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433 results for “FE”
Raw and processed anomalous diffraction data for crystals of metal-free R2lox soaked with Mn, Fe and Co or Zn
<p>Raw and processed anomalous diffraction data for crystals of metal-free <em>Geobacillus kaustophilus</em> R2-like ligand-binding oxidase (R2lox) soaked with 5 mM each MnCl<sub>2</sub>, (NH<sub>4</sub>)<sub>2</sub>Fe(SO<sub>4</sub>)<sub>2</sub> and CoCl<sub>2</sub> or ZnCl<sub>2</sub>. Data were collected on two crystals each after soaking with Mn, Fe and Co or Mn, Fe and Zn, respectively. For each crystal, one dataset each was collected at the Fe K edge (7162 eV), Mn K edge (6589 eV) and Co K edge (7721 eV) or Zn K edge (9664 eV; X-ray energies corresponding to the theoretical K edge + 50 eV). Data were collected at 100 K on a Pilatus 6M detector at beamline X06SA of the Swiss Light Source (SLS, Villigen, Switzerland) on September 23, 2012, and processed with XDS and XSCALE. All raw and processed diffraction data for each crystal are compressed into one file. </p>
Additional information for Acidification from microbial oxidation of N, S, Fe and Mn as potential key mechanism for sprayed concrete deterioration in a subsea road tunnel
<p>Here we include additional files for Karacic <em>et al</em>. <strong>Acidification from microbial oxidation of N, S, Fe and Mn as potential key mechanism for sprayed concrete deterioration in a subsea road tunnel</strong></p> <p>Metagenome reads and MAGs are avaliable in the NCBI BioProject PRJNA755678</p> <p>The following files are included here</p> <ul> <li><strong>MAGs_summary_Oslofjord.tsv</strong>: Information about the Oslofjord MAGs (GTDB R207 taxonomy, relative abundance, Completness, Contamination, NCBI accessions)</li> <li><strong>gtdbtk.ar53.summary.</strong> Output from GTDB-Tk v2.1.0 with GTDB R207_v2. Archaeal MAGs</li> <li><strong>gtdbtk.bac120.summary.tsv</strong>. Output from GTDB-Tk v2.1.0 with GTDB R207_v2. Bacterial MAGs</li> <li><strong>FeGenie-geneSummary.csv</strong>: Output from FeGenie</li> <li><strong>Annotations_1.tsv</strong> : Output from DRAM (215 MAGs)</li> <li><strong>Annotations_2.tsv</strong>: Output from DRAM (186 MAGs)</li> <li><strong>OFTMs_DRAM_genes.DiSCo.filtered.txt</strong>. Output from DiSCo</li> <li><strong>code_R.zip</strong>: R-code and additional files used for making MAGs figures</li> </ul> <p>This is version 2 of the dataset and it replaces version 1 (https://doi.org/10.5281/zenodo.5292093) </p>
4D STEM acquisition on an atom probe specimen of an ultrafine grain Fe-51.4at% Cr alloy
<p>Material: Fe-51.4at% Cr alloy processed by high pressure torsion </p> <p>Microscope: JEOL F 200<br>Accelration voltage: 200 kV<br>Aperture: 10 µm<br>Camera length: 200 mm<br>Detector size in pixel: 512 x 512<br>Scanned area size in pixel: 250 x 150<br>Scanned area size in nm2: 625 x 375</p>
Accessing Homo- and Heteroleptic α-Diimin Complexes (M = Fe, Co)
<p>The follwoing repository contains the cartesian coordinates of the calculated structures and the energies obtained by DFT-calculations. Please cite the original source/paper.</p>
Source code of tables for the publication "K- and L-shell theoretical fluorescence yields for the Fe isonuclear sequence"
<p>In this work, we present K- and L- shell fluorescence yield values of the full isonuclear sequence of Fe ions, using a state-of-the-art multiconfiguration Dirac-Fock approach. These results may be of importance for spectral fitting and plasma modeling, both in laboratory and astrophysical studies, where Fe is an important benchmark element. The K-shell fluorescence yields were found to be very similar up to the removal of 14 electrons.</p>
Supplementary Table S1. Combined analysis of variance containing the degrees of freedom (DF), mean squares (MS), P value (P val.), mean, coefficient of experimental variation (CEV%) and selective accuracy (SA) for the traits of luminosity (L*), chromaticity a* (a*), chromaticity b* (b*), grain length (length, mm), grain width (width, mm), grain thickness (thickness, mm), mass of 100 grains (Mass, g), normal grains (Ng, %), water absorption (absorption, %), cooking time (Ct, min:s), and concentrations of potassium (K, g kg-1 dry matter - DM), phosphorus (P, g kg-1 DM), calcium (Ca, g kg-1 DM), magnesium (Mg, g kg-1 DM), iron (Fe, mg kg-1 DM), zinc (Zn, mg kg-1 DM), and copper (Cu, mg kg-1 DM) obtained in 25 common bean cultivars evaluated in four experiments carried out from 2019 to 2021
<p><strong><span>Table S1.</span></strong><span> Combined analysis of variance.</span></p> <p><strong><span>Indirect selection for multiple technological and nutritional traits in common bean cultivars under different degrees of multicollinearity</span></strong></p> <p><strong><span>Bragantia, 2024.</span></strong></p>
The P-V-T dataset of liquid Fe-C alloys from FP-MD simulations
<p>The <em>P</em>-<em>V</em>-<em>T</em> dataset of liquid Fe-C alloys with different carbon contents (<em>X</em><sub>C</sub> = 0, 2.1, 4.7, 7.6, and 11.2 wt%) under the <em>P</em>-<em>T</em> conditions of the outer core (~136-330 GPa, 4000-6000 K) are obtained via first-principles molecular dynamics simulations.</p>
Reduced atomic models for large-scale computations: Fe XIII near-infrared lines
<p>The tar file contains two directories. One contains the CHIANTI v.8-11 format main files<br>produced relative to a 33 merged states Fe XIII model.</p> <p>The other contains CHIANTI and P-CORONA format files for a 55-states Fe XIII model.</p> <p>In both cases the models were built to obtain accurate emissivities of the Fe XIII near-infrared lines withtin the ground configuration. </p> <p><br>The models are described in Del Zanna and Hebbur Dayananda, 2024, submitted to MNRAS.</p> <p>Information on the CHIANTI programs can be found in chianti-vip.com</p> <p>Information on P-CORONA can be found on https://research.iac.es/proyecto/polmag/pages/codes/p-corona.php</p>
Occupant Simulation Database and FE-Model based on Honda Accord 2024 Simplified Passenger Model and SOBOL Sampling with 8,192 samples and HIII05F, HIII50M, HIII95M
<p>Database and FE-models with 24,576 Honda Accord 2014 passenger occupant simulations. </p> <p> </p>
Occupant Simulation Database and FE-Model based on Honda Accord 2024 Simplified Passenger Model and SOBOL Sampling with 256 samples and HIII05F, HIII50M, HIII95M
<p>Database and FE-models with 768 Honda Accord 2014 passenger occupant FE-simulations. </p>
Obras estratégicas en la ciudad de Santa Fe
<p>Fuente: Álvarez, Tesis doctoral:<strong> “</strong>La Iniciativa para la Integración en Infraestructura Regional Suramericana. Estudio del eje Hidrovía Paraguay-Paraná a partir del proyecto de reconversión del Puerto de Santa Fe” 2019, 263.</p>
Discovery of a Seven-Coordinated High Pressure CrSb2 Phase: Experimental Equation of State of TMSb2 (TM = Cr, Fe, Ru, Os)
<p>DFT calculations from: Discovery of a Seven-Coordinated High Pressure CrSb2 Phase: Experimental Equation of State of TMSb2 (TM = Cr, Fe, Ru, Os); Emma Ehrenreich-Petersen, Mads F. Hansen, Justin Jeanneau, Davide Ceresoli, Francesca Menescardi, Martin Ottesen, Vitali Prakapenka, Sergey N. Tkachev and Martin Bremholm; submitted to Inorg. Chem. (2023)</p>
Seasonal concentrations and fluxes of dissolved, soluble, and colloidal Fe and dissolved organic matter amount and composition (DOC and PARAFAC)
<p>These datasets accompany the following manuscript:</p> <p>Logozzo, L.A.*, Hosen, J.D., McArthur, J., and Raymond, P.A. Distinct drivers of two size fractions of operationally dissolved Fe in a temperate river. Limnology and Oceanography.</p> <p>*Corresponding Author: Laura A. Logozzo, laura.logozzo@uleth.ca</p> <p>Datasets:</p> <p>1- Fe-DOM-EMMA-merged.xlsx: this dataset includes operationally dissolved (<0.22 µm), colloidal (0.02-0.22 µm), and soluble (<0.02 µm) DOC concentrations, total Fe concentrations, PARAFAC component scores <0.22 µm, and end-member mixing model scores <0.22 µm. Samples were collected approximately bi-weekly from the Connecticut River at Thompsonville from April 2018 to March 2020.</p> <p>2- Loadest-merged.xlsx: this dataset includes LOADEST-modeled daily-average and monthly-average fluxes of operationally dissolved (<0.22 µm), colloidal (0.02-0.22 µm), and soluble (<0.02 µm) Fe, DOC <0.22 µm, and allochthonous-like DOC <0.22 µm.</p> <p>All methodology is described in the accompanied manuscript.</p>
Mg and Fe isotopes and other geochemical data for Gangdese arc mafic plutonic rocks and trench sediments
<p>These files content unpublished Mg and Fe isotopes and other geochemical data for the Gangdese arc mafic plutonic rocks and trench sediments.</p>
The contribution of Fe(III) reduction to soil carbon mineralization in montane meadows depends on soil chemistry, not parent material or microbial community
<p>The long-term stability of soil carbon (C) is strongly influenced by organo-mineral interactions. Iron (Fe)-oxides can both inhibit microbial decomposition by providing physicochemical protection for organic molecules and enhance rates of C mineralization by serving as a terminal electron acceptor, depending on redox conditions. Restoration of floodplain hydrology in montane meadows has been proposed as a method of sequestering C for climate change mitigation. However, dissimilatory microbial reduction of Fe(III) could lead to C losses under increased reducing conditions. In this study, we explored variations in Fe-C interactions over a range of redox conditions and in soils derived from two distinct parent materials to elucidate biochemical and microbial controls on soil C cycling in Sierra Nevada montane meadows. Differences in parent material were associated with different rates of Fe(III) reduction at increasing soil moisture levels, but not with differences in soil C mineralization. Known Fe(III)-reducing taxa were present in all samples but neither the relative abundance nor richness of Fe(III) reducers corresponded with measured rates of Fe(III) reduction. Under reducing conditions, our results suggest that Fe(III) reduction contributes to C mineralization only when Fe-bound C is present. However, Fe-bound C was not present in all of our soils and was below theoretical limits for C sorption onto Fe-oxides where it was found. Overall, our results suggest that meadow-specific soil chemistry drives Fe-C interactions and that the impact of Fe on C cycling in montane meadows may be smaller than in other ecosystems.</p>
HLY0503-JPC22 Hiatus Low Fe-Grain Intervals
<p>Supplementary data for Shannon Cofield dissertation July 2023:</p> <p>COFIELD, S. et al., 2023. DATA: HISTORY OF ICE-RAFTING IN THE ARCTIC OCEAN DURING GLACIAL MAXIMA THROUGH MARINE ISOTOPE STAGE 6. Old Dominion University, Dissertation.</p> <p> </p> <p>Calculations for hiatus intervals exceeding:</p> <p>Barents-Svalbard Source Areas during MIS 2 (>0.12 kyr)</p> <p>All other Source Areas during MIS 2, 4 and 6 (>1.00 kyr)</p>
Combined P-V-T Data for hcp-Fe with Reevaluated Pressures and Pressure Uncertainties
<p>This dataset consists of unit-cell volumes, temperatures, and reevaluated pressures, and their related uncertainties for <em>hcp-</em>Fe. The volumes and temperatures are taken from previous studies (indicated under the column "Original Publication"), and the pressures were reevaluated using the internally consistent pressure scales of Fei <em>et al</em>., 2007. The pressure uncertainties presented here propagate uncertainties in the volume and temperature measurements, as well as the uncertainty and covariance in the equation of state parameters used to determine the pressure. Also listed are the beamline the data were originally collected at, and the compression technique (DAC= Diamond Anvil Cell; MAP= Multi-Anvil Press).</p>
Figura 3 in Cicádidos (Insecta: Hemiptera: Cicadidae) Del Museo Provincial De Ciencias Naturales "Florentino Ameghino" Santa Fe, Argentina
Figura 3: Mapa de la distribución geográfica de especies elaborado por Torres (1946).
Quesada gigas Olivier, 1970(Figura 1l) in Cicádidos (Insecta: Hemiptera: Cicadidae) Del Museo Provincial De Ciencias Naturales "Florentino Ameghino" Santa Fe, Argentina
Quesada gigas Olivier, 1970(Figura 1l)
Figura 2 in Cicádidos (Insecta: Hemiptera: Cicadidae) Del Museo Provincial De Ciencias Naturales "Florentino Ameghino" Santa Fe, Argentina
Figura 2: Mapa de la distribución geográfica de especies elaborado por Torres (1945).
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Allen Brain Atlas
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DANDI Archive for NWB datasets
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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
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.