cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.10207682
title: TRANSLATION STUDIES AND ITS IMPORTANCE IN TECHNOLOGICAL ERA. ASPECTS, TYPES AND METHODS OF TRANSLATION
DOI: 10.5281/zenodo.7942986
title: Django ecosystem's reusable applications

description: Repositories retrieved regarding the Django ecosystem, including specific files for each research question of the paper "On the Adoption of Reusable Web Applications: The Django Ecosystem Case".
DOI: 10.5281/zenodo.7942985
title: Django ecosystem's reusable applications

description: Repositories retrieved regarding the Django ecosystem, including specific files for each research question of the paper "Assessing Reusable Web Applications: The Django Ecosystem Case".
DOI: 10.5281/zenodo.8003371
title: Django ecosystem's reusable applications

description: Repositories retrieved regarding the Django ecosystem, including specific files for each research question of the paper "Assessing Reusable Web Applications: The Django Ecosystem Case".
DOI: 10.5517/ccdc.csd.cc2fc2pl
title: CCDC 2244979: Experimental Crystal Structure Determination

description: Related Article: Dumitrela Diaconu, Violeta Mangalagiu, Simona Dunca, Dorina Amariucai-Mantu, Vasilichia Antoci, Tiberiu Roman, Ionel I. Mangalagiu|2023|Heliyon|9|e21518|doi:10.1016/j.heliyon.2023.e21518
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.34740/kaggle/dsv/6510919
title: Mouth and Oral Diseases (MOD)
DOI: 10.21979/n9/3zwugj
title: Replication Data for: Nonlinear Parametric Scattering of Exciton Polaritons in Perovskite Microcavities

description: Experimental data and simulation
DOI: 10.5281/zenodo.10207722
title: SPORTS TERMINOLOGY AND ITS NATIONAL-CULTURAL CHARACTERISTICS IN ENGLISH AND UZBEKI
DOI: 10.5281/zenodo.10207723
title: SPORTS TERMINOLOGY AND ITS NATIONAL-CULTURAL CHARACTERISTICS IN ENGLISH AND UZBEKI
DOI: 10.5281/zenodo.10207726
title: FEATURES OF PREVENTING CORRUPTION
DOI: 10.5281/zenodo.10207727
title: FEATURES OF PREVENTING CORRUPTION
DOI: 10.5281/zenodo.10207734
title: Large-scale Comparison of Fe and Ru Polyolefin C–H Activation Catalysts

description: We performed a large-scale density functional theory comparison of polyolefin C–H hydroxylation trends across over 200 Fe and Ru catalysts that are identical except for their metal centers for the radical-rebound conversion of propane to propanol. 
This ZIP contains optimized structures of all reactive intermediates of the Fe and Ru catalysts in the final dataset; approximate transition state structures from the calculated reaction coordinates; raw electronic energies and reaction energies for all Fe and Ru catalysts in the final dataset; electronic properties of all intermediates of the Fe and Ru catalysts in the final dataset; Fe and Ru catalysts that were discarded during DFT (ZIP)
DOI: 10.5281/zenodo.10207735
title: Large-scale Comparison of Fe and Ru Polyolefin C–H Activation Catalysts

description: We performed a large-scale density functional theory comparison of polyolefin C–H hydroxylation trends across over 200 Fe and Ru catalysts that are identical except for their metal centers for the radical-rebound conversion of propane to propanol. 
This ZIP contains optimized structures of all reactive intermediates of the Fe and Ru catalysts in the final dataset; approximate transition state structures from the calculated reaction coordinates; raw electronic energies and reaction energies for all Fe and Ru catalysts in the final dataset; electronic properties of all intermediates of the Fe and Ru catalysts in the final dataset; Fe and Ru catalysts that were discarded during DFT (ZIP)
DOI: 10.6084/m9.figshare.24635343
title: Third best-ranked covariate model (M2)

description: Cmdstanr generated output files (containing posterior samples).
DOI: 10.6084/m9.figshare.24635334
title: Second best-ranked covariate model (M2)

description: Cmdstanr generated output files (containing posterior samples).
DOI: 10.6084/m9.figshare.24635334.v1
title: Second best-ranked covariate model (M2)

description: Cmdstanr generated output files (containing posterior samples).
DOI: 10.6084/m9.figshare.24635346
title: Fourth best-ranked covariate model (M2)

description: Cmdstanr generated output files (containing posterior samples).
DOI: 10.6084/m9.figshare.24635346.v1
title: Fourth best-ranked covariate model (M2)

description: Cmdstanr generated output files (containing posterior samples).
DOI: 10.5281/zenodo.10207742
title: NATURE AND FEATURES OF INNOVATION POTENTIAL OF AN INDUSTRIAL ENTERPRISE IN CONDITIONS OF LIMITED RESOURCES
DOI: 10.5281/zenodo.10207743
title: NATURE AND FEATURES OF INNOVATION POTENTIAL OF AN INDUSTRIAL ENTERPRISE IN CONDITIONS OF LIMITED RESOURCES
DOI: 10.6084/m9.figshare.21081955
title: Professional Development in Reading Comprehension

description: Codebooks for meta-analysis on teacher professional development.
DOI: 10.6084/m9.figshare.21081955.v1
title: Professional Development in Reading Comprehension

description: Codebooks for meta-analysis on teacher professional development.
DOI: 10.5517/ccdc.csd.cc2h1h57
title: CCDC 2295338: Experimental Crystal Structure Determination

description: Related Article: Renshi Luo, Yuqiu Liang, Sen Wang, Jianhua Liao, Lu Ouyang|2023|J.Catalysis|428|115184|doi:10.1016/j.jcat.2023.115184
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5281/zenodo.10206454
title: IODP Expedition 391 X-ray fluorescence (XRF)

description: Elemental peak intensities in section halves were measured by an Avaatech X-ray fluorescence (XRF) Core Scanner postexpedition. Each measurement position may be measured at multiple XRF conditions in order to excite and measure specific ranges of elements (e.g., 10 kV and no filter for light elements). Peak intensity changes (concentrations not provided) are then used to help recognize and define major chemostratigraphic units without the need for destructive sampling. Data are presented in comma-delimited (CSV) files by section and by energy/instrumental conditions.
DOI: 10.5281/zenodo.10206455
title: IODP Expedition 391 X-ray fluorescence (XRF)

description: Elemental peak intensities in section halves were measured by an Avaatech X-ray fluorescence (XRF) Core Scanner postexpedition. Each measurement position may be measured at multiple XRF conditions in order to excite and measure specific ranges of elements (e.g., 10 kV and no filter for light elements). Peak intensity changes (concentrations not provided) are then used to help recognize and define major chemostratigraphic units without the need for destructive sampling. Data are presented in comma-delimited (CSV) files by section and by energy/instrumental conditions.
DOI: 10.5281/zenodo.10206452
title: IODP Expedition 391 X-ray diffraction (XRD)

description: X-ray diffraction (XRD) is used to identify minerals and their proportions in sediment or hard rock sample powders on a Bruker AXS D4 Endeavor X-ray diffractometer. Results are returned as diffractograms in a viewable format (either PDF or PNG).
DOI: 10.5281/zenodo.10206453
title: IODP Expedition 391 X-ray diffraction (XRD)

description: X-ray diffraction (XRD) is used to identify minerals and their proportions in sediment or hard rock sample powders on a Bruker AXS D4 Endeavor X-ray diffractometer. Results are returned as diffractograms in a viewable format (either PDF or PNG).
DOI: 10.5281/zenodo.10206450
title: IODP Expedition 391 Thermal conductivity

description: Thermal conductivity was measured using the heated needle method in either full-space needle configuration (soft/saturated sediments) or half-space needle configuration (harder materials) of a TeKa Berlin TK-04 thermal conductivity meter. Heat is applied to the sample and then thermal equilibrium is sought. The heating and equilibration curve is reduced to derive the thermal conductivity value. Raw data are stored if a user wishes to do off-line or postexpedition reduction.
DOI: 10.5281/zenodo.10206451
title: IODP Expedition 391 Thermal conductivity

description: Thermal conductivity was measured using the heated needle method in either full-space needle configuration (soft/saturated sediments) or half-space needle configuration (harder materials) of a TeKa Berlin TK-04 thermal conductivity meter. Heat is applied to the sample and then thermal equilibrium is sought. The heating and equilibration curve is reduced to derive the thermal conductivity value. Raw data are stored if a user wishes to do off-line or postexpedition reduction.
DOI: 10.5281/zenodo.10206448
title: IODP Expedition 391 Magnetic remanence (SRM-longcore)

description: Magnetic remanence was measured on section halves (and rarely on whole-round sections) using a 2G Enterprises 760R cryogenic magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization steps were performed on the samples by alternating field (AF) demagnetizer coils mounted in-line within the instrument.
DOI: 10.5281/zenodo.10206449
title: IODP Expedition 391 Magnetic remanence (SRM-longcore)

description: Magnetic remanence was measured on section halves (and rarely on whole-round sections) using a 2G Enterprises 760R cryogenic magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization steps were performed on the samples by alternating field (AF) demagnetizer coils mounted in-line within the instrument.
DOI: 10.5281/zenodo.10206446
title: IODP Expedition 391 Magnetic remanence (spinner)

description: Magnetic remanence was measured on discrete samples by an Agico JR-6A spinner magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization or remagnetization steps were performed on the samples (e.g., alternating field [AF] demagnetization, thermal demagnetization [TD], or isothermal remanent magnetization [IRM]).
DOI: 10.5281/zenodo.10206447
title: IODP Expedition 391 Magnetic remanence (spinner)

description: Magnetic remanence was measured on discrete samples by an Agico JR-6A spinner magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization or remagnetization steps were performed on the samples (e.g., alternating field [AF] demagnetization, thermal demagnetization [TD], or isothermal remanent magnetization [IRM]).
DOI: 10.34740/kaggle/dsv/7058967
title: 🐧 Palmer Penguins for binary classification
DOI: 10.5281/zenodo.10206444
title: IODP Expedition 391 Spectrophotometry

description: Interstitial water constitutents were measured by UV-VIS spectrometry using colorimetric methods (e.g., ammonium, nitrate, nitrite, phosphate, silica, and sulfide) by an Agilent CARY 100 UV-VIS spectrophotometer.
DOI: 10.5281/zenodo.10206445
title: IODP Expedition 391 Spectrophotometry

description: Interstitial water constitutents were measured by UV-VIS spectrometry using colorimetric methods (e.g., ammonium, nitrate, nitrite, phosphate, silica, and sulfide) by an Agilent CARY 100 UV-VIS spectrophotometer.
DOI: 10.5281/zenodo.10206441
title: IODP Expedition 391 Sample report

description: Report includes detailed information about samples taken for testing: location/depth, type/form factor, test, request number, and database identifier.
DOI: 10.5281/zenodo.10206440
title: IODP Expedition 391 Sample report

description: Report includes detailed information about samples taken for testing: location/depth, type/form factor, test, request number, and database identifier.
DOI: 10.5281/zenodo.10206436
title: IODP Expedition 391 Color reflectance

description: Color reflectance data were measured on section halves using an integration sphere and a UV-VIS spectrophotometer mounted on the Section Half Multisensor Logger (SHMSL). Spectral counts are recorded in the range of 380 to 700 nm, covering the visible spectrum, and binned in ~2 nm bins. Spectral data are reduced from spectra and recorded in tristimulus XYZ values, CieLAB L*a*b* values, and other units.
DOI: 10.5281/zenodo.10206437
title: IODP Expedition 391 Color reflectance

description: Color reflectance data were measured on section halves using an integration sphere and a UV-VIS spectrophotometer mounted on the Section Half Multisensor Logger (SHMSL). Spectral counts are recorded in the range of 380 to 700 nm, covering the visible spectrum, and binned in ~2 nm bins. Spectral data are reduced from spectra and recorded in tristimulus XYZ values, CieLAB L*a*b* values, and other units.
DOI: 10.5281/zenodo.10206434
title: IODP Expedition 391 RGB channels (calculated from core photos)

description: Red, green, and blue pixel data were extracted from Section Half Imaging Logger (SHIL) linescan images, typically binned at 0.5 cm resolution using the central 2 cm of the image.
DOI: 10.5281/zenodo.10206435
title: IODP Expedition 391 RGB channels (calculated from core photos)

description: Red, green, and blue pixel data were extracted from Section Half Imaging Logger (SHIL) linescan images, typically binned at 0.5 cm resolution using the central 2 cm of the image.
DOI: 10.5281/zenodo.10206432
title: IODP Expedition 391 Portable X-ray fluorescence (p-XRF)

description: Energy-Dispersive X-Ray Fluorescence (ED-XRF) is a rapid, non-destructive technique for determining qualitative and quantitative changes in chemical composition. Aboard the JOIDES Resolution, pXRF is used for measuring points on section halves, rock pieces, and sometimes powders. Spots are typically irradiated at multiple conditions to excite and measure a wide range of elements. The peak intensity changes (we do not provide concentrations) are then used to help recognize and define major chemo-stratigraphic units without the need for destructive sampling.
DOI: 10.5281/zenodo.10206433
title: IODP Expedition 391 Portable X-ray fluorescence (p-XRF)

description: Energy-Dispersive X-Ray Fluorescence (ED-XRF) is a rapid, non-destructive technique for determining qualitative and quantitative changes in chemical composition. Aboard the JOIDES Resolution, pXRF is used for measuring points on section halves, rock pieces, and sometimes powders. Spots are typically irradiated at multiple conditions to excite and measure a wide range of elements. The peak intensity changes (we do not provide concentrations) are then used to help recognize and define major chemo-stratigraphic units without the need for destructive sampling.
DOI: 10.5281/zenodo.10206430
title: IODP Expedition 391 P-wave velocity logger (whole round)

description: P-wave velocity data were measured on whole-round sections on the Whole-Round Multisensor Logger (WRMSL) using pairs of piezoelectric transducers mounted on a caliper system. Measurements may be affected by degassing of pore fluid and microfracturing during core recovery. Report includes P-wave velocity in x-y plane and distance and traveltime between transducers.
DOI: 10.5281/zenodo.10206431
title: IODP Expedition 391 P-wave velocity logger (whole round)

description: P-wave velocity data were measured on whole-round sections on the Whole-Round Multisensor Logger (WRMSL) using pairs of piezoelectric transducers mounted on a caliper system. Measurements may be affected by degassing of pore fluid and microfracturing during core recovery. Report includes P-wave velocity in x-y plane and distance and traveltime between transducers.
DOI: 10.5281/zenodo.10206426
title: IODP Expedition 391 P-wave velocity bayonet (section)

description: P-wave velocity data were measured on undisturbed section halves using pairs of piezoelectric transducers mounted in bayonets that are inserted into soft sediment along the JRSO-defined y-axis and/or z-axis. Report includes P-wave velocity in y and/or z direction, bayonet separation, traveltime between transducers, and first arrival picks.
DOI: 10.5281/zenodo.10206427
title: IODP Expedition 391 P-wave velocity bayonet (section)

description: P-wave velocity data were measured on undisturbed section halves using pairs of piezoelectric transducers mounted in bayonets that are inserted into soft sediment along the JRSO-defined y-axis and/or z-axis. Report includes P-wave velocity in y and/or z direction, bayonet separation, traveltime between transducers, and first arrival picks.
DOI: 10.5281/zenodo.10206422
title: IODP Expedition 391 Laser height profile (section half)

description: Height profile data were measured on the Section Half Multisensor Logger (SHMSL) by a rangefinding laser and recorded in uncorrected height units in millimeters in CSV files.
DOI: 10.5281/zenodo.10206423
title: IODP Expedition 391 Laser height profile (section half)

description: Height profile data were measured on the Section Half Multisensor Logger (SHMSL) by a rangefinding laser and recorded in uncorrected height units in millimeters in CSV files.
DOI: 10.5281/zenodo.10206420
title: IODP Expedition 391 Piece log

description: Dataset includes length data for every whole-round piece: bin length, whole-round piece length (measured by curation staff), and both the archive- and working-half piece lengths (optionally measured by scientists).
DOI: 10.5281/zenodo.10206421
title: IODP Expedition 391 Piece log

description: Dataset includes length data for every whole-round piece: bin length, whole-round piece length (measured by curation staff), and both the archive- and working-half piece lengths (optionally measured by scientists).
DOI: 10.5281/zenodo.10206418
title: IODP Expedition 391 Natural gamma radiation

description: Natural gamma radiation (NGR) data in the ~0.1 to 3.0 MeV range were measured using eight custom-designed sodium iodide (thallium) [NaI(Tl)] detectors arranged along the core measurement axis at 20 cm intervals. The NGR system uses layers of passive shielding (lead) and active shielding (plastic scintillators and coincidence electronics) to reduce the cosmic-ray signal for low-count analysis of sediment core sections and to obtain the maximum signal-to-noise ratio. Data are reported on a total counts per second basis and the raw spectral files are available as compressed files for later analysis.
DOI: 10.5281/zenodo.10206419
title: IODP Expedition 391 Natural gamma radiation

description: Natural gamma radiation (NGR) data in the ~0.1 to 3.0 MeV range were measured using eight custom-designed sodium iodide (thallium) [NaI(Tl)] detectors arranged along the core measurement axis at 20 cm intervals. The NGR system uses layers of passive shielding (lead) and active shielding (plastic scintillators and coincidence electronics) to reduce the cosmic-ray signal for low-count analysis of sediment core sections and to obtain the maximum signal-to-noise ratio. Data are reported on a total counts per second basis and the raw spectral files are available as compressed files for later analysis.
DOI: 10.5281/zenodo.10206416
title: IODP Expedition 391 Magnetic susceptibility (point or contact system)

description: Magnetic susceptibility was measured on section halves on the Section Half Multisensor Logger (SHMSL) using a Bartington MS2 meter and either a MS2E or MS2K probe. Because all JRSO cores meet minimum size requirements for these two probes, MSPOINT data are corrected for volume and recorded in SI susceptibility units (x10-5).
DOI: 10.5281/zenodo.10206417
title: IODP Expedition 391 Magnetic susceptibility (point or contact system)

description: Magnetic susceptibility was measured on section halves on the Section Half Multisensor Logger (SHMSL) using a Bartington MS2 meter and either a MS2E or MS2K probe. Because all JRSO cores meet minimum size requirements for these two probes, MSPOINT data are corrected for volume and recorded in SI susceptibility units (x10-5).
DOI: 10.5281/zenodo.10206415
title: IODP Expedition 391 Magnetic susceptibility (whole round)

description: Magnetic susceptibility was measured on whole-round sections (and rarely section halves) on the Whole-Round Multisensor Logger (WRMSL) and/or Special Task Multisensor Logger (STMSL) using a Bartington MS2 meter and a 90 mm or 80 mm MS2C loop. As volume of the sample is not controlled for this experiment, susceptibility units are recorded in instrument units and are not volume-corrected.
DOI: 10.5281/zenodo.10206414
title: IODP Expedition 391 Magnetic susceptibility (whole round)

description: Magnetic susceptibility was measured on whole-round sections (and rarely section halves) on the Whole-Round Multisensor Logger (WRMSL) and/or Special Task Multisensor Logger (STMSL) using a Bartington MS2 meter and a 90 mm or 80 mm MS2C loop. As volume of the sample is not controlled for this experiment, susceptibility units are recorded in instrument units and are not volume-corrected.
DOI: 10.5281/zenodo.10206410
title: IODP Expedition 391 Moisture and Density

description: Moisture and density (MAD) data were acquired on ~10 mL sediment or rock samples by measuring three out of four material parameters: wet (saturated) mass, wet volume, dry mass, and/or dry volume after 24 h drying in a convection oven at 105 degrees C. From the moisture and volume measurements, the following phase relationships are calculated: wet and dry water content, wet bulk density, dry bulk density, grain density, porosity, and void ratio. The combination of measurements is defined by the submethod chosen: A, B, C, or D. Wet (A, B, or C) and dry (A, B, C, or D) mass is determined using motion-compensated balances.  Wet volume is determined either by helium pycnometry (A) or by the sample's geometric dimensions using calipers (A or D).  Dry volume (C or D) is measured by helium pycnometry.  Submethods A and B are not recommended by IODP.  Submethod C is suitable for saturated materials such as fine-grained sediments.  Submethod D is suitable for unsaturated porous material such as certain limestones and basalts.
DOI: 10.5281/zenodo.10206411
title: IODP Expedition 391 Moisture and Density

description: Moisture and density (MAD) data were acquired on ~10 mL sediment or rock samples by measuring three out of four material parameters: wet (saturated) mass, wet volume, dry mass, and/or dry volume after 24 h drying in a convection oven at 105 degrees C. From the moisture and volume measurements, the following phase relationships are calculated: wet and dry water content, wet bulk density, dry bulk density, grain density, porosity, and void ratio. The combination of measurements is defined by the submethod chosen: A, B, C, or D. Wet (A, B, or C) and dry (A, B, C, or D) mass is determined using motion-compensated balances.  Wet volume is determined either by helium pycnometry (A) or by the sample's geometric dimensions using calipers (A or D).  Dry volume (C or D) is measured by helium pycnometry.  Submethods A and B are not recommended by IODP.  Submethod C is suitable for saturated materials such as fine-grained sediments.  Submethod D is suitable for unsaturated porous material such as certain limestones and basalts.
DOI: 10.5281/zenodo.10206406
title: IODP Expedition 391 Magnetic susceptibility (Kappabridge)

description: Bulk magnetic susceptibility and anisotropy of magnetic susceptibility (AMS) were measured on discrete samples using an Agico KLY-4 Kappabridge susceptibility meter. Report includes individual and average principal susceptibilities, inclination and declination of principal susceptibilities, and volume-corrected bulk susceptibility.
DOI: 10.5281/zenodo.10206407
title: IODP Expedition 391 Magnetic susceptibility (Kappabridge)

description: Bulk magnetic susceptibility and anisotropy of magnetic susceptibility (AMS) were measured on discrete samples using an Agico KLY-4 Kappabridge susceptibility meter. Report includes individual and average principal susceptibilities, inclination and declination of principal susceptibilities, and volume-corrected bulk susceptibility.