropionic acide) by acute serous pulpit. The total number of 140 patients, age 35-40 (Tobacco-smokers 80, non-smokers - 60) have been investigated. The results suggested, that tobacco-smokers chisel tooth and molars contains less alpha-ketopropionic acide than non-smokers individuals. These studies support the hypothesis of cigarette smoke important role in the tooth support mechanisms. The biochemical activity and function of tooth proteins and amino acids composition must by compared to concentration of tobacco-smoke components.
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So I Sat Down with My Mother: Connectedness Orientation and Pupils' Independence
NASA Astrophysics Data System (ADS)
Eklöf, Anders; Nilsson, Lars-Erik; Svensson, Peter
Swedish educational policy underlines the importance of independence. In this paper we use socio-cultural theory and Foucault to explain how pupils’ independency is transformed into something else in their work. Our results derive from analyses of filmed sessions and entries in the pupils’ logbooks. Our findings demonstrate that the pupils’ definitions of independence differ from those of the course plan in several aspects: i) the use of certain resources is not considered to show lack of independence, ii) doing things yourself is considered being most independent and iii) to follow instructions, even if this means violating your unique personal thought, is considered a prerequisite for passing/getting good grades and as such a necessary adaption to the school context, sooner than a sign of dependency. Consequently we argue that pupil independency should be regarded as a phenomenon chiseled out within a community of practice rather than a personal capacity.
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[Multi-center study of the Jenaer model of the temporal bone].
Schneider, G; Müller, A
2004-06-01
Preparing exercises at the temporal bone are a prerequisite for the knowledge of the anatomical special features of this region and for learning the fundamentals of the tympanic cavity surgery. Since however fewer human temporal bones are available, the search for back-up models already took place in the last years. Based on the experiences of the handling and visualization of CT data for the 3D-implant construction in the ent department Jena a temporal bone model was developed. The model was sent away to surgeons of different training. On the basis of identification of anatomical structures and evaluation of general parameters by means of a point system the model was evaluated. The Jenaer temporal bone model is suitable as entrance into the preparing exercises. The anatomical structures are good to identify for the beginner. The handling with drill and chisel can be learned.
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Benchmarks for target tracking
NASA Astrophysics Data System (ADS)
Dunham, Darin T.; West, Philip D.
2011-09-01
The term benchmark originates from the chiseled horizontal marks that surveyors made, into which an angle-iron could be placed to bracket ("bench") a leveling rod, thus ensuring that the leveling rod can be repositioned in exactly the same place in the future. A benchmark in computer terms is the result of running a computer program, or a set of programs, in order to assess the relative performance of an object by running a number of standard tests and trials against it. This paper will discuss the history of simulation benchmarks that are being used by multiple branches of the military and agencies of the US government. These benchmarks range from missile defense applications to chemical biological situations. Typically, a benchmark is used with Monte Carlo runs in order to tease out how algorithms deal with variability and the range of possible inputs. We will also describe problems that can be solved by a benchmark.
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NASA Astrophysics Data System (ADS)
Bulakh, Andrey
2016-04-01
Soap stone represents soft Proterozoic rock type from the deposit Nunnalahti situated on the western shore of the big Lake Pielinen in Eastern Finland. It consists of talc (40 - 50 %), magnesite MgCO3 (40 - 50 %), chlorite (5 - 8 %), dolomite, calcite, etc. The colour of the stone is very spectacular and varies from yellow and brownish-yellow to grey, greenish grey. The soft stone is a highly workable material for a sculptor's chisel. It was one of the most popular ornamental rocks used architecture of the Modern style in St Petersburg, Helsinki, Turku, Tampere and other North European cities lately in the XIX-th centuries. Examples are given and discussed. References: Bulakh, A.G., Abakumova, N.B., and Romanovsky, J.V. St Petersburg: a History in Stone. 2010. Print House of St Petersburg State University. 173 p. (In English).
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Sainju, Upendra M; Singh, Bharat P; Whitehead, Wayne F; Wang, Shirley
2006-01-01
Soil carbon (C) sequestration in tilled and nontilled areas can be influenced by crop management practices due to differences in plant C inputs and their rate of mineralization. We examined the influence of four cover crops {legume [hairy vetch (Vicia villosa Roth)], nonlegume [rye (Secale cereale L.)], biculture of legume and nonlegume (vetch and rye), and no cover crops (or winter weeds)} and three nitrogen (N) fertilization rates (0, 60 to 65, and 120 to 130 kg N ha(-1)) on C inputs from cover crops, cotton (Gossypium hirsutum L.), and sorghum [Sorghum bicolor (L.) Moench)], and soil organic carbon (SOC) at the 0- to 120-cm depth in tilled and nontilled areas. A field experiment was conducted on Dothan sandy loam (fine-loamy, siliceous, thermic Plinthic Paleudults) from 1999 to 2002 in central Georgia. Total C inputs to the soil from cover crops, cotton, and sorghum from 2000 to 2002 ranged from 6.8 to 22.8 Mg ha(-1). The SOC at 0 to 10 cm fluctuated with C input from October 1999 to November 2002 and was greater from cover crops than from weeds in no-tilled plots. In contrast, SOC values at 10 to 30 cm in no-tilled and at 0 to 60 cm in chisel-tilled plots were greater for biculture than for weeds. As a result, C at 0 to 30 cm was sequestered at rates of 267, 33, -133, and -967 kg C ha(-1) yr(-1) for biculture, rye, vetch, and weeds, respectively, in the no-tilled plot. In strip-tilled and chisel-tilled plots, SOC at 0 to 30 cm decreased at rates of 233 to 1233 kg C ha(-1) yr(-1). The SOC at 0 to 30 cm increased more in cover crops with 120 to 130 kg N ha(-1) yr(-1) than in weeds with 0 kg N ha(-1) yr(-1), regardless of tillage. In the subtropical humid region of the southeastern United States, cover crops and N fertilization can increase the amount of C input and storage in tilled and nontilled soils, and hairy vetch and rye biculture was more effective in sequestering C than monocultures or no cover crop.
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Strength Properties and Organic Carbon of Soils in the North Apalachian Region
DOE Office of Scientific and Technical Information (OSTI.GOV)
Blanco-Canqui, H; Lal, Rattan; Owen, L B.
2005-04-01
Soil strength influenced by management and soil properties controls plant growth, root development, and soil-moisture relations. The impact of textural and structural parameters on soil strength is moderated by soil organic C (SOC) concentration. Therefore, the objectives of this study were to assess differences in soil strength and SOC concentration in watersheds under long-term (>15 yr) management practices in the North Appalachian region on a predominantly Typic Hapludults on undulating slopes (>6% slope). Seven watersheds without field replication under moldboard plow (MP), chisel plow, disk with beef cattle manure (DiskM), no-till with beef cattle manure (NTm), no-till with no beefmore » cattle manure (NTnm), pasture, and forest were studied. Cone index (CI), shear strength, bulk density (b), volumetric moisture content (v), and SOC concentration were determined at the summit, backslope, and footslope landscape positions at the 0- to 10-, 10- to 20-, and 20- to 30-cm depths. The SOC concentration was slightly higher at the footslope than at the summit position in the cultivated watersheds. The b was lower at the footslope than at the summit in NTm (1.22 vs. 1.42 Mg m{sup -3}) and chisel (1.34 vs. 1.47 Mg m{sup -3}) treatments. Forest had the lowest CI (0.19 MPa), shear strength (6.11 kPa), and b (0.93 Mg m{sup -3}) and the highest SOC concentration (62.7 g kg{sup -1}), whereas MP had the highest CI (0.67 MPa), shear strength (25.5 kPa), b (1.44 Mg m{sup -3}), and the lowest SOC concentration (13.6 g kg{sup -1}) in the 0- to 10-cm depth (P < 0.01). The SOC concentration in NTm was 1.7 times higher than that in NTnm, and both no-till treatments had lower b (<1.21 Mg m{sup -3}) than MP (1.44 Mg m{sup -3}) at 0- to 10-cm depth (P < 0.01). Manuring decreased both CI and shear strength, but increased SOC concentration. The b, v, and SOC concentration were potential predictors of CI; whereas b and SOC concentration were of shear strength (r2 > 0.42; P < 0.01). Results show that landscape positions had small effect, but management, particularly manuring, had large and significant effects on soil strength and SOC concentration.« less
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Research Amplitudo Vibration On Holder Due To The Process Of Lathe Nozzle Rocket RX 450
NASA Astrophysics Data System (ADS)
Ediwan; Budi Djatmiko, Agus; Dody Arisandi, EfFendy; Purnomo, Heri; Ibadi, Mahfud
2018-04-01
The main function of the rocket nozzle is to convert the enthalpy efficiency from combustion gas to kinetic energy and also to make high velocity out of the gas. The rocket nozzle usually consists of a converging and diverging part. With a smaller area on the neck and enlarged at the exit area. The velocity flow through the nozzle enlarges into the speed of sound through the neck and then becomes super sonic in the divergent part. Nozzle making or machining using conventional lathes, first performed is drilling on a massive metal that is bonded to the veneer, then after a sufficient gap is done deep-boring. At the time of the process of lathe in the nozzle RX 450 there is an obstacle that is vibrating tool holder chisel or holder so it is worried about not precision of the process of lathe. This should not happen because it can cause failure in the latter for it needs to be studied and studied further so that the lathe process goes accordingly. The holder material of ST 60 with a modulus of elasticity 200 GPa and a nozzle material of AISI 4340 alloy steel with σyield = 470 MPa, Shear Modulus G = 80 GPa. The purpose of this research is to observe the amplitude of vibration on the holder due to RX- 450 nozzle lathe processing for the purpose of amplitude that occurs in accordance with the desired so that the nozzle structure is no damage process. The result of the research was obtained holder with length (L) 80cm, profile width (B) 5 cm, height of profile (H) 10 cm, turning machine ω = 8.98 rad / sec and natural holder frequency ωn = 89.8 rad / second, Amplitude of vibration of δ = 1.21 mm, while the amplitude of the design X = 1.22 mm From the results of this study it can be said that the holder of a chisel or holder can be used as a tool at the time of RX nozzle retrieval process and is quite safe because it works under the condition ω/ω n <0 3 (Plans and Specifications of A Suborbital Rocket Payload "AKPV Engineering University of Wyoming 2009 )
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Rotary Percussive Auto-Gopher for Deep Drilling and Sampling
NASA Technical Reports Server (NTRS)
Bar-Cohen, Yoseph; Badescu, Mircea; Sherrit, Stewart
2009-01-01
The term "rotary percussive auto-gopher" denotes a proposed addition to a family of apparatuses, based on ultrasonic/ sonic drill corers (USDCs), that have been described in numerous previous NASA Tech Briefs articles. These apparatuses have been designed, variously, for boring into, and/or acquiring samples of, rock or other hard, brittle materials of geological interest. In the case of the rotary percussive autogopher, the emphasis would be on developing an apparatus capable of penetrating to, and acquiring samples at, depths that could otherwise be reached only by use of much longer, heavier, conventional drilling-and-sampling apparatuses. To recapitulate from the prior articles about USDCs: A USDC can be characterized as a lightweight, low-power jackhammer in which a piezoelectrically driven actuator generates ultrasonic vibrations and is coupled to a tool bit through a free mass. The bouncing of the free mass between the actuator horn and the drill bit converts the actuator ultrasonic vibrations into sonic hammering of the drill bit. The combination of ultrasonic and sonic vibrations gives rise to a hammering action (and a resulting chiseling action at the tip of the tool bit) that is more effective for drilling than is the microhammering action of ultrasonic vibrations alone. The hammering and chiseling actions are so effective that the size of the axial force needed to make the tool bit advance into soil, rock, or another material of interest is much smaller than in ordinary rotary drilling, ordinary hammering, or ordinary steady pushing. The predecessor of the rotary percussive auto-gopher is an apparatus, now denoted an ultrasonic/sonic gopher and previously denoted an ultrasonic gopher, described in "Ultrasonic/ Sonic Mechanism for Drilling and Coring" (NPO-30291), NASA Tech Briefs Vol. 27, No. 9 (September 2003), page 65. The ultrasonic/sonic gopher is intended for use mainly in acquiring cores. The name of the apparatus reflects the fact that, like a gopher, it periodically stops advancing at the end of the hole to bring excavated material (in this case, a core sample) to the surface, then re-enters the hole to resume the advance of the end of the hole. By use of a cable suspended from a reel on the surface, the gopher is lifted from the hole to remove a core sample, then lowered into the hole to resume the advance and acquire the next core sample.
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[Applicational evaluation of split tooth extractions of upper molars using piezosurgery].
Li, D; Guo, C B; Liu, Y; Wang, E B
2016-02-18
To evaluate the efficacy of Piezosurgery in split teeth extractions. A single-center, randomized, split-mouth study was performed using a consecutive serious of unrelated healthy patients attending the departing of oral and maxillofacial surgery, Peking University School and Hospital of Stomatology. 40 patients were selected for extraction of maxillary molars without reservation value,splitting or nonvital teeth. They were divided into control (20 patients) and test groups (20 patients) randomly. Surgical treatments for both groups were under local anesthesia. Molar teeth of control group were extracted by common equipments like dental elevators, chisels, forceps, etc. While molar teeth of experimental group were extracted by Piezosurgery, aided with the use of common equipments if needed. Then we compared the duration of surgery, frequency of the usage of chisels, expansion of postoperative bony socket surgical discomfort and postoperative pain between two groups. The average of operation time was (629.5±171.0) s in control group and (456.0±337.2) s in test group. The buccal alveolar bone reduced (1.07±0.64) mm in control group and (1.49±0.61) mm in test group. There was a significant difference between the two groups (P<0.05). The duration of surgery for experimental group was significantly longer than that of the control group, but the change of buccal alveolar bone was lower than the control group. For visual analogue scale (VAS) value of surgical discomfort, expansion of postoperative bony socket and the operative fear rate, there were no significant difference between the two groups (P>0.05). Piezosugery can be better to preserve alveolar bone, reduce trauma and patient's fear. Application of the piezosugery reflect the characteristics of minimally invasive extraction, which has the value of promotion. The Piezosurgery technique have the advantage of reducing change of buccal alveolar bone during the surgery, but a longer surgical time was required when compared with the conventional technique. VAS value of surgical discomfort, expansion of postoperative bony socket and the operative fear rate, there were no significant difference. Minimally invasive tooth extraction technique has good clinical results and high satisfaction. Piezosurgery proved its worth as the instrument adapted to limiting the destruction of bone tissue.
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[Applicational evaluation of split tooth extractions of upper molars using piezosurgery].
Li, D; Guo, C B; Liu, Y; Wang, E B
2016-08-18
To evaluate the efficacy of Piezosurgery in split teeth extractions. A single-center, randomized, split-mouth study was performed using a consecutive serious of unrelated healthy patients attending the departing of oral and maxillofacial surgery, Peking University School and Hospital of Stomatology. 40 patients were selected for extraction of maxillary molars without reservation value,splitting or nonvital teeth. They were divided into control (20 patients) and test groups (20 patients) randomly. Surgical treatments for both groups were under local anesthesia. Molar teeth of control group were extracted by common equipments like dental elevators, chisels, forceps, etc. While molar teeth of experimental group were extracted by Piezosurgery, aided with the use of common equipments if needed. Then we compared the duration of surgery, frequency of the usage of chisels, expansion of postoperative bony socket surgical discomfort and postoperative pain between two groups. The average of operation time was (629.5±171.0) s in control group and (456.0±337.2) s in test group. The buccal alveolar bone reduced (1.07±0.64) mm in control group and (1.49±0.61) mm in test group. There was a significant difference between the two groups (P<0.05). The duration of surgery for experimental group was significantly longer than that of the control group, but the change of buccal alveolar bone was lower than the control group. For visual analogue scale (VAS) value of surgical discomfort, expansion of postoperative bony socket and the operative fear rate, there were no significant difference between the two groups (P>0.05). Piezosugery can be better to preserve alveolar bone, reduce trauma and patient's fear. Application of the piezosugery reflect the characteristics of minimally invasive extraction, which has the value of promotion. The Piezosurgery technique have the advantage of reducing change of buccal alveolar bone during the surgery, but a longer surgical time was required when compared with the conventional technique. VAS value of surgical discomfort, expansion of postoperative bony socket and the operative fear rate, there were no significant difference. Minimally invasive tooth extraction technique has good clinical results and high satisfaction. Piezosurgery proved its worth as the instrument adapted to limiting the destruction of bone tissue.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Almgren, Ann; DeMar, Phil; Vetter, Jeffrey
The widespread use of computing in the American economy would not be possible without a thoughtful, exploratory research and development (R&D) community pushing the performance edge of operating systems, computer languages, and software libraries. These are the tools and building blocks — the hammers, chisels, bricks, and mortar — of the smartphone, the cloud, and the computing services on which we rely. Engineers and scientists need ever-more specialized computing tools to discover new material properties for manufacturing, make energy generation safer and more efficient, and provide insight into the fundamentals of the universe, for example. The research division of themore » U.S. Department of Energy’s (DOE’s) Office of Advanced Scientific Computing and Research (ASCR Research) ensures that these tools and building blocks are being developed and honed to meet the extreme needs of modern science. See also http://exascaleage.org/ascr/ for additional information.« less
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A ballistic performance study on multiphase particulate systems impacted by various projectiles
NASA Astrophysics Data System (ADS)
Comtois-Arnaldo, Christian; Petel, Oren
2017-06-01
The present study investigates the complex multiscale dynamic response of particulate composites, in an effort to link the bulk material behavior to strain-rate activated microstructures. These investigations involve multiphase systems containing micron-sized ceramic particles integrated into a siloxane elastomer to create flexible nanocomposites with varying inclusion properties. In particular, the effects of varying particle morphology, strength, volume fraction, and density are under investigation. The experimental focus of the study concerns the ballistic penetration of the nanocomposite targets. The targets are impacted by fragment simulating steel projectiles of constant mass and varying nose shapes (i.e., flat, ogive, and chisel-nose) to identify variations in the penetration mechanics. The projectiles are accelerated in a single-stage gas gun to velocities ranging from 200 m/s to 900 m/s prior to impact. The results for each projectile type are compared to analytical penetration models in order to shed light on the dominant penetration mechanisms and their relationship to the microstructure of the nanocomposites.
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Use of Scheimpflug imaging in the management of intra-lenticular foreign body.
Singh, R; Ram, J; Gupta, R
2015-01-01
Asymptomatic traumatic intra-lenticular foreign body is very uncommon and few case reports have been published. To report a case of post-traumatic intra-lenticular foreign body and use of Scheimpflug imaging in its management. A 41-year-old male with history of injury to right eye during hammering a chisel 1 year back presented with decreased vision since 6 months. An intra-lenticular foreign body was found on slit lamp bio-microscopy and was confrmed by Scheimpflug imaging. Posterior capsule was intact on Scheimpflug imaging. Thus, Scheimpflug imaging helps in exact localization of the foreign body in the intralenticular space or behind the iris. We ruled out other foreign bodies by x-ray and ultrasonography of the orbit. The foreign body with post-traumatic cataract was removed using phacoemulsification and three piece foldable intraocular lens was implanted in the bag. An intra- lenticular foreign body may remain asymptomatic for months. Scheimpflug imaging can be useful in its localization. It can be removed during phacoemulsification. © NEPjOPH.
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NASA Astrophysics Data System (ADS)
McLeod, Edward; McLeod, Roger
2006-03-01
Chisel-quarried recycled granite in MA is datable by runes to 1069 CE; it could corroborate dating by a LIDAR. Associated sites, possibly used by Vikings to dry-dock their ships, could have exploited lock-like controls, possibly a continued technology. Site-leveling at the Giza Pyramids proves water was used. `Locks' and body-immersion worked for building, moving, erecting, or watering, at sites like Stonehenge, The Hanging Gardens at Babylon, the Moas of Easter Island, or The Pyramids, where the eroding water discharge was deliberately flushed over the Sphinx complex. It enhance the electromagnetically excited blue light signals we can detect, especially at sites frequented by Molocket of ME. Information, as at America's Stonehenge, in NH, and constructions at Acton MA, at Giza or at Rumford ME proves that the Pyramids and Sphinx were engineered and built about 4500 BP.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
2014-08-21
Recent advancements in technology scaling have shown a trend towards greater integration with large-scale chips containing thousands of processors connected to memories and other I/O devices using non-trivial network topologies. Software simulation proves insufficient to study the tradeoffs in such complex systems due to slow execution time, whereas hardware RTL development is too time-consuming. We present OpenSoC Fabric, an on-chip network generation infrastructure which aims to provide a parameterizable and powerful on-chip network generator for evaluating future high performance computing architectures based on SoC technology. OpenSoC Fabric leverages a new hardware DSL, Chisel, which contains powerful abstractions provided by itsmore » base language, Scala, and generates both software (C++) and hardware (Verilog) models from a single code base. The OpenSoC Fabric2 infrastructure is modeled after existing state-of-the-art simulators, offers large and powerful collections of configuration options, and follows object-oriented design and functional programming to make functionality extension as easy as possible.« less
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Song, Juan; Bi, Xiaoqin
2012-08-01
To study the nursing methods and its effect in mandibular mesioangular impacted third molar extraction with reversal high-speed air turbine. 60 patients with mandibular mesioangular impacted third molar were selected in this study, who were treated in Department of Senior Dentists, West China School of Stomatology, Sichuan University, between June to December 2010. They were randomly and equally divided into control group and experimental group (n=30). The former was treated with tradition chisel splint method while the latter was treated with reversal high-speed air turbine extraction and provided appropriate nursing interventions. Postoperative reactions and wound healing status were evaluated through consultation. There were significant differences between control group and experimental group in terms of postoperative bleeding wound, swelling, dry socket and so on (P<0.05). Mandibular mesioangular impacted third molar extraction with reversal high-speed air turbine is effective, and the corresponding nursing measure is worthy further promotion.
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Heritage stones and their deterioration in rock-cut monuments in India
NASA Astrophysics Data System (ADS)
Sharma, Vinod K.
2017-04-01
India is dotted with thousands of rock- cut monuments of considerable antiquity having artwork of global importance. It is evident from the location of many of these monuments that knowledge of viable selection of site, geotechnical considerations and amenability to sculptures' chisel was vital for construction of rock-cut monuments and sculptures. These rock-cut structures also represent significant achievements of geotechnical and structural engineering and craftsmanship of contemporary period. The paper deals with some of the sites where natural rock-mass exposures were used to hew the monuments and highlight the deterioration owing to geological and climatic conditions. The Kailash temple in Ellora and Ajanta rock-cut caves are among the greatest architectural feats which owe their grandeur to amenability and consistency of basalt of Deccan Volcanic Province from which it is hewn. The Kailash Temple was created through a single, huge top-down excavation 100 feet deep down into the volcanic basaltic cliff rock. These ancient rock cut structures are amazing achievements of structural engineering and craftsmanship. The lava flows are nearly horizontal, competent rock medium facilitated the chiseling for the sculptures. The deterioration of these basalts are seen where the amygdule, vesicles and opening in rock discontinuity had the medium of construction or excavation. The monolithic rock- cut monuments of Mahabalipuram temples are constructed in the form of rathas or chriot and adjoining caves by excavating solid charnockite/granites. The large rock exposures are excavated and cut to perfection with wall decorations and sculptured art. The charnockites are the strongest and the most durable rock, yet quite amenable to fine dressing. These monolithic monuments in charnockite and are cut out of the hillock. The 7th Century monuments now exhibit somewhat rough surface probably due to weathering effect of salt laden winds from the sea side and alteration of feldspars. The Rock shelters of Bhimbetka, a World Heritage Site, are located within Vindhyan sandstone, yielded primitive tools and decorative rock paintings.The rock-cut caves in twin hills Udayagiri and Khandagiri , contain carvings sculptured in coarse grained grey to buff coloured sandstone of Gondwana group of rocks. The Badami cave temples constructed out of escarpment of the hill in sandstone represent some of the earliest known examples of Hindu temples. Utilizing in situ rock exposures, natural rocks and landscape of Deccan basalts, granites of peninsular shield, sandstones and limestone for rock cut architecture in India, thus, holds varied examples of rock-cut architectures.
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Draenert, Florian Guy; Huetzen, Dominic; Kämmerer, Peer; Wagner, Wilfried
2011-09-01
Bone transplants are mostly prepared with cutting drills, chisels, and rasps. These techniques are difficult for unexperienced surgeons, and the implant interface is less precise due to unstandardized preparation. Cylindrical bone transplants are a known alternative. Current techniques include fixation methods with osteosynthesis screws or the dental implant. A new bone cylinder transplant technique is presented using a twin-drill principle resulting in a customized pressfit of the transplant without fixation devices and combining this with the superior grinding properties of a diamond coating. New cylindrical diamond hollow drills are used for customized press fit bone transplants in a case series of five patients for socket reconstruction in the front and molar region of maxilla and mandibula with and without simultaneous implant placement. The technical approach was successful without intra or postoperative complications during the acute healing phase. The customized press fit completes a technological trias of bone cylinder transplant techniques adding to the assisted press fit with either osteosynthesis screws or the dental implant itself. © 2009 Wiley Periodicals, Inc.
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The handedness of Michelangelo Buonarroti.
Lazzeri, Davide
2018-05-07
The handedness of Michelangelo Buonarroti (1475-1564), one of the greatest artists of all time, is still controversial. Although there is no doubt that almost all of his well-attributed drawings were drawn with the right hand, the hatch marks of the shading going downward from right to left; it has been often neglected in the literature that he was an innate left-hander. An unfairly unknown autobiography of Raffaello da Montelupo stated that Michelangelo, a natural left-hander, trained himself from a young age to become right-handed. The same biography also underlined that Michelangelo restricted the use of his left hand only to works requiring force such as hammering, carving, and chiseling marble. The sign of the wooden crucifix donated to Santo Spirito in 1492 and two autographic sketches by Michelangelo-one left alongside a poem in 1509, and the other in the dress of the Vittoria Colonna sketch in 1525-are useful tools for analyzing the artist's evolution from left to right handedness when drawing, writing, and painting. Clin. Anat., 2018. © 2018 Wiley Periodicals, Inc. © 2018 Wiley Periodicals, Inc.
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Use of scleractinian corals to indicate marine pollution in the northern Gulf of Aqaba, Jordan.
Barakat, S A; Al-Rousan, S; Al-Trabeen, M S
2015-02-01
The actual and fatal concentrations of selected heavy metals, including cadmium, cobalt, copper, lead, nickel, and zinc in corals from the Gulf of Aqaba were determined. Several living coral samples of different species (e.g., Porites) were collected from shallow depths (of about 5 m) at a number of sites along the Jordanian Gulf of Aqaba coast. The coral samples were collected using either a pneumatic diamond drill corer (for Porites) or a hammer and chisel (for other branched species). Some of the corals that had been collected were analyzed for heavy metals using atomic absorption spectrometry, and other samples were used in incubation experiments. The heavy metal concentrations were determined separately in the coral skeleton and the tissue layer. Heavy metal concentrations have not previously been determined in corals from the Gulf of Aqaba. We conclude that corals are suitable for use as proxy tools for assessing environmental pollution (i.e., they are bioindicators) in the Gulf of Aqaba and the Red Sea. Therefore, this study provides useful information on the degree of heavy metal contamination in the study area.
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[Application of micro-power system in the surgery of tooth extraction].
Kaijin, Hu; Yongfeng, Li
2015-02-01
Tooth extraction is a common operation in oral surgery. Traditional-extraction instruments, such as bone chisel, elevator, and bone hammer, lead to not only severe trauma but also unnecessary complications, and patients easily become nervous and apprehensive if tooth extraction is performed using these violent instruments. In recent years, with the develop- ment of minimally invasive concept and technology, various micro-power instruments have been used for tooth extraction. This innovative technology can reduce the iatrogenic trauma and complications of tooth extraction. Additionally, this technology can greatly decrease the patient's physical and mental pressure. The new equipment compensates for the deficiency of traditional tooth extraction equipment and facilitates the gradual replacement of the latter. Diverse micro-power systems have distinct strengths and weaknesses, so some auxiliary instruments are still needed during tooth extraction. This paper focuses on the various micro-power systems for tooth extraction and tries to compare the advantages and disadvantages of these systems. Selection and usage of auxiliary equipment are also introduced. Thus, this paper provides reference for the proper application of the micro-power systems in tooth extraction.
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Skirted projectiles for railguns
Hawke, Ronald S.; Susoeff, Allan R.
1994-01-01
A single skirt projectile (20) having an insulating skirt (22) at its rear, or a dual trailing skirt projectile (30, 40, 50, 60) having an insulating skirt (32, 42, 52, 62) succeeded by an arc extinguishing skirt (34, 44, 54, 64), is accelerated by a railgun accelerator 10 having a pair of parallel conducting rails (1a, 1b) which are separated by insulating wall spacers (11). The insulating skirt (22, 32, 42, 52, 62) includes a plasma channel (38). The arc extinguishing skirt (34, 44, 54, 64) interrupts the conduction that occurs in the insulating skirt channel (38) by blocking the plasma arc (3) from conducting current from rail to rail (1a, 1b) at the rear of the projectile (30, 40, 50, 60). The arc extinguishing skirt may be comprised of two plates (36a, 36b) which form a horseshoe wherein the plates are parallel to the rails (1a, b); a chisel-shape design; cross-shaped, or it may be a cylindrical (64). The length of the insulating skirt channel is selected such that there is sufficient plasma in the channel to enable adequate current conduction between the rails (1a, 1b).
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Root-knot nematode management in double-cropped plasticulture vegetables.
Desaeger, J A; Csinos, A S
2006-03-01
Combination treatments of chisel-injected fumigants (methyl bromide, 1,3-D, metam sodium, and chloropicrin) on a first crop, followed by drip-applied fumigants (metam sodium and 1,3-D +/- chloropicrin) on a second crop, with and without oxamyl drip applications were evaluated for control of Meloidogyne incognita in three different tests (2002 to 2004) in Tifton, GA. First crops were eggplant or tomato, and second crops were cantaloupe, squash, or jalapeno pepper. Double-cropped vegetables suffered much greater root-knot nematode (RKN) pressure than first crops, and almost-total yield loss occurred when second crops received no nematicide treatment. On a first crop of eggplant, all fumigants provided good nematode control and average yield increases of 10% to 15 %. On second crops, higher application rates and fumigant combinations (metam sodium and 1,3-D +/- chloropicrin) improved RKN control and increased yields on average by 20% to 35 % compared to the nonfumigated control. Oxamyl increased yields of the first crop in 2003 on average by 10% to 15% but had no effect in 2004 when RKN failed to establish itself. On double-cropped squash in 2003, oxamyl following fumigation provided significant additional reduction in nematode infection and increased squash yields on average by 30% to 75%.
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Bakkar, Mohammed; Liu, Younan; Fang, Dongdong; Stegen, Camille; Su, Xinyun; Ramamoorthi, Murali; Lin, Li-Chieh; Kawasaki, Takako; Makhoul, Nicholas; Pham, Huan; Sumita, Yoshinori; Tran, Simon D
2017-01-01
This chapter describes a simplified method that allows the systematic isolation of multiple types of dental stem cells such as dental pulp stem cells (DPSC), periodontal ligament stem cells (PDLSC), and stem cells of the apical papilla (SCAP) from a single tooth. Of specific interest is the modified laboratory approach to harvest/retrieve the dental pulp tissue by minimizing trauma to DPSC by continuous irrigation, reduction of frictional heat from the bur rotation, and reduction of the bur contact time with the dentin. Also, the use of a chisel and a mallet will maximize the number of live DPSC for culture. Steps demonstrating the potential for multiple cell differentiation lineages of each type of dental stem cell into either osteocytes, adipocytes, or chondrocytes are described. Flow cytometry, with a detailed strategy for cell gating and analysis, is described to verify characteristic markers of human mesenchymal multipotent stromal cells (MSC) from DPSC, PDLSC, or SCAP for subsequent experiments in cell therapy and in tissue engineering. Overall, this method can be adapted to any laboratory with a general setup for cell culture experiments.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Kronoveter, K.J.
1978-06-01
In response to a request from the McDaniel Art Studio, located in Cincinnati, Ohio, an investigation was made of possible hazardous working conditions at the site, specifically the exposure to dust during sculpturing. Air sampling revealed potential dust exposures as high as 50 mg/m3 of total dust while using a powered disc grinder to sculpt. The sculpting process involved grinding with a 6-inch electric disc grinder or using such hand tools as files and chisels. The sculptor used primarily limestone, marble, talc, and onyx, working about 6 hours per day. The talc sculpting stone showed the presence of asbestos onmore » bulk analysis. The sculptor wore safety glasses with side shields and an appropriate, approved respirator. An industrial vacuum cleaner was used for dust cleanup. The author recommends that the sculptor continue to use the NIOSH approved respirator and that, if possible, the disc grinder not be used on potential asbestos sources such as serpentine and talc. Wet working of the stone would reduce the dust levels significantly. Several precautionary measures are listed from a publication dealing with the health risks associated with common art and hobby materials.« less
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Walory kulturowe Krainy Otwartych Okiennic
NASA Astrophysics Data System (ADS)
Matus, Irena
2009-01-01
The Open Shutters Land is an ethnographic-tourist project realizing in the territory of three villages in the north-east part of Poland. The shape of two of those villages (Soce and Trześcianka) as royal villages was created during
włóka measurement in the 16th century. However Puchły was a private village. The aim of this project is to save wooden, unique, richly ornamented folk building industry. That enterprise came into being in the interwar period and was continued in the post-war period. Characteristic style of houses' decoration: geometric decorated shutters, subtle fretted label moulds, under-windows, boards corners sheltered, wind-protector are typical of that Land. Decorative shuttered timbered gables were graced. Street village ribbon development was built mainly gables to the street, whereas other inventory buildings were done in that same line. Two parish Orthodox churches, wooden, decorated in chisel style in Trześcianka and Puchły villages, a cemetery chapel in Trześcianka, two shrines nearby Soce and Trześcianka, interesting plague and intent crosses as well as original pillar shrines are worth seeing. Moreover, the Narew river, its inflow Rudnia and forests surrounding the villages exalt attraction of that terrain. -
Yardang-Sculpted Deposits from Apollonaris Patera
2015-08-12
This observation from NASA Mars Reconnaissance Orbiter spacecraft shows a terrain of relatively smooth region that transitions into sharp ridges called yardangs on Apollonaris Patera. These ridges, aligned in the nearly same direction, are called yardangs. Yardangs are not unique to Mars. Many yardangs can be found on Earth, in very dry regions with strong prevailing winds. Yardangs are formed when a surface that is composed of materials of differing strengths (i.e., of both harder and softer materials) is shaped by the abrasive action of sand and dust carried by the wind. In this case, and given the proximity of the Apollonaris Patera volcanic center, we think that these wind-carved deposits are comprised of volcanic ash and pyroclastics that erupted from Apollonaris when it was last active in the not-too-distant geologic past. Over time, the softer materials (likely volcanic ash) were eroded away, leaving behind the harder materials in the form of elongated ridges that are parallel to the direction of the prevailing wind. The end result is a stunning, out-of-this-world display of yardangs, sculpted with the artistic chisel of the Martian wind. http://photojournal.jpl.nasa.gov/catalog/PIA19869
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Creep and rupture of an ODS alloy with high stress rupture ductility. [Oxide Dispersion Strengthened
NASA Technical Reports Server (NTRS)
Mcalarney, M. E.; Arsons, R. M.; Howson, T. E.; Tien, J. K.; Baranow, S.
1982-01-01
The creep and stress rupture properties of an oxide (Y2O3) dispersion strengthened nickel-base alloy, which also is strengthened by gamma-prime precipitates, was studied at 760 and 1093 C. At both temperatures, the alloy YDNiCrAl exhibits unusually high stress rupture ductility as measured by both elongation and reduction in area. Failure was transgranular, and different modes of failure were observed including crystallographic fracture at intermediate temperatures and tearing or necking almost to a chisel point at higher temperatures. While the rupture ductility was high, the creep strength of the alloy was low relative to conventional gamma prime strengthened superalloys in the intermediate temperature range and to ODS alloys in the higher temperature range. These findings are discussed with respect to the alloy composition; the strengthening oxide phases, which are inhomogeneously dispersed; the grain morphology, which is coarse and elongated and exhibits many included grains; and the second phase inclusion particles occurring at grain boundaries and in the matrix. The creep properties, in particular the high stress dependencies and high creep activation energies measured, are discussed with respect to the resisting stress model of creep in particle strengthened alloys.
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Skirted projectiles for railguns
Hawke, R.S.; Susoeff, A.R.
1994-01-04
A single skirt projectile (20) having an insulating skirt (22) at its rear, or a dual trailing skirt projectile (30, 40, 50, 60) having an insulating skirt (32, 42, 52, 62) succeeded by an arc extinguishing skirt (34, 44, 54, 64), is accelerated by a railgun accelerator 10 having a pair of parallel conducting rails (1a, 1b) which are separated by insulating wall spacers (11). The insulating skirt (22, 32, 42, 52, 62) includes a plasma channel (38). The arc extinguishing skirt (34, 44, 54, 64) interrupts the conduction that occurs in the insulating skirt channel (38) by blocking the plasma arc (3) from conducting current from rail to rail (1a, 1b) at the rear of the projectile (30, 40, 50, 60). The arc extinguishing skirt may be comprised of two plates (36a, 36b) which form a horseshoe wherein the plates are parallel to the rails (1a, b); a chisel-shape design; cross-shaped, or it may be a cylindrical (64). The length of the insulating skirt channel is selected such that there is sufficient plasma in the channel to enable adequate current conduction between the rails (1a, 1b).
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New hydrologic instrumentation in the U.S. Geological Survey
Latkovich, V.J.; Shope, W.G.; ,
1991-01-01
New water-level sensing and recording instrumentation is being used by the U.S. Geological Survey for monitoring water levels, stream velocities, and water-quality characteristics. Several of these instruments are briefly described. The Basic Data Recorder (BDR) is an electronic data logger, that interfaces to sensor systems through a serial-digital interface standard (SDI-12), which was proposed by the data-logger industry; the Incremental Shaft Encoder is an intelligent water-level sensor, which interfaces to the BDR through the SDI-12; the Pressure Sensor is an intelligent, nonsubmersible pressure sensor, which interfaces to the BDR through the SDI-12 and monitors water levels from 0 to 50 feet; the Ultrasonic Velocity Meter is an intelligent, water-velocity sensor, which interfaces to the BDR through the SDI-12 and measures the velocity across a stream up to 500 feet in width; the Collapsible Hand Sampler can be collapsed for insertion through holes in the ice and opened under the ice to collect a water sample; the Lighweight Ice Auger, weighing only 32 pounds, can auger 6- and 8-inch holes through approximately 3.5 feet of ice; and the Ice Chisel has a specially hardened steel blade and 6-foot long, hickory D-handle.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Sachs, Marius; Schmidt, Jochen; Peukert, Wolfgang
2016-03-09
The recent development of rapid prototyping technologies towards additive manufacturing reveals some major drawbacks of processes such as laser beam melting (LBM). This contribution focuses on the lack of suitable polymer material with a fine particle size and good flowability. Polymer particles obtained by a wet grinding process 1 are treated in a heated downer reactor. This treatment changes the particles’ morphology from a chiselled state towards a spherical form by surface tension forces in a molten state 2 and leads to an improved flowability. To reach the required amount of rounded polymer powder, a downer reactor in semi-industrial scalemore » has been established and will be characterized in this article. For the purpose of particle rounding it is necessary to avoid contact of molten particles with each other and with the hot reactor walls. Furthermore, the heat distribution has been investigated as one of the key parameters of the process. Finally, a proof of concept by rounding wet grinded PBT material was successfully conducted. The product was examined to obtain data about a change in particle size and flowability.« less
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Comparison of the effect of three autogenous bone harvesting methods on cell viability in rabbits
Moradi Haghgoo, Janet; Arabi, Seyed Reza; Hosseinipanah, Seyyed Mohammad; Solgi, Ghasem; Rastegarfard, Neda; Farhadian, Maryam
2017-01-01
Background. This study was designed to compare the viability of autogenous bone grafts, harvested using different methods, in order to determine the best harvesting technique with respect to more viable cells. Methods. In this animal experimental study, three harvesting methods, including manual instrument (chisel), rotary device and piezosurgery, were used for harvesting bone grafts from the lateral body of the mandible on the left and right sides of 10 rabbits. In each group, 20 bone samples were collected and their viability was assessed using MTS kit. Statistical analyses, including ANOVA and post hoc Tukey tests, were used for evaluating significant differences between the groups. Results. One-way ANOVA showed significant differences between all the groups (P=0.000). Data analysis using post hoc Tukey tests indicated that manual instrument and piezosurgery had no significant differences with regard to cell viability (P=0.749) and the cell viability in both groups was higher than that with the use of a rotary instrument (P=0.000). Conclusion. Autogenous bone grafts harvested with a manual instrument and piezosurgery had more viable cells in comparison to the bone chips harvested with a rotary device. PMID:28748046
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A comparison of the weights-of-evidence method and probabilistic neural networks
Singer, Donald A.; Kouda, Ryoichi
1999-01-01
The need to integrate large quantities of digital geoscience information to classify locations as mineral deposits or nondeposits has been met by the weights-of-evidence method in many situations. Widespread selection of this method may be more the result of its ease of use and interpretation rather than comparisons with alternative methods. A comparison of the weights-of-evidence method to probabilistic neural networks is performed here with data from Chisel Lake-Andeson Lake, Manitoba, Canada. Each method is designed to estimate the probability of belonging to learned classes where the estimated probabilities are used to classify the unknowns. Using these data, significantly lower classification error rates were observed for the neural network, not only when test and training data were the same (0.02 versus 23%), but also when validation data, not used in any training, were used to test the efficiency of classification (0.7 versus 17%). Despite these data containing too few deposits, these tests of this set of data demonstrate the neural network's ability at making unbiased probability estimates and lower error rates when measured by number of polygons or by the area of land misclassified. For both methods, independent validation tests are required to ensure that estimates are representative of real-world results. Results from the weights-of-evidence method demonstrate a strong bias where most errors are barren areas misclassified as deposits. The weights-of-evidence method is based on Bayes rule, which requires independent variables in order to make unbiased estimates. The chi-square test for independence indicates no significant correlations among the variables in the Chisel Lake–Andeson Lake data. However, the expected number of deposits test clearly demonstrates that these data violate the independence assumption. Other, independent simulations with three variables show that using variables with correlations of 1.0 can double the expected number of deposits as can correlations of −1.0. Studies done in the 1970s on methods that use Bayes rule show that moderate correlations among attributes seriously affect estimates and even small correlations lead to increases in misclassifications. Adverse effects have been observed with small to moderate correlations when only six to eight variables were used. Consistent evidence of upward biased probability estimates from multivariate methods founded on Bayes rule must be of considerable concern to institutions and governmental agencies where unbiased estimates are required. In addition to increasing the misclassification rate, biased probability estimates make classification into deposit and nondeposit classes an arbitrary subjective decision. The probabilistic neural network has no problem dealing with correlated variables—its performance depends strongly on having a thoroughly representative training set. Probabilistic neural networks or logistic regression should receive serious consideration where unbiased estimates are required. The weights-of-evidence method would serve to estimate thresholds between anomalies and background and for exploratory data analysis.
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Tillage and residue burning affects weed populations and seed banks.
Narwal, S; Sindel, B M; Jessop, R S
2006-01-01
An integrated weed management approach requires alternative management practices to herbicide use such as tillage, crop rotations and cultural controls to reduce soil weed seed banks. The objective of this study was to examine the value of different tillage practices and stubble burning to exhaust the seed bank of common weeds from the northern grain region of Australia. Five tillage and burning treatments were incorporated in a field experiment, at Armidale (30 degrees 30'S, 151 degrees 40'E), New South Wales, Australia in July 2004 in a randomized block design replicated four times. The trial was continued and treatments repeated in July 2005 with all the mature plants from the first year being allowed to shed seed in their respective treatment plots. The treatments were (i) no tillage (NT), (ii) chisel ploughing (CP), (iii) mould board ploughing (MBP), (iv) wheat straw burning with no tillage (SBNT) and (v) wheat straw burning with chisel ploughing (SBC). Soil samples were collected before applying treatments and before the weeds flowered to establish the seed bank status of the various weeds in the soil. Wheat was sown after the tillage treatments. Burning treatments were only initiated in the second year, one month prior to tillage treatments. The major weeds present in the seed bank before initiating the trial were Polygonum aviculare, Sonchus oleraceus and Avena fatua. Tillage promoted the germination of other weeds like Hibiscus trionum, Medicago sativa, Vicia sp. and Phalaris paradoxa later in the season in 2004 and Convolvulus erubescens emerged as a new weed in 2005. The MBP treatment in 2004 reduced the weed biomass to a significantly lower level of 55 g/m2 than the other treatments of CP (118 g/m2) and NT plots (196 g/m2) (P < 0.05). However, in 2005 SBC and MBP treatments were similar in reducing the weed biomass. In 2004, the grain yield trend of wheat was significantly different between CP and NT, and MBP and NT (P < 0.05) with maximum yield of 5898 kg/ha in CP and 5731 kg/ha in MBP. Rainfall before the start of the second trial season promoted the germination of a large numbers of weeds. SBC and MBP treatments reduced the numbers of most of the individual weed species compared with CP, SBNT and NT. SBC was able to destroy a large proportion of seeds most likely through burning and burying some in the soil and was found to be the best treatment in exhausting the seed bank followed closely by MBP which probably buried large number of seeds deep in the soil and promoted others to germinate. CP might have buried some of the seeds in the top 5-10 cm but also promoted parts of the seed bank to germinate. SBNT and NT provided an ideal medium for weeds to germinate and resulted in heavy infestations of weeds.
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Describing soil surface microrelief by crossover length and fractal dimension
NASA Astrophysics Data System (ADS)
Vidal Vázquez, E.; Miranda, J. G. V.; Paz González, A.
2007-05-01
Accurate description of soil surface topography is essential because different tillage tools produce different soil surface roughness conditions, which in turn affects many processes across the soil surface boundary. Advantages of fractal analysis in soil microrelief assessment have been recognised but the use of fractal indices in practice remains challenging. There is also little information on how soil surface roughness decays under natural rainfall conditions. The objectives of this work were to investigate the decay of initial surface roughness induced by natural rainfall under different soil tillage systems and to compare the performances of a classical statistical index and fractal microrelief indices. Field experiments were performed on an Oxisol at Campinas, São Paulo State (Brazil). Six tillage treatments, namely, disc harrow, disc plow, chisel plow, disc harrow + disc level, disc plow + disc level and chisel plow + disc level were tested. Measurements were made four times, firstly just after tillage and subsequently with increasing amounts of natural rainfall. Duplicated measurements were taken per treatment and date, yielding a total of 48 experimental surfaces. The sampling scheme was a square grid with 25×25 mm point spacing and the plot size was 1350×1350 mm, so that each data set consisted of 3025 individual elevation points. Statistical and fractal indices were calculated both for oriented and random roughness conditions, i.e. after height reading have been corrected for slope and for slope and tillage tool marks. The main drawback of the standard statistical index random roughness, RR, lies in its no spatial nature. The fractal approach requires two indices, fractal dimension, D, which describes how roughness changes with scale, and crossover length, l, specifying the variance of surface microrelief at a reference scale. Fractal parameters D and l, were estimated by two independent self-affine models, semivariogram (SMV) and local root mean square (RMS). Both algorithms, SMV and RMS, gave equivalent results for D and l indices, irrespective of trend removal procedure, even if some bias was present which is in accordance with previous work. Treatments with two tillage operations had the greatest D values, irrespective of evolution stage under rainfall and trend removal procedure. Primary tillage had the greatest initial values of RR and l. Differences in D values between treatments with primary tillage and those with two successive tillage operations were significant for oriented but not for random conditions. The statistical index RR and the fractal indices l and D decreased with increasing cumulative rainfall following different patterns. The l and D decay from initial value was very sharp after the first 24.4 mm cumulative rainfall. For five out of six tillage treatments a significant relationship between D and l was found for the random microrelief conditions allowing a covariance analysis. It was concluded that using RR or l together with D best allow joint description of vertical and horizontal soil roughness variations.
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Chumbley, Scott; Zhang, Song; Morris, Max; ...
2016-11-16
Since the development of the striagraph, various attempts have been made to enhance forensic investigation through the use of measuring and imaging equipment. This study describes the development of a prototype system employing an easy-to-use software interface designed to provide forensic examiners with the ability to measure topography of a toolmarked surface and then conduct various comparisons using a statistical algorithm. Acquisition of the data is carried out using a portable 3D optical profilometer, and comparison of the resulting data files is made using software named “MANTIS” (Mark and Tool Inspection Suite). The system has been tested on laboratory-produced markingsmore » that include fully striated marks (e.g., screwdriver markings), quasistriated markings produced by shear-cut pliers, impression marks left by chisels, rifling marks on bullets, and cut marks produced by knives. Using the system, an examiner has the potential to (i) visually compare two toolmarked surfaces in a manner similar to a comparison microscope and (ii) use the quantitative information embedded within the acquired data to obtain an objective statistical comparison of the data files. Finally, this study shows that, based on the results from laboratory samples, the system has great potential for aiding examiners in conducting comparisons of toolmarks.« less
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Corn stover harvest increases herbicide movement to subsurface drains: RZWQM simulations
Shipitalo, Martin J.; Malone, Robert W.; Ma, Liwang; Nolan, Bernard T.; Kanwar, Rameshwar S.; Shaner, Dale L.; Pederson, Carl H.
2016-01-01
BACKGROUND Crop residue removal for bioenergy production can alter soil hydrologic properties and the movement of agrochemicals to subsurface drains. The Root Zone Water Quality Model (RZWQM), previously calibrated using measured flow and atrazine concentrations in drainage from a 0.4 ha chisel-tilled plot, was used to investigate effects of 50 and 100% corn (Zea mays L.) stover harvest and the accompanying reductions in soil crust hydraulic conductivity and total macroporosity on transport of atrazine, metolachlor, and metolachlor oxanilic acid (OXA). RESULTS The model accurately simulated field-measured metolachlor transport in drainage. A 3-yr simulation indicated that 50% residue removal decreased subsurface drainage by 31% and increased atrazine and metolachlor transport in drainage 4 to 5-fold when surface crust conductivity and macroporosity were reduced by 25%. Based on its measured sorption coefficient, ~ 2-fold reductions in OXA losses were simulated with residue removal. CONCLUSION RZWQM indicated that if corn stover harvest reduces crust conductivity and soil macroporosity, losses of atrazine and metolachlor in subsurface drainage will increase due to reduced sorption related to more water moving through fewer macropores. Losses of the metolachlor degradation product OXA will decrease due to the more rapid movement of the parent compound into the soil.
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Push the flash floating gate memories toward the future low energy application
NASA Astrophysics Data System (ADS)
Della Marca, V.; Just, G.; Regnier, A.; Ogier, J.-L.; Simola, R.; Niel, S.; Postel-Pellerin, J.; Lalande, F.; Masoero, L.; Molas, G.
2013-01-01
In this paper the energy consumption of flash floating gate cell, during a channel hot electron operation, is investigated. We characterize the device using different ramp and box pulses on control gate, to find the best solution to have low energy consumption and good cell performances. We use a new dynamic method to measure the drain current absorption in order to evaluate the impact of different bias conditions, and to study the cell behavior. The programming window and the energy consumption are considered as fundamental parameters. Using this dynamic technique, three zones of work are found; it is possible to optimize the drain voltage during the programming operation to minimize the energy consumption. Moreover, the cell's performances are improved using the CHISEL effect, with a reverse body bias. After the study concerning the programming pulses adjusting, we show the results obtained by increasing the channel doping dose parameter. Considering a channel hot electron programming operation, it is important to focus our attention on the bitline leakage consumption contribution. We measured it for the unselected bitline cells, and we show the effects of the lightly doped drain implantation energy on the leakage current. In this way the impact of gate induced drain leakage in band-to-band tunneling regime decreases, improving the cell's performances in a memory array.
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Root-Knot Nematode Management in Double-Cropped Plasticulture Vegetables
Desaeger, J. A.; Csinos, A. S.
2006-01-01
Combination treatments of chisel-injected fumigants (methyl bromide, 1,3-D, metam sodium, and chloropicrin) on a first crop, followed by drip-applied fumigants (metam sodium and 1,3-D ± chloropicrin) on a second crop, with and without oxamyl drip applications were evaluated for control of Meloidogyne incognita in three different tests (2002 to 2004) in Tifton, GA. First crops were eggplant or tomato, and second crops were cantaloupe, squash, or jalapeno pepper. Double-cropped vegetables suffered much greater root-knot nematode (RKN) pressure than first crops, and almost-total yield loss occurred when second crops received no nematicide treatment. On a first crop of eggplant, all fumigants provided good nematode control and average yield increases of 10% to 15 %. On second crops, higher application rates and fumigant combinations (metam sodium and 1,3-D ± chloropicrin) improved RKN control and increased yields on average by 20% to 35 % compared to the nonfumigated control. Oxamyl increased yields of the first crop in 2003 on average by 10% to 15% but had no effect in 2004 when RKN failed to establish itself. On double-cropped squash in 2003, oxamyl following fumigation provided significant additional reduction in nematode infection and increased squash yields on average by 30% to 75%. PMID:19259431
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A new species of Deltaspis Audinet-Serville (Coleoptera: Cerambycidae: Cerambycinae) from Mexico.
Eya, Bryan K
2017-03-27
As currently defined, the genus Deltaspis Audinet-Serville, 1834, contains 16 species ranging in distribution from the southwestern United States to eastern Mexico. However, the generic distinction between Deltaspis and its closely allied genera, such as Crossidius LeConte, 1851 and Muscidora Thomson, 1864, is in need of clarification. According to Audinet-Serville, Deltaspis is so named due to its distinctive triangular scutellum (i.e., Δετα, delta, ασπιζ écusson), which is actually a commonly shared character of all these genera. Members of the tribe Trachyderini Dupont (1836), which includes the above genera, also have mandibles with an emarginate-truncate apex with the edge chisel-like or bifid. This modification of mouthpart appears to be for consumption of pollen and/or petals from composite flowers visited by the adult beetles (Krenn et al., 2005; Beierl & Barchet-Beierl, 1999). Other genera from this tribe with this modification of mandibles from North America, and mostly from Mexico, include: Chemsakiella Monné, 2006, Giesbertia Chemsak & Linsley, 1984, Hoegea Bates, 1885, Neocrossidius Chemsak, 1959, Paroxoplus Chemsak, 1959, Plionoma Casey, 1912, Schizax LeConte, 1873, and Tylosis LeConte, 1850. The remainder of Trachyderini genera have unmodified or simple mandibles with apex acute.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Chumbley, Scott; Zhang, Song; Morris, Max
Since the development of the striagraph, various attempts have been made to enhance forensic investigation through the use of measuring and imaging equipment. This study describes the development of a prototype system employing an easy-to-use software interface designed to provide forensic examiners with the ability to measure topography of a toolmarked surface and then conduct various comparisons using a statistical algorithm. Acquisition of the data is carried out using a portable 3D optical profilometer, and comparison of the resulting data files is made using software named “MANTIS” (Mark and Tool Inspection Suite). The system has been tested on laboratory-produced markingsmore » that include fully striated marks (e.g., screwdriver markings), quasistriated markings produced by shear-cut pliers, impression marks left by chisels, rifling marks on bullets, and cut marks produced by knives. Using the system, an examiner has the potential to (i) visually compare two toolmarked surfaces in a manner similar to a comparison microscope and (ii) use the quantitative information embedded within the acquired data to obtain an objective statistical comparison of the data files. Finally, this study shows that, based on the results from laboratory samples, the system has great potential for aiding examiners in conducting comparisons of toolmarks.« less
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Effect of tillage system on yield and weed populations of soybean ( Glycin Max L.).
Hosseini, Seyed Z; Firouzi, Saeed; Aminpanah, Hashem; Sadeghnejhad, Hamid R
2016-03-01
Field experiment was conducted at Agricultural and Natural Resources Research Center of Golestan Province, Iran, to determine the effects of tillage system and weed management regime on yield and weed populations in soybean ( Glycin max L.). The experimental design was a split plot where the whole plot portion was a randomized complete block with three replicates. Main plots were tillage system: 1- No-till row crop seeding, 2- No-till seed drilling, 3- Tillage with disc harrow and drill planting, 4- Tillage with chisel packer and drill planting. The subplots were weed management regimes: 1-Weed control with herbicide application, 2- Hand weeding, 3- Herbicide application plus hand weeding, and 4- Non-weeding. Results indicated that the main effects of tillage system and weed management regime were significant for seed yield, pod number per plant, seed number per pod, weed density and biomass, while their interaction were significant only for weed density, weed biomass, and seed number per pod. The highest grain yields (3838 kg ha-1) were recorded for No-till row crop seeding. The highest seed yield (3877 kg ha-1) also was recorded for weed control with herbicide and hand weeding treatment, followed by hand weeding (3379 kg ha-1).
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Transnational pharmaceutical corporations and neo-liberal business ethics in India.
D'Mello, Bernard
2002-03-01
The author critiques the expedient application of market valuation principles by the transnational corporations and other large firms in the Indian pharmaceutical industry on a number of issues like patents, pricing, irrational drugs, clinical trials, etc. He contends that ethics in business is chiseled and etched within the confines of particular social structures of accumulation. An ascendant neo-liberal social structure of accumulation has basically shaped these firms' sharp opposition to the Indian Patents Act, 1970, government administered pricing, etc. The author contents that the practice of neo-liberal economics is strongly associated with a "one-dimensional" ethics that privileges market valuation principles over all others. This seems to inevitably generate a social counter-movement that struggles for social protections. He critiques neo-liberal business practices from a perspective that derives from the work of the economic anthropologist Karl Polanyi. Before the present phase of liberalization in India, markets were "managed", but without a "welfare state" in place. Moving toward deregulation of the markets without a welfare state in place is unethical. Keeping the debilities of the institutional framework of public policy in mind, the author adopts a Polanyian perspective that places its trust and hope in the growing social legitimacy of the counter-movement in opposition to both neo-liberal business practices and the degenerate behavior of state agencies.
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Feasibility of Piezoelectric Endoscopic Transsphenoidal Craniotomy: A Cadaveric Study
Tomazic, Peter Valentin; Gellner, Verena; Koele, Wolfgang; Hammer, Georg Philipp; Braun, Eva Maria; Gerstenberger, Claus; Clarici, Georg; Holl, Etienne; Braun, Hannes; Stammberger, Heinz; Mokry, Michael
2014-01-01
Objective. Endoscopic transsphenoidal approach has become the gold standard for surgical treatment of treating pituitary adenomas or other lesions in that area. Opening of bony skull base has been performed with burrs, chisels, and hammers or standard instruments like punches and circular top knives. The creation of primary bone flaps—as in external craniotomies—is difficult.The piezoelectric osteotomes used in the present study allows creating a bone flap for endoscopic transnasal approaches in certain areas. The aim of this study was to prove the feasibility of piezoelectric endoscopic transnasal craniotomies. Study Design. Cadaveric study. Methods. On cadaveric specimens (N = 5), a piezoelectric system with specially designed hardware for endonasal application was applied and endoscopic transsphenoidal craniotomies at the sellar floor, tuberculum sellae, and planum sphenoidale were performed up to a size of 3–5 cm2. Results. Bone flaps could be created without fracturing with the piezoosteotome and could be reimplanted. Endoscopic handling was unproblematic and time required was not exceeding standard procedures. Conclusion. In a cadaveric model, the piezoelectric endoscopic transsphenoidal craniotomy (PETC) is technically feasible. This technique allows the surgeon to create a bone flap in endoscopic transnasal approaches similar to existing standard transcranial craniotomies. Future trials will focus on skull base reconstruction using this bone flap. PMID:24689037
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Ultrasonic/Sonic Rotary-Hammer Drills
NASA Technical Reports Server (NTRS)
Badescu, Mircea; Sherrit, Stewart; Bar-Cohen, Yoseph; Bao, Xiaoqi; Kassab, Steve
2010-01-01
Ultrasonic/sonic rotary-hammer drill (USRoHD) is a recent addition to the collection of apparatuses based on ultrasonic/sonic drill corer (USDC). As described below, the USRoHD has several features, not present in a basic USDC, that increase efficiency and provide some redundancy against partial failure. USDCs and related apparatuses were conceived for boring into, and/or acquiring samples of, rock or other hard, brittle materials of geological interest. They have been described in numerous previous NASA Tech Briefs articles. To recapitulate: A USDC can be characterized as a lightweight, lowpower, piezoelectrically driven jackhammer in which ultrasonic and sonic vibrations are generated and coupled to a tool bit. A basic USDC includes a piezoelectric stack, an ultrasonic transducer horn connected to the stack, a free mass ( free in the sense that it can bounce axially a short distance between hard stops on the horn and the bit), and a tool bit. The piezoelectric stack creates ultrasonic vibrations that are mechanically amplified by the horn. The bouncing of the free mass between the hard stops generates the sonic vibrations. The combination of ultrasonic and sonic vibrations gives rise to a hammering action (and a resulting chiseling action at the tip of the tool bit) that is more effective for drilling than is the microhammering action of ultrasonic vibrations alone. The hammering and chiseling actions are so effective that unlike in conventional twist drilling, little applied axial force is needed to make the apparatus advance into the material of interest. There are numerous potential applications for USDCs and related apparatuses in geological exploration on Earth and on remote planets. In early USDC experiments, it was observed that accumulation of cuttings in a drilled hole causes the rate of penetration of the USDC to decrease steeply with depth, and that the rate of penetration can be increased by removing the cuttings. The USRoHD concept provides for removal of cuttings in the same manner as that of a twist drill: An USRoHD includes a USDC and a motor with gearhead (see figure). The USDC provides the bit hammering and the motor provides the bit rotation. Like a twist drill bit, the shank of the tool bit of the USRoHD is fluted. As in the operation of a twist drill, the rotation of the fluted drill bit removes cuttings from the drilled hole. The USRoHD tool bit is tipped with a replaceable crown having cutting teeth on its front surface. The teeth are shaped to promote fracturing of the rock face through a combination of hammering and rotation of the tool bit. Helical channels on the outer cylindrical surface of the crown serve as a continuation of the fluted surface of the shank, helping to remove cuttings. In the event of a failure of the USDC, the USRoHD can continue to operate with reduced efficiency as a twist drill. Similarly, in the event of a failure of the gearmotor, the USRoHD can continue to operate with reduced efficiency as a USDC.
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Li, Datao; Zhang, Ruhong; Zhang, Qun; Xu, Zhicheng; Xu, Feng; Li, Yiyuan; Sun, Nan; Wang, Cheng
2014-05-01
Prior reports of ear reconstruction have cited favorable results. Although greater attention has been devoted to fabricating a more refined cartilaginous framework, many patients still complain that the contours are unnatural. The authors' aim was to offer a new technique that resolves some lingering issues. To fabricate the antihelix complex optimally, the authors modified an existing method. Rather than chiseling a sharp, Y-shaped graft of cartilage for structural prominence, the superior crus is broadened, and a gentle slope is sculpted on both aspects. Simultaneously, a groove in the base frame is carved for smooth attachment. The width of the inferior crus is limited to roughly one-third that of the superior crus, and the inferior crus is maintained in high relief. A gentle slope is shaped on the antihelix, and a groove for placement of the antihelix is carved into the base frame. Between 2011 and 2013, a total of 162 patients underwent reconstruction using this modified technique. Three such subjects have been selected to highlight the favorable results achieved. Given modifications confer natural contours to superior and inferior crura, antihelix, and surrounding structures, providing a cohesive framework for the integrity of a reconstructed ear. The antihelix complex is critical for creating a natural auricle. Harmonious integration of superior and inferior crura and antihelix enhances the overall aesthetics, increasing procedural satisfaction for patient and surgeon alike. Therapeutic, IV.
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Hackmann, Timothy J; Ngugi, David Kamanda; Firkins, Jeffrey L; Tao, Junyi
2017-11-01
Bacteria have been thought to follow only a few well-recognized biochemical pathways when fermenting glucose or other hexoses. These pathways have been chiseled in the stone of textbooks for decades, with most sources rendering them as they appear in the classic 1986 text by Gottschalk. Still, it is unclear how broadly these pathways apply, given that they were established and delineated biochemically with only a few model organisms. Here, we show that well-recognized pathways often cannot explain fermentation products formed by bacteria. In the most extensive analysis of its kind, we reconstructed pathways for glucose fermentation from genomes of 48 species and subspecies of bacteria from one environment (the rumen). In total, 44% of these bacteria had atypical pathways, including several that are completely unprecedented for bacteria or any organism. In detail, 8% of bacteria had an atypical pathway for acetate formation; 21% of bacteria had an atypical pathway for propionate or succinate formation; 6% of bacteria had an atypical pathway for butyrate formation and 33% of bacteria had an atypical or incomplete Embden-Meyerhof-Parnas pathway. This study shows that reconstruction of metabolic pathways - a common goal of omics studies - could be incorrect if well-recognized pathways are used for reference. Furthermore, it calls for renewed efforts to delineate fermentation pathways biochemically. © 2017 Society for Applied Microbiology and John Wiley & Sons Ltd.
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Xu, Fang; Zhang, Hui-Xia
2016-10-01
To compare minimally invasive extraction and traditional method in the extraction of impacted mandibular third molar. One hundred and sixty patients with impacted mandibular third molar were equally divided into two groups. Patients in the experimental group were treated with minimally invasive extraction, using implant machine and luxator, while patients in the control group were treated with traditional methods including use of orthodox chisel. The operation time, intraoperative and postoperative complications including deformation of extraction sockets, dry socket, limitation of mouth opening, pain and swelling, and fear were observed and compared between the two groups. The data were analyzed with SPSS18.0 software package. The operation time was (17.32±1.01) min in the experimental group, significantly shorter than the control group which was (33.46±1.12）min (P<0.05); significant difference was found in the incidence of root fracture, medium or severe tooth sockets deformation and incidence of psychological fear during operation between the control group and experimental group(P<0.05); the degree of mouth opening after surgery, the incidence of moderate or severe pain after surgery was significantly lower in the experimental than in the control group(P<0.05). Minimally invasive extraction of mandibular impacted wisdom tooth is better than traditional method, with shorter operation time and less intraoperative and postoperative complications, which should be widely applied in clinic.
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NASA Astrophysics Data System (ADS)
Taina, I. A.; Heck, R. J.; Scaiff, N. T.
2009-05-01
One of the most important applications of X-ray computed tomography (CT) for the study of soil is the characterization of the shape and spatial distribution of pores. Analysis of 3D X-ray CT image data, related to different pore categories, can provide insight to soil structural changes, which have implications in water infiltration and soil aeration, resulting from agricultural practices. The aim of this study was to evaluate changes in the spatial characteristics of voids, due to tillage practices, in the Ap horizon of an Orthic Grey- Brown Luvisol (located at the Elora Research Station of the University of Guelph). Undisturbed oriented soil samples were collected from ten plots representing different tillage treatments: spring moldboard plow, spring moldboard plow, cultivate and pack, fall moldboard plow, cultivate and pack, spring tandem disc, no cultivator, fall offset disc, fall offset disc, cultivate and pack, fall chisel plow, cultivate and pack, zero zone till (soys twin rows), zero tillage (long term), and zero tillage (corn residue removed in row, soys twin rows). Since the utilization of standardized classes, in the quantification of similar features, proved to be necessary in order to obtain comparable results, categories of pores, separated according to their size, circularity and orientation were considered in the interpretation of data. Total volume of pores and volume percentage of each class were calculated, revealing substantial differences among the analyzed soil samples.
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Nadel, Dani; Danin, Avinoam; Power, Robert C; Rosen, Arlene M; Bocquentin, Fanny; Tsatskin, Alexander; Rosenberg, Danny; Yeshurun, Reuven; Weissbrod, Lior; Rebollo, Noemi R; Barzilai, Omry; Boaretto, Elisabetta
2013-07-16
Flowering plants possess mechanisms that stimulate positive emotional and social responses in humans. It is difficult to establish when people started to use flowers in public and ceremonial events because of the scarcity of relevant evidence in the archaeological record. We report on uniquely preserved 13,700-11,700-y-old grave linings made of flowers, suggesting that such use began much earlier than previously thought. The only potentially older instance is the questionable use of flowers in the Shanidar IV Neanderthal grave. The earliest cemeteries (ca. 15,000-11,500 y ago) in the Levant are known from Natufian sites in northern Israel, where dozens of burials reflect a wide range of inhumation practices. The newly discovered flower linings were found in four Natufian graves at the burial site of Raqefet Cave, Mt. Carmel, Israel. Large identified plant impressions in the graves include stems of sage and other Lamiaceae (Labiatae; mint family) or Scrophulariaceae (figwort family) species; accompanied by a plethora of phytoliths, they provide the earliest direct evidence now known for such preparation and decoration of graves. Some of the plant species attest to spring burials with a strong emphasis on colorful and aromatic flowers. Cave floor chiseling to accommodate the desired grave location and depth is also evident at the site. Thus, grave preparation was a sophisticated planned process, embedded with social and spiritual meanings reflecting a complex preagricultural society undergoing profound changes at the end of the Pleistocene.
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Gailani, Joseph Z; Lackey, Tahirih C; King, David B; Bryant, Duncan; Kim, Sung-Chan; Shafer, Deborah J
2016-03-01
Model studies were conducted to investigate the potential coral reef sediment exposure from dredging associated with proposed development of a deepwater wharf in Apra Harbor, Guam. The Particle Tracking Model (PTM) was applied to quantify the exposure of coral reefs to material suspended by the dredging operations at two alternative sites. Key PTM features include the flexible capability of continuous multiple releases of sediment parcels, control of parcel/substrate interaction, and the ability to efficiently track vast numbers of parcels. This flexibility has facilitated simulating the combined effects of sediment released from clamshell dredging and chiseling within Apra Harbor. Because the rate of material released into the water column by some of the processes is not well understood or known a priori, the modeling approach was to bracket parameters within reasonable ranges to produce a suite of potential results from multiple model runs. Sensitivity analysis to model parameters is used to select the appropriate parameter values for bracketing. Data analysis results include mapping the time series and the maximum values of sedimentation, suspended sediment concentration, and deposition rate. Data were used to quantify various exposure processes that affect coral species in Apra Harbor. The goal of this research is to develop a robust methodology for quantifying and bracketing exposure mechanisms to coral (or other receptors) from dredging operations. These exposure values were utilized in an ecological assessment to predict effects (coral reef impacts) from various dredging scenarios. Copyright © 2015. Published by Elsevier Ltd.
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Mimura, Hiroshi
2013-08-01
A woman, aged 47 years 6 months, with an anterior open bite and a left-shifted mandible was treated with a mandibular right first molar extraction and without orthognathic surgery. However, her mandibular second molar did not move mesially during treatment because of the dense lamina dura; therefore, corticision was applied only on the mesial aspect of the mandibular second molar, and a miniscrew was inserted simultaneously. Corticision was introduced as a supplemental dentoalveolar surgery in orthodontic therapy to achieve accelerated tooth movement with minimal surgical intervention. In this technique, a reinforced scalpel was used as a thin chisel to separate the interproximal cortices transmucosally without a flap. This technique was applied not to accelerate tooth movement, but to protract the mandibular molars. One miniscrew was inserted on the mesiobuccal side of the mandibular right molar for protraction and intrusion. In addition, 2 miniscrews were inserted in the buccal sides of the maxillary first and second molars and the palatal side of the maxillary first molar to intrude them for correction of the mandibular shift and the cant of the occlusal plane. Excellent occlusion and correction of the anterior open bite were achieved without surgery. At the 2-year follow-up examination, the patient had a good occlusion and showed good stability with no opening of the extraction space. A partial corticision is an effective option for facilitating movement of mandibular molars. Copyright © 2013 American Association of Orthodontists. Published by Mosby, Inc. All rights reserved.
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Palmer, Steve; Groves, Nicola; Schindeler, Aaron; Yeoh, Thomas; Biben, Christine; Wang, Cheng-Chun; Sparrow, Duncan B.; Barnett, Louise; Jenkins, Nancy A.; Copeland, Neal G.; Koentgen, Frank; Mohun, Tim; Harvey, Richard P.
2001-01-01
We have isolated a murine cDNA encoding a 9-kD protein, Chisel (Csl), in a screen for transcriptional targets of the cardiac homeodomain factor Nkx2-5. Csl transcripts were detected in atria and ventricles of the heart and in all skeletal muscles and smooth muscles of the stomach and pulmonary veins. Csl protein was distributed throughout the cytoplasm in fetal muscles, although costameric and M-line localization to the muscle cytoskeleton became obvious after further maturation. Targeted disruption of Csl showed no overt muscle phenotype. However, ectopic expression in C2C12 myoblasts induced formation of lamellipodia in which Csl protein became tethered to membrane ruffles. Migration of these cells was retarded in a monolayer wound repair assay. Csl-expressing myoblasts differentiated and fused normally, although in the presence of insulin-like growth factor (IGF)-1 they showed dramatically enhanced fusion, leading to formation of large dysmorphogenic “myosacs.” The activities of transcription factors nuclear factor of activated T cells (NFAT) and myocyte enhancer–binding factor (MEF)2, were also enhanced in an IGF-1 signaling–dependent manner. The dynamic cytoskeletal localization of Csl and its dominant effects on cell shape and behavior and transcription factor activity suggest that Csl plays a role in the regulatory network through which muscle cells coordinate their structural and functional states during growth, adaptation, and repair. PMID:11381084
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Shipitalo, Martin J; Malone, Robert W; Ma, Liwang; Nolan, Bernard T; Kanwar, Rameshwar S; Shaner, Dale L; Pederson, Carl H
2016-06-01
Crop residue removal for bioenergy production can alter soil hydrologic properties and the movement of agrochemicals to subsurface drains. The Root Zone Water Quality Model (RZWQM), previously calibrated using measured flow and atrazine concentrations in drainage from a 0.4 ha chisel-tilled plot, was used to investigate effects of 50 and 100% corn (Zea mays L.) stover harvest and the accompanying reductions in soil crust hydraulic conductivity and total macroporosity on transport of atrazine, metolachlor and metolachlor oxanilic acid (OXA). The model accurately simulated field-measured metolachlor transport in drainage. A 3 year simulation indicated that 50% residue removal reduced subsurface drainage by 31% and increased atrazine and metolachlor transport in drainage 4-5-fold when surface crust conductivity and macroporosity were reduced by 25%. Based on its measured sorption coefficient, approximately twofold reductions in OXA losses were simulated with residue removal. The RZWQM indicated that, if corn stover harvest reduces crust conductivity and soil macroporosity, losses of atrazine and metolachlor in subsurface drainage will increase owing to reduced sorption related to more water moving through fewer macropores. Losses of the metolachlor degradation product OXA will decrease as a result of the more rapid movement of the parent compound into the soil. Published 2015. This article is a U.S. Government work and is in the public domain in the USA. Published 2015. This article is a U.S. Government work and is in the public domain in the USA.
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An interactive local flattening operator to support digital investigations on artwork surfaces.
Pietroni, Nico; Massimiliano, Corsini; Cignoni, Paolo; Scopigno, Roberto
2011-12-01
Analyzing either high-frequency shape detail or any other 2D fields (scalar or vector) embedded over a 3D geometry is a complex task, since detaching the detail from the overall shape can be tricky. An alternative approach is to move to the 2D space, resolving shape reasoning to easier image processing techniques. In this paper we propose a novel framework for the analysis of 2D information distributed over 3D geometry, based on a locally smooth parametrization technique that allows us to treat local 3D data in terms of image content. The proposed approach has been implemented as a sketch-based system that allows to design with a few gestures a set of (possibly overlapping) parameterizations of rectangular portions of the surface. We demonstrate that, due to the locality of the parametrization, the distortion is under an acceptable threshold, while discontinuities can be avoided since the parametrized geometry is always homeomorphic to a disk. We show the effectiveness of the proposed technique to solve specific Cultural Heritage (CH) tasks: the analysis of chisel marks over the surface of a unfinished sculpture and the local comparison of multiple photographs mapped over the surface of an artwork. For this very difficult task, we believe that our framework and the corresponding tool are the first steps toward a computer-based shape reasoning system, able to support CH scholars with a medium they are more used to. © 2011 IEEE
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Thomas, John E; Allen, L Hartwell; McCormack, Leslie A; Vu, Joseph C; Dickson, Donald W; Ou, Li-Tse
2004-01-01
The fumigant 1,3-dichloropropene (1,3-D) is considered to be a potential replacement for methyl bromide when methyl bromide is phased out in 2005. This study on surface emissions and subsurface diffusion of 1,3-D in a Florida sandy soil was conducted in field beds with or without plastic covers. After injection of the commercial fumigant Telone II by conventional chisels to field beds at 30cm depth which were covered with polyethylene film (PE), virtually impermeable film, or no cover (bare), (Z)- and (E)-1,3-D rapidly diffused upward. Twenty hours after injection, majority of (Z)- and (E)-1,3-D had moved upward from 30 cm depth to the layer of 5-20 cm depth. Downward movement of the two isomers in the beds with or without a plastic cover was not significant. (Z)-1,3-D diffused more rapidly than (E)-1,3-D. Virtually impermeable films (VIF) had a good capacity to retain (Z)- and (E)-1,3-D in soil pore air space. Vapor concentrations of the two isomers in the shallow subsurface of the field bed covered with VIF were greater than that in the two beds covered with polyethylene film (PE) or no cover (bare). In addition, VIF cover provided more uniform distribution of (Z)- and (E)-1,3-D in shallow subsurface than PE cover or no cover. Virtually impermeable film also had a better capability to retard surface emissions of the two isomers from soil in field beds than PE cover or no cover.
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Maïssa, Cécile; Guillon, Michel; Garofalo, Renee J
2012-01-01
The principal objective of the study was to measure the conjunctival staining produced in the circumlimbal region by silicone hydrogel contact lenses with different edge designs. The secondary objective was to investigate the association between circumlimbal staining and comfort. Four silicone hydrogel contact lenses: ACUVUE OASYS (knife edge design), AIR OPTIX, Biofinity (chisel edge rounded edge combination), and PureVision (rounded edge design), and 1 hydrogel contact lens, ACUVUE 2 (knife edge design), were tested. The study was conducted on a cohort population of 27 established soft contact lens wearers, who wore each contact lens type, in a random order, for a period of 10 (±2) days. Circumlimbal staining was measured in a double-masked fashion through image analysis of digital photographs of lissamine green taken under controlled experimental conditions. The results obtained showed that contact lens edge design was the primary factor controlling circumlimbal staining for silicone hydrogel lenses: a rounded edge away from the ocular surface produced the lowest staining (average, 0.19%) and a knife edge in close apposition to the ocular surface produced the highest staining (average, 1.34%). Contact lens material rigidity was also identified to affect circumlimbal staining and an inverse association between circumlimbal staining and contact lens comfort was demonstrated: the rounded edge design produced the lowest comfort (72 of 100) and the knife edge design produced the highest (87 out of 100). Soft contact lens wear induces circumlimbal staining, the level of staining being influenced by the contact lens edge design. However, high level of circumlimbal staining is not associated with decreased comfort.
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Correction of lobule-type microtia: I. The first stage of costal cartilage grafting.
Yotsuyanagi, Takatoshi; Yamashita, Ken; Yamauchi, Makoto; Sugai, Asuka; Kayama, Musashi; Gonda, Ayako; Kita, Arisa
2014-01-01
Recently, auriculoplasty with costal cartilage grafting has been successfully used for correcting microtia and creating a clearly refined contour and a natural appearance of the ear. However, several important problems remain unsolved in these techniques. The authors describe an improved technique for harvesting costal cartilage with minimal morbidity and a new procedure for fabricating a cartilage frame that ensures a refined shape and rigid structure of the constructed ear. Costal cartilage is harvested directly with a chisel. This technique enables some of the cartilage at the chest wall to remain intact. The base frame is fabricated by two cartilage blocks partly overlapped on the area of the antihelix. The thickness in the overlapping area emphasizes the contour between the antihelix and the helical crus. To prevent absorption of the cartilage, helical and antihelical parts are created using the outer rigid layer of the harvested cartilage and are covered as much as possible by perichondrium. A total of 137 ears in 121 patients were corrected with the authors' technique and followed up for at least 3 years. Almost all of the patients could walk within 2 days after the operation. The structure and contour of the constructed ear were well maintained. Attention should be given not only to successful outcomes of construction of the ear but also to minimal morbidity for the patients. Our technique made it possible to construct a cosmetically refined ear that could be maintained for a long period and minimize the pain and deformity of the donor's chest.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Thibodeaux, J.; Hensley, J.
2013-01-01
The biomass thermochemical conversion platform at the National Renewable Energy Laboratory (NREL) develops and demonstrates processes for the conversion of biomass to fuels and chemicals including gasification, pyrolysis, syngas clean-up, and catalytic synthesis of alcohol and hydrocarbon fuels. In this talk, I will discuss the challenges of being a technician in this type of research environment, including handling and working with catalytic materials and hazardous chemicals, building systems without being given all of the necessary specifications, pushing the limits of the systems through ever-changing experiments, and achieving two-way communication with engineers and supervisors. I will do this by way ofmore » two examples from recent research. First, I will describe a unique operate-to-failure experiment in the gasification of chicken litter that resulted in the formation of a solid plug in the gasifier, requiring several technicians to chisel the material out. Second, I will compare and contrast bench scale and pilot scale catalyst research, including instances where both are conducted simultaneously from common upstream equipment. By way of example, I hope to illustrate the importance of researchers 1) understanding the technicians' perspective on tasks, 2) openly communicating among all team members, and 3) knowing when to voice opinions. I believe the examples in this talk will highlight the crucial role of a technical staff: skills attained by years of experience to build and operate research and production systems. The talk will also showcase the responsibilities of NREL technicians and highlight some interesting behind-the-scenes work that makes data generation from NREL's thermochemical process development unit possible.« less
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Bekić, Marijo; Davila, Slavko; Hrskanović, Mato; Bekić, Marijana; Seiwerth, Sven; Erdeljić, Viktorija; Capak, Darko; Butković, Vladimir
2008-12-01
Previous studies have shown substantial effect thermal damage can have on new bone formation following osteotomy. In this study we evaluated the extent of thermal damage which occurs in four different methods of osteotomy and the effects it can have on bone healing. We further wanted to test whether a special osteotomy plate we constructed can lead to diminished heat generation during osteotomy and enhanced bone healing. The four methods evaluated included osteotomy performed by chisel, a newly constructed osteotomy plate, Gigly and oscillating saw. Twelve adult sheep underwent osteotomy performed on both tibiae. Bone fragments were stabilized using a fixation plate. Callus size was assessed using standard radiographs. Densitometry and histological evaluation were performed at 8 weeks following osteotomy. Temperature measurements were performed both in vivo during the operation, and ex vivo on explanted tibiae. The defects healed without complications and showed typical course of secondary fracture healing with callus ingrowth into the osteotomy gap. Radiographic examination of bone healing showed a tendency towards more callus formation in bones osteotomized using Gigly and oscillating saw, but this difference lacked significance. Use of Gigly and oscillating saw elicited much higher temperatures at the bone cortex surface, which subsequently lead to slightly impaired bone healing according to histological analysis. BMD was equal among all bones. In conclusion, the time required for complete healing of the defect differed depended greatly on the instruments used. The newly constructed osteotomy plate showed best results based on histological findings of capillary and osteoblast density.
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Kron, Tomas; Chesson, Brent; Hardcastle, Nicholas; Crain, Melissa; Clements, Natalie; Burns, Mark; Ball, David
2018-05-01
A randomised clinical trial comparing stereotactic ablative body radiotherapy (SABR) with conventional radiotherapy for early stage lung cancer has been conducted in Australia and New Zealand under the auspices of the TransTasman Radiation Oncology Group (NCT01014130). We report on the technical credentialing program as prerequisite for centres joining the trial. Participating centres were asked to develop treatment plans for two test cases to assess their ability to create plans according to protocol. Dose delivery in the presence of inhomogeneity and motion was assessed during a site visit using a phantom with moving inserts. Site visits for the trial were conducted in 16 Australian and 3 New Zealand radiotherapy facilities. The tests with low density inhomogeneities confirmed shortcomings of the AAA algorithm for dose calculation. Dose was assessed for a typical treatment delivery including at least one non-coplanar beam in a stationary and moving phantom. This end-to-end test confirmed that all participating centres were able to deliver stereotactic ablative body radiotherapy with the required accuracy while the planning study demonstrated that they were able to produce acceptable plans for both test cases. The credentialing process documented that participating centres were able to deliver dose as required in the trial protocol. It also gave an opportunity to provide education about the trial and discuss technical issues such as four-dimensional CT, small field dosimetry and patient immobilisation with staff in participating centres. Advances in knowledge: Credentialing is an important quality assurance tool for radiotherapy trials using advanced technology. In addition to confirming technical competence, it provides an opportunity for education and discussion about the trial.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Robb, A.J. III; Hoggatt, P.R.
Hydrocarbon containing soil was bioremediated at a combination wastewater and slop oil skim evaporation pond utilizing cost effective low technology resources. Fluids and sludge from the football field-sized pond were extraction procedure toxicity and purgeable organics tested, and total petroleum hydrocarbon (TPH) concentrations determined. An impact risk analysis was performed, and a corrective action plan developed and implemented. The three year project was closely coordinated with the Kansas Corporation Commission (KCC) and the Kansas Department of Health and Environment (KDHE) who established the closure level. The impacted soils at the pond were completely excavated and closure was immediately granted bymore » KDHE for the excavated area. The 24,000 cubic yards of excavated soil were then surface spread on adjacent Mobil property. A nutrient and microbial base was applied to bioaugment the soil. The preapplication land surface and the subsequently land farmed soil was periodically disced and chiseled. A job safety plan including industrial hygiene measures to eliminate workforce exposure was developed and implemented. The final remediation cost analysis amounts to $1.48 per cubic yard compared to the $30 to $150 per cubic yard industry o estimates for similar projects. Several factors were critical in ailing costs to remain so low: (1) assessment and implementation by local in-house staff, (2) conservative remedial action plan and sampling strategy; (3) local contractors; (4) locally available soil amendment; and (5) effective regulatory coordination. The methods described can be used to cost effectively characterize and bioremediate other sites where hydrocarbon-impacted soils exist in similar dry-land environments.« less
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Telling stories out of school: experiencing the paramedic's oral traditions and role dissonance.
Lazarsfeld-Jensen, Ann
2014-11-01
Role dissonance is an uncomfortable experience for graduate paramedics, and some blame their university education for the problem. For paramedics the conflict is between identifying as a rescuer and acting largely as a care giver. With vocational pathways into so many uniformed professions closing down in preference for graduate entrants, young new professionals have to negotiate a rapidly changing work culture. Their older colleagues may be challenged and threatened by the new order. For paramedics the problem is compounded by the newness of its place in the tertiary landscape. Since 9/11 young people have been increasingly attracted to rescue roles. Yet in Australia there is increasing need and scope for health workers in remote and aging populations, a preference not immediately attractive to young people hoping for a more heroic future. While the near professions such as nursing have established their discourses around culture, role and pedagogy, paramedics is still trying to chisel its identity. The myths of paramedic glories past tend to add to the confusion of graduates. Due to a lack of empirical studies of non-clinical aspects of paramedicine, a bricolage methodology was used to refresh data from two discrete qualitative research projects conducted in 2011. Both projects had originally been interested in optimal paramedic preceptorship before and after graduation, but neither had explored the implicit theme which revealed the role of rescue experiences in paramedic culture and identity. The bricolage included a new search of literature from near professions and applied new theoretical frameworks to the analysis of the extant data, to demonstrate how storytelling as an element of paramedic collegiality perpetuates rescue stories that are then used to define paramedic work. Copyright © 2014 Elsevier Ltd. All rights reserved.
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Mistry, Freddy Kersi; Hegde, Nidarsh Diwakar; Hegde, Mithra Nidarsh
2016-01-01
One of the most critical and crucial steps in surgical extraction is cutting the bone or osteotomy, for which many techniques are used, e.g., chisels and mallet, rotary instruments, and ultrasound bone-cutting instruments. If they are not used judiciously, they can be hazardous. To assess the efficiency of piezosurgery unit over micromotor while performing surgical extraction of lower third molars by assessing the time taken for the surgery and measuring postoperative parameters such as pain, trismus, and swelling. Thirty patients having bilateral impacted third molars with the same difficulty index were selected for the study. One side surgical removal was done using micromotor and other side by piezosurgery with an interval of 15 days. After each surgery, time taken to finish was measured and patients were followed up on postoperative days 1, 3, 5, 7, and 15 for assessing pain, trismus, and swelling. Data obtained were statistically analyzed. The mean time taken for the micromotor group is 37.90 min whereas by the piezosurgery group is 54.63 min, showing a statistically significant difference ( P < 0.001). Furthermore, there is statistically significant difference ( P < 0.001) in the level of pain, trismus, and swelling on postoperative days 1, 3, 5, and 7. Even the intragroup comparison of piezosurgical group for trismus and swelling showed no statistically significant difference on postoperative day 7, indicating faster recovery of trismus and swelling. On postoperative day 15, there was no difference in any parameter in both groups indicating complete symptom-free recovery in both groups. It takes more time to perform surgical extraction of third molars when piezosurgical unit is used. Despite that, it causes less pain postoperatively with faster improvement in trismus and quicker reduction in swelling.
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Postsurgical consequences in lower third molar surgical extraction using micromotor and piezosurgery
Mistry, Freddy Kersi; Hegde, Nidarsh Diwakar; Hegde, Mithra Nidarsh
2016-01-01
Background: One of the most critical and crucial steps in surgical extraction is cutting the bone or osteotomy, for which many techniques are used, e.g., chisels and mallet, rotary instruments, and ultrasound bone-cutting instruments. If they are not used judiciously, they can be hazardous. Objectives: To assess the efficiency of piezosurgery unit over micromotor while performing surgical extraction of lower third molars by assessing the time taken for the surgery and measuring postoperative parameters such as pain, trismus, and swelling. Materials and Methods: Thirty patients having bilateral impacted third molars with the same difficulty index were selected for the study. One side surgical removal was done using micromotor and other side by piezosurgery with an interval of 15 days. After each surgery, time taken to finish was measured and patients were followed up on postoperative days 1, 3, 5, 7, and 15 for assessing pain, trismus, and swelling. Data obtained were statistically analyzed. Results: The mean time taken for the micromotor group is 37.90 min whereas by the piezosurgery group is 54.63 min, showing a statistically significant difference (P < 0.001). Furthermore, there is statistically significant difference (P < 0.001) in the level of pain, trismus, and swelling on postoperative days 1, 3, 5, and 7. Even the intragroup comparison of piezosurgical group for trismus and swelling showed no statistically significant difference on postoperative day 7, indicating faster recovery of trismus and swelling. On postoperative day 15, there was no difference in any parameter in both groups indicating complete symptom-free recovery in both groups. Conclusion: It takes more time to perform surgical extraction of third molars when piezosurgical unit is used. Despite that, it causes less pain postoperatively with faster improvement in trismus and quicker reduction in swelling. PMID:28299267
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Metri, Malasiddappa; Hegde, Swaroop; Dinesh, K; Indiresha, H N; Nagaraj, Shruthi; Bhandi, Shilpa H
2015-11-01
To evaluate the effectiveness of two final irrigation techniques for the removal of precipitate formed by the interaction between sodium hypochlorite (NaOCl) and chlorhexidine (CHX). Sixty freshly extracted human maxillary incisor teeth were taken and randomly divided into three groups, containing 20 teeth each. Group 1 (control group), were irrigated with 5 ml of 2.5% NaOCl and a final flush with 5 ml of 2% chlorhexidine. Group 2 were irrigated with 5 ml of 2.5% NaOCl and 5 ml of 2% chlorhexidine followed by 5 ml of saline and agitated with F-files. Group 3 were irrigated with 5 ml of 2.5% NaOCl and 5 ml of 2% chlorhexidine followed by 5 ml of 15% citric acid and passively agitated with ultrasonics. A thin longitudinal groove was made along the buccal and lingual aspect of the root using diamond disks and split with chisel and mallet. Both halves of the split tooth will be examined under stereomicroscope. Results were tabulated and analyzed statistically using analysis of variance (ANOVA) and Mann-Whitney U test. There was a significant difference between the mean values (p < 0.05) in groups 2 and 3 compared to group 1 at each level. Passive ultrasonic irrigation is more effective than the F-file agitation technique to remove the precipitate at all three levels measured. Combination of sodium hypochlorite and chlorhexidine irrigation protocol has been practiced since from many years to achieve good results. However, it has adverse effect in the form of precipitate and which is considered to be a carcinogenic in nature, hence this precipitate should be removed.
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Venkataram, V; Gokhale, S T; Kenchappa, M; Nagarajappa, R
2013-08-01
Endodontic success depends heavily on effective chemo-mechanical debridement of root canals through the use of instruments and irrigating solutions. To compare the effectiveness of chamomile hydroalcoholic extract, Biopure™ mixture of tetracycline isomer, acid and detergent (MTAD) and 2.5 % sodium hypochlorite (NaOCl) on removal of the smear layer. Randomised controlled trial. Thirty extracted single-rooted, primary human teeth were allocated at random into three experimental groups of 10 teeth each. For each tooth, the canal was prepared using the step-back technique. During instrumentation, 2 ml of the irrigant was used for at least 10 s after each file and 10 ml as a final flush for 2 min for chamomile and NaOCL irrigants. Whereas for MTAD, an initial rinse with 1.3 % NaOCl for a cumulated period of 20 min, and use of MTAD as the final rinse for a period of 5 min was followed. Longitudinal grooves were made on root segments, then split into two halves with a chisel, stored in 2.5 % glutaraldehyde solution and fixed in ethanol series. Specimens were examined for the smear layer according to Hulsmann et al. (Int Endod J 35:668-679, 2002) criteria using a scanning electron microscope. Kruskal-Wallis and Mann-Whitney U tests were used. The most effective result in removal of smear layer occurred with the use of MTAD, followed by chamomile extract. The chamomile extract was found to be significantly more effective than 2.5 % NaOCl solution which had only minor effects. The efficacy of chamomile to remove the smear layer was superior to 2.5 % NaOCl alone, but less effective than MTAD mixture.
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Breeze, J; Carr, D J; Mabbott, A; Beckett, S; Clasper, J C
2015-05-01
Explosively propelled fragments are the most common cause of injury to UK service personnel in modern conflicts. Numerical injury models to simulate such injuries utilise algorithms based upon gelatin and animal tissue testing but data is limited on many fragment simulating projectiles and these simulants cannot represent human anatomy. Testing with post mortem specimens may overcome this limitation but no information exists about how post mortem tissue changes and storage conditions in humans or animals may affect projectile penetration. Two chisel nosed cylinders (0.49 g and 1.10 g) and a 0.51 g (5 mm) sphere were fired into three groups of porcine tissue (fresh, refrigerated and frozen then refrigerated) and compared to 20% gelatin. Depth of projectile penetration was ascertained with the assistance of computed tomography and kinetic energy absorption by tissues measured using Doppler radar and high speed photography. No difference in depth of penetration was found between porcine tissue stored in the different manners compared with 20% gelatin by impact velocities less than 100 m/s. Insufficient numbers of projectiles were retained in tissue at higher velocities for statistical analysis to be undertaken. Energy absorbed per millimetre of tissue ranged between 0.42 and 0.98 J/mm for different porcine tissue despite differing storage. This pilot study would suggest that the effect of refrigerating or freezing porcine tissue followed by thawing has no effect on its ability to retard these projectiles. Further research is required to ascertain if these results occur at greater velocities and for other types of projectile. Crown Copyright © 2015. Published by Elsevier Ltd. All rights reserved.
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The current status and future prospects of computer-assisted hip surgery.
Inaba, Yutaka; Kobayashi, Naomi; Ike, Hiroyuki; Kubota, So; Saito, Tomoyuki
2016-03-01
The advances in computer assistance technology have allowed detailed three-dimensional preoperative planning and simulation of preoperative plans. The use of a navigation system as an intraoperative assistance tool allows more accurate execution of the preoperative plan, compared to manual operation without assistance of the navigation system. In total hip arthroplasty using CT-based navigation, three-dimensional preoperative planning with computer software allows the surgeon to determine the optimal angle of implant placement at which implant impingement is unlikely to occur in the range of hip joint motion necessary for daily activities of living, and to determine the amount of three-dimensional correction for leg length and offset. With the use of computer navigation for intraoperative assistance, the preoperative plan can be precisely executed. In hip osteotomy using CT-based navigation, the navigation allows three-dimensional preoperative planning, intraoperative confirmation of osteotomy sites, safe performance of osteotomy even under poor visual conditions, and a reduction in exposure doses from intraoperative fluoroscopy. Positions of the tips of chisels can be displayed on the computer monitor during surgery in real time, and staff other than the operator can also be aware of the progress of surgery. Thus, computer navigation also has an educational value. On the other hand, its limitations include the need for placement of trackers, increased radiation exposure from preoperative CT scans, and prolonged operative time. Moreover, because the position of a bone fragment cannot be traced after osteotomy, methods to find its precise position after its movement need to be developed. Despite the need to develop methods for the postoperative evaluation of accuracy for osteotomy, further application and development of these systems are expected in the future. Copyright © 2016 The Japanese Orthopaedic Association. Published by Elsevier B.V. All rights reserved.
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Hemalatha, Hiremath; Sandeep, Metgud; Kulkarni, Sadanand; Yakub, Shoeb Sheikh
2009-08-01
To compare the reinforcement and strengthening ability of resilon, gutta-percha, and ribbond in endodontically treated roots of immature teeth. Sixty five freshly extracted human maxillary anterior teeth were prepared with a Peeso no. 6 to simulate immature teeth (Cvek's stage 3 root development). After instrumentation, each root was irrigated with sodium hypochlorite and with ethylene diamino tetra acetic acid to remove the smear layer. To simulate single visit apexification technique a 4-5 mm white Pro Root mineral trioxide aggregate plug was placed apically using schilder carrier. The teeth were divided into three experimental groups and one control group. Group I--control group (root canals instrumented but not filled); Group II--backfilled with thermoplastisized gutta-percha using AH plus sealer; Group III--reinforced with Resilon using epiphany sealer; Group IV--reinforced with Ribbond fibers using Panavia F luting cement. A Universal Testing Machine was used to apply a load, at the level of the lingual cementoenamel junction with a chisel-shaped tip The peak load to fracture was recorded and statistical analysis was completed using student's t-test. Values of peak load to fracture were 1320.8, 1604.88, 1620, and 1851 newtons for Group I to Group IV respectively. The results of student's t-test, revealed no significant difference (P > 0.05,) between Group II and Group III. Comparison between Group IV and Group III and between Group IV and Group II revealed highly significant difference (P > 0.001). Teeth reinforced with Ribbond fibers using Panavia F luting cement showed the highest resistance to fracture. Resilon could not strengthen the roots and showed no statistically significant difference when compared with thermoplastisized gutta-percha in reinforcing immature tooth when tested with universal testing machine in an experimental model of immature tooth.
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Oliveira, Adauê S; Barwaldt, Caroline K; Bublitz, Luana S; Moraes, Rafael R
2014-06-01
This study investigated the the influence of bracket displacement or rotation during fixation and the time of excess adhesive removal from around the bracket on bond strength to enamel. Stainless steel brackets were bonded to the buccal faces of bovine incisors using Transbond XT® adhesive resin. The teeth were divided into five groups (n = 20). In the control group, no displacement or rotation of the bracket was carried out. In the Displac-A group, excess adhesive was removed after the bracket was displaced 2 mm incisally. In the B-Displac group, excess adhesive was removed before the bracket was displaced incisally. In the Rotat-A group, excess adhesive was removed after the bracket was rotated 45°. In the B-Rotat group, excess adhesive was removed before the bracket was rotated. Photoactivation was carried out on the lateral sides of the bracket. A shear test was conducted 10 min after fixation using a knife-edged chisel. Bond strength data were analysed using ANOVA and Fisher's test (5%). The adhesive remnant index (ARI) was scored under magnification. ARI data were analysed using the Kruskal-Wallis test (5%). No significant differences were detected among the Control, Displac-A, Rotat-A and B-Rotat groups. The B-Displac group showed lower bond strength than all of the other groups, except Displac-A. No significant differences were observed in ARI scores across groups. Displacements of the brackets during fixation did not seem to affect the enamel bond strength when excess adhesive is removed after the final positioning of the bracket. © 2014 British Orthodontic Society.
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Thompson, R B; Meisinger, J J
2002-01-01
Ammonia (NH3) volatilization commonly causes a substantial loss of crop-available N from surface-applied cattle slurry. Field studies were conducted with small wind tunnels to assess the effect of management factors on NH3 volatilization. Two studies compared NH3 volatilization from grass sward and bare soil. The average total NH3 loss was 1.5 times greater from slurry applied to grass sward. Two studies examined the effect of slurry dry matter (DM) content on NH3 loss under hot, summer conditions in Maryland, USA. Slurry DM contents were between 54 and 134 g kg(-1). Dry matter content did not affect total NH3 loss, but did influence the time course of NH3 loss. Higher DM content slurries had relatively higher rates of NH3 volatilization during the first 12 to 24 h, but lower rates thereafter. Under the hot conditions, the higher DM content slurries appeared to dry and crust more rapidly causing smaller rates of NH3 volatilization after 12 to 24 h, which offset the earlier positive effects of DM content on NH3 volatilization. Three studies compared immediate incorporation with different tillage implements. Total NH3 loss from unincorporated slurry was 45% of applied slurry NH4+-N, while losses following immediate incorporation with a moldboard plow, tandem-disk harrow, or chisel plow were, respectively, 0 to 3, 2 to 8, and 8 to 12%. These ground cover and DM content data can be used to improve predictions of NH3 loss under specific farming conditions. The immediate incorporation data demonstrate management practices that can reduce NH3 volatilization, which can improve slurry N utilization in crop-forage production.
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Paruchuri, Yasaswi; Siuniak, Amanda; Johnson, Nicole; Levin, Elena; Mitchell, Katherine; Goodrich, Jaclyn M.; Renne, Elisha P.; Basu, Niladri
2014-01-01
Mercury use in small-scale gold mining is ubiquitous across Ghana but little is known about the extent to which such activities have contaminated community residents and miners. Here, occupational exposures to elemental mercury (via urine sampling) and dietary exposures to methylmercury (via hair sampling) were assessed among 120 participants recruited from a mining community located in the Talensi-Nabdam District of Ghana’s Upper East region during summer 2009. More than one-fifth of the participants had moderately high levels of urinary mercury (>10 µg/L) and 5% had urine mercury levels that exceeded the WHO guideline value of 50 µg/L. When participants were stratified according to occupation, those active in the mining industry had the highest mercury levels. Specifically, individuals that burned amalgam had urine mercury levels (median: 43.8 µg/L; mean ± SD: 171.1 ± 296.5 µg/L; n=5) significantly higher than median values measured in mechanical operators (11.6 µg/L, n=4), concession managers/owners (5.6 µg/L, n=11), excavators that blast and chisel ore (4.9 µg/L, n=33), individuals that sift and grind crushed ore (2.2 µg/L, n=47), support workers (0.5 µg/L, n=14), and those with no role in the mining sector (2.5 µg/L, n=6). There was a significant positive spearman correlation between fish consumption and hair mercury levels (r = 0.30) but not with urine mercury (r = 0.18) though further studies are needed to document which types of fish are consumed as well as portion sizes. Given that 200,000 people in Ghana are involved in the small-scale gold mining industry and that the numbers are expected to grow in Ghana and many other regions of the world, elucidating mercury exposure pathways in such communities is important to help shape policies and behaviors that may minimize health risks. PMID:20875913
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Pristine Samples of Silicon Carbide Separated From the Canyon Diablo Meteorite
NASA Astrophysics Data System (ADS)
Leung, I. S.; Winston, R.
2008-12-01
The Canyon Diablo is an iron meteorite whose collision with Earth created Meteor Crater in Arizona. In a study of a large block (53 kg) of this meteorite, Henri Moissan reported his findings of green, hexagonal crystals of silicon carbide (SiC) which was given the name moissanite the following year by George Kunz (1905). Moissan did not report finding the cubic form of SiC. Subsequently, many erroneous reports appeared when the polishing compound (synthetic SiC) was mistakenly considered by researchers as a natural mineral associated with, rather than a contaminant of many rock types. Hence, the occurrence of SiC in the Canyon Diablo remains in doubt, and any proposal to investigate this problem was discouraged and regarded as predictably unproductive. This notion hampered further work on abundant materials housed in museums. SiC grains have been found in primitive meteorites and interplanetary dust particles. Some have been identified as presolar grains. The significance of SiC in the Canyon Diablo cannot be revealed unless we have abundant data from pristine samples, enough for us to classify them into presolar or other types. We report here a simple method we used to separate SiC crystals from the meteorite. We chose samples containing a carbon nodule composed of graphite, diamond-lonsdaleite, and SiC grains in the iron matrix. We broke up the carbon nodule with a sharp tungsten carbide chisel and hammer. After removing the large metal fragments, we put a small amount of the fine black grains in a Petri dish with acetone, then swerved the dish to scatter the grains sparingly on the bottom of the dish. Under a binocular microscope, SiC crystals can be spotted easily by their adamantine luster, color (blue, green, beige, etc.), and high birefringence when placed between crossed polarizers of a petrographic microscope. We also X-rayed individual grains, and have identified several hexagonal polytype structures as well as the cubic form (3C polytype).
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Rocha Junior, Paulo Roberto da; Andrade, Felipe Vaz; Mendonça, Eduardo de Sá; Donagemma, Guilherme Kangussú; Fernandes, Raphael Bragança Alves; Bhattharai, Rabin; Kalita, Prasanta Kumar
2017-04-01
The objective of this study was to evaluate sediment, water and nutrient losses from different pasture managements in the Atlantic Rainforest biome. A field study was carried out in Alegre Espiríto Santo, Brazil, on a Xanthic Ferralsol cultivated with braquiaria (Brachiaria brizantha). The six pasture managements studied were: control (CON), chisel (CHI), fertilizer (FER), burned (BUR), plowing and harrowing (PH), and integrated crop-livestock (iCL). Runoff and sediment samples were collected and analyzed for calcium (Ca), magnesium (Mg), potassium (K), phosphorus (P) and organic carbon contents. Soil physical attributes and above and below biomass were also evaluated. The results indicated that higher water loss was observed for iCL (129.90mm) and CON (123.25mm) managements, and the sediment losses were higher for CON (10.24tha -1 ) and BUR (5.20tha -1 ) managements when compared to the other managements. Majority of the nutrients losses occurred in dissolved fraction (99% of Ca, 99% of Mg, 96% of K, and 65% of P), whereas a significant fraction of organic carbon (80%) loss occurred in a particulate form. Except for P, other nutrients (Ca, Mg and K) and organic carbon losses were higher in coarse sediment compared to fine sediment. The greater losses of sediment, organic carbon, and nutrients were observed for CON followed by BUR management (p<0.05). Our findings indicated that the traditional pasture management adopted in the Atlantic Rainforest needs to be rethought and burned management should be avoided. Based on the water, soil, and nutrient losses from various practices, to reduce pasture degradation, farmers should adopt edaphic practices by applying lime and fertilize to improve pasture growth and soil cover, and reducing soil erosion in the hilly Brazilian Atlantic Rainforest biome. Copyright © 2016. Published by Elsevier B.V.
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Kravchenko, Alexandra; Falconer, Ruth E; Grinev, Dmitri; Otten, Wilfred
2011-06-01
Despite the importance of fungi in soil functioning they have received comparatively little attention, and our understanding of fungal interactions and communities is lacking. This study aims to combine a physiologically based model of fungal growth with digitized images of internal pore volume of samples of undisturbed soil from contrasting management practices to determine the effect of physical structure on fungal growth dynamics. We quantified pore geometries of the undisturbed-soil samples from two contrasting agricultural practices, conventionally plowed (chisel plow) (CT) and no till (NT), and from native-species vegetation land use on land that was taken out of production in 1989 (NS). Then we modeled invasion of a fungal species within the soil samples and evaluated the role of soil structure on the progress of fungal colonization of the soil pore space. The size of the studied pores was > or =110 microm. The dynamics of fungal invasion was quantified through parameters of a mathematical model fitted to the fungal invasion curves. Results indicated that NT had substantially lower porosity and connectivity than CT and NS soils. For example, the largest connected pore volume occupied 79% and 88% of pore space in CT and NS treatments, respectively, while it only occupied 45% in NT. Likewise, the proportion of pore space available to fungal colonization was much greater in NS and CT than in NT treatment, and the dynamics of the fungal invasion differed among the treatments. The relative rate of fungal invasion at the onset of simulation was higher in NT samples, while the invasion followed a more sigmoidal pattern with relatively slow invasion rates at the initial time steps in NS and CT samples. Simulations allowed us to elucidate the contribution of physical structure to the rates and magnitudes of fungal invasion processes. It appeared that fragmented pore space disadvantaged fungal invasion in soils under long-term no-till, while large connected pores in soils under native vegetation or in tilled agriculture promoted the invasion.
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2017-01-01
Exchange activities, formal or otherwise, serve a variety of purposes and were prominent in many Pacific Island societies, both during island settlement and in late prehistory. Recent Polynesian studies highlight the role of exchange in the region’s most hierarchical polities where it contributed to wealth economies, emergent leadership, and status rivalry in late prehistory. Building on this research, we hypothesized that exchange in low hierarchy chiefdoms (kin-based polities where there are distinctions between commoners and elites but ranking within the latter is lacking, weak, or ephemeral) would differ in frequency and function from that associated with strongly hierarchical polities. We address this hypothesis through geochemical, morphological, and distributional analyses of stone tools on Nuku Hiva, Marquesas Islands. Non-destructive Energy-Dispersive X-ray Fluorescence (EDXRF) and destructive Wavelength-Dispersive X-ray Fluorescence (WDXRF) analyses of 278 complete and broken tools (adzes, chisels, preforms) from four valleys identify use of stone from at least seven sources on three islands: five on Nuku Hiva and one each on Eiao and Ua Pou. A functional analysis demonstrates that no tool form is limited to a particular source, while inter-valley distributions reveal that the proportions of non-local or extra-valley tools (43 to 94%, mean = 77%) approximate or exceed results from other archipelagoes, including those from elite and ritual sites of Polynesian archaic states. Intra-valley patterns also are unexpected, with non-local stone tools being recovered from both elite and commoner residential areas in near-equal proportions. Our findings unambiguously demonstrate the importance of exchange in late prehistoric Marquesan society, at varied social and geographic scales. We propose the observed patterns are the result of elites using non-local tools as political currency, aimed at reinforcing status, cementing client-patron relations, and building extra-valley alliances, consistent with prestige societies elsewhere and early historic accounts from the Marquesan Islands. PMID:29281652
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Jung, Gyu-Un; Kim, Jun Hwan; Lim, Nam Hun; Yoon, Gil Ho; Han, Ji-Young
2017-06-01
Ridge splitting techniques are used for horizontal ridge augmentation in implant dentistry. Recently, a novel engine-driven ridge splitting technique was introduced. This study compared the mechanical forces produced by conventional and engine-driven ridge splitting techniques in porcine mandibles. In 33 pigs, mandibular premolar areas were selected for the ridge splitting procedures, designed as a randomized split-mouth study. The conventional group underwent a chisel-and-mallet procedure (control group, n = 20), and percussive impulse (Newton second, Ns) was measured using a sensor attached to the mallet. In the engine-driven ridge spreader group (test group, n = 23), a load cell was used to measure torque values (Newton centimeter, Ncm). Horizontal acceleration generated during procedures (control group, n = 10 and test group, n = 10) was compared between the groups. After ridge splitting, the alveolar crest width was significantly increased both in the control (1.23 ± 0.45 mm) and test (0.98 ± 0.41 mm) groups with no significant differences between the groups. The average impulse of the control group was 4.74 ± 1.05 Ns. Torque generated by rotation in the test group was 9.07 ± 2.15 Ncm. Horizontal acceleration was significantly less in the test group (0.82 ± 1.05 g) than the control group (64.07 ± 42.62 g) (P < 0.001). Narrow edentulous ridges can be expanded by novel engine-driven ridge spreaders. Within the limits of this study, the results suggested that an engine-driven ridge splitting technique may be less traumatic and less invasive than a conventional ridge splitting technique. © 2016 John Wiley & Sons A/S. Published by John Wiley & Sons Ltd.
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Characterizing phosphorus dynamics in tile-drained agricultural fieldsof eastern Wisconsin
Madison, Allison; Ruark, Matthew; Stuntebeck, Todd D.; Komiskey, Matthew J.; Good, Laura W.; Drummy, Nancy; Cooley, Eric
2014-01-01
Artificial subsurface drainage provides an avenue for the rapid transfer of phosphorus (P) from agricultural fields to surface waters. This is of particular interest in eastern Wisconsin, where there is a concentrated population of dairy farms and high clay content soils prone to macropore development. Through collaboration with private landowners, surface and tile drainage was measured and analyzed for dissolved reactive P (DRP) and total P (TP) losses at four field sites in eastern Wisconsin between 2005 and 2009. These sites, which received frequent manure applications, represent a range of crop management practices which include: two chisel plowed corn fields (CP1, CP2), a no-till corn–soybean field (NT), and a grazed pasture (GP). Subsurface drainage was the dominant pathway of water loss at each site accounting for 66–96% of total water discharge. Average annual flow-weighted (FW) TP concentrations were 0.88, 0.57, 0.21, and 1.32 mg L−1 for sites CP1, CP2, NT, and GP, respectively. Low TP concentrations at the NT site were due to tile drain interception of groundwater flow where large volumes of tile drainage water diluted the FW-TP concentrations. Subsurface pathways contributed between 17% and 41% of the TP loss across sites. On a drainage event basis, total drainage explained between 36% and 72% of the event DRP loads across CP1, CP2, and GP; there was no relationship between event drainflow and event DRP load at the NT site. Manure applications did not consistently increase P concentrations in drainflow, but annual FW-P concentrations were greater in years receiving manure applications compared to years without manure application. Based on these field measures, P losses from tile drainage must be integrated into field level P budgets and P loss calculations on heavily manured soils, while also acknowledging the unique drainage patterns observed in eastern Wisconsin.
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Tool-specific performance of vibration-reducing gloves for attenuating fingers-transmitted vibration
Welcome, Daniel E.; Dong, Ren G.; Xu, Xueyan S.; Warren, Christopher; McDowell, Thomas W.
2016-01-01
BACKGROUND Fingers-transmitted vibration can cause vibration-induced white finger. The effectiveness of vibration-reducing (VR) gloves for reducing hand transmitted vibration to the fingers has not been sufficiently examined. OBJECTIVE The objective of this study is to examine tool-specific performance of VR gloves for reducing finger-transmitted vibrations in three orthogonal directions (3D) from powered hand tools. METHODS A transfer function method was used to estimate the tool-specific effectiveness of four typical VR gloves. The transfer functions of the VR glove fingers in three directions were either measured in this study or during a previous study using a 3D laser vibrometer. More than seventy vibration spectra of various tools or machines were used in the estimations. RESULTS When assessed based on frequency-weighted acceleration, the gloves provided little vibration reduction. In some cases, the gloves amplified the vibration by more than 10%, especially the neoprene glove. However, the neoprene glove did the best when the assessment was based on unweighted acceleration. The neoprene glove was able to reduce the vibration by 10% or more of the unweighted vibration for 27 out of the 79 tools. If the dominant vibration of a tool handle or workpiece was in the shear direction relative to the fingers, as observed in the operation of needle scalers, hammer chisels, and bucking bars, the gloves did not reduce the vibration but increased it. CONCLUSIONS This study confirmed that the effectiveness for reducing vibration varied with the gloves and the vibration reduction of each glove depended on tool, vibration direction to the fingers, and finger location. VR gloves, including certified anti-vibration gloves do not provide much vibration reduction when judged based on frequency-weighted acceleration. However, some of the VR gloves can provide more than 10% reduction of the unweighted vibration for some tools or workpieces. Tools and gloves can be matched for better effectiveness for protecting the fingers. PMID:27867313
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Characterizing phosphorus dynamics in tile-drained agricultural fields of eastern Wisconsin
NASA Astrophysics Data System (ADS)
Madison, Allison M.; Ruark, Matthew D.; Stuntebeck, Todd D.; Komiskey, Matthew J.; Good, Lara W.; Drummy, Nancy; Cooley, Eric T.
2014-11-01
Artificial subsurface drainage provides an avenue for the rapid transfer of phosphorus (P) from agricultural fields to surface waters. This is of particular interest in eastern Wisconsin, where there is a concentrated population of dairy farms and high clay content soils prone to macropore development. Through collaboration with private landowners, surface and tile drainage was measured and analyzed for dissolved reactive P (DRP) and total P (TP) losses at four field sites in eastern Wisconsin between 2005 and 2009. These sites, which received frequent manure applications, represent a range of crop management practices which include: two chisel plowed corn fields (CP1, CP2), a no-till corn-soybean field (NT), and a grazed pasture (GP). Subsurface drainage was the dominant pathway of water loss at each site accounting for 66-96% of total water discharge. Average annual flow-weighted (FW) TP concentrations were 0.88, 0.57, 0.21, and 1.32 mg L-1 for sites CP1, CP2, NT, and GP, respectively. Low TP concentrations at the NT site were due to tile drain interception of groundwater flow where large volumes of tile drainage water diluted the FW-TP concentrations. Subsurface pathways contributed between 17% and 41% of the TP loss across sites. On a drainage event basis, total drainage explained between 36% and 72% of the event DRP loads across CP1, CP2, and GP; there was no relationship between event drainflow and event DRP load at the NT site. Manure applications did not consistently increase P concentrations in drainflow, but annual FW-P concentrations were greater in years receiving manure applications compared to years without manure application. Based on these field measures, P losses from tile drainage must be integrated into field level P budgets and P loss calculations on heavily manured soils, while also acknowledging the unique drainage patterns observed in eastern Wisconsin.
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Tam, Byron; Bollu, Prashanti; Chaudhry, Kishore; Subramani, Karthikeyan
2017-10-01
The purpose of this study was to determine the influence of linear and rotational pre-cure bracket displacement during the bonding procedure on shear bond strength (SBS) of orthodontic brackets. Stainless steel orthodontic premolar brackets were bonded to the buccal surfaces of 50 human pre-molars with a conventional two-step bonding protocol. Extracted human pre-molars were divided into 5 groups (n=10/group). In the Control Group, the brackets were bonded with no pre-cure bracket displacement or rotation. The Rotation Group was bonded with 45 degrees of pre-cure rotation. The Displacement Group was bonded with 2mm pre-cure linear displacement. The Rotation-Displacement Group was bonded with pre-cure movements of 45º counter-clockwise rotation and 2mm displacement. The Slippage Group was bonded with 2mm each of mesial and distal pre-cure linear displacement. Photo-activation was carried out on the lateral sides of the bracket. Shear debonding force was measured, 24 hours after initial bonding, with an Instron universal testing machine using a knife-edged chisel. Data was analyzed using one-way ANOVA test. Adhesive Remnant Index (ARI) was scored under 15x magnification. The ARI data was analyzed using the Chi-square test ( p -value < 0.05). No statistically significant differences were detected among the control and experimental groups ( p = 0.331). The rotation and displacement group showed the highest mean SBS than all other groups. Mean SBS for all groups were above the clinically acceptable range. No statistically significant differences were detected in ARI scores among groups ( p = 0.071). Linear and rotational pre-cure bracket displacements do not appear to effect the shear bond strength of orthodontic brackets. Key words: Shear bond strength, orthodontic bracket, displacement, rotation, adhesive remnant index, pre-cure movement.
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Objective forensic analysis of striated, quasi-striated and impressed toolmarks
NASA Astrophysics Data System (ADS)
Spotts, Ryan E.
Following the 1993 Daubert v. Merrell Dow Pharmaceuticals, Inc. court case and continuing to the 2010 National Academy of Sciences report, comparative forensic toolmark examination has received many challenges to its admissibility in court cases and its scientific foundations. Many of these challenges deal with the subjective nature in determining whether toolmarks are identifiable. This questioning of current identification methods has created a demand for objective methods of identification - "objective" implying known error rates and statistically reliability. The demand for objective methods has resulted in research that created a statistical algorithm capable of comparing toolmarks to determine their statistical similarity, and thus the ability to separate matching and nonmatching toolmarks. This was expanded to the creation of virtual toolmarking (characterization of a tool to predict the toolmark it will create). The statistical algorithm, originally designed for two-dimensional striated toolmarks, had been successfully applied to striated screwdriver and quasi-striated plier toolmarks. Following this success, a blind study was conducted to validate the virtual toolmarking capability using striated screwdriver marks created at various angles of incidence. Work was also performed to optimize the statistical algorithm by implementing means to ensure the algorithm operations were constrained to logical comparison regions (e.g. the opposite ends of two toolmarks do not need to be compared because they do not coincide with each other). This work was performed on quasi-striated shear cut marks made with pliers - a previously tested, more difficult application of the statistical algorithm that could demonstrate the difference in results due to optimization. The final research conducted was performed with pseudostriated impression toolmarks made with chisels. Impression marks, which are more complex than striated marks, were analyzed using the algorithm to separate matching and nonmatching toolmarks. Results of the conducted research are presented as well as evidence of the primary assumption of forensic toolmark examination; all tools can create identifiably unique toolmarks.
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Shipitalo, Martin J; Malone, Robert W; Owens, Lloyd B
2008-01-01
Residual herbicides used in the production of soybean [Glycine max (L.) Merr] and corn (Zea mays L.) are often detected in surface runoff at concentrations exceeding their maximum contaminant levels (MCL) or health advisory levels (HAL). With the advent of transgenic, glyphosate-tolerant soybean and glufosinate-tolerant corn this concern might be reduced by replacing some of the residual herbicides with short half-life, strongly sorbed, contact herbicides. We applied both herbicide types to two chiseled and two no-till watersheds in a 2-yr corn-soybean rotation and at half rates to three disked watersheds in a 3-yr corn/soybean/wheat (Triticum aestivum L.)-red clover (Trifolium pratense L.) rotation and monitored herbicide losses in runoff water for four crop years. In soybean years, average glyphosate loss (0.07%) was approximately 1/7 that of metribuzin (0.48%) and about one-half that of alachlor (0.12%), residual herbicides it can replace. Maximum, annual, flow-weighted concentration of glyphosate (9.2 microg L(-1)) was well below its 700 microg L(-1) MCL and metribuzin (9.5 microg L(-1)) was well below its 200 microg L(-1) HAL, whereas alachlor (44.5 microg L(-1)) was well above its 2 microg L(-1) MCL. In corn years, average glufosinate loss (0.10%) was similar to losses of alachlor (0.07%) and linuron (0.15%), but about one-fourth that of atrazine (0.37%). Maximum, annual, flow-weighted concentration of glufosinate (no MCL) was 3.5 microg L(-1), whereas atrazine (31.5 microg L(-1)) and alachlor (9.8 microg L(-1)) substantially exceeded their MCLs of 3 and 2 microg L(-1), respectively. Regardless of tillage system, flow-weighted atrazine and alachlor concentrations exceeded their MCLs in at least one crop year. Replacing these herbicides with glyphosate and glufosinate can reduce the occurrence of dissolved herbicide concentrations in runoff exceeding drinking water standards.
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Tillage, Mulch and N Fertilizer Affect Emissions of CO2 under the Rain Fed Condition
Tanveer, Sikander Khan; Wen, Xiaoxia; Lu, Xing Li; Zhang, Junli; Liao, Yuncheng
2013-01-01
A two year (2010–2012) study was conducted to assess the effects of different agronomic management practices on the emissions of CO2 from a field of non-irrigated wheat planted on China's Loess Plateau. Management practices included four tillage methods i.e. T1: (chisel plow tillage), T2: (zero-tillage), T3: (rotary tillage) and T4: (mold board plow tillage), 2 mulch levels i.e., M0 (no corn residue mulch) and M1 (application of corn residue mulch) and 5 levels of N fertilizer (0, 80, 160, 240, 320 kg N/ha). A factorial experiment having a strip split-split arrangement, with tillage methods in the main plots, mulch levels in the sub plots and N-fertilizer levels in the sub-sub plots with three replicates, was used for this study. The CO2 data were recorded three times per week using a portable GXH-3010E1 gas analyzer. The highest CO2 emissions were recorded following rotary tillage, compared to the lowest emissions from the zero tillage planting method. The lowest emissions were recorded at the 160 kg N/ha, fertilizer level. Higher CO2 emissions were recorded during the cropping year 2010–11 relative to the year 2011–12. During cropping year 2010–11, applications of corn residue mulch significantly increased CO2 emissions in comparison to the non-mulched treatments, and during the year 2011–12, equal emissions were recorded for both types of mulch treatments. Higher CO2 emissions were recorded immediately after the tillage operations. Different environmental factors, i.e., rain, air temperatures, soil temperatures and soil moistures, had significant effects on the CO2 emissions. We conclude that conservation tillage practices, i.e., zero tillage, the use of corn residue mulch and optimum N fertilizer use, can reduce CO2 emissions, give better yields and provide environmentally friendly options. PMID:24086256
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High Strain Rate Testing of Welded DOP-26 Iridium
DOE Office of Scientific and Technical Information (OSTI.GOV)
Schneibel, J. H.; Miller, R. G.; Carmichael, C. A.
The iridium alloy DOP-26 is used to produce Clad Vent Set cups that protect the radioactive fuel in radioisotope thermoelectric generators (RTGs) which provide electric power for spacecraft and rovers. In a previous study, the tensile properties of DOP-26 were measured over a wide range of strain rates and temperatures and reported in ORNL/TM-2007/81. While that study established the properties of the base material, the fabrication of the heat sources requires welding, and the mechanical properties of welded DOP-26 have not been extensively characterized in the past. Therefore, this study was undertaken to determine the mechanical properties of DOP-26 specimensmore » containing a transverse weld in the center of their gage sections. Tensile tests were performed at room temperature, 750, 900, and 1090°C and engineering strain rates of 1×10 -3 and 10 s -1. Room temperature testing was performed in air, while testing at elevated temperatures was performed in a vacuum better than 1×10 -4 Torr. The welded specimens had a significantly higher yield stress, by up to a factor of ~2, than the non-welded base material. The yield stress did not depend on the strain rate except at 1090°C, where it was slightly higher for the faster strain rate. The ultimate tensile stress, on the other hand, was significantly higher for the faster strain rate at temperatures of 750°C and above. At 750°C and above, the specimens deformed at 1×10 -3 s -1 showed pronounced necking resulting sometimes in perfect chisel-edge fracture. The specimens deformed at 10 s -1 exhibited this fracture behavior only at the highest test temperature, 1090°C. Fracture occurred usually in the fusion zone of the weld and was, in most cases, primarily intergranular.« less
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Szleszkowski, Ł; Hałoń, A; Thannhäuser, A; Jurek, T
2015-01-01
Assessment of the usefulness of intravital lesions in the proximal attachment of the sternocleidomastoid muscle and the mastoid process of the temporal bone in medico-legal evaluation of death by hanging. The study material was obtained from the bodies of 35 people who died by hanging. The control group comprised specimens collected from 30 people who died of non-traumatic causes. The structures under study were examined macro- and microscopically. The basic change which could be recognized as a marker of intravitality of hanging was the presence of a macroscopically extensive blotchy area of abundant ecchymosis in the proximal muscle attachment, similar to that found in the distal attachment, and the presence of abundant diffuse intraosseous ecchymoses in the mastoid process. None of the cases revealed any ecchymoses in the proximal attachment of the muscle that would be similar to those present in the distal attachment. Discolourations within the mastoid processes, macroscopically suggestive of extensive intraosseous effusions arising from the mechanism of stretching, were not confirmed by microscopic evaluation and occurred at the same frequency as in the control group. Limitations of the study were related to the method which involved sample collection by means of bone chisels, decalcification and preparation of specimens, which had an effect, for example, on the measurable evaluation of the degree of congestion. The study has failed to provide convincing and unambiguous data on the usefulness of examining mastoid processes and proximal attachments of the sternocleidomastoid muscles during autopsy to determine the presence of intravitality features of hanging. A description of research methodology and its associated difficulties, e.g. with the interpretation of results, can also be useful for the planning of similar studies by other researchers.
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Rana, Majeed; Gellrich, Nils-Claudius; Rana, Madiha; Piffkó, Jozsef; Kater, Wolfgang
2013-02-17
Ultrasonic bone-cutting surgery has been introduced as a feasible alternative to the conventional sharp instruments used in craniomaxillofacial surgery because of its precision and safety. The piezosurgery medical device allows the efficient cutting of mineralized tissues with minimal trauma to soft tissues. Piezoelectric osteotome has found its role in surgically assisted rapid maxillary expansion (SARME), a procedure well established to correct transverse maxillary discrepancies. The advantages include minimal risk to critical anatomic structures. The purpose of this clinical comparative study (CIS 2007-237-M) was to present the advantages of the piezoelectric cut as a minimally invasive device in surgically assisted, rapid maxillary expansion by protecting the maxillary sinus mucosal lining. Thirty patients (18 females and 12 males) at the age of 18 to 54 underwent a surgically assisted palatal expansion of the maxilla with a combined orthodontic and surgical approach. The patients were randomly divided into two separate treatment groups. While Group 1 received conventional surgery using an oscillating saw, Group 2 was treated with piezosurgery. The following parameters were examined: blood pressure, blood values, required medication, bleeding level in the maxillary sinus, duration of inpatient stay, duration of surgery and height of body temperature. The results displayed no statistically significant differences between the two groups regarding laboratory blood values and inpatient stay. The duration of surgery revealed a significant discrepancy. Deploying piezosurgery took the surgeon an average of 10 minutes longer than working with a conventional-saw technique. However, the observation of the bleeding level in the paranasal sinus presented a major and statistically significant advantage of piezosurgery: on average the bleeding level was one category above the one of the remaining patients. This method of piezoelectric surgery with all its advantages is going to replace many conventional operating procedures in oral and maxillofacial surgery. CIS 2007-237-M.
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2013-01-01
Background Ultrasonic bone-cutting surgery has been introduced as a feasible alternative to the conventional sharp instruments used in craniomaxillofacial surgery because of its precision and safety. The piezosurgery medical device allows the efficient cutting of mineralized tissues with minimal trauma to soft tissues. Piezoelectric osteotome has found its role in surgically assisted rapid maxillary expansion (SARME), a procedure well established to correct transverse maxillary discrepancies. The advantages include minimal risk to critical anatomic structures. The purpose of this clinical comparative study (CIS 2007-237-M) was to present the advantages of the piezoelectric cut as a minimally invasive device in surgically assisted, rapid maxillary expansion by protecting the maxillary sinus mucosal lining. Methods Thirty patients (18 females and 12 males) at the age of 18 to 54 underwent a surgically assisted palatal expansion of the maxilla with a combined orthodontic and surgical approach. The patients were randomly divided into two separate treatment groups. While Group 1 received conventional surgery using an oscillating saw, Group 2 was treated with piezosurgery. The following parameters were examined: blood pressure, blood values, required medication, bleeding level in the maxillary sinus, duration of inpatient stay, duration of surgery and height of body temperature. Results The results displayed no statistically significant differences between the two groups regarding laboratory blood values and inpatient stay. The duration of surgery revealed a significant discrepancy. Deploying piezosurgery took the surgeon an average of 10 minutes longer than working with a conventional-saw technique. However, the observation of the bleeding level in the paranasal sinus presented a major and statistically significant advantage of piezosurgery: on average the bleeding level was one category above the one of the remaining patients. Conclusion This method of piezoelectric surgery with all its advantages is going to replace many conventional operating procedures in oral and maxillofacial surgery. Trial registration CIS 2007-237-M PMID:23414112
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Foldable Instrumented Bits for Ultrasonic/Sonic Penetrators
NASA Technical Reports Server (NTRS)
Bar-Cohen, Yoseph; Badescu, Mircea; Iskenderian, Theodore; Sherrit, Stewart; Bao, Xiaoqi; Linderman, Randel
2010-01-01
Long tool bits are undergoing development that can be stowed compactly until used as rock- or ground-penetrating probes actuated by ultrasonic/sonic mechanisms. These bits are designed to be folded or rolled into compact form for transport to exploration sites, where they are to be connected to their ultrasonic/ sonic actuation mechanisms and unfolded or unrolled to their full lengths for penetrating ground or rock to relatively large depths. These bits can be designed to acquire rock or soil samples and/or to be equipped with sensors for measuring properties of rock or soil in situ. These bits can also be designed to be withdrawn from the ground, restowed, and transported for reuse at different exploration sites. Apparatuses based on the concept of a probe actuated by an ultrasonic/sonic mechanism have been described in numerous prior NASA Tech Briefs articles, the most recent and relevant being "Ultrasonic/ Sonic Impacting Penetrators" (NPO-41666) NASA Tech Briefs, Vol. 32, No. 4 (April 2008), page 58. All of those apparatuses are variations on the basic theme of the earliest ones, denoted ultrasonic/sonic drill corers (USDCs). To recapitulate: An apparatus of this type includes a lightweight, low-power, piezoelectrically driven actuator in which ultrasonic and sonic vibrations are generated and coupled to a tool bit. The combination of ultrasonic and sonic vibrations gives rise to a hammering action (and a resulting chiseling action at the tip of the tool bit) that is more effective for drilling than is the microhammering action of ultrasonic vibrations alone. The hammering and chiseling actions are so effective that the size of the axial force needed to make the tool bit advance into soil, rock, or another material of interest is much smaller than in ordinary twist drilling, ordinary hammering, or ordinary steady pushing. Examples of properties that could be measured by use of an instrumented tool bit include electrical conductivity, permittivity, magnetic field, magnetic permeability, temperature, and any other properties that can be measured by fiber-optic sensors. The problem of instrumenting a probe of this type is simplified, relative to the problem of attaching electrodes in a rotating drill bit, in two ways: (1) Unlike a rotating drill bit, a bit of this type does not have flutes, which would compound the problem of ensuring contact between sensors and the side wall of a hole; and (2) there is no need for slip rings for electrical contact between sensor electronic circuitry and external circuitry because, unlike a rotating drill, a tool bit of this type is not rotated continuously during operation. One design for a tool bit of the present type is a segmented bit with a segmented, hinged support structure (see figure). The bit and its ultrasonic/sonic actuator are supported by a slider/guiding fixture, and its displacement and preload are controlled by a motor. For deployment from the folded configuration, a spring-loaded mechanism rotates the lower segment about the hinges, causing the lower segment to become axially aligned with the upper segment. A latching mechanism then locks the segments of the bit and the corresponding segments of the slider/guiding fixture. Then the entire resulting assembly is maneuvered into position for drilling into the ground. Another design provides for a bit comprising multiple tubular segments with an inner alignment string, similar to a foldable tent pole comprising multiple tubular segments with an inner elastic cable connecting the two ends. At the beginning of deployment, all segments except the first (lowermost) one remain folded, and the ultrasonic/sonic actuator is clamped to the top of the lowermost segment and used to drive this segment into the ground. When the first segment has penetrated to a specified depth, the second segment is connected to the upper end of the first segment to form a longer rigid tubular bit and the actuator is moved to the upper end of the second segnt. The process as described thus far is repeated, adding segments until the desired depth of penetration has been attained. Yet other designs provide for bits in the form of bistable circular- or rectangular- cross-section tubes that can be stowed compactly like rolls of flat tape and become rigidified upon extension to full length, in a manner partly similar to that of a common steel tape measure. Albeit not marketed for use in tool bits, a bistable reeled composite product that transforms itself from a flat coil to a rigid tube of circular cross section when unrolled, is commercially available under the trade name RolaTube(TradeMark) and serves as a model for the further development of tool bits of this subtype.
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Reducing temperature elevation of robotic bone drilling.
Feldmann, Arne; Wandel, Jasmin; Zysset, Philippe
2016-12-01
This research work aims at reducing temperature elevation of bone drilling. An extensive experimental study was conducted which focused on the investigation of three main measures to reduce the temperature elevation as used in industry: irrigation, interval drilling and drill bit designs. Different external irrigation rates (0 ml/min, 15 ml/min, 30 ml/min), continuously drilled interval lengths (2 mm, 1 mm, 0.5 mm) as well as two drill bit designs were tested. A custom single flute drill bit was designed with a higher rake angle and smaller chisel edge to generate less heat compared to a standard surgical drill bit. A new experimental setup was developed to measure drilling forces and torques as well as the 2D temperature field at any depth using a high resolution thermal camera. The results show that external irrigation is a main factor to reduce temperature elevation due not primarily to its effect on cooling but rather due to the prevention of drill bit clogging. During drilling, the build up of bone material in the drill bit flutes result in excessive temperatures due to an increase in thrust forces and torques. Drilling in intervals allows the removal of bone chips and cleaning of flutes when the drill bit is extracted as well as cooling of the bone in-between intervals which limits the accumulation of heat. However, reducing the length of the drilled interval was found only to be beneficial for temperature reduction using the newly designed drill bit due to the improved cutting geometry. To evaluate possible tissue damage caused by the generated heat increase, cumulative equivalent minutes (CEM43) were calculated and it was found that the combination of small interval length (0.5 mm), high irrigation rate (30 ml/min) and the newly designed drill bit was the only parameter combination which allowed drilling below the time-thermal threshold for tissue damage. In conclusion, an optimized drilling method has been found which might also enable drilling in more delicate procedures such as that performed during minimally invasive robotic cochlear implantation. Copyright © 2016 IPEM. Published by Elsevier Ltd. All rights reserved.
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Pilot task-based assessment of noise levels among firefighters.
Neitzel, Rl; Hong, O; Quinlan, P; Hulea, R
2013-11-01
Over one million American firefighters are routinely exposed to various occupational hazards agents. While efforts have been made to identify and reduce some causes of injuries and illnesses among firefighters, relatively little has been done to evaluate and understand occupational noise exposures in this group. The purpose of this pilot study was to apply a task-based noise exposure assessment methodology to firefighting operations to evaluate potential noise exposure sources, and to use collected task-based noise levels to create noise exposure estimates for evaluation of risk of noise-induced hearing loss by comparison to the 8-hr and 24-hr recommended exposure limits (RELs) for noise of 85 and 80.3 dBA, respectively. Task-based noise exposures (n=100 measurements) were measured in three different fire departments (a rural department in Southeast Michigan and suburban and urban departments in Northern California). These levels were then combined with time-at-task information collected from firefighters to estimate 8-hr noise exposures for the rural and suburban fire departments (n=6 estimates for each department). Data from 24-hr dosimetry measurements and crude self-reported activity categories from the urban fire department (n=4 measurements) were used to create 24-hr exposure estimates to evaluate the bias associated with the task-based estimates. Task-based noise levels were found to range from 82-109 dBA, with the highest levels resulting from use of saws and pneumatic chisels. Some short (e.g., 30 min) sequences of common tasks were found to result in nearly an entire allowable daily exposure. The majority of estimated 8-hr and 24-hr exposures exceeded the relevant recommended exposure limit. Predicted 24-hr exposures showed substantial imprecision in some cases, suggesting the need for increased task specificity. The results indicate potential for overexposure to noise from a variety of firefighting tasks and equipment, and suggest a need for further exposure characterization and additional hearing loss prevention efforts. Firefighters may be at risk of noise-induced hearing loss, which can affect their fitness for duty and ability to respond effectively to emergencies. The results of this study suggest that additional efforts at hearing loss prevention among firefighters are warranted.
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Paruchuri, Yasaswi; Siuniak, Amanda; Johnson, Nicole; Levin, Elena; Mitchell, Katherine; Goodrich, Jaclyn M; Renne, Elisha P; Basu, Niladri
2010-11-15
Mercury use in small-scale gold mining is ubiquitous across Ghana but little is known about the extent to which such activities have contaminated community residents and miners. Here, occupational exposures to elemental mercury (via urine sampling) and dietary exposures to methylmercury (via hair sampling) were assessed among 120 participants recruited from a mining community located in the Talensi-Nabdam District of Ghana's Upper East region during summer 2009. More than one-fifth of the participants had moderately high levels of urinary mercury (>10μg/L) and 5% had urine mercury levels that exceeded the WHO guideline value of 50μg/L. When participants were stratified according to occupation, those active in the mining industry had the highest mercury levels. Specifically, individuals that burned amalgam had urine mercury levels (median: 43.8μg/L; mean ± SD: 171.1±296.5μg/L; n=5) significantly higher than median values measured in mechanical operators (11.6μg/L, n=4), concession managers/owners (5.6μg/L, n=11), excavators that blast and chisel ore (4.9μg/L, n=33), individuals that sift and grind crushed ore (2.2μg/L, n=47), support workers (0.5μg/L, n=14), and those with no role in the mining sector (2.5μg/L, n=6). There was a significant positive Spearman correlation between fish consumption and hair mercury levels (r=0.30) but not with urine mercury (r=0.18) though further studies are needed to document which types of fish are consumed as well as portion sizes. Given that 200,000 people in Ghana are involved in the small-scale gold mining industry and that the numbers are expected to grow in Ghana and many other regions of the world, elucidating mercury exposure pathways in such communities is important to help shape policies and behaviors that may minimize health risks. Copyright © 2010 Elsevier B.V. All rights reserved.
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Archaeometallurgical investigation of the iron anchor from the Tantura F shipwreck
DOE Office of Scientific and Technical Information (OSTI.GOV)
Aronson, A.; Ashkenazi, D., E-mail: dana@eng.tau.ac.il; Barkai, O.
2013-04-15
The Tantura F shipwreck was a coaster or a fishing vessel about 15.7 m long, discovered in the Dor/Tantura lagoon, Israel in 1995. It was dated to between the mid-7th and the end of the 8th centuries CE. Among the finds excavated were two T-shaped type iron anchors. Of the two anchors, one (anchor A) was thoroughly studied by archaeometallurgical methods in order to identify forge-welding lines, to determine the welding quality and to understand the manufacturing technology. The examinations included X-ray radiography, XRF analysis, optical microscopy, SEM/EDS observation and analysis, OES analysis and microhardness tests. The investigation included characterizationmore » of the composition, microstructure, thermal treatments, forge-welding junctions and slag analysis. The results revealed a heterogeneous microstructure, rich in glassy, fayalite and wüstite slag. Iron based phases included ferrite, pearlite, cementite and Widmanstätten plates, all typical to wrought iron. The forge-welds of Anchor A were located. Each arm was made of one piece, weighing about 2.5–3 kg and the shank was made of a few 1.5–2 kg pieces. The second anchor (anchor B) was only briefly examined visually and with a few radiographs, which support the results from anchor A. The research results revealed significant information about T-shaped anchors and their manufacturing process, including hot-working processes without any additional heat treatments, and folding techniques. The microstructure was similar to other ancient simple tools such as saws, sickles, axes and mortise chisels, and though the technology to make complicated structures and objects, such as swords, existed at that time, the anchors did not require this sophistication; thus simpler techniques were used, presumably because they were more cost-effective. - Highlights: ► Tantura F was a coaster dated to mid-7th–end-8th centuries. ► Two iron anchors were discovered at the Tantura F shipwreck-site. ► Anchor A was manufactured from heterogeneous wrought iron blooms. ► Forge-welding lines were detected using archaeometallurgical methods.« less
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Shear Bond Strength of Ceramic Brackets with Different Base Designs: Comparative In-vitro Study
Ansari, Mohd. Younus; Agarwal, Deepak K; Bhattacharya, Preeti; Ansar, Juhi; Bhandari, Ravi
2016-01-01
Introduction Knowledge about the Shear Bond Strength (SBS) of ceramic brackets with different base design is essential as it affects bond strength to enamel. Aim The aim of the present study was to evaluate and compare the effect of base designs of different ceramic brackets on SBS, and to determine the fracture site after debonding. Materials and Methods Four groups of ceramic brackets and one group of metal brackets with different base designs were used. Adhesive precoated base of Clarity Advanced (APC Flash-free) (Unitek/3M, Monrovia, California), microcrystalline base of Clarity Advanced (Unitek/3M, Monrovia, California), polymer mesh base of InVu (TP Orthodontics, Inc., La Porte, IN, United States), patented bead ball base of Inspire Ice (Ormco, Glendora, California), and a mechanical mesh base of Gemini Metal bracket (Unitek/3M, Monrovia, California). Ten brackets of each type were bonded to 50 maxillary premolars with Transbond XT (Unitek/3M). Samples were stored in distilled water at room temperature for 24 hours and subsequently tested in shear mode on a universal testing machine (Model 3382; Instron Corp., Canton, Massachusetts, USA) at a cross head speed of 1mm/minute with the help of a chisel. The debonded interface was recorded and analyzed to determine the predominant bond failure site under an optical microscope (Stereomicroscope) at 10X magnification. One way analysis of variance (ANOVA) was used to compare SBS. Tukey’s significant differences tests were used for post-hoc comparisons. The Adhesive Remnant Index (ARI) scores were compared by chi-square test. Results Mean SBS of microcrystalline base (27.26±1.73), was the highest followed by bead ball base (23.45±5.09), adhesive precoated base (20.13±5.20), polymer mesh base (17.54±1.91), and mechanical mesh base (17.50±2.41) the least. Comparing the frequency (%) of ARI Score among the groups, chi-square test showed significantly different ARI scores among the groups (χ2 = 34.07, p<0.001). Conclusion Different base designs of metal and ceramic brackets influence SBS to enamel and all were clinically acceptable. PMID:28050507
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NASA Astrophysics Data System (ADS)
Moraru, P. I.; Rusu, T.
2012-04-01
Soil respiration leads to CO2 emissions from soil to the atmosphere, in significant amounts for the global carbon cycle. Soil capacity to produce CO2 varies depending on soil, season, intensity and quality of agrotechnical tillage, soil water, cultivated plant, fertilizer etc. The data presented in this paper were obtained on argic-stagnic Faeoziom (SRTS, 2003). These areas were was our research, presents a medium multiannual temperature of 8.20C, medium of multiannual rain drowns: 613 mm. The experimental variants chosen were: A. Conventional system (CS): V1-reversible plough (22-25 cm)+rotary grape (8-10 cm); B. Minimum tillage system (MT): V2 - paraplow (18-22 cm) + rotary grape (8-10 cm); V3 - chisel (18-22 cm) + rotary grape (8-10 cm);V4 - rotary grape (10-12 cm); C. No-Tillage systems (NT): V5 - direct sowing. The experimental design was a split-plot design with three replications. In one variant the area of a plot was 300 m2. The experimental variants were studied in the 3 years crop rotation: maize - soy-bean - autumn wheat. To soil respiration under different tillage practices, determinations were made for each crop in four vegetative stages (spring, 5-6 leaves, bean forming, harvest) using ACE Automated Soil CO2 Exchange System. Soil respiration varies throughout the year for all three crops of rotation, with a maximum in late spring (1383 to 2480 mmoli m-2s-1) and another in fall (2141 to 2350 mmoli m-2s-1). The determinations confirm the effect of soil tillage system on soil respiration, the daily average is lower at NT (315-1914 mmoli m-2s-1), followed by MT (318-2395 mmoli m-2s-1) and is higher in the CS (321-2480 mmol m-2s-1). Productions obtained at MT and NT don't have significant differences at wheat and are higher at soybean. The differences in crop yields are recorded at maize and can be a direct consequence of loosening, mineralization and intensive mobilization of soil fertility. Acknowledgments: This work was supported by CNCSIS-UEFISCSU, project number PN II-RU 273/2010.
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DOE Office of Scientific and Technical Information (OSTI.GOV)
Srinivasan, Sriram Goverapet; Shivaramaiah, Radha; Kent, Paul R. C.
2016-07-11
Bastnasite is a fluoro-carbonate mineral that is the largest source of rare earth elements such as Y, La and Ce. With increasing demand for REE in many emerging technologies, there is an urgent need for improving the efficiency of ore beneficiation by froth flotation. In order to design improved flotation agents that can selectively bind to the mineral surface, a fundamental understanding of the bulk and surface properties of bastnasite is essential. Density functional theory calculations using the PBEsol exchange correlation functional and the DFT-D3 dispersion correction reveal that the most stable form of La bastnsite is isomorphic to themore » structure of Ce bastnasite belonging to the P2c space group, while the Inorganic Crystal Structure Database structure in the P2m space group is ca. 11.3 kJ/mol higher in energy per LaFCO 3 formula unit. We report powder X-ray diffraction measurements on synthetic of La bastnasite to support these theoretical findings. Six different surfaces are studied by DFT, namely [100], [0001], [101], [102], [104] and [112]. Among these, the [100] surface is the most stable with a surface energy of 0.73 J/m 2 in vacuum and 0.45 J/m 2 in aqueous solution. We predicted the shape of a La bastnasite nanoparticle via thermodynamic Wulff construction to be a hexagonal prism with [100] and [0001] facets, chiseled at its ends by the [101] and [102] facets. The average surface energy of the nanoparticle in the gas phase is estimated to be 0.86 J/m 2, in good agreement with a value of 1.11 J/m 2 measured by calorimetry. The calculated adsorption energy of a water molecule varies widely with the surface plane and specific adsorption sites on a given surface. Moreover, the first layer of water molecules is predicted to adsorb strongly on the La-bastnasite surface, in agreement with water adsorption calorimetry experiments. Our work provides an important step towards a detailed atomistic understanding of the bastnasite water interface and designing collector molecules that can bind specifically to bastnasite.« less
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FY 2016 Status Report: CIRFT Testing Data Analyses and Updated Curvature Measurements
DOE Office of Scientific and Technical Information (OSTI.GOV)
Wang, Jy-An John; Wang, Hong
This report provides a detailed description of FY15 test result corrections/analysis based on the FY16 Cyclic Integrated Reversible-Bending Fatigue Tester (CIRFT) test program methodology update used to evaluate the vibration integrity of spent nuclear fuel (SNF) under normal transportation conditions. The CIRFT consists of a U-frame testing setup and a real-time curvature measurement method. The three-component U-frame setup of the CIRFT has two rigid arms and linkages to a universal testing machine. The curvature of rod bending is obtained through a three-point deflection measurement method. Three linear variable differential transformers (LVDTs) are used and clamped to the side connecting platesmore » of the U-frame to capture the deformation of the rod. The contact-based measurement, or three-LVDT-based curvature measurement system, on SNF rods has been proven to be quite reliable in CIRFT testing. However, how the LVDT head contacts the SNF rod may have a significant effect on the curvature measurement, depending on the magnitude and direction of rod curvature. It has been demonstrated that the contact/curvature issues can be corrected by using a correction on the sensor spacing. The sensor spacing defines the separation of the three LVDT probes and is a critical quantity in calculating the rod curvature once the deflections are obtained. The sensor spacing correction can be determined by using chisel-type probes. The method has been critically examined this year and has been shown to be difficult to implement in a hot cell environment, and thus cannot be implemented effectively. A correction based on the proposed equivalent gauge-length has the required flexibility and accuracy and can be appropriately used as a correction factor. The correction method based on the equivalent gauge length has been successfully demonstrated in CIRFT data analysis for the dynamic tests conducted on Limerick (LMK) (17 tests), North Anna (NA) (6 tests), and Catawba mixed oxide (MOX) (10 tests) SNF samples. These CIRFT tests were completed in FY14 and FY15. Specifically, the data sets obtained from measurement and monitoring were processed and analyzed. The fatigue life of rods has been characterized in terms of moment, curvature, and equivalent stress and strain..« less
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NASA Astrophysics Data System (ADS)
Rusu, Dr.; Gus, Dr.; Bogdan, Dr.; Moraru, Dr.; Pop, Dr.; Clapa, Dr.; Pop, Drd.
2009-04-01
The energetic function of the soil expressed through the potential energy accumulated through humus, the biogeochemical function (the circuit of the nutrient elements) are significantly influenced by its hydrophysical function and especially by the state of the bedding- consolidation, soil capacity of retaining an optimal quantity of water, and then its gradual disponibility for plant consumption. The understanding of soil functions and management including nutrient production, stocking, filtering and transforming minerals, water , organic matter , gas circuit and furnishing breeding material, all make the basis of human activity, Earth's past, present and especially future. The minimum tillage soil systems - paraplow, chisel or rotary grape - are polyvalent alternatives for basic preparation, germination bed preparation and sowing, for fields and crops with moderate loose requirements being optimized technologies for: soil natural fertility activation and rationalization, reduction of erosion, increasing the accumulation capacity for water and realization of sowing in the optimal period. By continuously applying for 10 years the minimum tillage system in a crop rotation: corn - soy-bean - wheat - potato / rape, an improvement in physical, hydro-physical and biological properties of soil was observed, together with the rebuilt of structure and increase of water permeability of soil. The minimum tillage systems ensure an adequate aerial-hydrical regime for the biological activity intensity and for the nutrients solubility equilibrium. The vegetal material remaining at the soil surface or superficially incorporated has its contribution to intensifying the biological activity, being an important resource of organic matter. The minimum tillage systems rebuild the soil structure, improving the global drainage of soil which allows a rapid infiltration of water in soil. The result is a more productive soil, better protected against wind and water erosion and needing less fuel for preparing the germination bed. Presently it is necessary a change concerning the concept of conservation practices and a new approach regarding the control of erosion. The real conservation of soil must be expanded beyond the traditional understanding of soil erosion. The real soil conservation is represented by carbon management. We need to focus to another level concerning conservation by focusing on of soil quality. Carbon management is necessary for a complex of matters including soil, water management, field productivity, biological fuel and climatic change. Profound research is necessary in order to establish the carbon sequestration practices and their implementation impact.
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NASA Astrophysics Data System (ADS)
Rusu, T.; Gus, P.; Bogdan, I.; Moraru, P.; Pop, A.; Clapa, D.; Pop, L.
2009-04-01
The energetic function of the soil expressed through the potential energy accumulated through humus, the biogeochemical function (the circuit of the nutrient elements) are significantly influenced by its hydrophysical function and especially by the state of the bedding- consolidation, soil capacity of retaining an optimal quantity of water, and then its gradual disponibility for plant consumption. The understanding of soil functions and management including nutrient production, stocking, filtering and transforming minerals, water , organic matter, gas circuit and furnishing breeding material, all make the basis of human activity, Earth's past, present and especially future. The minimum tillage soil systems - paraplow, chisel or rotary grape - are polyvalent alternatives for basic preparation, germination bed preparation and sowing, for fields and crops with moderate loose requirements being optimized technologies for: soil natural fertility activation and rationalization, reduction of erosion, increasing the accumulation capacity for water and realization of sowing in the optimal period. By continuously applying for 10 years the minimum tillage system in a crop rotation: corn - soy-bean - wheat - potato / rape, an improvement in physical, hydro-physical and biological properties of soil was observed, together with the rebuilt of structure and increase of water permeability of soil. The minimum tillage systems ensure an adequate aerial-hydrical regime for the biological activity intensity and for the nutrients solubility equilibrium. The vegetal material remaining at the soil surface or superficially incorporated has its contribution to intensifying the biological activity, being an important resource of organic matter. The minimum tillage systems rebuild the soil structure, improving the global drainage of soil which allows a rapid infiltration of water in soil. The result is a more productive soil, better protected against wind and water erosion and needing less fuel for preparing the germination bed. Presently it is necessary a change concerning the concept of conservation practices and a new approach regarding the control of erosion. The real conservation of soil must be expanded beyond the traditional understanding of soil erosion. The real soil conservation is represented by carbon management. We need to focus to another level concerning conservation by focusing on of soil quality. Carbon management is necessary for a complex of matters including soil, water management, field productivity, biological fuel and climatic change.
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Handling Heavenly Jewels - 35 Years of Antarctic Meteorite Processing at Johnson Space Center
NASA Technical Reports Server (NTRS)
Satterwhite, C. E.; McBridge, K. M.; Harrington, R.; Schwarz, C. M.
2011-01-01
The ANSMET program began in 1976, and since that time more than 18,000 meteorites have been processed in the Meteorite Processing Lab at Johnson Space Center in Houston, TX[1]. The meteorites are collected and returned to JSC on a freezer truck and remain frozen until they are initially processed. Initial Processing of Meteorites: Initial processing involves drying the meteorites in a nitrogen glove box for 24 to 48 hours, photographing, measuring, weighing and writing a description of the interior and exterior. The meteorite is broken and a representative sample is sent to the Smithsonian Institution for classification. Newsletter & Requests: Once initial processing has been complete and the meteorites have been classified, the information is published in the Antarctic Meteorite Newsletter[2,3]. The newsletter is published twice yearly and is sent electronically to researchers around the world and is also available on line. Researchers are asked to fill out a request form and submit it to the Meteorite Working Group secretary. All sample requests will be reviewed by either the meteorite curator or the Meteorite Working Group de-pending on the type of meteorite and the research being conducted. Processing for Sample Requests: In the meteorite processing lab, meteorite samples are prepared several different ways. Most samples are prepared as chips obtained by use of stainless steel chisels in a chipping bowl or rock splitter. In special situations where a researcher needs a slab the meteorite samples can be bandsawed in a dry nitrogen glove box with a diamond blade, no liquids are ever introduced into the cabinet. The last type of sample preparation is thin/thick sections. The meteorite thin section lab at JSC can prepare standard 30-micron thin sections, thick sections of variable thickness (100 to 200 microns), or demountable sections using superglue. Information for researchers: It is important that re-searchers fill the sample request form completely, in order to make sure the meteorite is processed correctly[4]. Re-searchers should list any special requirements on the form, i.e. packaging of samples (poly vs. stainless), thick sections and thickness needed, superglue needed, interior chips, exterior chips, fusion crust, contamination issues, all concerns should be listed so processing can be done accurately and any concerns the researcher has can be addressed be-fore the meteorites are broken.
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Effect of Jig Design and Assessment of Stress Distribution in Testing Metal-Ceramic Adhesion.
Özcan, Mutlu; Kojima, Alberto Noriyuki; Nishioka, Renato Sussumu; Mesquita, Alfredo Mikail Melo; Bottino, Marco Antonio; Filho, Gilberto Duarte
2016-12-01
In testing adhesion using shear bond test, a combination of shear and tensile forces occur at the interface, resulting in complex stresses. The jig designs used for this kind of test show variations in published studies, complicating direct comparison between studies. This study evaluated the effect of different jig designs on metal-ceramic bond strength and assessed the stress distribution at the interface using finite element analysis (FEA). Metal-ceramic (Metal: Ni-Cr, Wiron 99, Bego; Ceramic: Vita Omega 900, Vita) specimens (N = 36) (diameter: 4 mm, veneer thickness: 4 mm; base diameter: 5 mm, thickness: 1 mm) were fabricated and randomly divided into three groups (n = 12 per group) to be tested using one of the following jig designs: (a) chisel (CH) (ISO 11405), (b) steel strip (SS), (c) piston (PI). Metal-ceramic interfaces were loaded under shear until debonding in a universal testing machine (0.5 mm/min). Failure types were evaluated using scanning electron microscopy (SEM). FEA was used to study the stress distribution using different jigs. Metal-ceramic bond strength data (MPa) were analyzed using ANOVA and Tukey's tests (α = 0.05). The jig type significantly affected the bond results (p = 0.0001). PI type of jig presented the highest results (MPa) (p < 0.05) (58.2 ± 14.8), followed by CH (38.7 ± 7.6) and SS jig type (23.3 ± 4.2) (p < 0.05). Failure types were exclusively a combination of cohesive failure in the opaque ceramic and adhesive interface failure. FEA analysis indicated that the SS jig presented slightly more stress formation than with the CH jig. The PI jig presented small stress concentration with more homogeneous force distribution compared to the CH jig where the stress concentrated in the area where the force was applied. Metal-ceramic bond strength was affected by the jig design. Accordingly, the results of in vitro studies on metal-ceramic adhesion should be evaluated with caution. When adhesion of ceramic materials to metals is evaluated in in vitro studies, it should be noted that the loading jig type affects the results. Clinical observations should report on the location and type of ceramic fractures in metal-ceramic reconstructions so that the most relevant test method can be identified. © 2015 by the American College of Prosthodontists.
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Guo, Zhao-zhong; Zhang, Heng; Li, Yan; Li, Xin; Liu, Yin; Wang, Yang; Yuan, Chun-xia; Liu, Xue
2012-04-01
To investigate complications in extraction of complicated impacted wisdom teeth whose root apex near to the inferior alveolar nerve(IAN) by using routine method(chisels),high speed turbine handpiece and piezosurgery device respectively. Three hundred qualified patients with impacted wisdom teeth were divided into three groups randomly,one hundred patients in group A were extracted by routine method, one hundred patients in group B were extracted by high speed turbine handpiece, and one hundred patients in group C were extracted by piezosurgery device. The operation time, postoperative pain duration,dry socket and IAN injury were compared between each two groups. All statistical analysis was performed using SPSS 13.0 software package. Differences between groups were compared using a paired t test (quantitative data) or Chi-square test (qualitative data). The operation time in group A was(14.12±0.12)min, (7.22±0.15)min in group B, (25.23±0.32)min in group C; Significant difference was found between group A and group B(P<0.05), group B and group C(P<0.05),group A and group C(P<0.05).Postoperative pain duration was(62.15±1.51)h in group A, (48.23±1.23)h in group B, (14.34±O.80)h in group C; Significant difference was found between group A and group B(P<0.05), group B and group C(P<0.05),group A and group C(P<0.05).9 patients developed dry socket in group A, 2 in group B, and 1 in group C; Significant difference was found between group A and group B(P<0.05), group A and group C(P<0.05). Six patients had IAN injury in group A, 2 in group B, 0 in group C. Significant difference was found between group A and group C. Compared with routine method, high speed turbine is better in extraction of impacted wisdom teeth, which can shorten operation time, lessen postoperative complications. Although there was longer operation time compared with group A and B, piezosurgery device is more effective in reducing postoperative complications.
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φq-field theory for portfolio optimization: “fat tails” and nonlinear correlations
NASA Astrophysics Data System (ADS)
Sornette, D.; Simonetti, P.; Andersen, J. V.
2000-08-01
Physics and finance are both fundamentally based on the theory of random walks (and their generalizations to higher dimensions) and on the collective behavior of large numbers of correlated variables. The archetype examplifying this situation in finance is the portfolio optimization problem in which one desires to diversify on a set of possibly dependent assets to optimize the return and minimize the risks. The standard mean-variance solution introduced by Markovitz and its subsequent developments is basically a mean-field Gaussian solution. It has severe limitations for practical applications due to the strongly non-Gaussian structure of distributions and the nonlinear dependence between assets. Here, we present in details a general analytical characterization of the distribution of returns for a portfolio constituted of assets whose returns are described by an arbitrary joint multivariate distribution. In this goal, we introduce a non-linear transformation that maps the returns onto Gaussian variables whose covariance matrix provides a new measure of dependence between the non-normal returns, generalizing the covariance matrix into a nonlinear covariance matrix. This nonlinear covariance matrix is chiseled to the specific fat tail structure of the underlying marginal distributions, thus ensuring stability and good conditioning. The portfolio distribution is then obtained as the solution of a mapping to a so-called φq field theory in particle physics, of which we offer an extensive treatment using Feynman diagrammatic techniques and large deviation theory, that we illustrate in details for multivariate Weibull distributions. The interaction (non-mean field) structure in this field theory is a direct consequence of the non-Gaussian nature of the distribution of asset price returns. We find that minimizing the portfolio variance (i.e. the relatively “small” risks) may often increase the large risks, as measured by higher normalized cumulants. Extensive empirical tests are presented on the foreign exchange market that validate satisfactorily the theory. For “fat tail” distributions, we show that an adequate prediction of the risks of a portfolio relies much more on the correct description of the tail structure rather than on their correlations. For the case of asymmetric return distributions, our theory allows us to generalize the return-risk efficient frontier concept to incorporate the dimensions of large risks embedded in the tail of the asset distributions. We demonstrate that it is often possible to increase the portfolio return while decreasing the large risks as quantified by the fourth and higher-order cumulants. Exact theoretical formulas are validated by empirical tests.
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Single Piezo-Actuator Rotary-Hammering Drill
NASA Technical Reports Server (NTRS)
Sherrit, Stewart; Bao, Xiaoqi; Badescu, Mircea; Bar-Cohen, Yoseph
2011-01-01
This innovation comprises a compact drill that uses low-axial preload, via vibrations, that fractures the rock under the bit kerf, and rotates the bit to remove the powdered cuttings while augmenting the rock fracture via shear forces. The vibrations fluidize the powered cuttings inside the flutes around the bit, reducing the friction with the auger surface. These combined actions reduce the consumed power and the heating of the drilled medium, helping to preserve the pristine content of the produced samples. The drill consists of an actuator that simultaneously impacts and rotates the bit by applying force and torque via a single piezoelectric stack actuator without the need for a gearbox or lever mechanism. This reduces the development/fabrication cost and complexity. The piezoelectric actuator impacts the surface and generates shear forces, fragmenting the drilled medium directly under the bit kerf by exceeding the tensile and/or shear strength of the struck surface. The percussive impact action of the actuator leads to penetration of the medium by producing a zone of finely crushed rock directly underneath the struck location. This fracturing process is highly enhanced by the shear forces from the rotation and twisting action. To remove the formed cuttings, the bit is constructed with an auger on its internal or external surface. One of the problems with pure hammering is that, as the teeth become embedded in the sample, the drilling efficiency drops unless the teeth are moved away from the specific footprint location. By rotating the teeth, they are moved to areas that were not fragmented, and thus the rock fracturing is enhanced via shear forces. The shear motion creates ripping or chiseling action to produce larger fragments to increase the drilling efficiency, and to reduce the required power. The actuator of the drill consists of a piezoelectric stack that vibrates the horn. The stack is compressed by a bolt between the backing and the horn in order to prevent it from being subjected to tensile stress that will cause it to fail. The backing is intended to transfer the generated mechanical vibrations towards the horn. In order to cause rotation, the horn is configured asymmetrically with helical segments and, upon impacting the bit, it introduces longitudinal along the axis of the actuator and tangential force causing twisting action that rotates the bit. The longitudinal component of the vibrations of the stack introduces percussion impulses between the bit and the rock to fracture it when the ultimate strain is exceeded under the bit.
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NASA Astrophysics Data System (ADS)
Surböck, Andreas; Gollner, Gabriele; Klik, Andreas; Freyer, Bernhard; Friedel, Jürgen K.
2017-04-01
A continuous investment in soil fertility is necessary to achieve sustainable yields in organic arable farming. Crucial factors here besides the crop rotation are organic fertilization and the soil tillage system. On this topic, an operational group (Project BIOBO*) was established in the frame of an European Innovation Partnership in 2016 consisting of organic farmers, consultants and scientists in the farming region of eastern Austria. The aim of this group is the development and testing of innovative, reduced soil cultivation, green manure and organic fertilization systems under on-farm and on-station conditions to facilitate the sharing and transfer of experience and knowledge within and outside the group. Possibilities for optimization of the farm-specific reduced soil tillage system in combination with green manuring are being studied in field trials on six organic farms. The aim is to determine, how these measures contribute to an increase in soil organic matter contents, yields and income, to an improved nitrogen and nutrient supply to the crops, as well as support soil fertility in general. Within a long-term monitoring project (MUBIL), the effects of different organic fertilization systems on plant and soil traits have been investigated since 2003, when the farm was converted to organic management. The examined organic fertilization systems, i.e. four treatments representing stockless and livestock keeping systems, differ in lucerne management and the supply of organic manure (communal compost, farmyard manure, digestate from a biogas plant). Previous results of this on-station experiment have shown an improvement of some soil properties, especially soil physical properties, since 2003 in all fertilization systems and without differences between them. The infiltration rate of rainwater has increased because of higher hydraulic conductivity. The aggregate stability has shown also positive trends, which reduces the susceptibility to soil erosion by wind and water. The improvements are attributed to the crop rotation with two-year lucerne and other crops with a dense root system. In autumn 2015, the soil tillage in the trial was converted from an intensive use of the plough to a reduced tillage system with a chisel. With this change, further improvements in soil properties, especially in connection with organic fertilizers, are expected and are further examined. Plots in which the previous tillage with the plough is continued, allow a comparison of the effects of the different soil tillage systems. * The project BIOBO is supported by the Austrian Federal Government, Austrian Federal Provinces and the European Union.
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NASA Astrophysics Data System (ADS)
Kuhwald, Michael; Augustin, Katja; Duttmann, Rainer
2017-04-01
The positive effects of reduced tillage on soil stability and on various soil functions such as infiltrability or saturated hydraulic conductivity are known in general. However, long-term employment of conservation tillage can increase weed pressure, damage by mice and soil compaction. Thus, the application of one-time inversion tillage (occasional or strategic tillage) is customarily used as a method for overcoming these drawbacks. Hitherto, the effects of one-time inversion tillage on soil physical properties have not been investigated. This study focuses on analysing whether the improved soil physical properties derived by long-term reduced tillage remain after one-time inversion tillage by mouldboard plough. The study was carried out in a 5.5 ha field in the southern part of Lower Saxony, Germany. Since 1996, this field has been subdivided into three plots, one managed conventionally by using a mouldboard plough (CT), while in the others a chisel plough (RT1) and a disk harrow (RT2) were employed. In October 2014, the entire field was ploughed by mouldboard plough to a depth of 30 cm. During the following year, four field studies were conducted to analyse the effects of this one-time inversion tillage on volumetric soil water content, bulk density, saturated hydraulic conductivity and infiltration rate. Additionally, penetration resistance measurements taken across the entire field were interpolated by kriging to analyse the spatial distribution of soil characteristics. The surveys of RT1 and RT2 were compared with CT and with analyses conducted before the one-time inversion tillage. This study shows that positive effects of long-term conservation tillage on several soil physical characteristics still remain after one-time mouldboard ploughing. Throughout the entire cropping season, the topsoil tilled under former conservation tillage practices revealed significantly higher (p < 0.05) values of saturated hydraulic conductivities and infiltration rates compared to the plot that experienced continuously conventional tillage. Moreover, field-wide measuring of penetration resistance indicated the removal of the compaction zone developed under conservation tillage in soil depths between 10 and 20 cm. After mouldboard ploughing, penetration resistance in the topsoil was significantly (p < 0.05) reduced in both plots, showing the same order of magnitude as measured in the conventionally managed plot. The results of this study suggest that one-time inversion tillage with a mouldboard plough offers a suitable management option for overcoming some of the main disadvantages associated with long-term conservation tillage, while conserving the improved soil physical properties and functions.
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Kumar, Pawan; Prasad, Narayana; Darawade, Ashish; Bhagat, Shresht Kumar; Narayana, Narayana; Darawade, Pradyma
2015-09-01
The objective of this study was to compare the efficiency of four commonly used chemicals in their ability to remove smear layer after instrumentation using scanning electron microscope (SEM). Seventy-five extracted single canaled teeth of roots ranging 10-12 mm in length were used for the study. Teeth were divided into 4 study groups and 1 control group of 15 teeth each. Standard access to the pulp chambers were performed with diamond burs. The lengths of the teeth were determined by the introduction of a size 15 K-file into the root canal until the tip reached the apical foramen. The working length for preparation of the canal is set 0.5 mm shorter than the measurement. Irrigation was performed using 2 ml of irrigant for every instrument change and finally rinsed using 5 ml of the respective solutions. The roots were then split with a chisel and hammer. One-half of each tooth was selected and prepared for SEM examination. After assembly on coded stubs, the specimens were placed in a vacuum chamber and sputter-coated with a 300 Å gold layer. The specimens were then analyzed using a Philips SEM XL 30. The dentinal wall of the cervical, middle and apical thirds was observed at magnifications of up to ×1000 for the presence/absence of smear layer and visualization of the entrance to dentinal tubules. Photomicrographs (×1000) of these areas on each of the coronal, middle and apical thirds were made Data were analyzed using Kruskal-Wallis test and Mann-Whitney U test. SEM study done on these prepared teeth with the popularly used four chemicals, namely, 3% NaOCl (Group A), 3% NaOCl followed by 17% ethylene diamine-tetra-acetic acid (Group B), 0.2% chlorhexidine (Group C) and 3% NaOCl followed by MTAD (Group D), with distilled water (Group E) which is used as control, revealed that NaOCl showed statistically significant, better cleansing effect than distilled water. Chlorhexidine and NaOCl showed equal kind of efficacy but were statistically significant, with lower efficacy than MTAD. It may be concluded that MTAD appears to be the most effective solution compared to the rest. The study demonstrated that MTAD as a final rinse after the entire instrumentation with 3% NaOCl as irrigant provided the best cleansing in all parts of the root canal system. The smear layer has been shown to hinder the penetration of intracanal disinfectants and sealers into dentinal tubules and has the potential of compromising the seal of the root filling. Degradation of the smear layer after treatment may contribute to leakage and reinfection of the root canal space. Removal of the smear layer reduced the penetration of bacteria through the root canal system after root filling.
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NASA Technical Reports Server (NTRS)
2002-01-01
Rich in antiquities and picturesque landscapes, the island provinces of Corsica, France, (top) and Sardinia, Italy, (bottom) have captured the imaginations of historians and poets alike for centuries. Corsica, crowned with snow-capped mountains, jeweled with shimmering lakes, and cloaked in misty emerald forests, is situated in the sapphire blue Mediterranean Sea southeast of mainland France. The island enjoys a relatively warm climate consisting of hot, dry summers full of sunshine, and mild winters that rarely dip below 0oC (32oF). In this scene, Corsica is the smaller island to the north. The island has almost 1,700 hills and mountains, ranging from 300 to over 2,700 meters in height. The tallest of these peaks is the snow-capped Monte Cinto toward the northern end of the island. Coursing throughout the island is an extensive network of rivers, carved into Corsica's granite face by snowmelt and rainwater runoff. The Corsican Cape sits on the island's northern finger; its eastern slope is somewhat hilly. There are quite a few agricultural fields and vineyards visible as the light green swath to the south all along the eastern shore. Along the southern shore are the dazzling cliffs of Bonifacio. Moving up the west coast in the state of Ajaccio we see a jagged, chiseled water front, reminiscent of the famous fjords of Norway. There are four large gulfs and many smaller rocky inlets sculpted into Corsica's west coast. Moving soutward, they are the Gulfs of Porto, Sagone, Ajaccio, and Valinco. The larger island to the south--across the Strait of Bonifacio--is Sardinia, Italy, one the earliest populated lands of Europe. Some ancient artifacts date human populations there as old as 6000 B.C. Around 1500 B.C., another group of settlers arrived on the island (historians don't know where they came from) and spread quickly across the island. Known as the Nuragic people, these settlers built almost 30,000 circular fortresses--called 'nuraghe'-- around the island; each strategically located so that they were within eyesight of their nearest neighbors. Today, about 7,000 nuraghe ruins still stand, unlike any other ruins in the world. Sardinia is the second largest island in the Mediterranean, situated due west of mainland Italy. Stretching across the central, eastern part of Sardinia is the rugged terrain of Gennargentu--mountainous and thickly vegetated. Mostly uninhabited by people, the 50,000-hectare wilderness of Monte Arcosu is home to a unique population of fallow deer as well as wild boar, hares, foxes, golden eagles, and the Sardinian wildcat. Founded in the ninth century by Phoenicians, the port city of Cagliari sits on the large bay on Sardinia's southeastern coast. To the north lies the old city of Sassari (originally an ancient settlement called Tathari), situated on a hillside overlooking the large Gulf of Asinara. This true-color image was acquired by the Moderate-resolution Imaging Spectroradiometer (MODIS), flying aboard NASA's Terra satellite, on December 7, 2001. Image courtesy Liam Gumley, Space Science and Engineering Center, University of Wisconsin-Madison
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NASA Astrophysics Data System (ADS)
Antonella Dino, Giovanna; Borghi, Alessandro; Cavallo, Alessandro; Primavori, Piero
2016-04-01
The Verbano-Cusio-Ossola quarrying district (Piedmont, northern Italy) produces many different ornamental stones (granites, gneisses, marbles): two really important categories are represented by Serizzo and Beola gneisses. Several varieties of Serizzo and Beola crop out in the upper and middle Ossola Valley: Serizzo derives from the Antigorio, Monte Leone and Monte Rosa Penninic Units, whereas Beola from the Monte Leone, Orselina-Moncucco-Isorno and Monte Rosa Penninic Units, as well from the Fobello-Rimella schists (Austroalpine). The Serizzo, represented by a group of foliated granitoid orthogneisses (Serizzo Antigorio, Serizzo Formazza, Serizzo Sempione and Serizzo Monte Rosa varieties), is probably the most important and extensively exploited ornamental stones from the VCO province (about 70% of the VCO stone production). The quarries are mostly concentrated in the Antigorio and Formazza valleys, where the Antigorio nappe has a sub-horizontal attitude and reaches its greatest thickness (up to 1000 m). This stone was largely used to produce columns since the end of XV century (e.g. the old Ospedale Maggiore in Milano, now University of Milano) and later on it was replaced with granites. It was also used in the building structure of the Duomo di Milano, for the plinth and the piers. Nowadays, thanks to its good wear resistance and low cost, it is mainly used in polished slabs for paving: a recent application is the Frankfurt airport floor. Beola is the name of a group of heterogeneous orthogneisses with mylonitic foliation and strong mineralogical lineation (Beola Grigia, Bianca, Ghiandonata, Striata varieties), easy to split into thin slabs with hammer and chisel, occurring in the middle Ossola Valley, between Vogogna and Montecrestese. The quarries of Beola are probably the oldest of the Ossola Valley, although the precise period in which the stone started to be exported is unknown. The Beola trade probably started at the end of the XIII century, with the opening of the Naviglio Grande channel (a Leonardo da Vinci's project) connecting the Ticino river to Milano. However, during the Roman Empire, these stones were already exploited and exported, as testified by the ancient Roman road, visible near the village of Beura. In general, Beola and Serizzo gneisses have also been used for ornamental purposes and for the construction of churches, palaces and monuments, widely documented in many towns and villages of the Ossola Valley (San Gaudenzio church, Montecrestese bell-tower, rural villages, Domodossola city center, etc…) and in the north of Italy (Milano and Torino). The trade of these stones, which characterized (and still characterize) the VCO territory, was affected by the recent economic crisis in the national and international market, so that in the recent years lot of quarries, even if active, are not productive. Due to the global economy situation and the strong competition with other countries (China, India,…), the risk of a collapse in the serizzi and beole production is tangible. The present contribution aim at evidencing the history and peculiarity of these materials, their importance in local culture, and the necessity not to obliterate less famous, but culturally important, stone materials.
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NASA Astrophysics Data System (ADS)
Parras-Alcántara, Luis; Lozano-García, Beatriz
2014-05-01
INTRODUCTION Soils play a key role in the carbon geochemical cycle. Agriculture contributes to carbon sequestration through photosynthesis and the incorporation of carbon into carbohydrates. Soil management is one of the best tools for climate change mitigation. Small increases or decreases in soil carbon content due to changes in land use or management practices, may result in a significant net exchange of carbon between the soil carbon pool and the atmosphere. In the last decades arable crops (AC) have been transformed into olive grove cultivations (OG) or vineyards (V) in Mediterranean areas. A field study was conducted to determine long-term effects of land use change (LUC) (AC by OG and V) on soil organic carbon (SOC), total nitrogen (TN), C:N ratio and their stratification in Calcic-Chromic Luvisols (LVcc/cr) in Mediterranean conditions. MATERIAL AND METHODS An unirrigated farm in Montilla-Moriles (Córdoba, Spain) cultivated under conventional tillage (animal power with lightweight reversible plows and non-mineral fertilization or pesticides) was selected for study in 1965. In 1966, the farm was divided into three plots with three different uses (AC, OG and V). The preliminary analyses were realized in 1965 for AC (AC1), and the second analyses were realized in 2011 for AC (AC2 - winter crop rotation with annual wheat and barley, receiving mineral fertilization or pesticides), OG (annual passes with disk harrow and cultivator in the spring, followed by a tine harrow in the summer receiving mineral fertilization and weed control with residual herbicides), and V (with three or five chisel passes a year from early spring to early autumn with mineral fertilization or pesticides.). In all cases (AC1, AC2, OG and V) were collected soil entire profiles. Soil properties determined were: soil particle size, bulk density, SOC, TN, C:N ratio, stocks and SRs. The statistical significance of the differences in the variables between land use practices was tested using the Anderson-Darling test at each horizon or a combination of horizons for each soil type. RESULTS The LUC had a negative impact in the soil, reducing the SOC and TN stocks. The conversion from AC to V and OG involved the loss of the SOC stock (52.7% and 64.9% to V and OG respectively) and the loss of the TN stock (42.6% and 38.1% to V and OG respectively). The reduction of SOC by LUC, can be explained by a degraded process (due to vegetation losses and unsustainable soil management, which result in progressive impoverishment in the soil organic matter (OM) content, causing low productivity, which derived in unsuitable chemical properties) and by the reduced input of OM in cultivated soils, which reduced physical protection of soil and increased water erosion. However, 46 years of LUC had a positive effect in the soil, increasing the SR (in V and OG) of SOC, TN and C:N ratio (Parras-Alcántara et al., 2013). REFERENCES Parras-Alcántara, L., Martín-Carrillo, M., Lozano-García, B. 2013. Impacts of land use change in soil carbon and nitrogen in a Mediterranean agricultural area (Southern Spain). Solid Earth, 4: 167-177.
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U-series dating of pillow rim glass from recent volcanism at an Axial Volcanic Ridge
NASA Astrophysics Data System (ADS)
Thomas, L. E.; van Calsteren, P. W.; Jc024 Shipboard Party
2010-12-01
Visual observations using camera systems on the tethered ROV Isis deployed during the 2008 JC024 cruise to the Mid Atlantic Ridge at 45°N showed1 numerous monogenetic volcanoes that are essentially piles of lava pillows. The pillows are usually ˜1m diameter and >2m long and form mounds with average dimensions around 300m diameter, ˜150m altitude, and 0.005km3 volume. Small protrusions, 10-50cm long, which are numerous on pillows appear to be the youngest regions, were sampled using the pincers on the hydraulic arms of Isis, and returned to the surface. On the surface, any glass crust on the pillow protrusions was chiselled off using clean tools and double bagged in polythene. In the laboratory a portion of the glass was crushed in a jeweller’s roller mill and sieved using stainless steel sieves to obtain a sufficient amount of the fraction 0.125-0.250mm for hand picking, using a binocular microscope with the glass submerged in a mix of water and iso-propyl alcohol. The samples were subsequently leached using the procedure of Standish & Sims2. Samples were spiked with a mixed 229Th-236U spike and the U, Th and Ra fractions were separated and purified using standard chemistry methods. U and Th isotope ratios were determined using a Nu Instruments MC-ICPMS and Ra isotope ratios were determined using a MAT-262-RPQII TIMS instrument. The U-series data were evaluated using a MathCad program based on published4,5,6 equations. The data can be successfully modelled by assuming the ‘accepted’ mantle upwelling rate for the region of 11mm.y-1. The U-Th characteristics are mostly derived during ‘porous flow’ magma upwelling in the garnet stability zone, ranging to a depth of 60km with incipient melting starting at 70km. Above 60km depth the melt fraction will be >3% and the mantle mineralogy devoid of phases that fractionate U-Th significantly. Moreover, at melt fractions >3%, channel flow will be dominant and magma will transit to eruption on time-scales that are short enough to retain the U-Th characteristics from the garnet zone. The rheology of the deep mantle is such that melt generation should be in ‘steady state’ and U-Th characteristics should be constant. On that assumption, measured differences in collected samples can be used to calculate model ages relative to the ‘youngest’ sample, thus allowing the construction of a relative eruption timescale. However, significant fractional crystallisation is taking place in the oceanic crust, as testified by the frequent presence of plagioclase crystals up to mm-size in the glass samples. A ‘magma chamber’ on a scale larger than the magma channels is not required and we aim to assess the rate of plagioclase crystal growth using a 226Ra chronometer. This chronometer requires the assumption that Ba-Ra fractionation is constant and can then also be used to calculate a relative model age timescale, provided that not all samples are >8000 y old, which we consider unlikely. 1Searle, RC et al, EPSL in press, 2010 2Standish, JJ & Sims, KWW. Nature Geoscience V3, 2010 3Murton, BJ et al, in prep, 2010 4Williams, RW and Gill, JB, GCA 53, 1989 5Spiegelman, M and Elliott, T, EPSL 118, 1993 6Richardson, C and McKenzie, D, EPSL 128, 1994
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NASA Astrophysics Data System (ADS)
López-Vicente, Manuel; García-Ruiz, Roberto; Guzmán, Gema; Vicente-Vicente, José Luis; Gómez, José Alfonso
2016-04-01
The study of overland flow connectivity (QC) allows understanding the redistribution dynamics of runoff and soil components as an emergent property of the spatio-temporal interactions of hydrological and geomorphic processes. However, very few studies have dealt with runoff connectivity in olive orchards. In this study we simulated QC in four olive orchard plots, located on the Santa Marta farm (37° 20' 33.6" N, 6° 13' 44" W), in Seville province (Andalusia) in SW Spain. The olive plantation was established in 1985 with trees planted at 8 m x 6 m. Each bounded plot is 8 m wide (between 2 tree lines) and 60 m long (total area of 480 m2), laid out with the longest dimension parallel to the maximum slope and to the tree lines. The slope is uniform, with an average steepness of 11%. Two plots (P2 and P4) were devoted to conventional tillage (CT) consisting of regular chisel plow passes depending on weed growth. Another set of two plots had two types of cover crops (CC) in the inter tree rows (the area outside the vertical olive canopy projection): uniform CC of Lolium multiflorum (P3) and a mixture of L. rigidum and L. multiflorum together with other species (P5). The tree rows were treated with herbicide to keep bare soil. We selected the Index of runoff and sediment Connectivity (IC) of Borselli et al. (2008) to simulate three rainfall scenarios: i) low rainfall intensity (Sc-LowInt) and using the MD flow accumulation algorithm; ii) moderate rainfall intensity (Sc-ModInt) and using MD8; and iii) high rainfall intensity (Sc-HighInt) and using D8. After analysing the values of rainfall intensity during two hydrological years (Oct'09-Sep'10 and Oct'10-Sep'11) we associated the three scenarios with the followings months: Sc-LowInt during the period Jan-Mar, that summarizes 42% of all annual rainfall events; Sc-ModInt during Oct-Nov and Apr-May (32% of all events); and Sc-HighInt during the period Jun-Sep and in December (26% of all events). Instead of using the C-RUSLE factor as it is indicated in the original version of the IC model, we chosen the product between the C (cover-management) and P (support-practices) factors. Previous studies in olive orchards (Gómez et al., 2003) demonstrated that this product is advisable in soil erosion studies. We distinguished four areas within the plots: inter-row-CC, inter-row-CT, olive trees and bare soil under the tree line. Values of the C-RUSLE factor were obtained from previous studies (e.g. Moreira-Madueño, 1991 in Andalusia; Panagos et al., 2015 in Europe). The minimum, mean and maximum values of connectivity in the two plots with CC were lower (-8% on average) than the corresponding values in the two plots under CT. This trend remained by using any of the three algorithms. CC efficiently reduced overland flow connectivity. Areas with low connectivity (deposition-prone areas) appeared more frequently in inter-row-CC in comparison with CT. The assessment of the C-RUSLE factor for each month according to the phenology of the CC and the sowing practices will be explored in further research.
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NASA Astrophysics Data System (ADS)
Rusu, Teodor; Ioana Moraru, Paula; Muresan, Liliana; Andriuca, Valentina; Cojocaru, Olesea
2017-04-01
Soil Tillage Conservation (STC) is considered major components of agricultural technology for soil conservation strategies and part of Sustainable Agriculture (SA). Human action upon soil by tillage determines important morphological, physical-chemical and biological changes, with different intensities and evaluative directions. Nowadays, internationally is unanimous accepted the fact that global climatic changes are the results of human intervention in the bio-geo-chemical water and material cycle, and the sequestration of carbon in soil is considered an important intervention to limit these changes. STC involves reducing the number of tillage's (minimum tillage) to direct sowing (no-tillage) and plant debris remains at the soil surface in the ratio of at least 30%. Plant debris left on the soil surface or superficial incorporated contributes to increased biological activity and is an important source of carbon sequestration. STC restore soil structure and improve overall soil drainage, allowing more rapid infiltration of water into soil. The result is a soil bioremediation, more productive, better protected against wind and water erosion and requires less fuel for preparing the germinative bed. Carbon sequestration in soil is net advantageous, improving the productivity and sustainability. We present the influence of conventional plough tillage system on soil, water and organic matter conservation in comparison with an alternative minimum tillage (paraplow, chisel plow and rotary harrow) and no-tillage system. The application of STC increased the organic matter content 0.8 to 22.1% and water stabile aggregate content from 1.3 to 13.6%, in the 0-30 cm depth, as compared to the conventional system. For the organic matter content and the wet aggregate stability, the statistical analysis of the data showed, increasing positive significance of STC. While the soil fertility and the wet aggregate stability were initially low, the effect of conservation practices on the soil features resulted in a positive impact on the water permeability of the soil. Availability of soil moisture during the crop growth resulted in better plant water status. Subsequent release of conserved soil water regulated proper plant water status, soil structure, and lowered soil penetrometer resistance. Productions obtained at STC did not have significant differences for the wheat and maize crop but were higher for soybean. The advantages of minimum soil tillage systems for Romanian pedo-climatic conditions can be used to improve methods in low producing soils with reduced structural stability on sloped fields, as well as measures of water and soil conservation on the whole agroecosystem. Presently, it is necessary to make a change concerning the concept of conservation practices and to consider a new approach regarding the good agricultural practice. We need to focus on an upper level concerning conservation by focusing on soil quality. Carbon management is necessary for a complexity of matters including soil, water management, field productivity, biological fuel and climatic change. In conclusion a Sustainable Agriculture includes a range of complementary agricultural practices: (i) minimum soil tillage (through a system of reduced tillage or no-tillage) to preserve the structure, fauna and soil organic matter; (ii) permanent soil cover (cover crops, residues and mulches) to protect the soil and help to remove and control weeds; (iii) various combinations and rotations of the crops which stimulate the micro-organisms in the soil and controls pests, weeds and plant diseases. Acknowledgements: This paper was performed under the frame of the Partnership in priority domains - PNII, developed with the support of MEN-UEFISCDI, project no. PN-II-PT-PCCA-2013-4-0015: Expert System for Risk Monitoring in Agriculture and Adaptation of Conservative Agricultural Technologies to Climate Change, and International Cooperation Program - Sub-3.1. Bilateral AGROCEO c. no. 21BM/2016, PN-III-P3-3.1-PM-RO-MD-2016-0034: The comparative evaluation of conventional and conservative tillage systems regarding carbon sequestration and foundation of sustainable agroecosystems.
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40 Years of Processing Pieces of Space
NASA Technical Reports Server (NTRS)
Satterwhite, C. E.; Funk, R. C.; Righter, K.; Harrington, R. H.
2016-01-01
This year marks the 40th year anniversary for the Antarctic Search for Meteorite (ANSMET) program. In 1976, the ANSMET program led the first expedition to Antarctica. The ANSMET program is a US-led field-based science project that recovers meteorite samples from Antarctica. Once a year from late November to late January, a field team consisting of 8 to 12 people, spends 6-8 weeks camping on the ice and collecting meteorites. Since 1976, more than 22,000 meteorite samples have been recovered. These meteorites come from asteroids, planets and other bodies of the solar system. Once collected, the Antarctic meteorites are shipped to NASA/Johnson Space Center (JSC) Houston, TX. in a refrigerated truck and are kept frozen to minimize oxidation until they are ready for initial processing. In Antarctica each meteorite is given a field tag which consists of numbers, once in the lab, this is replaced by an official tag, consisting of the Antarctic field location and year collected. The types and numbers of meteorites that have been classified include 849 carbonaceous chondrites, 135 enstatites, 512 achondrites, 64 stony, 115 irons, 48 others (27 R chondrites, 7 ungrouped), 6,161 H chondrites, 7,668 L chondrites, and 4,589 LL chondrites. Although 80-85 percent of the collected meteorites fall in the ordinary chondrite group, the other approximately 15 percent represent rare types of achondrites and carbonaceous chondrites. These rare meteorites include 25 lunar meteorites, 15 Martian meteorites, scores of various types of carbonaceous chondrites, and unique achondrites. The Antarctic meteorites that have been collected are processed in the Meteorite Processing Lab at JSC in Houston, TX. Initial processing of the meteorites begins with thawing/drying the meteorites in a nitrogen glove box for 24 to 48 hours. The meteorites are then photographed, measured, weighed and a description of the interior and exterior of each meteorite is written. The meteorite is broken and a representative sample, either a 1-3 gram chip or thin section is sent to the Smithsonian Institution for classification. After Antarctic meteorites have been classified and approved by the Nomenclature Committee of the Meteoritical Society, they are announced in the Antarctic Meteorite Newsletter, which is published twice per year (fall and spring) so that scientists may review which meteorites are available to study. Requests for Antarctic Meteorite samples are welcomed from research scientists, regardless of their current state of funding for meteorite studies. Since its inception over 3,300 requests have been made for pieces of these meteorites and over 400 investigators worldwide are active in the study of meteorites.. Research on these samples has been published in more than1500 peer reviewed articles; a listing of papers for any meteorite sample can be generated by accessing http://curator.jsc.nasa.gov/antmet/referencesearch.cfm. Antarctic meteorite samples requested by scientists are prepared several different ways. Most samples are prepared as chips, either using a rock splitter or using a chisel and chipping bowl. In special situations, a researcher may request a meteorite slab in which case the samples are cut using a diamond-bladed bandsaw inside of a dry nitrogen glove box. The meteorites are always cut in a 100 percent liquid-free environment. Additionally, thin/thick sections of Antarctic meteorites are also prepared at JSC. The meteorite thin section lab at JSC can prepare standard 30-micron thin sections, thick sections of variable thickness (100 to 200 microns), or demountable sections using superglue, all section are prepared without using water. Although many of the techniques used back in the '70's are still used today, advances in computers, software, databases, available tools and instrumentation have helped to streamline and shorten the duration of the classification process. In conjunction with present day missions to asteroids and other planets, meteorite studies have not only led to a better understanding of the complex histories of these bodies but have also tied certain meteorite groups to particular asteroid bodies. New meteorite discoveries by the ANSMET program provide a cost effective method for obtaining samples of previously unsampled bodies, allowing scientists to learn more about the origin, composition, and evolution of the solar system. Preservation in our cleanrooms at NASA allows material to be archived for future generations and advances in instrumentation and analysis.
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NASA Astrophysics Data System (ADS)
Bodner, G.; Loiskandl, W.; Kaul, H.-P.
2009-04-01
Soil structure is a dynamic property subject to numerous natural and human influences. It is recognized as fundamental for sustainable functioning of soil. Therefore knowledge of management impacts on the sensitive structural states of soil is decisive in order to avoid soil degradation. The stabilization of the soil's (macro)pore system and eventually the improvement of its infiltrability are essential to avoid runoff and soil erosion, particularly in view of an increasing probability of intense rainfall events. However structure-related soil properties generally have a high natural spatiotemporal variability that interacts with the potential influence of agricultural land use. This complicates a clear determination of management vs. environmental effects and requires adequate measurement methods, allowing a sufficient spatiotemporal resolution to estimate the impact of the targeted management factors within the natural dynamics of soil structure. A common method to assess structure-related soil hydraulic properties is tension infiltrometry. A major advantage of tension infiltrometer measurements is that no or only minimum soil disturbance is necessary and several structure-controlled water transmission properties can readily be derived. The method is more time- and cost-efficient compared to laboratory measurements of soil hydraulic properties, thus enabling more replications. Furthermore in situ measurements of hydraulic properties generally allow a more accurate reproduction of field soil water dynamics. The present study analyses the impact of two common agricultural management options on structure related hydraulic properties based on tension infiltrometer measurements. Its focus is the identification of the role of management within the natural spatiotemporal variability, particularly in respect to seasonal temporal dynamics. Two management approaches are analysed, (i) cover cropping as a "plant-based" agro-environmental measure, and (ii) tillage with different intensities including conventional tillage with a mouldboard plough, reduced tillage with a chisel plough and no-tillage. The results showed that the plant-based management measure of cover cropping had only minor influence on near-saturated hydraulic conductivity (kh) and flow weighted mean pore radius (λm). Substantial over-winter changes were found with a significant increase in kh and a reduction in the pore radius. A spatial trend in soil texture along the cover cropped slope resulted in a higher kh at lower pressure heads at the summit with higher fractions of coarse particles, while kh tended to be highest at the toeslope towards saturation. Cover crop management accounted for a maximum of 9.7% of the total variability in kh, with a decreasing impact towards the unsaturated range. A substantial difference to bare soil in the cover cropped treatments could be identified in relation to a stabilization of macro-pores over winter. The different tillage treatments had a substantial impact on near-saturated kh and pore radius. Although conventional tillage showed the highest values in kh and λm, settling of the soil after the ploughing event tended to reduce differences over time compared to the other tillage methods. The long-term no-tillage (10 years) however had the lowest values of kh at all measurement dates. The high contents of silt and fine sand probably resulted in soil densification that was not counterbalanced sufficiently by biological structure forming agents. The study could show that soil structure related hydraulic properties are subject to a substantial seasonal variability. A comprehensive assessment of agricultural measures such as tillage or cover cropping requires an estimate of these temporal dynamics and their interaction with the management strategies. Particularly for plant-based management measures such as cover cropping, which represent a less intense intervention in the structural states of the soil compared to tillage, this was evident, as the main mechanism revealed for this measure was structure stabilization over time. While spatial variability is mostly controlled in designed experiments, the role of temporal variability is often underestimated. From our study we concluded that (i) a proper understanding of processes involved in management effects on soil structure must take into consideration the dynamic nature of the respective soil properties, (ii) experimental planning for studies regarding management impacts on soil structure should allow an estimation of temporal variability, and (iii) for this purpose tension infiltrometry provides an efficient measurement tool to assess structure related soil hydraulic properties.
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The "green stones" of Valtellina and Valchiavenna (central Alps, northern Italy)
NASA Astrophysics Data System (ADS)
Cavallo, Alessandro
2015-04-01
Valtellina and Val Chiavenna (Sondrio, Central Alps, northern Italy) are traditionally areas of production of building and ornamental stones (e.g. Serizzo Ghiandone, Serizzo Valmasino, San Fedelino Granite), and among these the "green stones" have a leading position. These stones had an extensive use in Lombardy, as well as abroad (e.g Switzerland). The "green stones" are related to the two mafic-ultramafic bodies of Valmalenco and Chiavenna, where the two largest quarrying districts of the Province of Sondrio are located. Until the early decades of the XX century, serpentinites (and other lithologies from Valtellina) were also extracted from the erratic boulders of Brianza (north of Milan), but at present time the law protects the few remaining boulders. The extracted and processed materials are various: serpentinites, ophicalcites, soapstones. Even the "Stone of Tresivio", used in the past in important monuments of Valtellina, could be classified among the "green stones" in a broad sense: it is a green chloritic schist with scarce and thin ferriferous calcitic veins, pertaining to the sedimentary "Servino" Formation. In recent times, the ancient quarries of this stone were rediscovered near the homonymous village, a few kilometers from Sondrio. There are also historic reports about other "green stones", used in ancient times, such as the "Stone of Grosio", a chloritic schist, and the "Bormio Prasinite". Currently the extraction and processing of "green stones" occurs mostly in Valmalenco, with 22 active serpentinite quarries and a gross volume of 70000 m3 extracted per year, with a yield of about 50%. The Malenco serpentinite (interpreted as sub-continental mantle rocks) forms a 1-2 km thick tabular body, outcropping over an area of about 170 km2, almost entirely confined within the boundaries of the valley. The antigoritic serpentinites (with variable amounts of olivine, clinopyroxene, chlorite and magnetite) are moderately up to strongly foliated, sometimes folded, and are processed in two main commercial varieties: schistose ("serpentinoscisto") and massive ("serpentino da taglio"). In Valmalenco, the extraction and processing of schistose serpentinites for the production of slabs ("piode", splitted by hand with hammer and chisel), used in roofing and flooring, dates back at least to the XIV century. From the traditional underground extraction, the quarrying activities moved to the modern open-cast extraction in the seventies. The renowned quality of the secular serpentinite roof coverings is related to the excellent physical and mechanical properties, especially the flexural strength (average values around 90-100 MPa), very low porosity and the thaw/freezing resistance. The "massive" serpentinite achieved a special place in the national and international market of ornamental stones: the several extracted varieties (Serpentino Classico, Verde Vittoria, Verde Perlato, Verde Mare, Verde Principe, Verde Torre S. Maria), in addition to the excellent technical properties (flexural strength and thermal properties) that promote specific uses, make these stones much appreciated worldwide (e.g. Bundestag in Berlin, Germany). As part of the "green stones" of Valmalenco, two currently abandoned ophicalcite quarries have been active in the recent past. The extraction and processing of soapstone ("pietra ollare" or "pietra laugera", a talc and/or chlorite rich ultramafic/mafic rock) in Valmalenco and Valchiavenna probably dates back to the Iron Age; in Valchiavenna it is documented with certainty since Roman times and the Middle Ages. The extraction and processing of soapstone peaked around the middle of the XVIII century, with a dozen quarries and about 300 workers involved, between Chiavenna and Piuro. A limited production of soapstone is still active in the municipalities of Piuro (talc-olivine-tremolite fels) and Chiesa in Valmalenco (chlorite schist), where in addition to the traditional cooking pots ("Lavecc"), there is a growing art work and gift items production. With the exception of two companies that have reached an industrial production level, the remaining 24 companies operating in Valmalenco are on an artisan level, and are grouped in the "Consorzio Artigiani Cavatori Valmalenco". The consortium, already engaged in the management of a permanent storage of explosives at the service of the quarries, promotes and subsidizes economically various initiatives aimed at the enhancement of stone products and the development of this craft. The consortium is a promoter of a cultural initiative aimed at the restoration of an underground quarry and the ancient paths of "Giovello", a historic site for the extraction and processing of serpentinite.
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NASA Astrophysics Data System (ADS)
Bodner, G.; Schwen, A.; Scholl, P.; Kammerer, G.; Buchan, G.; Kaul, H.-P.; Loiskandl, W.
2010-05-01
Soil macroporosity is a highly dynamic property influenced by environmental factors, such as raindrop impact, wetting-drying and freezing-thawing cycles, soil biota and plant roots, as well as agricultural management measures. Macroporosity represents an important indicator of soil physical quality, particularly in relation to the site specific water transmission properties, and can be used as a sensitive measure to assess soil structural degradation. Its quantification is also required for the parameterization of dual porosity models that are frequently used in environmental impact studies on erosion and solute (pesticide, nitrate) leaching. The importance of soil macroporosity for the water transport properties of the soil and its complexity due to high spatio-temporal heterogeneity make its quantitative assessment still a challenging task. Tension infiltrometers have been shown to be adequate measurement devices to obtain data in the near-saturated range of water flow where structural (macro)pores are dominating the transport process. Different methods have been used to derive water transmission characteristics from tension infiltrometer measurements. Moret and Arrúe (2007) differentiated between using a minimum equivalent capillary pore radius and a flow weighted mean pore radius to obtain representative macropore flow properties from tension infiltrometer data. Beside direct approaches based on Wooding's equation, also inverse methods have been applied to obtain soil hydraulic properties (Šimůnek et al. 1998). Using a dual porosity model in the inverse procedure allows estimating parameters in the dynamic near-saturated range by numerical optimization to the infiltration measurements, while fixing parameters in the more stable textural range of small pores using e.g. pressure plate data or even pedotransfer functions. The present work presents a comparison of quantitative measures of soil macroporosity derived from tension infiltrometer data by different approaches (direct vs. inverse evaluation, capillary vs. flow weighted pore radius). We will show the influence of the distinct evaluation procedures on the resulting effective macroporosity, as well as on the relationships between macropore radius and hydraulic conductivity (Moret and Arrúe, 2007) and pore fraction respectively (Carey et al., 2007). The infiltration measurements used in this study were obtained in a long-term tillage trial located in the semi-arid region of Eastern Austria. Measurements were taken five times over the vegetation period, starting immediately after tillage until harvest of the winter wheat crop. Three tillage systems were evaluated, being conventional tillage with plough, minimum tillage with chisel and no-tillage. Additional to infiltration measurements, also soil water content was monitored continuously by a capacitance probe in all three replicates of each tillage treatment in 10, 20 and 40 cm soil depth. Water content time series are used to derive flow velocity in the wet range by cross-correlation analysis (Wu et al., 1997). This effective parameter of water transmission will then be compared to the flow behaviour expected from the characterization of soil macroporosity. We will show that mainly in no-tillage systems large macropores contribute essentially to flow and therefore the decision on pore measure and evaluation procedure to be used leads to substantial differences. For a detailed comparison of tillage effects on soil hydraulic properties it is therefore essential to analyse the contribution of different tension infiltrometry based evaluation methods to explain effective water transmission through the complex porous network of the soil. References Carey, S.K., Quinton, W.L., Goeller, N.T. 2007. Field and laboratory estimates of pore size properties and hydraulic characteristics for subarctic organic soils. Hydrol. Process. 21, 2560-2571. Moret, D., Arrúe, J.L. 2007. Characterizing soil water conducting macro- and mesoporosity as influences by tillage using tension infiltrmetry. Soil Sci. Soc. Am. J. 71, 500-506. Šimůnek, J., Wang Dong, Shouse, P. J., van Genuchten, M. T. 1998. Analysis of field tension disc infiltrometer data by parameter estimation. Int. Agrophys. 12. 167-180. Wu, L., Jury, W.A., Chang, A.C. 1997. Time series analysis of field-measured watr content of a sandy soil. Soil Sci. Soc. Am. J. 61. 742-745.
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NASA Technical Reports Server (NTRS)
2002-01-01
(Released 16 April 2002) The Science This THEMIS visible image was acquired near 11o N, 159o W (201o E) and shows examples of the remarkable variations that can be seen in the erosion of the Medusae Fossae Formation. This Formation is a soft, easily eroded deposit that extends for nearly 1,000 km along the equator of Mars. In this region, like many others throughout the Medusae Fossae Formation, the surface has been eroded by the wind into a series of linear ridges called yardangs. These ridges generally point in direction of the prevailing winds that carved them, and demonstrate the power of martian winds to erode the landscape of Mars. The easily eroded nature of the Medusae Fossae Formation suggests that it is composed of weakly cemented particles, and was most likely formed by the deposition of wind-blown dust or volcanic ash. Within this single image it is possible to see differing amounts of erosion and stripping of layers in the Medusae Fossae Formation. Near the bottom (southern) edge of the image a rock layer with a relatively smooth upper surface covers much of the image. Moving upwards (north) in the image this layer becomes more and more eroded. At first there are isolated regions where the smooth unit has been eroded to produce sets of parallel ridges and knobs. Further north these linear knobs increase in number, and only small, isolated patches of the smooth upper surface remain. Finally, at the top of the image, even the ridges have been removed, exposing the remarkably smooth top of hard, resistant layer below. This sequence of layers with differing hardness and resistance to erosion is common on Earth and on Mars, and suggests significant variations in the physical properties, composition, particle size, and/or cementation of these martian layers. As is common throughout the Medusae Fossae Formation, very few impact craters are visible, indicating that the surface exposed is relatively young, and that the process of erosion may be active today. The Story 'Yardang!' Now, that may seem like a peculiar-sounding curse word, but nobody would get in trouble for using it. A yardang is one of the very cool-sounding words geologists use to describe long, irregular features like the ones seen in this image. Yardangs are grooved, furrowed ridges that form as the wind erodes away weakly cemented material in the region. Rippling across the surface, yardangs tell the story of how the powerful Martian wind carved the surface into such a gorgeous pattern over time. (Don't miss clicking on the above image to see a detailed view, in which the beauty and almost dance-like symmetry of the waving terrain pops out in highly compelling, three-dimensional texture.) It may be easy to see which way the wind blows in this area, since these streamlined features point in the direction of prevailing winds. But how can geologists understand the various kinds of terrain seen here? First, they have to study the different patterns of erosion, looking closely at how the wind has stripped off certain layers and not others. Want to be a geologist yourself? Start at the bottom of the image and scroll upward, and see how the relatively smooth, higher terrain toward the south gradually becomes more and more eroded. Moving up the image, at first you?ll see only a few, isolated regions of parallel ridges and knolls. Go a little farther north with your eyes (toward the center of the image), and you?ll see how these linear knobs really get going! Once you get to the top of the image, only patches of these grooved ridges remain, leaving an incredibly smooth, wind-scrubbed surface behind. You know this layer has to be made of pretty hard material, because it seems impervious to further erosion. Geologists studying Mars can compare these Martian yardangs to examples found on Earth, such as those in the Lut desert of Iran. Humans have even been known to use the wind as their inspiration, sculpting the shape of yardangs themselves. The famous sphynx at Giza in Egypt is thought to be a yardang that's been whittled down a little more by ancient human chiselers.
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The barley straw residues avoid high erosion rates in persimmon plantations. Eastern Spain
NASA Astrophysics Data System (ADS)
Cerdà, Artemi; González Pelayo, Óscar; Giménez-Morera, Antonio; Jordán, Antonio; Novara, Agata; Pereira, Paulo; Mataix-Solera, Jorge
2015-04-01
World persimmon production is 4 Millions tones and China produce more than 80 % of the total world yield. Korea and Japan are the second and the third producers respectively with 0.4 and 0.2 millions tones, and all three Asian countries concentrate more than 95 % of the world production. Spain produce less than 0.1 million tones but there is a sudden increase in new plantations due to the high prices and the new marked developed in Europe, Brazil and Arabic countries. The new chemically managed and highly mechanized plantations in Eastern Spain are using high doses of herbicides and the lack of vegetation is triggering high erosion rates. This paper aims to contribute with information about the soil losses on this new persimmon plantations and to develop strategies to reduce the soil and water losses. A 15 years old plantation of persimmon (Dyospirus lotus) was selected in Eastern Spain (Canals Municipality, La Costera District) to measure the soil losses on No-Tillage bare (herbicide treatments) management and on barley straw covered plots. The straw cover was applied 3 days before the expereriments at at doses that cover more than 50 % of the soil surface using 75 gr of straw per m2. Rainfall simulations under 55 mm h-1 rainfall intensity during one hour on 0.25 m2 plots were carried out on plots paired plots: bare and covered with straw. The measurements were carried out during July 2014 on paired plots, under very dry soil moisture contents ranging from 4.65 to 7.87 %. The results show that the 3% cover of vegetation of the control plots moved to more than 60% due to the application of the straw. This induced a delayed ponding (from 60 to 309 seconds) and surface runoff (from 262 to 815 seconds) and runoff outlet (418 to 1221 seconds). The runoff coefficients moved from 60 % in the control plots to 29 % in the straw covered and the runoff sediment concentration was dramatically reduced from 11 to 1 g l-1. The total soil losses were higher that 1 Kg per plot in the bare control plots to 47 gr in the straw covered plots, which resulted in a low erosion rate when the soil is covered with straw (0.23 Mg ha-1 y-1), but extremely high when the soil is not covered (5.07 Mg ha-1 y-1). The results show also a delayed runoff generation due to the effect of the straw. From ponding to surface runoff the bare plots last 198 seconds, but under straw covered soils the time is 506 seconds. Moreover, when runoff is found on the soil surface the time to reach the plot outlet is much delayed under the straw cover, as range from 156 seconds on the bare plots to 406 to the straw covered plots. The management of the agriculture soils in many parts of the Planet is triggering land degradation (Borelli et al., 2013; Haregeweyn et al., 2013; Zhao et al., 2013). The most intense soil erosion rates use to affect agriculture land (Cerdà et al., 2009), and in Eastern Spain it was found that citrus orchards are being seeing as one of the crops with the highest erosion rates due to the managements that avoid the catch crops, weeds or litter, and this is also found in China (Cerdà and Jurgensen, 2008; 2009; Cerdà et al., 2009a; 2009b; Cerdà et al., 2011; 2012) and in China (Wu et al., 1997; Xu et al., 2010; Wang et al., 2011; Wu et al., 2011; Liu et al., 2011; Lü et al., 2011; Xu et al., 2012). The worse land managements found in many of the citrus plantations results in soil degradation too (Lu et al., 1997; Lü et al., 2012; Xu et al., 2012) and we can confirm here that the new Persimmon plantations are triggering the same effect and it is necessary to develop new strategies to reduce the soil losses. The use of cover crops to reduce the soil losses (Lavigne et al., 2012; Le Bellec et al., 2012) and the use of residues such as dried citrus peel has been found successful, but also it is well know the effect of the litter it is a key cover to avoid soil erosion. Meginnis (1935) was one of the pioneers on the research of the cover of litter to avoid the high erosion losses. There is a need to find new plants or residues to protect the soils on persimmon orchards and they should be developed now that the farmers are increasing the land that produce persimmon. Straw has been seen as a very efficient to reduce the water losses in other agriculture lands (García Moreno et al., 2013), the soil losses in fire affected land (Robichaud et al., 2013a; 2013b; Fernandez and Vega, 2014), and soil properties on agriculture land (García Orenes et al., 2009; 2010; Jordán et al., 2010; García Orenes 2012). Those findings and the ones we show here must support the change to a more sustainable agriculture. This new advances in agronomy affect the control of the soil erosion (Tejeda and Benitez, 2014) but also the recovery of the soil quality (Mahmoud and Abd El-Kader, 2015). More research is need to find the right doses to be also sustainable from the economical point of view, and it is necessary to convince the farmers of the need to protect the soil. Acknowledgements The research projects GL2008-02879/BTE, LEDDRA 243857 and RECARE supported this research. References Bombino, G., Denisi, P., Fortugno, D., Tamburino, V., Zema, D.A., Zimbone, S.M. 2010. Land spreading of solar-dried citrus peel to control runoff and soil erosion. WIT Transactions on Ecology and the Environment 140,145-154. Borrelli, P., Märker, M., Schütt, B. 2013. Modelling post-tree-haversting soil erosion and sediment deposi- tion potential in the Turano River Basin (Italian Central Apennine). Land Degradation & Development, DOI 10.1002/ldr.2214 Cerdà, A., Flanagan, D.C., le Bissonnais, Y., Boardman, J. 2009. Soil erosion and agriculture Soil and Tillage Research 106, 107-108. DOI: 10.1016/j.still.2009.1 Cerdà, A., Jurgensen, M.F. 2008. The influence of ants on soil and water losses from an orange orchard in eastern Spain. Journal of Applied Entomology 132, 306-314. Cerdà, A., Jurgensen, M.F. 2011. Ant mounds as a source of sediment on citrus orchard plantations in eastern Spain. A three-scale rainfall simulation approach. Catena 85, 231-236. Cerdà, A., Jurgensen, M.F., Bodi, M.B. 2009. Effects of ants on water and soil losses from organically-managed citrus orchards in eastern Spain. Biologia 64, 527-531. Cerdà, A., Morera, A.G., Bodí, M.B. 2009. Soil and water losses from new citrus orchards growing on sloped soils in the western Mediterranean basin. Earth Surface Processes and Landforms 34, 1822-1830. Fernández, C., Vega, J.A. 2014. Efficacy of bark strands and straw mulching after wildfire in NW Spain: Effects on erosion control and vegetation recovery. Ecological Engineering 63, 50-57 García-Moreno, J., Gordillo-Rivero, Á.J., Zavala, L.M., Jordán, A., Pereira, P. 2013. Mulch application in fruit orchards increases the persistence of soil water repellency during a 15-years period. Soil and Tillage Research 130, 62-68. García-Orenes, F., Cerdà, A., Mataix-Solera, J., Guerrero, C., Bodí, M.B., Arcenegui, V., Zornoza, R. & Sempere, J.G. 2009. Effects of agricultural management on surface soil properties and soil-water losses in eastern Spain. Soil and Tillage Research 106, 117-123. 10.1016/j.still.2009.06.002 García-Orenes, F., Guerrero, C., Roldán, A.,Mataix-Solera, J., Cerdà, A., Campoy, M., Zornoza, R., Bárcenas, G., Caravaca. F. 2010. Soil microbial biomass and activity under different agricultural management systems in a semiarid Mediterranean agroecosystem. Soil and Tillage Research 109, 110-115. 10.1016/j.still.2010.05.005. García-Orenes, F., Roldán, A., Mataix-Solera, J., Cerdà, A., Campoy, M., Arcenegui, V., Caravaca, F. 2012. Soil structural stability and erosion rates influenced by agricultural management practices in a semi-arid Mediterranean agro-ecosystem. Soil Use and Management 28, 571-579. DOI: 10.1111/j.1475-2743.2012.00451.x Haregeweyn, N., Poesen, J., Verstraeten, G., Govers, G., de Vente, J., Nyssen, J., Deckers, J., Moeyersons, J. 2013. Assessing the performance of a Spatially distributed soil erosion and sediment delivery model (WATEM/SEDEM) in Northern Ethiopia. Land Degradation & Development 24, 188-204. DOI 10.1002/ldr.1121 Lavigne, C., Achard, R., Tixier, P., Lesueur Jannoyer, M. 2012. How to integrate cover crops to enhance sustainability in banana and citrus cropping systems. Acta Horticulturae 928, 351-358. Le Bellec, F., Damas, O., Boullenger, G., Vannière, H., Lesueur Jannoyer, M., Tournebize, R., Ozier Lafontaine, H. 2012. Weed control with a cover crop (Neonotonia wightii) in mandarin orchards in Guadeloupe (FWI). Acta Horticulturae 928, 359-366. Liu, Y., Tao, Y., Wan, K.Y., Zhang, G.S., Liu, D.B., Xiong, G.Y., Chen, F. 2012. Runoff and nutrient losses in citrus orchards on sloping land subjected to different surface mulching practices in the Danjiangkou Reservoir area of China. Agricultural Water Management 110, 34-40. Lu, J., Wilson, M.J., Yu, J. 1997. Effects of trench planting and soil chiselling on soil properties and citrus production in hilly ultisols of China Soil and Tillage Research 43, 309-318. Lü, W., Zhang, H., Wu, Y., Cheng, J., Li, J., Wang, X. 2012. The impact of plant hedgerow in Three Gorges on the soil chemicophysical properties and soil erosion. Key Engineering Materials 500 142-148. Liu, Y., Tao, Y., Wan, K.Y., Zhang, G.S., Liu, D.B., Xiong, G.Y., Chen, F. 2012. Runoff and nutrient losses in citrus orchards on sloping land subjected to different surface mulching practices in the Danjiangkou Reservoir area of China. Agricultural Water Management 110, 34-40. Lu, J., Wilson, M.J., Yu, J. 1997. Effects of trench planting and soil chiselling on soil properties and citrus production in hilly ultisols of China Soil and Tillage Research 43, 309-318. Lü, W., Zhang, H., Wu, Y., Cheng, J., Li, J., Wang, X. 2012. The impact of plant hedgerow in Three Gorges on the soil chemicophysical properties and soil erosion. Key Engineering Materials 500 142-148. Mahmoud, E., Abd El-Kader, N. 2014. Heavy metal immobilization in contamined soils using phosphogypsum and rice straw compost. Land Degradation & Development. DOI: 10.1002/ldr.2288 Meginnis, H. G. 1935. Influence of forest litter on surface run-off and soil erosion. Soil Science Society of America Journal, 16(2001), 115-118. Robichaud, P.R., Lewis, S.A., Wagenbrenner, J.W., Ashmun, L.E., Brown, R.E. 2013a. Post-fire mulching for runoff and erosion mitigation. Part I: Effectiveness at reducing hillslope erosion rates. Catena 105, 75-92. Robichaud, P.R., Wagenbrenner, J.W., Lewis, S.A., Ashmun, L.E., Brown, R.E., Wohlgemuth, P.M. 2013b. Post-fire mulching for runoff and erosion mitigation. Part II: Effectiveness in reducing runoff and sediment yields from small catchments. Catena 105, 93-111. Tejada M. Benítez, C. 2014. Effects of crushed maize Straw residues on soil biological properties and soil restoration. Land Degradation and Development, 25, 501-509. DOI: 10.1002/ldr.2316 Wu J., Li Q., Yan L. 1997. Effect of intercropping on soil erosion in young citrus plantation - a simulation study. Chinese Journal of Applied Ecology 8, 143-146. Wu, D.-M., Yu, Y.-C., Xia, L.-Z., Yin, S.-X., Yang, L.-Z. 2011. Soil fertility indices of citrus orchard land along topographic gradients in the three gorges area of China. Pedosphere 21, 782-792. Xu, Q. X., Wang, T. W., Cai, C. F., Li, Z. X., Shi, Z. H. 2012. Effects of soil conservation on soil properties of citrus orchards in the Three-Gorges Area, China. Land Degradation & Development, 23(1), 34-42. Xu, Q., Wang, T., Li, Z., Cai, C., Shi, Z., Jiang, C. 2010. Effect of soil conservation measurements on runoff, erosion and plant production: A case study on steeplands from the Three Gorges Area, China. Journal of Food, Agriculture and Environment 8, 980-984. Xu, Q.X., Wang, T.W., Cai, C.F., Li, Z.X., Shi, Z.H. 2012. Effects of soil conservation on soil properties of citrus orchards in the Three-Gorges Area, China. Land Degradation and Development 23, 34-42. Zhao, G., Mu, X., Wen, Z., Wang, F., Gao, P. 2013. Soil erosion, conservation, and eco-environment changes in the Loess Plateau of China. Land Degradation & Development, 24, 499- 510. DOI 10.1002/ldr.2246SP
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Extreme soil erosion rates in citrus slope plantations and control strategies. A literature review
NASA Astrophysics Data System (ADS)
Cerdà, Artemi; Ángel González Peñaloza, Félix; Pereira, Paulo; Reyes Ruiz Gallardo, José; García Orenes, Fuensanta; Burguet, María
2013-04-01
Soil Erosion is a natural process that shapes the Earth. Due to the impact of agriculture, soil erosion rates increase, landforms show gullies and rills, and soils are depleted. In the Mediterranean, wheat, olive and vineyards were the main agriculture products, but new plantations are being found in sloping terrain due to the drip-irrigation. This new strategy results in the removal of the traditional terraces in order to make suitable for mechanization the agriculture plantation. Citrus is a clear example of the impact of the new chemical agriculture with a high investment in herbicides, pesticides, mechanisation, land levelling and drip computer controlled irrigation systems. The new plantation of citrus orchards is found in the Mediterranean, but also in California, Florida, China and Brazil. Chile, Argentina, and South Africa are other producers that are moving to an industrial production of citrus. This paper shows how the citrus plantations are found as one of the most aggressive plantation due to the increase in soil erosion, and how we can apply successful control strategies. The research into the high erosion rates of citrus orchard built on the slopes are mainly found in China (Wu et al., 1997; Xu et al., 2010; Wang et al., 2011; Wu et al., 2011; Liu et al., 2011; Lü et al., 2011; Xu et al., 2012) and in the Mediterranean (Cerdà and Jurgensen, 2008; 2009; Cerdà et al., 2009a; 2009b; Cerdà et al., 2011; 2012) Most of the research done devoted to the measurements of the soil losses but also some research is done related to the soil properties (Lu et al., 1997; Lü et al., 2012; Xu et al., 2012) and the impact of cover crops to reduce the soil losses (Lavigne et al., 2012; Le Bellec et al., 2012) and the use of residues such as dried citrus peel in order to reduce the soil losses. There are 116 million tonnes of citrus produced yearly, and this affects a large surface of the best land. The citrus orchards are moving from flood irrigated to drip irrigated land, and this contributes to increase the soil losses due to the sloping terrain. Although citrus is a world wide food, and occupy a large surface little is being researched on their impact on soil erosion, land degradation and strategies to control the soil, water and nutrient losses. This paper review the research developed until now and the results show that there is a poor background on this topic. It is necessary to develop research projects to improve the knowledge on the impact of citrus plantations on soil degradation and soil erosion. Another key information from the literature review done, is that most of the research was done in two regions of China and one of the Mediterranean. Definitively, a poor understanding of a huge environmental problem that need more scientific research. Acknowledgements The research projects GL2008-02879/BTE and LEDDRA 243857 supported this research. References Bombino, G., Denisi, P., Fortugno, D., Tamburino, V., Zema, D.A., Zimbone, S.M. 2010. Land spreading of solar-dried citrus peel to control runoff and soil erosion. WIT Transactions on Ecology and the Environment, 140, 145-154. Cerdà, A., Giménez Morera, A., Burguet, M., Arcenegui, V., González Peñaloza, F.A., García-Orenes, F., Pereira, P. 2012. The impact of the farming, abandonment and agricultural intensification on loss of water and soil. The example of the northern slopes of the Serra Grossa, Eastern Spain [El impacto del cultivo, el abandono y la intensificación de la agricultura en la pérdida de agua y suelo. el ejemplo de la vertiente norte de la serra grossa en el este peninsular] Cuadernos de Investigacion Geografica, 38 (1), 75-94. Cerdà, A., Jurgensen, M.F. 2008. The influence of ants on soil and water losses from an orange orchard in eastern Spain. Journal of Applied Entomology, 132 (4), 306-314. Cerdà, A., Jurgensen, M.F. 2011. Ant mounds as a source of sediment on citrus orchard plantations in eastern Spain. A three-scale rainfall simulation approach. Catena, 85 (3), 231-236. Cerdà, A., Jurgensen, M.F., Bodi, M.B. 2009. Effects of ants on water and soil losses from organically-managed citrus orchards in eastern Spain. Biologia, 64 (3), 527-531. Cerdà, A., Morera, A.G., Bodí, M.B. 2009. Soil and water losses from new citrus orchards growing on sloped soils in the western Mediterranean basin. Earth Surface Processes and Landforms, 34 (13), 1822-1830. Lavigne, C., Achard, R., Tixier, P., Lesueur Jannoyer, M. 2012. How to integrate cover crops to enhance sustainability in banana and citrus cropping systems. Acta Horticulturae, 928, 351-358. Le Bellec, F., Damas, O., Boullenger, G., Vannière, H., Lesueur Jannoyer, M., Tournebize, R., Ozier Lafontaine, H. 2012. Weed control with a cover crop (Neonotonia wightii) in mandarin orchards in Guadeloupe (FWI). Acta Horticulturae, 928, 359-366. Liu, Y., Tao, Y., Wan, K.Y., Zhang, G.S., Liu, D.B., Xiong, G.Y., Chen, F. 2012. Runoff and nutrient losses in citrus orchards on sloping land subjected to different surface mulching practices in the Danjiangkou Reservoir area of China. Agricultural Water Management, 110, 34-40. Lu, J., Wilson, M.J., Yu, J. 1997. Effects of trench planting and soil chiselling on soil properties and citrus production in hilly ultisols of China Soil and Tillage Research, 43 (3-4), 309-318. Lü, W., Zhang, H., Wu, Y., Cheng, J., Li, J., Wang, X. 2012. The impact of plant hedgerow in Three Gorges on the soil chemicophysical properties and soil erosion. Key Engineering Materials, 500, 142-148. Wang, L., Tang, L., Wang, X., Chen, F. 2010. Effects of alley crop planting on soil and nutrient losses in the citrus orchards of the Three Gorges Region. Soil and Tillage Research, 110 (2), 243-250. Wu J., Li Q., Yan L. 1997. Effect of intercropping on soil erosion in young citrus plantation - a simulation study. Chinese Journal of Applied Ecology, 8 (2), 143-146. Wu, D.-M., Yu, Y.-C., Xia, L.-Z., Yin, S.-X., Yang, L.-Z. 2011. Soil fertility indices of citrus orchard land along topographic gradients in the three gorges area of China. Pedosphere, 21 (6), 782-792. Xu, Q., Wang, T., Li, Z., Cai, C., Shi, Z., Jiang, C. 2010. Effect of soil conservation measurements on runoff, erosion and plant production: A case study on steeplands from the Three Gorges Area, China. Journal of Food, Agriculture and Environment, 8 (3-4 PART 2), 980-984. Xu, Q.X., Wang, T.W., Cai, C.F., Li, Z.X., Shi, Z.H. 2012. Effects of soil conservation on soil properties of citrus orchards in the Three-Gorges Area, China. Land Degradation and Development, 23 (1), 34-42.
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NASA Astrophysics Data System (ADS)
Thiry, M.; Liron, M. N.
2009-04-01
Landscape features The geomorphology of the Fontainebleau Massif is noteworthy for its spectacular narrow ridges, up to 10 km long and 0.5 km wide, armored by tightly cemented sandstone lenses and which overhang sandy depressions of about 50m. Denudation of the sandstone pans lead to a highly contrasted landscape, with sandstone ridges ("platières") towering sandy depressions ("vallées") and limestone plateaus ("monts"). This forms the geological frame of the spectacular sceneries of the Fontainebleau Massif (Thiry & Liron, 2007). Nevertheless, there is little know about the erosive processes that have built-up these landscapes. Periglacial processes, and among them aeolian ones, appear significant in the development of the Fontainebleau Massif physiography. The periglacial aeolian geomorphology Dunes and dune fields are known since long and cover about 15% to 25% of the Fontainebleau Massif. The aeolian dunes developed as well on the higher parts of the landscape, as well as in the lower parts of the landscape. The dunes are especially well developed in the whole eastern part of the massif, whereas the western part of the massif is almost devoid of dunes. Nevertheless, detailed mapping shows that dunes can locally be found in the western district, they are of limited extension, restricted to the east facing backslope of outliers. Loamy-sand covers the limestone plateaus of the "monts". The loam cover is of variable thickness: schematically thicker in the central part of the plateaus, where it my reach 3 m; elsewhere it may thin down to 0,20-0,30 m, especially at the plateau edges. Blowout hollows are "negative" morphologies from where the sand has been withdrawed. Often these blowouts are decametric sized and well-delimited structures. Others, more complex structures, are made up of several elongated hectometric hollows relaying each other from and which outline deflation corridor more than 1 km long. A characteristic feature of these blowout hollows is the erosion of the sand beneath the bordering sandstone benches, resulting in overhangs. These structures are the most common in the western district of the Fontainebleau Massif. Ponds develop on the tightly silicified and impermeable sandstone pans that form the "platières". There are permanent ponds and temporary wet zones, formed of interconnected or isolated depressions. The origin of these ponds has to be questioned with regard to the landscape shaping. Their origin is directly bound to the hollowing of uncemented, sandy zones, within the sandstone pans forming the "platières". Erosion by runoff cannot be considered; the only way to hollow them out is by deflation processes. No direct dating of the Quaternary dune and loess deposits of the Fontainebleau Massif exists. Nevertheless, dating of paleopodzols interlayered between drift sands, pond deposits and bones within congelifracts allow relating these periglacial features with the end of the last glacial period. For now, there is no dating to assess what belongs to older glacial periods. Distribution of the aeolian patterns The Fontainebleau Massif displays noteworthy morphological diversities in the various districts of the forest. Some of these differentiations result from geological features, but most of them are related to erosion processes, and among them deflation processes leaved different imprints in the western and eastern districts of the Fontainebleau Massif. The topography played an important role controlling the aeolian processes. Deflation was important in the westerly upwind district. In the westerly front face, aeolian erosion was activated by turbulences around the topographic obstacles. The reliefs funneled the winds and gave rise to swirls that hollow the blowouts. This area displays the sharpest and more chiseled landforms of the massif. Moreover, the sandstone scarps at the edge of the "platières" are high and uncovered, with frequent overhangs. The collapsed sandstone blocks of the "chaos" are imposing, with blocks piling up and rising well off the sandy slopes. The sandstone "platières" are mostly bare as say above. Downwind, in the eastern district, the landforms are more subdued. The deflation is less extensive, the sandstone scarps and chaos are partly sanded up, with drift sand amassing at the lee side of the scarps. The "platières" have a sand cover that favours often the development of a tree stratum composed almost entirely of pine and birch trees. Aeolian landforms and biodiversity Despite the Atlantic climate forest cover and the human interventions, the imprints of the aeolian features inherited from the Quaternary periglacial climates still mark deeply the Fontainebleau landscapes. The aeolian actions command partly the present-day relief and vegetation biodiversity: (1) Tall oak and beech groves on the plateaus and in the lowlands covered with fine calcareous sand dunes and loess on which develop brown soils (prevailing in the eastern district of the massif); (2) Birch, pine trees and herbaceous stratum on the dry and acidic podzols established on the quartzose Fontainebleau Sand forming the windup scraps, sandstone chaos and associated dunes (dominant in the western district); (3) And finally dry moors with calluna, heather and birch on the sandstone "platières" stripped off by the aeolian deflation together with wet and peaty moors with sphagnum and moor-grass in the blowout depressions. The opposition between the western and the eastern districts of the massif was even more pronounced a few centuries ago, before man intervened vigorously to wooden the western area with massive import of pine trees. This phytogeographical diversity of the landscape is directly inherited from the periglacial aeolian actions and contributes to the striking biodiversity of the Fontainebleau Massif. The biological richness of the Fontainebleau Massif has been noticed as soon as 1664 (Barillon d'Amoncourt, 1664) and today have been inventoried 6.000 vegetable species among them 1350 flowering plants, some 460 mosses, about 500 algae, 675 lichens, 2.700 fungus, plus the insects, the birds, the mammals and batrachians (Testut et al., 1998). This exceptional biodiversity has been recognized in 1998 by the creation of a reserve of "Man and Biosphere" under the aegis of UNESCO. The "platières" landscapes are of special interest for biodiversity. The acidic soils on the sandstone "platières" are mainly covered by Atlantic moors. The dry moors with Calluna vulgaris and Erica cinerea relate to the Ulici-Ericion cinereae and the wet peaty moors are linked to the Ulici-Ericion tetralicis (Habitats 31.11 and 31.2 of the Corine Biotope Code). These dry and peaty moors interweave in a complex patchwork depending on the local, even metric scale, topography and soil moisture. The main interest in the flora of the "platières" lies in the vegetation of the network of pools, which develop in the sandstone depressions (Liron & Thiry, 2005). These wet zones include seven Natural Habitats of Community interest and nearly twenty protected plants species. The temporary ponds (Habitat 22.31 of the Corine Biotope Code), with an irregular hydraulic regime, favor a suite of annual plants, outstanding "intermittent" species, such as the endemic Franco-Iberian Ranunculus nodiflorus. In the acidic and oligotrophic waters of the permanent pools develop Utricularia australis along with Potamogeton polygonifolius. The peaty zones are valuable for their bryophyte biodiversity. For example thirteen species of Sphagnum (30 % of the European flora) have been recorded including Sphagnum magellanicum which is a rare species in the lowlands. There is also a wealth of bryophytes and lichens on the strata, with for instance fifty species of the lichen genus Cladonia. This species richness is strengthened by the limited area of the "platières" which represent only 15-20% of the whole massif. Main biodiversity interest is related to the almost bare "platières" of the western district eroded by deflation. The eastern platières that have a more continuous sand cover are support much less wet zones and only very few sites with protected plant species. Therefore, aeolian landscape evolution still triggers development and distribution of peculiar ecological sites. It suits to continue and to deepen the cartographic studies and the inventories to highlight these very particular landscapes of the Fontainebleau Massif and to protect them. Indeed, with 17 millions visitors per year, the problems are now mainly of managing natural areas, let them accessible, while protecting them. In the future, with forecasted climatic changes, a main concern will be how to preserve the biodiversity, knowing that the foresters manage generally the forest with a 150 years plan. Education and awareness campaign of the public and of the local actors of the sustainable development are essential, they require the knowledge of these fragile environments inherited from the past. References Barillon d'Amoncourt P., 1664-1665. Réformation générale de la forest de Bière et des autres bois dépendants de la maîtrise des Eaux et Forets du Baillage de Melun établie à Fontainebleau. Archives Départementales de Seine et Marne, France. Liron M.N., Thiry M., 2005, Peaty micro-zones on the sandstone ridges of the Fontainebleau Massif (France): hydrology and vegetation biodiversity. in : Ch. Ries & Y. Krippel (eds.), Sandstone landscapes in Europe. Past, Present and Future. Proceedings of the 2nd Intern. Conference on Sandstone Landscapes, Vianden (Luxembourg), 25-28 may 2005, Ferrantia, Luxembourg, 44, p. 215-220. Testut A., Hermeline M., Rey G., 1998. Lettres de la Forêt. Fontainebleau, abcédaire photographique. Textuel Ed., Paris, 223 p. Thiry M., Liron M.N., 2007, Fontainebleau Sandstones (France). In : Härtel H., Cílek V., Herben T., Jackson A. and Williams R. (eds.): Sandstone Landscapes.- Academia, Praha, p. 359-361.
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NASA Astrophysics Data System (ADS)
Cerdà, Artemi; Giménez-Morera, Antonio; Jordán, Antonio; Pereira, Paulo; Novara, Agata; García-Orenes, Fuensanta
2014-05-01
Not only the Sahel (Haregeweyn et al., 2013), the deforested land (Borelli et al., 2013) the chinese Plateau are affected by intense soil erosion rates (Zhao et al., 2013). Soil erosion affect agriculture land (Cerdà et al., 2009), and citrus orchards are being seeing as one of the crops with the highest erosion rates due to the managements that avoid the catch crops, weeds or litter. Example of the research carried out on citrus orchards is found in the Mediterranean (Cerdà and Jurgensen, 2008; 2009; Cerdà et al., 2009a; 2009b; Cerdà et al., 2011; 2012) and in China (Wu et al., 1997; Xu et al., 2010; Wang et al., 2011; Wu et al., 2011; Liu et al., 2011; Lü et al., 2011; Xu et al., 2012), and they confirm the non sustainable soil losses measured. The land management in citrus plantations results in soil degradation too (Lu et al., 1997; Lü et al., 2012; Xu et al., 2012). The use of cover crops to reduce the soil losses (Lavigne et al., 2012; Le Bellec et al., 2012) and the use of residues such as dried citrus peel has been found successful. There is a need to find new plants or residues to protect the soils on citrus orchards. Agriculture produces a high amount of residues. The pruning can contribute with a valuable source of nutrients and a good soil protection. The leaves of the trees, and some parts of the plants, once harvest can contribute to reduce the soil losses. Due to the mechanization of the agriculture, and the reduction of the draft animals (mainly horses, mules, donkeys and oxen) the straw is being a residue instead of a resource. The Valencia region is the largest producer of citrus in Europe, and the largest exporter in the world. This citrus production region is located in the eastern cost of Spain where we can find the rice production area of the l'Albufera Lagoon paddy fields, the third largest production region in Spain. This means, a rice production region surrounded by the huge citrus production region. There, the rice straw is not used in the paddy fields after harvesting and the straw is being as a residue that damages the air quality when burnt, the water quality due to the decomposition and the methane production, and is not accepted in the field by the farmers. This is a new problem as few years ago the rice straw was use for animal feeding. Many attempts were developed in the last decade to remove and use the straw to avoid fires and water pollution (Iranzo et al., 2004; Silvestre et al., 2013). Our goal is to test if a residue such as the rice straw can be transformed as a resource: soil erosion control. Straw has been seen as a very efficient to reduce the water losses in agriculture land (García Moreno et al., 2013), the soil losses in fire affected land (Robichaud et al., 2013a; 2013b; Fernandez and Vega, 2014), and soil properties (García Orenes et al., 2009; 2010; Jordán et al., 2010; García Orenes 2012). Rainfall simulations under 55 mm h-1 rainfall intensity during one hour on 0,25 m2 plots were carried out on plots paired plots: bare and covered with straw. The plots covered with straw had different straw mulch cover: from 10 to 100 % cover and from 0,005 g m2 to 300 g m2. The results show a positive effect of the straw cover that show an exponential relation between the straw cover and weight with the sediment yield. Acknowledgements The research projects GL2008-02879/BTE, LEDDRA 243857 and RECARE supported this research. References Bombino, G., Denisi, P., Fortugno, D., Tamburino, V., Zema, D.A., Zimbone, S.M. 2010. Land spreading of solar-dried citrus peel to control runoff and soil erosion. WIT Transactions on Ecology and the Environment 140,145-154. Borrelli, P., Märker, M., Schütt, B. 2013. Modelling post-tree-haversting soil erosion and sediment deposition potential in the Turano River Basin (Italian Central Apennine). Land Degradation & Development, DOI 10.1002/ldr.2214 Cerdà, A., Flanagan, D.C., le Bissonnais, Y., Boardman, J. 2009. Soil erosion and agriculture Soil and Tillage Research 106, 107-108. DOI: 10.1016/j.still.2009.1 Cerdà, A., Jurgensen, M.F. 2008. The influence of ants on soil and water losses from an orange orchard in eastern Spain. Journal of Applied Entomology 132, 306-314. Cerdà, A., Jurgensen, M.F. 2011. Ant mounds as a source of sediment on citrus orchard plantations in eastern Spain. A three-scale rainfall simulation approach. Catena 85, 231-236. Cerdà, A., Jurgensen, M.F., Bodi, M.B. 2009. Effects of ants on water and soil losses from organically-managed citrus orchards in eastern Spain. Biologia 64, 527-531. Cerdà, A., Morera, A.G., Bodí, M.B. 2009. Soil and water losses from new citrus orchards growing on sloped soils in the western Mediterranean basin. Earth Surface Processes and Landforms 34, 1822-1830. Lavigne, C., Achard, R., Tixier, P., Lesueur Jannoyer, M. 2012. How to integrate cover crops to enhance sustainability in banana and citrus cropping systems. Acta Horticulturae 928, 351-358. Fernández, C., Vega, J.A. 2014. Efficacy of bark strands and straw mulching after wildfire in NW Spain: Effects on erosion control and vegetation recovery. Ecological Engineering 63, 50-57 García-Moreno, J., Gordillo-Rivero, Á.J., Zavala, L.M., Jordán, A., Pereira, P. 2013. Mulch application in fruit orchards increases the persistence of soil water repellency during a 15-years period. Soil and Tillage Research 130, 62-68. García-Orenes, F., Cerdà, A., Mataix-Solera, J., Guerrero, C., Bodí, M.B., Arcenegui, V., Zornoza, R. & Sempere, J.G. 2009. Effects of agricultural management on surface soil properties and soil-water losses in eastern Spain. Soil and Tillage Research 106, 117-123. 10.1016/j.still.2009.06.002 García-Orenes, F., Guerrero, C., Roldán, A.,Mataix-Solera, J., Cerdà, A., Campoy, M., Zornoza, R., Bárcenas, G., Caravaca. F. 2010. Soil microbial biomass and activity under different agricultural management systems in a semiarid Mediterranean agroecosystem. Soil and Tillage Research 109, 110-115. 10.1016/j.still.2010.05.005. García-Orenes, F., Roldán, A., Mataix-Solera, J., Cerdà, A., Campoy, M., Arcenegui, V., Caravaca, F. 2012. Soil structural stability and erosion rates influenced by agricultural management practices in a semi-arid Mediterranean agro-ecosystem. Soil Use and Management 28, 571-579. DOI: 10.1111/j.1475-2743.2012.00451.x Haregeweyn, N., Poesen, J., Verstraeten, G., Govers, G., de Vente, J., Nyssen, J., Deckers, J., Moeyersons, J. 2013. Assessing the performance of a Spatially distributed soil erosion and sediment delivery model (WATEM/SEDEM) in Northern Ethiopia. Land Degradation & Development 24, 188-204. DOI 10.1002/ldr.1121 Iranzo, M., Cañizares, J.V., Roca-Perez, L., Sainz-Pardo, I., Mormeneo, S., Boluda, R. 2004. Characteristics of rice straw and sewage sludge as composting materials in Valencia (Spain). Bioresource Technology 95, 107-112 Le Bellec, F., Damas, O., Boullenger, G., Vannière, H., Lesueur Jannoyer, M., Tournebize, R., Ozier Lafontaine, H. 2012. Weed control with a cover crop (Neonotonia wightii) in mandarin orchards in Guadeloupe (FWI). Acta Horticulturae 928, 359-366. Liu, Y., Tao, Y., Wan, K.Y., Zhang, G.S., Liu, D.B., Xiong, G.Y., Chen, F. 2012. Runoff and nutrient losses in citrus orchards on sloping land subjected to different surface mulching practices in the Danjiangkou Reservoir area of China. Agricultural Water Management 110, 34-40. Lu, J., Wilson, M.J., Yu, J. 1997. Effects of trench planting and soil chiselling on soil properties and citrusproduction in hilly ultisols of China Soil and Tillage Research 43, 309-318. Lü, W., Zhang, H., Wu, Y., Cheng, J., Li, J., Wang, X. 2012. The impact of plant hedgerow in Three Gorges on the soil chemicophysical properties and soil erosion. Key Engineering Materials 500 142-148. Robichaud, P.R., Lewis, S.A., Wagenbrenner, J.W., Ashmun, L.E., Brown, R.E. 2013a. Post-fire mulching for runoff and erosion mitigation. Part I: Effectiveness at reducing hillslope erosion rates. Catena 105, 75-92. Robichaud, P.R., Wagenbrenner, J.W., Lewis, S.A., Ashmun, L.E., Brown, R.E., Wohlgemuth, P.M. 2013b. Post-fire mulching for runoff and erosion mitigation. Part II: Effectiveness in reducing runoff and sediment yields from small catchments. Catena 105, 93-111. Silvestre, G., Gómez, M.P., Pascual, A., Ruiz, B. 2013. Anaerobic co-digestion of cattle manure with rice straw: Economic & energy feasibility. Water Science and Technology 67, 745-755 Wang, L., Tang, L., Wang, X., Chen, F. 2010. Effects of alley crop planting on soil and nutrient losses in the citrus orchards of the Three Gorges Region. Soil and Tillage Research 110, 243-250. Wu J., Li Q., Yan L. 1997. Effect of intercropping on soil erosion in young citrus plantation - a simulation study. Chinese Journal of Applied Ecology 8, 143-146. Wu, D.-M., Yu, Y.-C., Xia, L.-Z., Yin, S.-X., Yang, L.-Z. 2011. Soil fertility indices of citrus orchard land along topographic gradients in the three gorges area of China. Pedosphere 21, 782-792. Xu, Q., Wang, T., Li, Z., Cai, C., Shi, Z., Jiang, C. 2010. Effect of soil conservation measurements on runoff, erosion and plant production: A case study on steeplands from the Three Gorges Area, China. Journal of Food, Agriculture and Environment 8, 980-984. Xu, Q.X., Wang, T.W., Cai, C.F., Li, Z.X., Shi, Z.H. 2012. Effects of soil conservation on soil properties of citrus orchards in the Three-Gorges Area, China. Land Degradation and Development 23, 34-42. Zhao, G., Mu, X., Wen, Z., Wang, F., Gao, P. 2013. Soil erosion, conservation, and eco-environment changes in the Loess Plateau of China. Land Degradation & Development, 24, 499- 510. DOI 10.1002/ldr.2246SP
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hwhap_Ep30_Infamous Meteorites
2018-02-01
Gary Jordan (Host): Houston, We Have A Podcast. Welcome to the official podcast of the NASA Johnson Space Center, Episode 30, Infamous Meteorites. I'm Gary Jordan, and I'll be your host today. So on this podcast, we bring in the experts, NASA scientists, engineers, astronauts, all to let you know the coolest stuff about what's going on right here at NASA. So today, we're talking about some of the more unique findings that have been discovered in meteorites with David Mittlefehldt, goes by Duck. He's a planetary scientist here at the NASA Johnson Space Center in Houston, Texas, and we had a great discussion about curious findings in meteorites, and the adventures that are endured to procure them. So, with no further delay, let's go lightspeed and jump right ahead to our talk with Dr. Duck Mittlefehldt. Enjoy! [ Music & Radio Transmissions ] Host: Duck, thanks for coming to the podcast today. I know we've -- we've talked about searching for life and meteorites before, and it's -- it's such a fascinating topic, but I really wanted to dive deeper, just into like the meteorites portion. We really -- we really actually had a great conversation with Dr. Aaron Burton and -- and Dr. Marc Fries, not too long ago, actually, about life, but really just about the meteorites themselves. There's a -- there's a big story there, and you're one of the explorers that are going down and actually finding these meteorites, huh? Dr. Duck Mittlefehldt: Yeah, yeah. I've done that on a number of occasions. Host: Yeah. And it's -- is it -- is it mostly in Antarctica, or are you going other places? Dr. Duck Mittlefehldt: Well, okay, so most of the times I've been searching for meteorites has been in Antarctica, so I've been down there five times, meteorite collecting expeditions, but I -- I've [pause] -- I was on vacation in Israel once, and I met up with a couple of geologists at a coffee house, and one of them had just published a paper where they -- he described, you know, old surfaces in the deserts of southern Israel that are, you know, have been stable for about 2 million years. And I'm thinking, you know, over 2 million years, you can accumulate a lot of meteorites, so, I actually went there the foll -- later that year, and met up with them again, and we searched some of these areas that are -- have very ancient pavements on the desert, and hunting for meteorites. We didn't find any, unfortunately, and, you know, I'm not quite sure why, there -- there should have been some there, but, you know, it was a small team searching large area over short time, so it may well be that they're there, but we just didn't find any, because the ones that, you know, are there are small. The other is there were a number of issues with that particular location. Meteorites, you know, when we find meteorites, they're typically black on the outside, because they've gone through the atmosphere and they're covered with this glassy, fusion crust, which is almost always black. The area we had searched in southern Israel actually had a number of dark rocks in it, as well. So, you know, the meteorites, if they were there, would not have stood out as -- like -- like, you know, the beacons that you see when you're in Antarctica, scooting across the bare ice, so. Host: I guess that -- is that the main reason why Antarctica is such a great place to find meteorites? Is because it's these black rocks against white snow? Dr. Duck Mittlefehldt: Well, that certainly makes it easy, because [Gary laughing] you -- you can see, you know, a rock, I'm going to use metric units because that's what I'm used to, I'll try and remember to throw in inches and feet as I can, but, so, you know, you can find a -- a black rock, a couple of centimeters across or about an inch across, from a great distance in Antarctica on the ice. And -- and, as you say, it's because you're looking at either pale blue ice or sometimes white snow, most of the meteorites we find are on the pale blue ice. But even so, it's very bright in comparison to rock. So they're easy to find there. The other thing is in Antarctica, we have a convenient concentration mechanism, which is the actual flow and ablation of the ice across the continent, and where we go to find them the meteorites is -- is actually in locations where the ice movement has been stalled, and ablation by the Antarctic winds and -- and warming by the Antarctic sun, allow a lag deposit to develop on the surface. So we're actually collecting meteorites that have been, you know, shoved from a great geographic area and then left behind in a smaller geographic area. So we have, you know, base -- we have both the easy-to-spot and -- and the concentration mechanism working in our favor. Host: Alright! Yeah, they're -- they're plentiful down there. So -- so you made quite a few trips. How many was it? You said five? Dr. Duck Mittlefehldt: Yeah, I've been down five times. The first time was in the '97, '98 field season. That was my first Antarctic experience, and I loved it so much I kept volunteering to go back again. Host: You loved Antarctica? Dr. Duck Mittlefehldt: Oh yeah [Gary laughing], I -- I love it, you know, just -- just last week, well, here in Houston, we had temperatures that Houstonians think of, or Texans think of as cold, but, me, I see that as maybe a cold fall day. Because I -- I was born and raised in western New York. Host: Alright. Dr. Duck Mittlefehldt: And at the same time, you know, my hometown was getting temperatures, okay, again, I've got to do some conversion here, about maybe, you know, between 0 and 5 degrees Fahrenheit. And, you know, that was the weather I grew up in winter, and I loved it. Winter was always my favorite season when I was a kid. Alright. So maybe it's a deep love of winter that really -- because I just came from this -- we're just coming back from the holidays now, and it was -- it was negative 2 in Pittsburgh when I -- when I was flying home, and, I mean, I was -- I was born and raised in Pennsylvania, moved around a lot, but I'm not used to it by any means. Like, I like the -- I like the, everyone, you know, saying, oh my gosh, 32 is really cold! And I'm like, [laughing], I'm okay with just that. Host: For me, I -- I loved the deep winter in western New York. Dr. Duck Mittlefehldt: Alright, a lot of snow there too. Host: So when was the last time you were down in Antarctica then? Dr. Duck Mittlefehldt: So I was down last year, 2016, 2017, it was kind of a disappointment for me, personally. Host: Oh. Dr. Duck Mittlefehldt: I -- I -- because of my experience, I've been down four times before, I -- I left early and was going to go out on a recon sweep with the -- the mountaineer field safety officer for the ANSMET program. ANSMET, by the way, stands for Antarctic Search for Meteorites, and that's the program that goes down to collect the rocks and has been doing so every year, but once, since 1976. Host: Alright! Dr. Duck Mittlefehldt: But, anyway, because of my experience, I was going to go down on this recon before the main season. We were going to go to one area, check it out for potential systematic work in a future season, and then stay for the first half of the main season, going to a location deep along the Antarctic, transAntarctic mountains. Well, it turns out logistics were badly broken last year. And partly because of weather, partly because of problems with the aircraft and so on, so I got out into the field for a week, in preseason, I got back to McMurdo Station while we were gearing up for the main season, but the logistics just broke and so they were not going to go out where they originally planned. The team ended up going to where I had been out on recon, but it was -- they got such a late start that it made more sense to ship me home early rather than, you know, go out for maybe a week and then come back into McMurdo and go home. Host: Yeah. Dr. Duck Mittlefehldt: So I -- I just spend one week out in the field last year. Host: Ahh... Dr. Duck Mittlefehldt: Much -- much to my chagrin. Host: [Laughing] So it was just the lack of time that you spent there, that was really the disappointment. Yeah, yeah, it was [inaudible] time, and, you know, in the brief time that John Scott [phonetic] and I, he's the mountaineer, were out on the ice, you know, we -- we'd spend a week in the field, two and a half days we were tent-bound because the weather was so bad, but even so, we found 46 meteorites in the short time we were there. Host: That's amazing! Yeah. Host: Wow. Dr. Duck Mittlefehldt: And -- and remind -- and remember, this was an area that had been heavily harvested back in the 80's, 70's and 80's, we were going to back to see whether there was still great potential for harvesting more meteorites there, and, in fact, I think last year they ended up coming -- picking up a total of 200 and some meteorites, even with, you know, going back to an area that had been searched before, and having a shortened season because the logistics. So, I mean, that -- that kind of shows you the -- the quality of Antarctica as a -- as a site for bringing back space rocks. It's just awesome! Host: Incredible! So is -- is that -- is it because there's just a fresh, I guess you could call it, supply of meteorites that are landing on the surface of Antarctica, or is it things are shifting? Dr. Duck Mittlefehldt: It's more things are shifting. In part, you know, deflation of the surface continues, as ablation goes on, and so new meteorites are poking through. In part, it's shifting winds blowing snow around, so an area that might have been snow covered earlier season, maybe now has been stripped bare and there's bare ice. And so that allows you to see things. So for a variety of reasons, you can go back to the same place you've searched once, and -- and still find meteorites out there. Host: Incredible. And hundreds of them, a little bit better than Israel, right? Dr. Duck Mittlefehldt: Yeah [laughter]. Might have been better than my experience trying to find meteorites in the Negev Desert. Host: [Laughing] So -- so you're saying a season. When you're going down to Antarctica, I'm assuming it's the summer there, right? Dr. Duck Mittlefehldt: Yeah, it's austral summer. Host: Yeah. So that means the sun is up 24/7, right? Dr. Duck Mittlefehldt: Right. Host: So you kind of have to deal with that when you're -- when you're down there, right? Dr. Duck Mittlefehldt: Yeah, you know, I've -- I've become accustomed to that. The first -- I was kind of -- there was a guy who used to work in our building who had been down I think a year or two before me, so I took advice from him, and he said, you know, one of the things is, you know, with the constant sunlight, sometimes sleep can be a problem. So I bought a heavy, black knit hat, and, you know, I just put that on as my sleep hat, and then pulled the brim over my eyes, and so everything was black. So I -- I could sleep fine down there. Host: Oh, nice! Dr. Duck Mittlefehldt: But the, you know, the main advantage is that because the sun's up 24/7, you're not really bound by the 9 to 5 time sequence. Host: Oh, yeah. Dr. Duck Mittlefehldt: So, as I said, when we -- when I was out last year in the -- in the recon site, we were there for a week, you know, we -- we landed, got our gear, and then went, spent a half a day out, then the -- the winds blew in, it was too windy and cold to go out, so the winds broke around noon one day, or a little bit after noon. We decided we would have an early supper and then go out and collect -- harvest meteorites. So that day, we ended up getting out of the tents maybe 5 o'clock in the evening, and we worked about till 30, 2 in the morning. Host: Woah! Dr. Duck Mittlefehldt: The sun was up, it was perfectly fine, it was just my age and body crapping out at 30 [Gary laughing]. I, you know, I just couldn't pick up another meteorite if -- if they beat me with a stick. You know, I was just so tired. But then, you know, that's -- that's something you can do down there that you can't do here. Host: Yeah, did you know the hours were going by, or did you have no sense of time with the -- with the sun being up? Dr. Duck Mittlefehldt: Well, you know, you can trace the sun, if you pay attention, you can get a sense of the day, because the sun does a lazy loop in the sky, and... Host: Oh. Dr. Duck Mittlefehldt:...and so, you know, once you've located yourself, you know where north, south is, [pause] there is still north and south, even that close to the pole. Host: Yeah. Dr. Duck Mittlefehldt: But, you know, you know at midnight, the sun is going to be, you know -- you know, at one -- at the one position, so. Host: Right. Dr. Duck Mittlefehldt: And it's kind of at the lowest point far north, and so, you know, you can track it that way, but basically I didn't pay attention. We were just so busy, you know, driving from place to place harvesting meteorites that, you know, it was just constantly moving, doing the next one, taking the data, collecting it, you know, cleanly and safely and getting it in the bag and moving on to the next location. Host: Oh, so are you -- are you not -- you're not stationary then when you -- when you kind of set up camp. Are you -- are you kind of mobile, like with your camp, and you just move it from one meteorite site? Dr. Duck Mittlefehldt: No, no. Host: Oh, okay. Dr. Duck Mittlefehldt: The camp is usually -- there are a couple -- there are a couple of ways that it is done. When we do systematic searching, the camp is stationary in one spot, perhaps for the whole field season, and you just go out, day-to-day, to different locations. And that's what we did here. We were on recon, so we -- we plunked the tent down, then we searched within easy skidoo range of the camp. Sometimes, and I've done this before, go down on a recon time, where -- where you go and you put camp down, you might prospect an area for two, three weeks, then you move camp to another area and prospect there for two or three weeks. So, there -- there are -- those -- there are those two types of scenarios, and even in the recon mode, you know, you're -- the tent -- the camp is stationary for two or three weeks, and you're skidooing all around that area to -- to search it, and then you only pick up tents and camp and move to a far distant area to recon that general region. Host: Alright! Alright, well I'm guessing, you know, going down there so many times, you're quite an expert in making sure that, you know, you can survive weeks and weeks and weeks in Antarctica. So, what are the -- some of the stuff that you're taking down there that I guess are unique to the Antarctic environment? Dr. Duck Mittlefehldt: Okay, so, most of the gear you get, you get in Christchurch, so, you know, living in Houston, I don't have a winter coat. Host: Oh! Dr. Duck Mittlefehldt: So, at -- at the clothing distribution center in Christchurch, you'll get outkitted -- outfitted with, you know, heavy -- heavy jackets, all the gloves you can want, thermal pants, fleece liners, boots, hats, everything you need to survive, and then in McMurdo Station, you actually get the camping gear, the tents, the cook stoves, the dishes, the food, sleeping bags, that sort of stuff. So all -- all the intrepid Antarctic explorer needs to take down with them are personal items, like I mentioned my knit hat, that -- that was mine, and that was because I knew I wanted something to sleep in. I, you know, I bought extra pairs of thermal underwear, because the first time I went down, you know, they -- they give you two sets, but you're out in the field for six or seven weeks, so you want to change, you know, once in a while. [Gary laughing] Other than that, you know, my glasses are prescription, and so I buy glasses that transition dark and sunlight, so I can just, you know, wear my normal glasses out on the skidoo, I have actually bought glacier glasses, so I have side shields and whatnot to block the light. You want to -- one of the things that really is critical down there is to block all light from your eyeballs, you know, other than what gets filtered through a dark lens, because, otherwise, snow blindness is a problem. Host: Oh, that's right! It's so bright down there, right? Yeah. Dr. Duck Mittlefehldt: So I do that, but, otherwise, you know, most of the gear they give you, they loan it to you for the time that you're out there, and -- and so, you know, you could survive on just what you get from the Antarctic program down in Antarctica. It wouldn't necessarily be entirely comfortable wearing the same clothes, you know, for seven weeks, but you could do it. Host: [Laughing] So -- so your -- this Antarctic program, that -- that's ANSMET, right? Dr. Duck Mittlefehldt: Right. Host: Okay, so what's the -- what's the relationship between ANSMET and NASA, and how that all works together? Dr. Duck Mittlefehldt: Well, originally, ANSMET was set up as a three agency agreement. So the -- the -- it was funded -- the actual Antarctic search for meteorites was funded through the National Science Foundation, because they have -- they do the scientific research in Antarctica. NASA funded the curation and allocation of meteorite samples here at NASA Johnson Space Center, and then the Smithsonian Institution did the initial classification and was the long-term repository for the meteorites collected in Antarctica. That, since -- since then, they've changed it, and now NASA actually funds the Antarctic, the ANSMET research component. NSF still supplies the logistics, but NASA pays NSF for those, those logistics, because they -- they are the, I mean, they have all the logistics in Antarctica. And -- and the rocks still go, ultimately, to the Smithsonian, a chip for initial classification, and rocks that are no longer actively being researched by scientists in the world end up being permanently curated at the Smithsonian Institution. So that is -- that is still the way things are run. Host: Alright. So -- so is the ones that people are researching, and actively studying, are all of them housed here at the Johnson Space Center? Dr. Duck Mittlefehldt: Yes. With some exceptions. We don't have the necessary facilities to easily deal with metal-rich meteorites. So iron meteorites, stony iron meteorites, automatically go, ah, nope, I'm going to pull that back. Iron meteorites automatically go to the Smithsonian Institution. Because they are equipped for -- to cut metal and -- and make samples available. We do do the stony meteorites here, I forgot about that, because I've gotten some from here. So those that have a significant stony component are still worked on here until they become no longer of scientific interest. But, you know, even though they go to the Smithsonian for permanent curation, they're -- they're not dead to science, so to speak. So I can request samples that have been housed at Johnson Space Center for years, and now transfer -- transformed permanently to the Smithsonian if -- if I find, you know, an interesting project to do on one of these old samples. And I actually have gotten, in the past, some samples from the Smithsonian that were originally from the Antarctic collection. Host: Wow. So back in Antarctica, when you're looking at these meteorites and you're trying to, you know, figure out what they are, are they, you know, more stony, more metal-rich, what are you using to -- to look at them, to find out more about them and say, yes, that's a meteorite that I want to get my hands on? How do you know what's the good stuff? Dr. Duck Mittlefehldt: Uh, decades of experience. Host: There you go [laughing]. Dr. Duck Mittlefehldt: So, I, you know, I can look at a rock in Antarctica, and I can already make a preliminary classification. Sometimes I'm wrong, and -- and, you know, the guy who has more experience than anyone is -- is our mountaineer field safety officer, John Scott, and, you know, he -- he can look at a rock, and, in many cases, give a pretty good guess as to what it's going to turn out to be. And, you know, I can do that with a lot of different types of rocks, especially those that I'm interested in, but all in all, there -- there are always those meteorites that come back that either no one has ever seen before, because it's totally new, or it's enough different from the norm for that class that it just doesn't -- doesn't appear to be what you think it is, in hand sample. So, and we don't -- and we don't, you know, in Antarctica, we don't do anymore than a very high-level classification. Yes, this is a stony meteorite, it's probably a chondrite, this is probably a carbonaceous chondrite, this is probably an achondrite, which is a type of meteorite that's been melted. This is probably a stony iron, an iron, and so forth. And, to some extent, we need to do that because certain types of meteorites have more scientific value than others. So -- so, for example, a very primitive carbonaceous chondrite is -- is probably going to get a lot of research attention when it's announced. And so we collect those in a special way to try and minimize contamination by organic compounds. And that's why we need to be able to say, oh, yeah, you know, stand back from this guy, we need to treat him differently than -- than this one over here. Host: Alright. And then, obviously, you know, knowing where to ship it too, right? Because some of the metals one have to go the Smithsonian...? Dr. Duck Mittlefehldt: So that -- no, that's all done here. Everything is shipped here to Johnson Space Center. Host: Oh, everything comes here, okay. Dr. Duck Mittlefehldt: And -- but the difference is when they -- when they open some that are listed in the -- in the notes as probably being iron meteorites, they -- they will warm them up in the dry nitrogen cabinets, look at them, and if they agree, you know, they'll do an external description, you know, this is a brown rock, you know, 10 centimeters in size and weigh so much, and we don't see anything in it, you know, out of the ordinary, from the outside, then the whole thing will -- then that whole rock will get shipped to the Smithsonian at that point, and there, they'll cut it open with a wire saw, if it's, you know, indeed, probably metal, and then make a polished mount and etch it to bring out the texture and so forth. Host: Alright! And then that's what you mean by the facilities, right? They have the -- the proper facilities to do that. So what about here? What kinds of equipment and facilities do we have to make sure that we're handling all of this properly? Dr. Duck Mittlefehldt: So, in the meteorite processing lab, we have [pause] -- we use tools of a very limited set of composition. So, typically, stainless steel hammers and chisels, and -- and the reason is, you know, no matter what we do with a rock from space, we're going to contaminate with something from earth. So the object is to, one, minimize that contamination. So we use materials that we know are not going to, you know, just shed particles everywhere, for example, but also if we -- we use always the tools of the same -- of a given composition so that we know that if we see something like this in the rock, oh yeah, that must have come from the tool. And, you know, I've seen this, rocks are hard to break, and so, you know, your -- your choices are to saw them open or to use a hammer and chisel, and I have seen on a rock that I've gotten, a flake from the chisel that rubbed off. Metal, you know, it's soft, even hardened steel will rub off on occasion. So, you know, I can see this, I can pull that contaminant off or isolate it, in the lab, but, you know, I know then I can do a simple test, yes, that's from the chisel, I don't have to worry about that. I've taken care of it, the rest of the sample is fine. So the object is to minimize contamination or to know what the potential contaminants are. And, you know, there's no way you know of getting -- there's -- with modern technology, we can't, you know, we don't have magnetic levitation devices that we then use a laser to slice them open cleanly. You know, we -- we do with what we got. This isn't Star Trek here yet. Host: [Laughing] We'll just stick with the hammer and chisel for now. So, I mean, when you're cutting these open, and you open them up, what -- what are you looking at? Are you looking at just the rock or are you taking even smaller chunks of that? How is that working? Dr. Duck Mittlefehldt: Well, that all depends on the question that you're trying to answer, and I've done both where I've asked for samples of a, what's called a bulk sample of the rock, so something as representative of the entire rock as possible, and I've looked for individual class in the rock, little fragments that are of a specific type within the rock. All of this is basic 19th century geology, in many respects. You know, in the 19th century, geologists would go out in the field with their hammers, they'd -- they'd beat on a rock and use a hands lens to look at the microscopic, yeah, microscopic texture, mineralogy in it, and, you know, a trained geologist can do the same with a meteorite, and say, yeah, okay, I can see -- I can see what this is, it's a certain type of rock type in there, and that's what I want, I don't want this part over here. So, you know, the traditional geologic methods,but with modern equipment, can be used, and -- and, you know, there's -- there's nothing like the human eye in the brain for sorting out who's who in the zoo. Host: [Laughing] So then how can you -- what -- what are some of the key differences for the -- for the non-geologically-trained eye for whenever you're looking at a rock and you can, you know, you cut it open and you look and you say, that's a meteorite, that's not from earth? Or, this is definitely from earth? Dr. Duck Mittlefehldt: Okay, the -- the first key is -- - is fusion crust. I mentioned this earlier. Host: Oh yeah. Dr. Duck Mittlefehldt: And that -- that's where, going through the atmosphere, friction with the air causes the outer surface to melt, and actually, you know, little bits are flying off all the time, the meteorite we get on the surface is just a small piece of what entered the atmosphere. Most -- sometimes the vast majority of it just ablated away in the atmosphere into little droplets or dust. Host: Wow. Dr. Duck Mittlefehldt: So, you know, if you see a fusion crust on the rock, right away, you know it's -- it's a meteorite, you don't have to go any farther than that. In terms of determining what type it is, more primitive meteorites, these are a type that still have textures and mineralogy that were inherited from condensation and accretion in the solar nebula, that's where individual mineral grains formed out of a gas that -- that was the nebula before the planets were around. And -- and then they glomerate together, these mineral grains, and in the -- in the solar nebula, the dust grains banged, you know, got melted into little, tiny objects which we call chondrules. So, these typical textures are plainly evident to the human eye, even without a microscope. But, you know, with a very low-power microscope you can see them quite easily. Most meteorites, especially primitive ones, contain iron metal, it's actually iron nickel metal. You know, you don't find that on earth except when humans have been involved in -- in smelting iron ore. But so iron metal in a -- in a rock is kind of an indicator that it's quite likely from outer space. Very few occurrences on earth of native metal in a rock. And then, as I said, in the dust in the solar nebula, went through periods of melting and formation of these little, round globules of basically melt globules, which we call chondrules, and -- and from that, we get the name chondrite for these primitive rocks. Well, those stand out in, you know, if you break open a rock, depending on -- on the type, you know, you can see those quite easily, and -- and that's a key. Host: And these have never -- they've been in space for all of time, right? They were formed in space and traveling through space, they've never -- they're not like from another planet or another, like, chipped off another...? Dr. Duck Mittlefehldt: Well, most...no, actually, all meteorites, the only way we get meteorites is for bad things to happen in the asteroid belt. Most meteorites are from asteroids, and when they collide, little fragments get knocked off, and it's -- it's from these fragments that we get meteorites. So they were originally on much larger bodies, I mean, much larger meaning asteroid size, not planet size. Host: Okay. Dr. Duck Mittlefehldt: And they were broken up and then distributed to the earth. You know, one of the, sorry, I'm going to -- I'm going to sort of go back into -- and get into my way back machine and go back to when I was a grad student. Host: Please do! Dr. Duck Mittlefehldt: When I -- you know, when I first started learning about meteorites, one of the mysteries at the time was there was a group of chondrite meteorites called the L chondrites, L was just the name, you know, the -- the name applied to them. That had ages on the order of 500 million years, and this was really odd, because all meteorites are about four and a half billion years old. Well these, they -- they -- these meteorites were originally about four and a half million -- billion years old, but were somehow affected by an event that reset the ages about 500 million years ago. Host: Woah. Dr. Duck Mittlefehldt: And so, you know, this was, you know, just kind of an anomaly. We knew something bad had happened to an asteroid then, about that time, well, fast forward to, I think the 90's, a Swedish geologist started finding in terrestrial sediments fossil meteorites. And, you know, all that's left is a few mineral grains. You -- you can tell, they were found in fine grain limestone, you know, formed on an ocean floor, and all that you could see was this halo of odd stuff, please a few mineral grains that remained from the original meteorite. Well, you know, this guy, and his compadres, studied these mineral grains and they -- they found out they were from the same type of meteorite as these chondrites that were about 500 million years old, and they were in layers in the rock of the earth that were about that age. So, sometime, 500 million years ago, you know, a couple of asteroids collided, and a whole rain of meteorites of this type hit the earth at about, you know, within a few million years when that occurred, and we can find them now. This layer in Sweden that's just chock full of these fossil meteorites. And, you know, to me, that's one of these really neat kind of science stories. Where everything starts tying together. And then to get even further, astronomers looking at what they call asteroid families, so they -- they find an asteroid, they find a whole bunch in orbits similar to it, spectroscopically, they all look to be about the same, and so they -- they figure out, well, these are all, you know, fragments of something that broke apart. Well, they found an asteroid that they figure, you know, based on the spectroscopy, it could be this type of, you know, that formed these L chondrites, and the -- they calculate the age of the family based on dispersion of the fragments, and it's about 500 million years. So, you know, between, you know, meteorite scientists, terrestrial geologists, and astronomers, we -- we've kind of got a neat picture of somehow, you know, about the time of dawn of -- of multicellular life on earth, two asteroids smashed together, and rained down on the earth, and we're still finding fragments coming down to earth now that we can confidently date when this happened in terrestrial laboratories. It's just kind of one of these things that, you know, I find fascinating! Host: [Laughing] I find it -- I mean, a lot of this is over my head, because I don't have the same background as you, but I just find it fascinating that you can look at these rocks and -- and get a story, get a story out of it, you know? Like the story of two asteroids around the time that cellular life was developing coming down to earth and raining down in these locations and telling their story, that's fantastic! Dr. Duck Mittlefehldt: Yeah, and multicellular. So this is when... Host: Multicellular. Dr. Duck Mittlefehldt: This is when, you know, fossils, shortly after the time when fossils started becoming really abundant in the terrestrial record. Host: Wow. Dr. Duck Mittlefehldt: So, yeah, it's just a neat story, and, you know, basically I think that's what got me into geology, originally, was, you know, all you've got is -- is a rock on the surface and somehow you can, you know, if you're smart enough and -- and do the right work, you can start to piece together an entire story of what the earth was like at that time, and so, you know, that's kind of what drew me into geology. Host: That's fantastic. I love it! Especially from -- from my background, marketing and journalistic sort of background, the story telling aspect is just fascinating to me. And that's kind of like, that, you know, the title of this episode is going to be, Infamous Meteorites, and that's kind of like what I really wanted to dive into is, you know, we've talked about where you're finding these meteorites, and then what you're doing with then, you're actually cracking them open and studying them, but then what are you finding? What are you finding inside of these meteorites? What stories? Dr. Duck Mittlefehldt: Yeah. Well, exactly! Host: Yeah, so, you know, one of the ones that I know that was brought to my attention was one of them called Allan Hills, and -- I'm going to -- is it 84001, or do you call it by something else? Dr. Duck Mittlefehldt: No, I call it that. Host: 84001? Okay. Dr. Duck Mittlefehldt: Sometimes it's simply referred to as that rock. Host: [Laughing] Because it's that infamous, huh? Wow! Alright, so what's the story behind -- behind this rock? Dr. Duck Mittlefehldt: Okay, so, this came -- this was found in Antarctica in 1984. And it -- it's [pause] -- it was originally classified as a -- as a type of asteroidal igneous rock that I, at the time, I was studying those -- those types of rocks. You know, my -- my background is heavily-weighted towards an interest in magnetic processes on the earth, the moon, Mars, and asteroids, and -- and so that's why this one was particularly of interest to me. So, I was studying that, along with a bunch of others, that were thought to be basically the same classification of rock, and, unfortunately, Allan Hill's had some puzzling features in it that were -- were a little bit off normal for -- for that rock type. But not so much so that I -- I really stayed up at night worrying about it. Host: [Gary laughing] Dr. Duck Mittlefehldt: And so I wrote a paper on -- on this group of rocks, finally, and sent it in, and one of the reviewers said, well, you know, you point out that there's this anomaly in this rock, and you really ought to try and chase down why it's -- what's going on there, why it's different. And, you know, being a -- a moderately good scientist, I said, okay. I, you know, he has pointed out, it's a problem, I knew it was a problem, but now I've really got to do something about it. So I started working at it, and, honestly, I -- I could not find out what was wrong with this particular rock. It -- it -- there was one mineral phase in it just did not match what anyone would expect for the class. Quite by chance, I got another sample of that rock for another reason. And but it really wasn't the sample I had asked for. So there was as mixup in the thin section. So a thin section is a very thin slice of a rock, it's about 30 microns thick, doubly polished on both sides, and it's used by people who look through microscopes to look at the minerals and textures in a rock, and then you can put that section into an electron microprobe and actually do analyses of the mineral phases in it. Host: Wow. Dr. Duck Mittlefehldt: And so I was -- that's what I was interested in. And this particular rock, which I thought I had, I was interested in the composition of sulfide phases in the rock. So I put the sample in the electron microprobe without actually looking at it in the microscope first, because I had seen this rock before, I knew what it was like, I knew what to expect, I just went straight to the electron microprobe, which actually probably was good because I may have turned the rock in and asked for a different one otherwise. But I'm getting -- I'm looking at it in the microprobe, looking for the mineral phases I'm looking for, and they just really aren't there in the abundance that I expected. Finally I found a grain and I'm -- I'm banging at it with the electron beam, collecting compositions, and the compositions weren't making sense. I was expecting it to be, so I was looking for sulfide phases, so I was expecting to have iron monosulfide, so one iron, one sulfur atom, and the composition that was coming out just was not right. And I checked the calibration, the calibration was perfect, so what's going on? I was looking at the data, not in atoms, but in mass, so weight percent. So when I converted it to atoms, I realized I had two sulfur atoms for every iron atom instead of one, and that's when it hit me what was wrong with this rock. I then backed off, looked at the -- looked at the texture in more detail in the electron microprobe, and realized I had a sample of Allan Hill's, not the meteorite that I thought I had, and I knew which type of rocks had pyrate, the iron disulfide, instead of the iron monosulfide, and I knew those were martian rocks. And so, you know, it was -- it was probably the most satisfying moment I've ever had in my life, excluding when my children were born, and -- and when I got married [Gary laughing], and if my wife listens to this, I hope she hears that, was, you know, suddenly it dawned on me that this was a martian rock that was totally unlike any other martian rock, except the key minerals were in it, and so, you know, it was just one of these aha moments that -- that you live for. And, you know, it was just so much fun. Host: Amazing. Dr. Duck Mittlefehldt: I tell you. Host: So what were those -- the key minerals? What -- what story did they tell? Dr. Duck Mittlefehldt: So the key was because it had the iron disulfide pyrate instead of the iron monosulfide troite, I knew it was martian, and it was a rock type not known amongst the martian meteorites. So what it meant was we had a new type of martian rock that was going to tell us even more about the geologic evolution of Mars then we already knew. And, you know, all of this hit me within like a fraction of a second when I realized what it was. Host: Wow! Dr. Duck Mittlefehldt: So, I mean, I immediately recognized it, it was an, you know, important meteorite. And that it would tell us big things, and, in fact, you know, it has opened up a whole host of, you know, basically this rock ultimately became a founding member of what you might consider astrobiology, and that came when my colleagues here at Johnson Space Center, Dave McKay, Edward Gibson, and Kathie Thomas and now Simon Clemett is at it, and then there were Simon's dissertation advisors, Stanford was on the paper and several other people, you know, they -- they proposed that a certain both mineralogical and compositional and textural objects in this rock were possibly signs of microscopic life that existed on Mars at one point. Host: Wow. Dr. Duck Mittlefehldt: And, you know, to some extent, then this really allowed the whole discipline of astrobiology to blossom because suddenly we had to figure out, you know, what -- how do we understand, how can we possibly search for life and other objects, other planets, you know, what do we need to look for? Because we're used to looking for life on earth, you know, it's -- it's simple. Just walking over here, I, you know, I had to wait while an opossum walked past me in front of, on the walkway. You know, life is everywhere on earth, whereas on Mars, you know, maybe it's not everywhere, and if it was there, how are we going to tell that it was there? What -- what do we need to do? So I would say the import of Allan Hill's not so much that it was hypothesized that life -- fossils of life are in that rock, but that it caused scientists to really take a much more rigorous look at how they will search for life other places of the universe. Host: Wow. And that's -- that's kind of, you know, like you said, the birth, maybe not the birth, but really the blossoming, and that was the word you used of, of astrobiology, life forming outside of earth. That's just a wild concept. How is that even possible? Dr. Duck Mittlefehldt: Yeah, and, you know, the other thing is it did, it was a strong impetus to driving NASA's Mars exploration program, you know, it is -- - a lot of it is geared towards finding evidence for habitability locations on Mars, and, ultimately, you know, from locations where we think there may have been a chance for life, you know, bringing back or -- or studying in situ samples for possible evidence of microbial or -- or larger life on Mars. Host: Yeah, and you said you were, before we started recording, you said you actually were working with Opportunity too, one of the rovers on Mars. Dr. Duck Mittlefehldt: Yeah. I, in 2005, I got attached to the Mars Exploration Rover mission. At the time, we had two rovers going, one Spirit in Gusev Crater, and the other, Opportunity, in Meridiani Planum. Subsequently, Spirit froze to death one winter. Basically, so Spirit lost mobility of one of its wheels, so we were driving backwards, dragging one of the front wheels like a boat anchor through the soil... Host: Oh, man. Dr. Duck Mittlefehldt: And we, you know, the Rover drivers and scientists are very careful. We drove over an area that looked like it was going to be solid, trafficable ground, but it turned out there was a basically a hardpan; layer on top of soil hardpan is kind of an indurated layer that's a little bit stiffer, so it didn't look like it was, you know, loose sand, but it turns out we broke through and got mired in a deep sandpit, basically, and we were unable to extract the rover from the sand, in spite of heroic efforts by the engineers, the Rover drivers at JPL, and the solar panel was tilted at a bad angle for, you know, the oncoming winter sun. So when the sun started getting lower and lower, relative to the tile of the -- of the solar panel, we -- we simply were not getting enough power to keep the rover going and although we tried to contact it again after that winter, we never heard from it again, so it basically just froze to death on Mars. Host: Oh, man, but is Opportunity its twin? Is it the... Dr. Duck Mittlefehldt: Yep, Opportunity is it's twin. Host: And that one's still going, right? Dr. Duck Mittlefehldt: And that one's still going. We're now so -- we're not -- what day is today? Host: The 8th. Yeah, we're now about two weeks away from the anniversary, the 16the anniversary of landing on Mars for Opportunity. Host: 14 years? Wow! Dr. Duck Mittlefehldt: It's still going strong, and we are still actively exploring the geology of Meridiani Planum. We don't have all the instruments we had when we landed, but we're still making great scientific discoveries, even with the limited rover ability. Host: How about that? So how is -- how was, you know, working with a rover on Mars different from looking at meteorites? Maybe even martian meteorites, like the Allan Hills, here on earth? How is that different? Well, so, you know, here on earth, I have the luxury of taking a sample into the lab and -- and using state-of-the-art scientific equipment to -- to tease out, tease out its story. On Mars, we have cameras that we can use to image the terrain. So right away, textures, and we have a microscopic camera, so textures allow us to, you know, make inferences about what the rock -- how the rock might have been formed. We have a camera with 13 color filters on it, so we can do some limited spectroscopy of the rock that helps us compare a limited set of mineralogical variations in the rocks, and then we have the alpha particle x-ray spectrometer, which allows us to do bulk compositions of surfaces. So, between them, we -- we can -- we can get a fairly good handle of the mineral -- well, mostly the textures and bulk composition, and, to some extent, neurology of a rock, and that helps us understand what processes might have formed the rock altogether. And, you know, to some extent, where Opportunity is a high-tech version of a 19th century terrestrial geologist. [Gary laughing] But, you know, the, obviously the spectrometer is better than what they had in the 19th century, and the chemical composition is as -- as good as we could do then and actually better for many elements, but we're still not at the cutting edge, as you -- as you could do if you had a, you know, a mobile laboratory up on Mars. Host: Yeah, definitely. And that's kind of your -- your trade-off, right? Is like, here, you know, you can bring into a lab with all the latest equipment and -- and study these meteorites, but, like you said before, like there's a certain amount of contamination that's going on with just the fact that a meteorite has come through the atmosphere and hit the -- hit the -- surface of the earth, you know, you have to deal with that, but then you have limited instruments right there on -- on Mars. So, I guess you just kind of have these tradeoffs [laughing]. Dr. Duck Mittlefehldt: Yep. Host: So another one that you mentioned, another infamous meteorite, was one called Orgueil, and that's one -- that one's much earlier than the Allan Hills one, right? Dr. Duck Mittlefehldt: So Orgueil fell in France in 1864, if I -- if I remember right, and what's key here is it's a -- it's a very primitive type of meteorite. It's a carbonaceous chondrite. The -- the two letter name for it is a CI carbonate -- chondrite. These are amongst the most primitive materials, primitive meteorites that we have for study. They're bulk compositions, basically are identical to what we see for the photosphere of the sun, excluding the most volatile elements like -- like helium, hydrogen, and oxygen and so forth, but if you could take the sun, you know, a cubic kilometer of the sun and condense out all the condensable matter, it would -- the composition would be very much like a carbonaceous, CI carbonaceous chondrite. So, these have always been the touchstone for understanding the chemical evolution of the solar system. They are our -- our basis for seeing who has varied from the original composition. But they're highly-altered, so they are almost completely made up of clays and other low-temperature alteration phases. So the original high-temperature phases have been replaced. So, at some point, these things were altered by water in their parent asteroid to the point where all that's left is -- is basically clay. This makes them [sigh] -- this made Orgueil susceptible to nefarious individual, tempting to prove something, what don't know, because we don't know who that individual was, but, you know, I would call Orgueil the Piltdown Man of meteorites. So Piltdown Man was -- was this fake fossil made in about 1912 I think to look like it had some of the attributes of an ape, but some of the attributes of a modern human, because someone that that's the way human evolution went, and they wanted to show that we had fossils that fit in within that theory. Well, Orgueil, at some point, was broken open, and it turns out, because this is clay, you can -- if you get it good and wet, you can kind of break it open like clay, and then they had stuffed in terrestrial seeds and plant fragments and coal, and then put it back together, and coated the outside with glue to make it look like it still had the fusion crust on it. Host: Oh my gosh! Dr. Duck Mittlefehldt: And then this sample was sealed in a bell jar in a museum from 1864, so apparently it happened very early, we don't know who did it, or why, you know, what were they trying to accomplish by this? Because it was going to be sealed in a bell jar, you know, did they think someone was going to then take it out and look at it, I don't know, but this -- this came to light in 1960's then. Host: Oh! Dr. Duck Mittlefehldt: And so, a well-known meteoriticist, by the name of Ed Anders, very famous, very smart man, he led a study that was published 100 years later, in 1964 in science, where he uncovered, you know, all of this forensic meteoritic work where he showed that, you know, the seeds were, you know, terrestrial seeds, the coal fragments were in there, that glue had been used to put it back together and make it look like it was whole, and -- and all of this, and -- and so that's why, you know, this is an infamous -- infamous meteorite for those who are in the know. Most people won't have heard of it, but, you know, like I said, it's kind of the Piltdown Man of meteoritics. Host: Wow! Dr. Duck Mittlefehldt: So someone had an agenda, they wanted -- they, for some reason, they wanted to show that life could form on an asteroid or -- or in space, or something, I don't know, but, obviously, they had -- they had some agenda when they did this. Host: Yeah, I know, but seeds and glue are not really a good way to convince people [laughter]. Dr. Duck Mittlefehldt: No. You know, back in the, you know, mid-19th century, you know, had it been opened up and studied then, maybe it would have caused quite a furor, but, as far as I know, this was only discovered in, you know, a century later. Host: Wow! A hundred years of people thinking this is some kind of like capsule of extraterrestrial life, how about that? So, you know, all of these kind of tell a story and, unfortunately, some of them, this [laughing] -- this particular one is a little bit of a lie, but, you know, we are cracking these open to search for evidence of -- of whatever we can find, right? Maybe -- maybe the formation of a planet, maybe the formation of solar system, maybe the formation of life. So, you know, what, in a perfect world, I guess, what would you like to do -- what would you like to study? What would you like to see and do to really maximize what you can find about learning more about our solar system and about life in the universe Dr. Duck Mittlefehldt: Well, I mean, that -- that's kind of a difficult question for a scientist to answer, because, you know, truth be told, we're all paid to pursue our hobbies, and so we all have our own hobby horses. So, as I -- as I mentioned, you know, my particular interests are in igneous processes, I, you know, on the earth, moon, Mars, asteroids, I -- I like magmatic rocks, and, you know, I couldn't tell you why, it's just the way I am [Gary laughing]. So, one of the things -- one of the things that's very curious about asteroidal igneous rocks is that asteroids were melted very early in the solar system, probably within a couple million years of the formation of the earliest-known solids in the solar system. So something had to heat up relatively small objects, maybe a few hundred kilometers, you know, 200 miles in -- or in radius, something like that, to the point where they were melted and then cooled down and then they completely shut off after that. So, it was a very, very intense heat source that acted early, died out, and then never came back. You know, we think we know what -- what caused this, but there, you know, and so the -- the leading contender is radioactive heating by a very short-lived isotope of aluminum. It has a half-life of about 730 million years, and so, and aluminum is a -- is a major element in rocks, so, if you -- if you accumulate an asteroid early enough, when there's this aluminum-27 still alive, you've, you know, -- you've then encapsulated a very potent heat source inside that rock. And so that's what we think happened, but, still, you know, we can admit, as scientists, we can imagine this process going on, but geology is always much more complicated than our imaginations. So there are things that I don't understand, things that, as far as I know, no one really understands about how asteroids went from being primitive objects that accumulated from minerals formed in the solar nebula to basically a molten ball that then crystallized out igneous magmatic rocks, similar to what we see on earth. I would desperately like to get, you know, be able to find out more about how -- what was going on, you know, what have we missed, because we, you know, we tend to think of things in -- in the simplest terms, you know, it was heated up, melted, crystallized, that's it, well, we know that -- that's not all the story. Host: Yeah. Dr. Duck Mittlefehldt: And I think all meteoriticists have, in the back of their minds, for their particular hobby horses, just things they don't quite understand. They know the -- the broader picture, but what are the finer details that went into -- to this. We -- we know we've got the basic story, but what are, you know, all the chapter and verse that go into this basic story? Host: Wow. Dr. Duck Mittlefehldt: So, you know, that's what drives me, and it's all -- it's all a matter of, you know, learning something new that -- that, you know, pushes forth human knowledge. You know, what I do is -- is nowhere near applied science. It's pure basic science. So I can't -- I can't talk to someone and say, you know, tomorrow, you're going to be able to have a better life because of what I do, only if, you know, unless you think a better life means knowing more [Gary laughing]. But you never know, because, in -- in general, a large fraction of basic research ultimately does find an application. Right now, I don't know what that application might be, but I won't say there's never going to be some application for what I do, but, for me, it's -- it's this sense of learning something that -- that drives me. Host: Yeah. Why learn if you don't think it's going to end up, you know, giving you a better life. I mean, honestly, like, you know, learning things kind of helps you understand things, helps things come together, to me, that makes me pretty happy. So I could see that, you know, better understanding, giving me a better life. Dr. Duck Mittlefehldt: Yeah, well, I mean, you know, humans have always been curious, and, you know, I suspect the reason we're curious is because it's beneficial for survival, because, you know, when -- when you're out on the savannah hunting lions, or hunting gazelles, if you see something moving the weeds over there, you know, okay, is that a gazelle or is that a lion about to eat me instead? So, you know, humans are geared to being curious about their environment, because it's a survival mechanism. Host: Yeah. Dr. Duck Mittlefehldt: And, for scientists, we have now transposed that, you know, away from worrying about whether we're going to be eaten to just, you know, a broad knowledge in general. Host: [Laughing] Well, I think last time we sat down with Dr. Burton, he said, he kept talking about this time machine, how easy it would be -- how nice it would be to just kind of hop in a time machine, watch these processes take place, and be like, ah [snapping fingers], that's how -- that's how it takes place. I mean, and then there's whole philosophical idea of, well, is that going to alter the universe if you go back in time and watch these things? So, you know, that was another tangient we could have gone on and we didn't, but [laughter], but it would be nice to, you know, for the, you know, to improve our knowledge a little bit of how all this stuff works and comes together. Alright, so, Duck, I think -- I think that about wraps it up for today. So, thank you so much for coming on the podcast and kind of... Dr. Duck Mittlefehldt: It's been a pleasure. I hope I've imparted something that makes sense to the listeners and -- and that they will find interesting. Host: It's actually you know, you know, we're talking about rocks, if you think about it, but it's absolutely fascinating, what you can found and the stories behind these rocks and what they tell you about the universe, and even just your trips to Antarctica are pretty fascinating as well, so, again, thanks so much for coming on and telling the stories of these beautiful rocks and your trips to Antarctica, and, yeah, hopefully we'll -- we'll find some cool evidence of life or, you know, you'll find that key ingredient as to why, you know, the asteroids did what they did. Dr. Duck Mittlefehldt: Yeah, well, I hope so, and thank you very much for the invite! Host: Absolutely. [ Music & Radio Transmissions ] Hey, thanks for sticking around. So, today, we talked with Dr. Duck Mittlefehldt about some of the cooler, infamous meteorites that have been discovered throughout the years, and then some interesting stories about Antarctica and how he's finding them, it's really a cool process, and he works with the ANSMET, it's the Antarctic Search for Meteorites. So if you want to learn more about ANSMET and some of the adventures that are going on in Antarctica, and some of the curious findings in these meteorites, especially some that may or may not be life, it turns out there was some, you know, fake meteorites at the end of there, which is kind of disappointing, but that's okay. You can go to ares.jsc.nasa.gov to get the full scoop on all of these cool meteorites, and -- and you can learn how to get your hands on one of these meteorite samples to study them. If you go to social media on the NASA Johnson Space Center accounts, or if you go to ARES, or astromaterials, NASA astromaterials, we got pages on Facebook, Twitter, and Instagram where we like to share these stories, just use the hashtag, ask NASA, on -- on your favorite platform to submit an idea, or if you have a question about meteorites, or if you want to submit a new topic for the show, to make sure to mention it's for, Houston, We Have A Podcast. So this podcast was recorded on January 8th, 2018. Thanks to Alex Perryman, Greg Wiseman, Tracy Calhoun, and Jenny Knots, and thanks again to Dr. Duck Mittlefehldt for coming on the show! We'll be back next week!
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NASA Astrophysics Data System (ADS)
László, Márton, ,, Dr.
2010-05-01
Sustainable agriculture is defined as the successful management of resources for agriculture to satisfy changing human needs while maintaining or enhancing the quality of the environment and conserving natural resources. A sustained increase of agricultural production becomes a great possibility for international community. In this process a green manure crops application for example crotalaria get a new chance for improvement process on soil fertility and soil conservation. Field experiment was carried out on a calcareous chernozem soil (Experiment station Nagyhörcsök of RISSAC-HAS) in partly of experiment series (3 years) at Hungary in 1998. The soil with about 20% clay, 3% humus, 5% CaCO3 in its ploughed layer. To ensure a sufficient macro and micronutrient supply in the whole experiment, 100 kg N, 100 kg P2O5 and 100 kg K2O were given hectare. The Crotalaria juncea L. and Crotalaria spectabilis ROTH were applied with 2 replications. Each plot has an area of 45 m2 with 230-230 individual plants. In vegetation grown period were measured green and dry matter yield. The soil and plant samples were analysed for the macro and microelements contents. The main results achieved in 1998 are summarized as follows: 1. The green matter yield at before flowering reached 63.8 t ha-1 in case of Crotalaria juncea L. 2. Total dry matter yield at harvest (without roots) fluctuated between 9.6 and 17.0 t ha-1, depending on the crotalaria species. 3. The average of element concentration (including stems, leaves of Crotalaria juncea L. and Crotalaria spectabilis ROTH) before flowering reached to 3.2 % N, 2.3 % Ca, 1.3 % K, 0.39 % Mg, 0.22 % P and 0.24 % S. The content of Al and Fe total 14 - 25, while that of Sr, Mn, Na, B and Ba 2 - 6 ppm in dry matter. The Zn, Cu, Mo, Cr, Se, Ni, As, Pb, Cd and Co concentration did not reach here the value of 1 ppm. 4. The average of biological activated element uptake (including stems, leaves of Crotalaria juncea L. and Crotalaria spectabilis ROTH) before flowering amounted to 368 kg N, 252 kg Ca, 96 kg K, 45 kg Mg, 30 kg P and 27 kg S ha-1. The content of Al and Fe total 2 - 3, while that of Ba, Zn, B, Cu, Na, Mn and Sr 180 - 650 g ha-1. The Co, Cd, As, Pb, Ni, Se, Cr and Mo concentration did not reach here the value of 10 g ha-1. By this means this green manures should have a vary important role in the design of rotations for sustainable agriculture. Not only do they help to retain and accumulate nitrogen and other nutrients, thus reducing leaching losses, they also maintain ground cover, protected the soil from erosion, and can make a contribution to pest and weed control. Key words: Sustainable agriculture, soil fertility, soil conservation, green manure, Crotalaria juncea L., Crotalaria spectabilis ROTH. INTRODUCTION Sustainable agriculture is defined as the successful management of resources for agriculture to satisfy changing human needs while maintaining or enhancing the quality of the environment and conserving natural resources. A sustained agricultural production can be achieved by a proper use of soil resources, which includes the maintance or the enhancement of soil fertility (Christian and Kurt 1996). The term soil fertility is cast here to encompass not only essential plant nutrients but also aspects of soil structure, including water holding capacity, soil organic matter content and biological activity that influence both the efficiency of use and sustainability of the resources. All these attributes are interrelated and contribute together to the soil potential productivity or fertility (Kádár 1992, Németh 1996). From that perspective, soil fertility can be assessed as a capital stock, which will produce interests when properly used , and yet will be eroded by a consumptive use. It is necessary to make here a clear distinction between actions aiming at the regeneration of the soil capital, i.e., "recapitalization of soil fertility" and actions, such as maintance of enhanced soil fertility. The first set of actions, such as lime application, erosion control measures, and chiseling of sub-surfacehardpan, are "one time" investments which often benefit not only the farming communities but also society at large, improved water quality, food security, etc. Costsharing among all beneficiaries in society should be the carefully thought about. The second set of actions relates to the protection and or maintance of the enhanced soil capital, through balanced plant nutrition applications, appropriate crop rotations, etc., the cost of which have definitely to be fully supported by farmers. However, farmers will bear these costs only if the economic, institutional and legal frame conditions are favourable, i. e. when there are enough incentives to reinvest instead of consuming the capital stock. Possible interventions to enhance soil fertility management, therefore, range from policies affecting farm gate prices, security of land use, access to credit, access to markets, relations between input and output prices, fertilizer supply and distribution right through to access to information on improved soil fertility management (soil organic matter management, prevention of nutrient losses by run off - leaching, efficient use of fertilizers). This cannot be obtained with isolated measures and projects but requires a coherent strategy for soil fertility enhancement and sustainable soil management (Janssen 1993). The implementation of such a strategy, finally, requires a strong commitment of national governments which was often lacking in the past, as well as support from the international community. Neither human needs are satisfied, especially food demands, nor are the natural resources protected. Gross plant production was decreased with twenty percent in the last 10 years. Morever, this inadequate rate is obtained partly by degradation of the environment resulting from overexploiting of soil resources. The reversal of this trend and a sustained increase of agricultural production becomes a great possibility for Hungary and the international community. In this process a green manure crop application for example crotalaria get a great chance for improvement process on soil fertility and soil coservation (Lazányi 1998, Márton 1999). This paper briefly outlines the major effects of Crotalaria juncea L. and Crotalaria spectabilis ROTH on soil fertility and soil conservation. MATERIAL AND METHOD Field experiment were carried out on a calcareous chernozem soil at Hungary (Experiment station Nagyhörcsök of Research Iinstitute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences) in partly of experiments series (3 years) in 1998. The soil with about 20% clay, 3% humus, 5 Ca CO3 in its ploughed layer. To ensure a sufficient macronutrient supply in the whole experiment, 100 kg N, 100 kg P2O5 and 100 kg K2O are given hectare in autumn of 1997. The Crotalaria juncea L. and Crotalaria spectabilis ROTH were applied with 2 replications. Each plot has an area of 45 m2 with 230-230 individual plants. Winter wheat was grown as a green crop (preceding the main product of a field) with commonly used agrotechnic. Soil samples are taken before the experiment set up on 27.04. 1998. Each composite sample consist of 20 subsamples drawn from the plow layer of each plot. Plant samples are taken during the vegetation period at least twice (20.07. 1998 and 02.11. 1998), using 5-5 plants per plot randomly. Plant material is dried, milled and digested in teflon bombs using cc.HNO3+cc.H2O2 and their total macro and microelement content with the exception of N was determined by ICP technics (JY 238 ULTRACE). N-content were determined by titration of hypobromit after the cc.H2SO4+cc.H2O2 digestion, N-NO3 content were determined by Griess-Ilosvai reaction after water extraction. Soil samples are extracted by ammonium-acetate+EDTA (Lakanen and Erviö 1971) and their available element content with the exception of N is mesaured using the ICP technics. N-contents (NO3+NH4) were determined by Bremner-Keeney method (1966). Dates of experiment were estimated by MANOVA. The main goal of the whole researh program was described erlier (Márton 1999). Easily soluble nitrogen, phosphorus and potassium content of soil on ploughed soil layer are presented in Table 1. RESULTS AND DISCUSSION The green matter yield at before flowering reached 63.8 t ha-1 in case of Crotalaria juncea L. Total dry matter yield at harvest (without roots) fluctuated between 9.6 and 17.0 t ha-1, depending on the crotalaria treatment (Table 2). Chemical composition were different between crotalaria species before flowering. The average of element concentration (including stems, leaves of Crotalaria juncea L. and Crotalaria spectabilis ROTH) before flowering reached to 3.2 % N, 2.3 % Ca, 1.3 % K, 0.39 % Mg, 0.22 % P and 0.24 % S. The content of Al and Fe total 14 - 25, while that of Sr, Mn, Na, B and Ba 2 - 6 ppm in dry matter. The Zn, Cu, Mo, Cr, Se, Ni, As, Pb, Cd and Co concentration did not reach here the value of 1 ppm (Table 3). The average of biological activated element uptake (including stems, leaves of Crotalaria juncea L. and Crotalaria spectabilis ROTH) before flowering amounted to 368 kg N, 252 kg Ca, 96 kg K, 45 kg Mg, 30 kg P and 27 kg S ha-1. The content of Al and Fe total 2 - 3, while that of Ba, Zn, B, Cu, Na, Mn and Sr 180 - 650 g ha-1. The Co, Cd, As, Pb, Ni, Se, Cr and Mo concentration did not reach here the value of 10 g ha-1 (Table 4). By this means this green manures should have been a very important role in the design of rotations for sustainable agriculture. Not only do they help to retain and accumulate nitrogen and other nutrients, thus reducing leaching losses, they also maintain ground cover, protected the soil from erosion, and can make a contribution to pest and weed control. For this reason based on earlier results crotalaria has the following charasteristics: nitrogen accumulation - maintenance-, reduction of nutrient leaching (N, Ca, K), reduction of soil erosion, improved utilisation of rainfall (water), shading of soil, aeration of soil, weed control and pest control. Crotalaria crops also provide cost reduction as a result of lower fertiliser use, improved nutrient utilisation, easier cultivation, reduced plant protection requirements. To a certain extent that this plant roots are involved in this process and green manure contribute to the biological stabilisation of soil structure following mechanical cultivation. Depending on soil type, the roots of crotalaria can extend down to 1.5-2 m according to earlier publications of autor. This result are presented that crotalaria has great advantagens in green manuring. ACKNOWLEDGEMENTS This research was supported by Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences, Budapest and Natinal Vegetable Crops Research Center, Brazília REFERENCES Bremner, J.M., Keeney, D.R. 1966. Determination and isotope-ratio analysis of different forms of nitrogen in soils. 3. Exchangeable ammonium, nitrate and nitrite by extraction destillation methods. Soil Sci. Soc. Amer. Proc. 30:577-582. Christian, P., Kurt, G.S 1996. The role of soil fertility in sustainable agriculture with special reference to Sub-Saharan Africa. Entwicklung. 4, 3-6. Janssen., B.H. 1993. Integrated nutrient management: use of organic and mineral fertilizers. In: Reulen and Prins, 1993. Kádár, I. 1992. Principles and methods in plant nutrition. RISSAC-HAS, Budapest. Lakanen, E. and Erviö, R. 1971. A comparison of eight extractants for the determination of plant available micronutrients in soil. Acta Agr. Fenn. 123. 223-232. Lazányi, J. 1998. Use of alternative crops for forage production and soil conservation. Research Center of Debrecen Agricultural University, Debrecen. Márton, L. 1999. From a new alternative crops (Crotalaria juncea L.) production and disease. Agroforum 5, 64. Németh, T. 1996. Organic matter and nitrogen content of soils. RISSAC-HAS, Budapest. Table 1. Easily soluble nitrogen, phosphorus and potassium content of calcareous chernozem soil in ploughed layer. Nagyhörcsök at spring of 1998. Easily soluble N,P,K (ppm) Ploghed layer N AL-P2O5 AL-K2O (cm) NO3 NH4 0-20 15.7 21.0 108.9 180.5 20-40 8.7 17.5 59.8 111.5 Average 12.2 19.2 84.3 146 Table 2. Green and dry matter production of Crotalaria juncea L. and Crotalaria spectabilis ROTH on calcareous chernozem soil. Nagyhörcsök, 1998 Treatment Yield before flowering 20.07. 1998. Green matter t ha-1 Dry matter t ha-1 Dry matter % Crotalaria ju. L. 63.8 13.1 20.6 Crotalaria sp. ROTH 39.8 9.3 23.3 LSD5% 4.5 2.0 0.5 Average 51.8 11.2 21.9 Yield at harvest 02.11. 1998. Crotalaria ju. L. 48.8 17.0 35.0 Crotalaria sp. ROTH 25.4 9.6 38.0 LSD5% 3.0 2.5 1.5 Average 37.1 13.3 36.5 Table 3. Chemical composition of Crotalaria juncea L. and Crotalaria spectabilis ROTH before flowering on calcareous chernozem soil. Nagyhörcsök, 1998 Element Concentr. Crotalaria Crotalaria Average LSD5% junc. L. spect. ROTH N % 3.70 2.70 3.20 0.60 Ca % 2.00 2.60 2.30 0.70 K % 1.70 0.90 1.30 0.30 Mg % 0.44 0.35 0.39 0.09 P % 0.27 0.18 0.22 0.01 S % 0.24 0.23 0.24 0.02 NO3 - N ppm 985.00 395.00 690.00 58.40 Fe ppm 317.50 210.50 264.00 25.10 Al ppm 249.00 152.50 200.70 14.00 Mn ppm 57.00 36.60 46.80 3.70 Sr ppm 53.60 72.90 63.20 2.30 Na ppm 49.50 24.90 37.20 4.70 B ppm 27.60 38.70 33.10 5.40 Zn ppm 16.10 17.30 16.70 0.40 Cu ppm 6.40 7.10 6.80 0.08 Ba ppm 4.80 38.50 21.70 6.40 Mo ppm 1.40 1.00 1.20 0.40 Cr ppm 0.60 0.50 0.50 0.50 Se ppm 0.60 0.30 0.50 0.10 Ni ppm 0.40 0.50 0.50 0.20 As ppm 0.27 0.07 0.17 0.08 Pb ppm 0.23 0.09 0.16 0.03 Cd ppm 0.11 0.07 0.09 0.02 Co ppm 0.06 0.01 0.07 0.04 Table 4. Element uptake of Crotalaria juncea L. and Crotalaria spectabilis ROTH before flowering on calcareous chernozem soil. Nagyhörcsök, 1998 Element Amount Cr. jun. L. Cr. sp. ROTH Average LSD5 % N kg ha-1 484.70 251.10 367.90 68.90 Ca kg ha-1 262.00 241.80 251.90 76.60 K kg ha-1 107.60 83.70 95.60 22.00 Mg kg ha-1 57.50 32.50 45.00 1.00 P kg ha-1 35.40 23.90 29.60 0.10 S kg ha-1 31.80 22.20 27.00 0.20 NO3 - N kg ha-1 12.90 3.60 8.20 0.60 Fe kg ha-1 4.10 1.90 3.00 0.280 Al kg ha-1 3.20 1.40 2.30 0.16 Sr g ha-1 700.00 600.00 650.00 20.00 Mn g ha-1 700.00 300.00 500.00 30.00 Na g ha-1 600.00 200.00 400.00 50.00 Cu g ha-1 500.00 60.00 280.00 3.00 B g ha-1 300.00 300.00 300.00 40.00 Zn g ha-1 200.00 100.00 150.00 3.00 Ba g ha-1 60.00 300.00 180.00 50.00 Mo g ha-1 10.00 9.00 8.00 2.00 Cr g ha-1 7.00 4.00 5.00 5.00 Se g ha-1 7.00 2.00 4.00 0.80 Ni g ha-1 5.00 4.00 4.00 1.00 Pb g ha-1 3.00 0.80 1.00 0.10 As g ha-1 3.00 0.60 1.00 0.40 Cd g ha-1 1.00 0.60 0.80 0.03 Co g ha-1 0.70 0.09 0.30 0.10 Address of the author: Márton László Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences. H - 1022 Budapest., Herman O. u. 15.
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Houston, We Have a Podcast. Episode 48: Moon Rocks
2018-06-08
Gary Jordan (Host): Houston, we have a podcast. Welcome to the official podcast of the NASA Johnson Space Center, episode 48, Moon Rocks. I'm Gary Jordan and I'll be your host today. So, in this podcast, we bring in the experts, NASA scientists, engineers, astronauts, all to let you know the coolest information about what's going on right here at NASA. So, today, we're talking to the keeper of all moon rocks in the world, Ryan Zeigler. Well, technically, they're all held here at the Johnson Space Center by NASA in the Lunar Curation Facility. But Ryan is the lunar sample curator here in Texas and he's also a planetary scientist. We had a great discussion about moon rocks, like the reason why we brought them back from moon during the Apollo Program, more about the facilities that keep them, and also what we're still learning from them. So, with no further delay, let's go lightspeed and jump right ahead to our talk with Dr. Ryan Zeigler. Enjoy. [ Music ] Host: Ryan, thanks for taking the time to come on the podcast today. I can't believe it, but we're actually finally going to talk about moon rocks. Ryan Zeigler: I know, I mean you'd think this was a cursed subject or something. Host: Well, it's interesting because -- and correct me if I'm wrong -- all of the moon rocks that were collected on the Apollo missions are here, correct? Ryan Zeigler: Most of our here, about -- about 85% are here or maybe 80% are here, 5% are out with scientists, and about 15% are at a secret remote storage facility at White Sands, so -- Host: Oh, okay. Ryan Zeigler: Not that secret, I guess, so. Host: The secret's out now. Okay. So -- but -- but the moon rocks were collected on just human missions, right, not robotic missions? Ryan Zeigler: For NASA, yes. Host: Okay. Okay. So, were there other lunar acquisition -- like robotic ones? Ryan Zeigler: Yeah, so the Soviets had three Luna missions -- Luna 16, 20, and 24, and they collected about a pound of samples. Host: Oh, really? Ryan Zeigler: Yeah. Yeah. Host: Robotically? Ryan Zeigler: Robotically, yup. Host: Okay. Very cool. Must have been a different profile. But we went a couple times, right? We did -- we did Apollo, you know, 11 through 17. Ryan Zeigler: Yeah. We had six missions that landed on the surface. Host: Exactly. All right, a lot of moon rocks. So. So, let's talk about moon rocks, themselves, because, you know, how I imagine it is just, you know, gray rocks. But I'm sure -- and I'm sure as -- from a geologist's perspective, there are interesting ones and there are -- there are not so interesting ones. And there was -- there was just some decision-making that went with the acquisition of them. Ryan Zeigler: No, absolutely. And you're right, though. If you look at moon rocks, most of them are kind of boring to look at. I mean they have a bit of an image problem. Most of them are sort of gray rocks but there's a few things about them that really set them apart. They're really old. They formed on a body with no atmosphere, so there's a lot of micrometeorite impacts into them. There's a lot of things that set them apart from Apollo's -- from terrestrial samples. And so, they are really interesting to scientists for a lot of those reasons, yeah. Host: For sure, definitely. So, some of the first ones were collected from NASA on Apollo 11, right? Ryan Zeigler: Yes. Host: Awesome. So, how much -- do you know how much they collected? Ryan Zeigler: It's about 25 kilograms, so about -- a little over 50 pounds. Host: All right. Ryan Zeigler: Yeah. Host: But I guess it felt different when they were actually collecting it. Ryan Zeigler: Well 1/6 as much. Yeah. I know. I mean everyone was super strong on the moon and it was great. You could jump super high, except for the spacesuits, I think. Host: Oh, yeah. Yeah. So, what did they used to collect it? Was it kind of bending over and picking it up or was it -- Ryan Zeigler: Well, they couldn't bend over very well and that was good for us because that kept them from touching them with their gloved hands because the gloves were a source of contamination. So, they had specially designed tools made out of either stainless steel or aluminum. And so, they -- like, basically one of those long claw things you see that -- like the t-rex with the two claw things, that's kind of like that, only NASA, so it was made of steel. Host: Okay. Ryan Zeigler: And then they had sieves and they had some rakes. And so, they had a couple different instruments -- tools to help them collect them. Host: Okay. And that was all planned ahead of time. They knew that the -- did they understand the surface of the moon before they went? Ryan Zeigler: They understood it pretty well. What they didn't -- they underestimated how important the impacts were on the surface. And on Earth, impacts are a relatively minor thing because we've got an atmosphere. So, you see shooting stars at night and that's little sand sized stuff being burned up. On the moon, all of that stuff, it's the moon going several kilometers per second. So, it's a much finer grained place and there's just -- yeah. So, the tools they use evolved over time. On Apollo 11, they had one set. And by Apollo 17, they had a much more evolved set. They learn from being there and sort of redesigned them on the fly, so to speak. Host: Okay. That makes sense. You go on the surface and you have people actually using the tools and then providing real-time feedback. Ryan Zeigler: Exactly. Host: Hey, this worked, this didn't. I need this bigger, this smaller, this longer, whatever, so. Okay, that makes a lot of sense. So, when they collected them, what was that process like? Did they kind of put it into bags and seal them up or was it like a bin? Ryan Zeigler: On Apollo 11 especially, because they didn't collect that many rocks, I mean 50 pounds sounds like a lot, but rocks are heavy. So, they had a special box with a metal-on-metal knife edge seal that allowed them to seal them away. And so, they would collect them with the tool, put it inside a Teflon bag, roll up the bag, and then the bag would go in the box. Host: Okay. Ryan Zeigler: And then at the end of Apollo 11, just before they were sealing them up to put them inside, Neil Armstrong looked at it and thought that the box looked kind of empty, so he got his shovel out and literally just shoveled a bunch of dirt into the box around all of the other samples. Host: Really? Ryan Zeigler: It's -- almost as an afterthought. And it ended up being like 11 kilograms or something. And it being almost a quarter of the sample they brought back. Host: Whoa. Ryan Zeigler: And it ended up being the largest single sample from Apollo 11 and probably one of the most important. And it was just -- he just looked at it and thought, this is silly, I'm going to go all the way to the moon and I'm going to bring back a half-full box of rocks. So, he shoveled some dirt in, sealed it up, and that came back. On later mission, when they started collecting more rocks and would fit in the rock boxes, some of them came back just in the Teflon bags, sealed up tight, like cookies or coffee or something. But those probably saw a little bit of atmosphere. Host: Oh, okay. So, the idea was to protect it from the Earth's atmosphere, once it got back, to avoid. Ryan Zeigler: Exactly. But the boxes are heavy and so they couldn't bring 10 boxes to bring back all those samples. So, they decided that for some samples, just being sealed up and minor exposure to air would be okay. Host: Okay. So, why did the dirt ended up being one of the more important pieces of Apollo 11? Ryan Zeigler: Well, one of the things they didn't realize -- because the impacts are so important on the moon, and a lot of the material just gets spread around. And so, the dirt -- the soil -- the regolith, official -- is the technical name for it -- is a really good average composition of a large area on the moon, whereas the rocks mostly come from that local area. So, you collect the rocks, you learn a lot about the local area. You collect the soil, you learn about the local area, but also exotic stuff coming from farther away. And it being so big, and hey, us having so much of it, everyone wanted Apollo samples when they came back, and obviously, we had a very limited mass. And so, them bringing back more than they expected opened up new studies just based on mass availability. And we also used those as a goodwill sample. We -- every country on Earth in 1970 got a piece of the moon as a gift that came from that soil -- that big shoveled soil. They took out the bigger particles, put them in plastic, took some flags they had flown to the moon, put it on a plaque, and they just handed it out to everybody. It was great, yeah. Host: I wish I -- Ryan Zeigler: All because -- all because Neil thought to shovel in a [inaudible] we're real close, so. I call him Neil, so. No, I mean all because he had the -- you know, the foresight to do something like that. Host: Exactly. So, what was interesting about the Sea of Tranquility, whenever they were picking the location for Apollo 11? Ryan Zeigler: Honestly, I think it really came down to safety. I mean they had some really strict constraints. They -- first time, they wanted something near the equator, so they used less Delta V, less fuel. They wanted something flat, so they'd have to worry about landing on, you know, a crater, which they almost did anyway, and they had to avoid it. So, a lot of it came down to it had to be on the equator and it had to be flat. And then they used spectroscopy. They looked at the light and it was bouncing off the surface and trying to find a place that was slightly unusual. And it turned out, Sea of Tranquility had a lot of titanium in it. And so, the light bouncing off it looked a little different and so they thought, let's go try that place. And then when they went to 12, they had similar constraints, but they went to the other end of the spectrum. And they got low titanium basalts. And so, you know, science wasn't driving the landing sights at that point, but they were still trying to maximize how much science they could get out of it. Host: Right and, you know, priority one was safety. Priority two was all right, in terms of the safest areas we could land, this one is also -- Ryan Zeigler: Exactly, that's how they did it. Yeah. Host: Okay. Cool. So, what's -- what was interesting about titanium then? Ryan Zeigler: On Earth -- I mean this is sort of a technical detail that almost no one's going to care about. But on Earth, you know, basalts only have a weight percent of titanium, 1% titanium. And on the moon, that's 8 or 9% titanium, and it tells you about the interior of the moon and what was melting to form these basalts. And it's quite different than Earth. And so, it was telling us about how the moon formed and evolved, all from one rock on the surface. And it wasn't the whole story, but it sure got things moving in the right direction. Host: All right. Ryan Zeigler: Otherwise, we've been wasting our time for 45 years. Host: Well, then so that was just a piece of the story. And then you went to -- we went to different areas to kind of let -- you know, we have these Apollo missions, let's use them to our fullest advantage. Let's figure out this story of the moon. So, what were some of the decisions -- and you said Apollo 12 was lower titanium -- but what were some of the other decisions for the later missions? Ryan Zeigler: So, for the later missions -- if you look up at the moon at night -- and this is super basic, but there's dark parts and light parts. And the first two missions went to the dark parts, those are mare basalts, like you would get in Hawaii. And then there was the bright parts, which actually make up about 80% of the moon, so they need -- they were like, we need to go to one of these bright parts and see what make up the Highlands. And so, same constraints, Apollo 14 landed pretty close to Apollo 12, near the equator, but in the Highlands. And then they got those samples back and realized, wow, everything's an impact, everything's a breccia, a rock made of pieces of other rock. It's like a jigsaw puzzle almost. And then after that, when they got to 15, 16, and 17, those were the J missions, so they had a Rover, they had much more -- better suits, they had a lot of other stuff. And so, then they were able to go to more technically challenging sites that were, at the junction, between the bright parts and the dark parts mostly. And so, also, I mean I'm sure you know this and all of the pilot -- all of the Apollo astronauts are pretty much test pilots. So, just landing on a flat bit, I don't think he was doing it for them. And so, Apollo 15 and Apollo 17, when you hear the astronauts talk about what it was like to land there, like landing in this little narrow valley on Apollo 17, and Apollo 15 landing and coming over this huge mountain. And then having to get down really fast and land onto -- before the big canyon. Host: Canyon. Ryan Zeigler: Yeah. You know, and so, you know, they were able to do more technically challenging things with flying too. Host: Okay. Yeah. Well, that was -- that was their thing, right? Ryan Zeigler: Yeah. Host: But then on -- was it Apollo 17, Jack Schmitt, now you finally have a geologist, right? Ryan Zeigler: Right. I mean, and Jack had played a really important part. I mean Jack comes to all of our science conferences. Jack has PhD in geology. He's way smarter than I'll ever be, and he still comes to all of the -- all of the conferences and many, many, many a debate ends with, well, when I was on the moon -- and that's when you know you've lost the argument because he's really [inaudible]. You know, you don't get to use that. No, Jack was there. And so, he was able to help select the sites but when they were on the ground, he was -- you know, everyone got a -- basically a master's degree in geology as part of their training. But he already had a PhD and was one of those people who trained the other astronauts in geology. And so, he really was able to spot and collect things from a different perspective. Host: Okay. And was -- did he have a part in deciding where they were going to land and what things to pick up and bring back? Ryan Zeigler: I'm sure he did. And I mean he started to tell a story at a meeting a couple months ago, about well, that's not how we selected that site. And he never finished the story, so I don't have the whole story yet. But I don't think the sites were selected that far ahead of time. As they were leading up to a new mission, the scientists and Jack, because he's one of the scientists, would get together and talk about where they wanted to go from science priorities. And then the mission safety people would be like, yeah, we're not landing in the middle of Tycho Crater, that's crazy, and then there would be some back-and-forth. And -- but yeah, no, Jack was definitely part of that discussion. Host: Okay cool. So, what were -- what were some of the -- besides titanium -- what were some of the more interesting things that you found? Because there's a finite number of samples we have from the moon, right? So, what are -- were some of the most interesting things that we found from those samples? Ryan Zeigler: Well, they're really old. I mean -- and that's -- that sounds very basic. But essentially, every rock from the moon is older than every rock on Earth. It's not perfectly true. There's some overlap in the middle. There's like four places on Earth where they're that old. But it turns -- so the moon is just an ancient body. The fact that everything was either a volcanic process of basalts, like what you'd see in Hawaii, or breccia, something from impact, that threw people off. There was no water on the moon and that's not true anymore. But compared to terrestrial rocks, which every rock you pick up on Earth has a mineral with water in it and they couldn't find any water in lunar samples until about 10 years ago. And it was only when instruments had evolved to the point where they could measure lower concentrations and new scientists came along and said, this doesn't make sense. We need to re-examine these. And so, there was a little bit of missed from earlier. But the moon is a very dry place and that throws people off. Host: So, you said there's-- parts of it, you said it's not true anymore. Ten years ago, we discovered there's a little bit of water on the moon. What was the instrument that found that and where is it? Ryan Zeigler: It was something called the SIMS, the secondary ion mass spectroscopy. And so, what you do is you take the sample, you bombard the surface with ions, either positively or negatively charged, and then that sputters off what's there. And before, we were using an electron probe, where you're doing essentially the same thing, but with electrons. And they just -- they started looking at a mineral called apatite and on every other planet where you find that mineral, there's water in it. And then when they started looking at it on the moon, there was a fair amount of water in it. And so -- and it was one of those cases where the analytical instruments in the '70s were very good, and Apollo helped revolutionized them. But the little bit of water -- the little bit that was missing, they just assumed was analytical error, and it was very hard to directly detect water because you're not doing it by mass, you're doing it by energy and so -- anyway. So, they -- so this -- these new instruments -- which weren't new in the -- in the 2000s. They were invented in the -- in the '80s. But by the 2000s, when new scientists came along, that's when they started to figure it out. Host: Okay. Isn't it also true that there are -- on the polar ends of the moon, there are [inaudible] shaded areas that have I guess never seen the Sun, are their deposits of water there too? Ryan Zeigler: Almost certainly. We have limited direct evidence of that, but we have a lot of circumstantial evidence. There's extra hydrogen there, so what's the hydrogen there as? They -- you get a different radar back scatter out of there and one of the only things that causes that is ice. And so, they did have the L Cross mission, which landed in one of these permanently shadowed regions, put up a plume of debris, and then it flew through it. And they did detect water, and so we do have some direct evidence, but -- so that's a different kind of water. So, I'm talking about water that came from the interior of the -- of the -- of the planet. And the water that's at the poles probably is from comets and meteorites slamming into the surface over time. And the ice that's in that, sort of migrating along the surface, and then freezing down in these cold areas. And so, I -- you know, I'm talking about intrinsic water to the moon versus external water. The external water might be more interesting for like refueling spacecraft someday. Intrinsic water, it's very minor and so it's always going to be of geologic interest, but probably not economic importance. Host: I see. So, when you say that you were looking at rocks and using these instruments to find little -- you know, use a different type of method to discover the water inside the rock, that was here on Earth, right? That was here -- Ryan Zeigler: All of that was done on Earth. In fact, the -- in Apollo missions -- I mean you see the Mars missions now and they have Rovers and they do all these cool measurements on the -- on Mars, they didn't do that on Apollo. They had some surface experiments where they did some geophysical experiments on the surface, but that was on the moon, as a whole, and not on the rocks. The rocks were really not studied until they came back because anything they might have done on the surface could be done much better back on Earth. And since they knew they were bringing the rocks back anyway, they didn't spend any mass, or time, or energy on that. They just collected the rocks and brought them back. Host: Plus, you risk the chance of contamination. Ryan Zeigler: Exactly. I mean we have a lot of talk now about, you know, what could be done on samples like on the way back and the answer is always like, don't touch the samples, just bring them back. Just don't touch the samples. We'll do it when you get them back here. And we is not me, and we is not NASA. We, is this -- the larger scientific community on the planet. And so, I keep using the royal we. And as my dad always asked, do you have a mouse in your pocket? No, it's just, you know, it's a very large and active science community that studies all these samples. Host: Well, and the -- and one of the more important parts about that is there is a finite number of samples that you have, right? Ryan Zeigler: There is. There is. Host: So, whenever they're bringing these samples back, the story from the Apollo days, what were some of the facilities that they were bringing them back to? What were some of the methods to make sure that they were acquired safely and properly? Ryan Zeigler: So, they had designed Building 37 here at Johnson Space Center was the Lunar Receiving Lab and they finished that in 1967, so a couple years before it came back. Because they had no real idea what lunar samples were like and because everyone has read War of the Worlds, they actually designed it as a quarantine facility. And so, both the astronauts and the samples went into quarantine for 21 days after Apollo's 11, 12, and 14, to make sure all the bugs from the moon didn't kill all life on Earth. And now once they got to the surface and they realized there was no water, and really no atmosphere, and they already knew that, they're like, there's no bugs in these samples. But through an abundance of caution, for the first three missions, they kept the quarantine going. And so, that was a facility designed to keep everything in, so everything leaked in. And the problem with that is everything leaks in on the samples, and we're trying to keep the samples clean. And so, once they realized, no, this isn't -- you know, this isn't a concern, we're not trying to keep the bugs in. They redesigned laboratories in the building next door -- in Building 31. And within about three or four years, they moved over and put most of the samples there in a positive pressure laboratory, where everything leaked out and everything leaked away from the samples. And the samples were stored in glove boxes surrounded by nitrogen and no one ever touched them, no one ever breathed on them, or coughed on them, like me. And so, yeah. So, that was -- that was a pretty quick change they had to make. Host: Okay. So, some of the later Apollo missions -- the samples collected from those I guess have some of the more pristine samples that you have here because of this method? Ryan Zeigler: Sort of. I mean there's more of them and so some of them were able to be held in reserve. But all of them originally came back and were open and then -- and initially analyzed in their lunar -- in the LRL, in the Lunar Receiving Lab. And then it wasn't till like '73, '74, when all of the samples got moved over to the next -- to the next thing, so yeah. Host: So, then the actual study of -- or the actual process of studying, what's that like? What is -- what do you do to actually figure out what's inside? Ryan Zeigler: Wow. There's so many different studies. So, I've been the Apollo curator for about six years now and I've had almost 400 individual requests to analyze sample. So, I'd like to go through them one by one -- no? Okay. So, yeah. Yeah. No, it could be a long podcast. You know, if you -- if you look at all of the collections in total, a lot of effort goes into dating the samples. And you would think, yeah, we already know the date of them. Well, as instruments and scientists get better -- oh, man -- the way they age date the samples has been refined over time. And there's a couple different camps still trying to figure out exactly the age of the moon. A lot of study has been on the new water they found. But there's even esoteric things. Like a guy in the UK wanted samples to do spectroscopy to figure out if he could see life on planet -- on exoplanets. And so, all life on Earth has a chirality, it's all left-handed or right-handed, and I'm not a biologist, so I don't remember. But if you look at the light that reflects off an atmosphere with that light in it, can have a chirality to it. And so, they're from orbit and Earth, they're trying to do that. And one of the main sources of contamination for them is light bouncing off the moon. So, he needed to see what light bouncing off the moon looked like to put into his equations to understand whether they could see life on exoplanets from their atmospheres -- from spectroscopy of their atmospheres. And so, every-- I mean everything in between. It's just crazy how diverse Apollo samples and samples, in general, can be used. Host: So, it's fair to say you're still studying them though, right? Ryan Zeigler: Oh, absolutely. This year, I -- you know, we have -- a new batch of requests just came in and we have 36 new requests for the -- to be considered by the committee that reviews all of these and they'll do that next month, so. I -- they might find out about it on here. They don't know how many we got, so they might be a little dismayed at how much work they have to do. Host: We'll put this out a little bit later, so we don't have any spoilers. Ryan Zeigler: No, that's okay. They wouldn't listen to me anyway. Host: Okay, so when you're cracking them open -- and some of the -- some of the first times you were actually -- you -- now you have scientists that have their hands on these lunar samples -- the first time. Ryan Zeigler: They better not. Host: Well, oh, okay. They have -- they have protective gloving -- gloves and -- Ryan Zeigler: Yeah. Sorry, sorry, sorry. Host: Proper equipment to analyze the samples for the first time, first time humans have ever done that. What were some -- was some of the first things that they wanted to look at and some of the first things that they found? Ryan Zeigler: So, some of the very first measurements that were done, after the Apollo 11 samples came back, were actually done here. So, the LRL was both the containment facility and the curation facility, but it also had a certain number of built-in instruments to do some of these initial preliminary examinations. And one of them was to look at the radiation in the sample. Now everyone hears radiation and thinks, Chernobyl or -- no, what they're trying to see is the natural radiation that every rock has. And so, they built a special pit underneath Building 37 that was lined with dunnite, a special type of rock from Earth, battleship armor from pre-nuclear tests. So, the -- it could drive down the low levels of natural background radiation. Put the samples in front of a detector and then see just how much radiation was coming off of these. And so that was one of the very first things done. They had a gas lab to see what kind of gases came off it, whether there was a, you know, measuring the solar wind. So, it was -- it was measurements like that that were initially done at Johnson Space Center. And then almost immediately after those initial measurements were done, they went out to I think 50 or 60 different groups around the country who were pre-approved, and they all had different stuff they were doing. Host: Unbelievable. So, I guess to work with this and to find out something specific, right, if you wanted to find out something more about radiation, there's something special that you have to design, something special that you have to do. It's not just chiseling at it and looking at it and say, ah, there's the radiation. There's like this huge -- this very unique type of experiment and facility that you have to design. Ryan Zeigler: Right. And that particular facility was both expensive and time-consuming. And so, that was the kind of thing that NASA was going to take on, where -- because they could use Apollo money on it. And then other things that didn't require quite such specialized equipment, that could be done better by the experts in those individual fields at the different universities and other institutions. Host: There you go. Okay, so I'm assuming that one of the main objectives, when you have these samples of moon rocks, is to find out what happened to the moon. What was the formation of the moon? So, does some of your findings support Giant Impact Theory? Ryan Zeigler: I think, at this point, pretty much all of the findings support Giant Impact. Now there's still -- yeah. I mean there's still a little bit of debate about how big the impactor was, or the exact timing, or -- but as far as I know -- and I go to all of these conferences, whether I like it or not, I'm -- and, you know, keep an eye on these guys. And no, I mean everyone -- no one's arguing about -- at these science conference -- whether there was a Giant Impact. They're arguing about the details of the Giant Impact. I know there are one or two holdouts, but that they are being increasingly marginalized, just by the -- by the data that's coming off the samples. Host: So, we can pretty much sit down and say, yeah, it was some kind of Giant Impact Theory that formed it. Ryan Zeigler: At this point, yes. I mean, although if you'd asked me 10 years ago if there was any water on the moon, I would have said absolutely not and everyone agrees on that. And so -- but there's physics involved here and I don't understand physics because I'm a geologists. But I mean the angular momentum of the Earth-moon system and the spin and all that, that's really hard to do any other way. And that's not going to change, like we're not going to learn how to measure angular momentum better. So, I don't think the Giant Impact is going away, yeah. Ryan Zeigler: Okay. Okay. That's fair. So, kind of going back to some of the facilities that you have. I'm imagining -- I'm imagining these guys in gloves and you said, oh, no, they're not going to be touching it. They're going to be wearing proper equipment and they're going to be using -- you know, they're going to make sure they're not -- nothing's going to get contaminated. What does that look like? What is this -- you say, bunny suit? Ryan Zeigler: Well, so in our lab, if you want to come and study the samples -- so, yeah, you would put on a full bunny suit. Think white polyester suit head-to-toe. Host: Okay. Ryan Zeigler: Basically, a pair of coveralls, cloth gloves, a hat. Not -- we don't have to wear masks most of the time. And then over boots. And then you go into a laboratory that's sterile -- not sterile because they're -- that's very clean. And then the samples are inside the cabinets. And then you put your hands through neoprene gloves and then if you needed to handle the samples, themselves, on the inside of the neoprene gloves -- excuse me -- you would put Teflon gloves. And so, you can only touch the samples with Teflon, or aluminum, or steel. So, you would have to actually handle the samples in our laboratory through three layers of gloves, inside of a controlled atmosphere cabinet. Yeah. And so, now not everyone in their own lab has to do that because we have to keep the samples ready for anyone to do anything, as near as we can. If somebody knows that they're not going to contaminate the samples by handling them in air, what -- when I did this at Washington University in Saint Louis, before I came here, we had a clean flow bench. We would take the samples to JSC [inaudible]. We would open them, we would pour them out, then you rinse them off with acetone, you get some of the dust off. Picked them up with tweezers, never touched them with my hands, despite what the pictures show. And then we would get them ready and when we send them off to the reactor to do -- to do -- to do measurements and stuff like that. So, clean space, controlled atmosphere, but not a controlled atmosphere -- sorry. Not inside of a nitrogen glovebox. And that's -- most people don't have the glove boxes we have. They cost a quarter of a million dollars each and there's all this infrastructure that goes into it, so. Host: Wow. Ryan Zeigler: Yeah. No. Host: Take your moon rocks very seriously. Ryan Zeigler: Yeah, well we spent 24 billion dollars to bring them back, we ought to -- we ought to keep -- you know, okay, we're trying to keep them safe for long term. Host: Exactly. And like you said, you're still studying them and there's still a lot of things to be discovered. So, the last thing you need is to -- is to waste any of the samples. Ryan Zeigler: You don't get to have two bad days in curation. You have one bad -- you can't un-contaminate a sample. If something goes wrong and water got on the samples, it's always going to have had water on it and it will eliminate certain number of measurements. And so, no, we -- yeah, you're right. We do -- we have procedures -- I mean I used to make fun of procedures before I came to NASA. Now I really make fun of procedures, but I understand why they're important and why we have them. And so -- and we have like 160 of them to run the lab and all the different things we have to do to them. Yeah. Host: Wow. Ryan Zeigler: Yeah. Auditors love us because we've got everything written down. It's great. Yeah. Host: Okay. So, then that brings me to the thought that there's a finite number of -- or finite amount of moon rocks that you have. So, how do you keep track of it? How do you make sure that you have -- that you're taking advantage of this finite amount? Ryan Zeigler: With great effort. So, every sample that we loan to a scientist to do study on -- to do a study on, we keep track of. And everything's a loan and they have to return it. So, if they destroy it, as part of the analysis, then great, then they have better have had permission to do that. Then that's great, we mark that off. But anything else, they would study, and they would come back. And so, once a year, I send them all an inventory, and they have to check off and they say, yes, I have all these samples or no I don't, in which case bad things happen. And no one ever says, no, I don't. They're very, very conscientious. And so, 125 inventories a year gets sent out and I have to -- you know, we all - we all take care of it. Now we do in -- an internal inventory with JSC security where once a year -- or once every other year, they come by and they ask us to find every sample for them. And so -- yeah, no. And so, we have to meet the same bar as everyone else, just every other year, because we have 100,000 samples and most scientists have 50 or 100, so. Host: So, the interesting thing about the moon rocks is that you're still -- you've collected them so long ago but you're still finding stuff out, right? And so -- so what are the -- some of the more recent findings that you've been having? Ryan Zeigler: Well, one of the more recent findings that has come out and in the last five or six years was that perhaps the Solar System didn't form the way we originally thought it did. People noticed that there was a preponderance of samples on the moon that are 3.9 billion years old. Now the age, itself, doesn't matter to you or me. But within the Solar -- and they were all formed by giant impacts. Now 600 million years after the Solar System formed, there shouldn't be a bunch of giant impacts. Everything should have quieted down by that. So, for -- to explain the lunar samples, they had to come up with a new dynamical model for the evolution of the entire Solar System. So, originally, it was -- the new one was called the Nice Model because it was formed by a bunch of scientists in Nice, France, which I hope is true or I'm going to get phone calls. And that said that Jupiter, and Saturn, and Uranus, and Neptune all formed in much closer to the Sun. They gravitationally interacted and then they spread out 3.9 million years ago. And when they did that, they took all of the asteroids and comments and spun them around the Solar System and that caused the Giant Impacts. Now people don't like the Nice Model anymore. Now they have something called the Grand Tack Model, but it doesn't matter. Any of the models for planetary formation actually have to explain the ages that we see in the Apollo samples. Now the ages, themselves, are actually old. They figured that out early on. But no one noticed how many ages were 3.9 and put two and two together with what it meant for the Solar System, as a whole, until more recently. And so -- you know. So, when people ask me what moon rocks can tell you about, I say, well, where Jupiter formed. And they always look at me like I'm lying. Host: Well, it's kind of amazing how we can find so much about our Solar System, just from studying so close to home. I've had a couple conversations with some -- some of the meteorite sample curators and like -- [ Inaudible ] Host: Yeah, I've had conversations with all of them and just the stories that you can find from analyzing these rocks are fantastic. Ryan Zeigler: And it's really nice because the meteorites are all really old. So, almost all the meteorites are older than all the Apollo samples. And all the Apollo samples are older than the Earth. And so, each of them gives you a different window into how the Solar System formed. And if we only had one, we wouldn't know the whole story, or even if we only had two. Having all three is really important to understanding how things work. Host: So, looking towards the future, are there missions that you are kind of planning for for possibly extra curation missions or anything that is going back to the moon to analyze something new? Ryan Zeigler: Well, I mean there was just a big announcement yesterday, obviously, that, you know, NASA is refocusing on the moon and I think want to send people back to the moon. And there was some talk about robotic missions, both to do in situ science, science on the surface, but also to hopefully bring back some samples. I stayed at Wash U to be part of the Moonrise Team, which was a new frontiers mission, so a billion dollar mission, to bring back samples back from the far side. We came in second twice to Juneau and OSIRIS-REx, I'm not bitter, especially while I was at the Juneau -- at the -- at the OSIRIS-REx launch. No. And then this most recent time, they just down selected Caesar and Dragonfly as the finalists for the next round of New Frontiers, so Moonrise won't go either. But within those two, Caesar is a sample return mission. It is a sample return mission from the surface of a comet. So, there was a Rosetta Mission by Europe and it went and it -- you know, it went into orbit around a comet. And then sent a lander and then studied that and I don't know that much about it. And I don't know that much about Caesar yet because it's brand new. But their plan is to bring back samples from the surface, both gas and ice, and I think rock samples, back from the surface of a comet, to Johnson Space Center, where we will curate them. So, we're going to have to figure out how to curate gas and ice. Host: Oh, yeah. Ryan Zeigler: And it's not that we don't have an idea. We do but we have never had to do it before. And so, we're going to spend the next -- luckily, we have about 15 years to build up the capabilities to get ready for that. Host: Okay, so capabilities in terms of facilities. Ryan Zeigler: Right. So, I mean keeping ice cold is easy. There's lots of ice labs around the country. But if you want to treat that ice like we treat rocks, where you're going to subdivide it, and that's different. If you want to work on it cold, that's harder. And also, there's cold and then there's cold. So, minus 20, great, that's easy. We can do that with a freezer. Minus 80, oh, that takes robotics and [inaudible] minus 160, like do you really want to keep it like the temperatures on the comet, itself? And these are things we still don't know all the answers to and we don't even know the requirements yet. But this is going to be what we spend the next decade figuring out. Host: Okay. All right. Well, best of luck to you. Ryan Zeigler: Yeah. Yeah. Host: It's going to be a long process. Ryan, thank you so much for coming on. That was -- that was fantastic to learn about everything -- all these moon rocks. I've been dying to have this conversation. Ryan Zeigler: It was my pleasure. Host: Fantastic. And it's crazy what the moon rocks can tell you, just from looking at these and that we're still finding stuff out and just, you know, the story of water that has to -- you have to rethink these thoughts that -- and findings from decades ago because there's something new that we found. So, it'll be interesting to see what comes up in the future. Ryan Zeigler: Yeah. Absolutely. Host: All right. Very cool. Thanks for coming on. Ryan Zeigler: All right. My pleasure. [ Music ] Host: Hey, thanks for sticking around. So, today, we talked with Ryan Ziegler about moon rocks and the facilities that are keeping them. And honestly, we're still hurting so much from these rocks. If you want to know more about the rocks, you can go to the ARES site, that's our Astromaterials group. It's ares.jsc.nasa.gov. You can go to that site also to find out how to get your hands on a meteorite sample if you actually want to study meteorites or moon rocks. On social media, you can follow the NASA Johnson Space Center accounts or the Astromaterials accounts, they have their own on Facebook, Twitter, and Instagram. You can go to any one of those accounts and use the hashtag ask NASA to submit an idea or question for the show or for I guess any other reason. But if you want it to be brought right here on Houston, we have a podcast, just make sure to mention the show, and then we'll actually bring it on, maybe answer it, or dedicate an entire episode to it. We have done in the past. This podcast episode was recorded on February 14, 2018. Thanks to Alex Perryman, and Tracy Calhoun, and Jenny Knotts. Thanks again to Dr. Ryan Zeigler for coming on the show. We'll be back next week.