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504 results for “pores”
Benchmark dataset for pore-scale CO2-water interaction
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Data from: Elucidating the impact of red blood cell membrane components on melittin-induced pore formation with molecular dynamics simulations
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Solid-state NMR data for: Sequential pore functionalization in MOFs for enhanced carbon dioxide capture
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Effect of pore collapse and grain crushing on the frequency dependence of elastic wave velocities in a porous sandstone
<p>Dataset for the article "Effect of pore collapse and grain crushing on the frequency dependence of elastic wave velocities in a porous sandstone"<br> by Sun, C., Borgomano, J.V.M., Fortin J., Wang, S.</p> <p> </p> <p>Please refer to the ReadMe file or to kang2008ping2008@163.com for more details.</p>
FIGURES 24–32. Neurisothrips species. Male sternal pore plates 24–29 in Diversity in the Hawaiian endemic genus Neurisothrips (Thysanoptera, Thripidae)
FIGURES 24–32. Neurisothrips species. Male sternal pore plates 24–29: (24) antennatus; (25) bidens sp. n.; (26) fran sp. n.; (27) karl sp. n.; (28) robbiei sp. n. [from Santalum]; (29) robbiei sp. n. [from Psychotria]; (30) saki sp. n.. Female sternites 31–32: (31) janis sp. n.; (32) bidens sp. n.
Integrative modeling of the in-cell architecture of the yeast Nuclear Pore Complex
<p>Repository with source code files and input files utilized for integrative modeling of the in-cell architecture of the yeast Nuclear Pore Complex (ScNPC). All output integrative models of ScNPCs associated with the following work are included:</p> <p>"In-cell architecture of the nuclear pore and snapshots of its turnover. Matteo Allegretti, Christian E. Zimmerli, Vasileios Rantos, Florian Wilfling, Paolo Ronchi, Herman K.H. Fung, Chia-Wei Lee, Wim Hagen, Beata Turonova, Kai Karius, Mandy Börmel, Xiaojie Zhang, Christoph Müller, Yannick Schwab, Julia Mahamid, Boris Pfander, Jan Kosinski, Martin Beck. Nature, 2020"</p> <p>For questions/support please <strong>contact</strong>: <a href="mailto:jan.kosinski@embl.de">jan.kosinski@embl.de</a> or <a href="mailto:vasileios.rantos@embl-hamburg.de">vasileios.rantos@embl-hamburg.de</a></p>
Soil water content determined at saturation and water holding capacity and calculated at 50% water filled pore space
<p>Optimizing soil microbial activity requires an equal balance between water- and air-filled porosity, i.e. 50% water filled pore space (WFPS). However, many soil biological investigations report water as some fraction of water-holding capacity (WHC). This study was conducted to fill a quantitative gap between WFPS and WHC. Soil samples (n=198) from 10 eastern U.S. states and one state in Brazil provided a wide distribution of clay (0.064-0.487 kg kg<sup>-1</sup>) and soil organic C (SOC, 5.2-52.0 g kg<sup>-1</sup>) concentrations (5-95% range). Gravimetric soil water content (SWC) was determined at WHC and at saturation. Both clay and SOC concentrations strongly influenced SWC; the effect of SOC was strongest and non-linear. To achieve 50% WFPS, gravimetric SWC was 0.69<u>+</u>0.10 times that of WHC and 0.59<u>+</u>0.03 times that of saturation. For soil biological assays, 50% WFPS could be reasonably accurately and simply achieved with calculations using gravimetric SWC at saturation multiplied by 0.59. </p>
Brittle faulting of ductile rock induced by pore fluid pressure build-up
<p>his is the ReadMe file corresponding to the study entitled: "Brittle faulting of ductile rock induced by pore fluid pressure build-up"</p> <p>By Noël C., Passelègue X. F., Violay M.</p> <p>This study is under review at JGR: Solid Earth</p> <p>This Read-Me file has been last edited in November 2020</p> <p>This readme file describes the data repository and supplementary files accompanying the above publication. <br> For any further queries please contact corentin.noel@epfl.ch</p>
Data from: Dynamic pore structure evolution of the ion adsorbed rare earth ore during the ion exchange process
<p><span>During the leaching process of the ion adsorbed rare earth ore, the pore structure evolution of the ore body plays a vital role in the seepage of the leaching solution. To investigate the evolution of the pore structure during the leaching process, experiments have been carried out with remodeled rare earth ore samples based on physical characteristics of in-situ ores. The seepage rate difference between deionized water leaching solution and 2% NH<sub>4</sub>Cl leaching solution during the active leaching period are analyzed. The porosity and the dynamic pore size evolution of pore structures in the ore body are discussed. Results indicate that along with ion exchange between the rare earth ore and the leaching solution, the porosity of the sample remains constant and the pore structure shows a decreasing trend in the first part and an increasing trend in the second part. Specifically, during the ion exchange process, the number of minimal pores (0~5μm), small pores (5~10μm), and medium pores (10~25μm) increases significantly and the number of medium-large pores (25~60μm), large pores (60~120μm), and mega pores (>120μm) decreases dramatically. Along with the completion of the ion exchange process, the evolution of porous structure shows an opposite trend. The mechanism study reveals that the evolution of pore structure is induced by the difference of ionic strength in the leaching solution during the ion exchange process, where the rare earth ore microparticles will be absorbed or desorbed on to the solid phase.</span></p>
FIGURES 23–25 in A taxonomic revision of the family Oncopodidae VI. Martensiellus, a new genus from Borneo, and the discovery of a tarsal pore organ in Oncopodidae (Opiliones: Laniatores)
FIGURES 23–25.?Martensiellus n. g. sp., female from Kaharian. SEMmicrographs of right tarsus I showing dorsal pore at different enlargements. Scale bars: 100 µm (23), 20 µm (24), 5 µm (25).
FIGURES 11–17. Martensiellus tenuipalpus n. g., n in A taxonomic revision of the family Oncopodidae VI. Martensiellus, a new genus from Borneo, and the discovery of a tarsal pore organ in Oncopodidae (Opiliones: Laniatores)
FIGURES 11–17. Martensiellus tenuipalpus n. g., n. sp., penis (11–14 holotype, 15–17 paratype). 11–12. Total penis (11 dorsal view, 12 lateral view). 13–15, 17. Apex of penis in resting position (13, 15 dorsal view, 14, 17 lateral view). 16. Apex of penis with expanded glans, dorsal view. Abbreviations: d.m. distal margin of truncus penis, l.s. lateral sclerite of glans, m.p. median plate of glans, m.t. membranous tubes of glans, s stylus. Scale bars: 0.5 mm (11–12), 0.1 mm (13–17).
FIGURES 18–22 in A taxonomic revision of the family Oncopodidae VI. Martensiellus, a new genus from Borneo, and the discovery of a tarsal pore organ in Oncopodidae (Opiliones: Laniatores)
FIGURES 18–22.?Martensiellus n. g. spp., female from Mulu N.P. (18, 19), female from Kaharian (20–22). 18. Anterior part of body and proximal part of palpus and of chelicera, lateral view. 19, 22. Distal part of leg II, lateral view. 20. Anterior part of body and proximal part of palpus, lateral view; 21. Chelicera, retrolateral view. Scale bars: 1 mm (18–19, 20–22 same scale).
FIGURES 1–3. Martensiellus tenuipalpus n. g., n in A taxonomic revision of the family Oncopodidae VI. Martensiellus, a new genus from Borneo, and the discovery of a tarsal pore organ in Oncopodidae (Opiliones: Laniatores)
FIGURES 1–3. Martensiellus tenuipalpus n. g., n. sp., male holotype, habitus (1 dorsal view, 2 ventral view, 3 lateral view). Scale bar: 1 mm.
FIGURES 4–10. Martensiellus tenuipalpus n. g., n in A taxonomic revision of the family Oncopodidae VI. Martensiellus, a new genus from Borneo, and the discovery of a tarsal pore organ in Oncopodidae (Opiliones: Laniatores)
FIGURES 4–10. Martensiellus tenuipalpus n. g., n. sp., male (4–9 holotype, 10 paratype). 4. Chelicera, lateral view. 5. Palpus, lateral view. 6. Distal parts of legs, lateral view (6 leg I, 7 leg II, 8 leg III, 9 leg IV). 10. Palpus and anterior part of body, lateral view. Scale bars: 1 mm (4–9 same scale).
FIGURE 5 in The mesopelagic copepod Gaussia princeps (Scott) (Calanoida: Metridinidae) from the Western Caribbean with notes on integumental pore patterns
FIGURE 5. The northwestern tropical Atlantic with the location and authorities of the regional records of Gaussia princeps (Scott). 1. Wilson (1950); 2. Grice (1963); 3. Owre & Foyo (1964); 4 Owre & Foyo (1967); 5. this survey.
FIGURE 4 in The mesopelagic copepod Gaussia princeps (Scott) (Calanoida: Metridinidae) from the Western Caribbean with notes on integumental pore patterns
FIGURE 4. Gaussia princeps (Scott, 1894) from the western Caribbean. Adult male. A. second swimming leg; B. detail of hook-like and spiniform processes on first endopodal segment of second swimming leg; C. third swimming leg; D. fourth swimming leg; E. fifth swimming leg, anterior view; F. basipod and exopod of left fifth leg, lateral view; G. detail of processes of second exopodal segment of left fifth leg; H. detail of distal exopodal segment of right fifth leg, showing ornamentation. Position of integumental pores indicated by solid circles. Scale bars A,C–E,H=0.7 mm, B,F,G=0.3 mm.
FIGURE 3 in The mesopelagic copepod Gaussia princeps (Scott) (Calanoida: Metridinidae) from the Western Caribbean with notes on integumental pore patterns
FIGURE 3. Gaussia princeps (Scott, 1894) from the western Caribbean. Adult male. A. antenna; B. mandibular palp; C. mandibular blade showing detail of teeth and blade ornamentation; D. maxilla; E. maxilliped; F. first swimming leg. G. rostral area, ventral view. Some setae cut short. Position of integumental pores indicated by solid circles. A,B–G= 0.7 mm, C=0.2 mm.
FIGURE 2 in The mesopelagic copepod Gaussia princeps (Scott) (Calanoida: Metridinidae) from the Western Caribbean with notes on integumental pore patterns
FIGURE 2. Gaussia princeps (Scott, 1894) from the western Caribbean. Adult male. A. left antennule segments 1–10; B. same, segments 11–16; C. same, segments 17–23. D. right antennule, segments 1–10; E. same, segments 11–20; F. detail of modified seta and aesthetasc; G. detail of segment 17 and distal acute process. Position of integumental pores indicated by solid circles. Scale bars: A–E=0.7 mm, F=0.05 mm, G=0.35 mm.
FIGURE 1 in The mesopelagic copepod Gaussia princeps (Scott) (Calanoida: Metridinidae) from the Western Caribbean with notes on integumental pore patterns
FIGURE 1. Gaussia princeps (Scott, 1894) from the western Caribbean. Adult male. A. habitus, lateral view; B. habitus, dorsal view; C. cephalic area showing frontal process and depression, lateral view; D. fifth pedigerous and first urosomites, dorsal view; E. anal somite and caudal rami, dorsal view; F. same, lateral. Scale bars: A,B= 3mm, C–F=0.7 mm.
FIGURES 1–9 in Sternal pore plates (glandular areas) of male Thripidae (Thysanoptera)
FIGURES 1–9. Pore plates of male Thysanoptera. Sternites VII–VIII: (1) Holopothrips tabebuia (Phlaeothripidae). (2) Psalidothrips taylori (Phlaeothripidae). (3) head, Merothrips floridensis (Merothripidae). (4) Sternite VII Holarthrothrips josephi (Adiheterothripidae). (5) Sternites VII–VIII Heterothrips peixotoae (Heterothripidae). (6) Sternites IV–VI Sericothrips staphylinus (Sericothripinae). Panchaetothripinae sternites IV–VI, 7–8: (7) Heliothrips haemorrhoidalis; (8) Parthenothrips dracaenae. (9) Sternites III–IV Desertathrips chuquiraga (Thripinae).
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
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DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
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