cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.5636891
title: Cassini SAR Raw and Ancillary Data Archive

description: This data archive contains raw Cassini downlinked telemetry and ancillary temperature data for use in reprocessing Cassini SAR data using the Cassini SAR processor. The Cassini SAR processor is now available at<br> https://github.com/nasa-jpl/Cassini_RADAR_Software.<br> <br> To remove artifacts in SAR imagery due to thermal noise and compression error the Cassini SAR processor needs to extract compression coefficients from the raw downlinked data stored in this archive. The data is not human readable and only of use for users of the SAR processing software. In addition to the raw data, ancillary temperature data is also provided. Without the temperature data the radiometric calibration of the SAR images produced by the SAR processor is slightly degraded.<br> <br> The data is arranged by observation. Each observation has a directory whose name is the observation identifier, specified by one or two letters to indicate the name of the target body and a number to indicate which flyby. For example, t108 indicates Titan flyby number 108. The observation directory contains two subdirectories: “raw” which contains the raw data file; and “anc” which contains the three ancillary temperature files E-2503.gph, E-2505.gph, and E-2507.gph.<br> <br> The work reported here was performed at the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration. <br> Copyright 2021 All Rights Reserved
DOI: 10.5281/zenodo.5636890
title: Cassini SAR Raw and Ancillary Data Archive

description: This data archive contains raw Cassini downlinked telemetry and ancillary temperature data for use in reprocessing Cassini SAR data using the Cassini SAR processor. The Cassini SAR processor is now available at<br> https://github.com/nasa-jpl/Cassini_RADAR_Software.<br> <br> To remove artifacts in SAR imagery due to thermal noise and compression error the Cassini SAR processor needs to extract compression coefficients from the raw downlinked data stored in this archive. The data is not human readable and only of use for users of the SAR processing software. In addition to the raw data, ancillary temperature data is also provided. Without the temperature data the radiometric calibration of the SAR images produced by the SAR processor is slightly degraded.<br> <br> The data is arranged by observation. Each observation has a directory whose name is the observation identifier, specified by one or two letters to indicate the name of the target body and a number to indicate which flyby. For example, t108 indicates Titan flyby number 108. The observation directory contains two subdirectories: “raw” which contains the raw data file; and “anc” which contains the three ancillary temperature files E-2503.gph, E-2505.gph, and E-2507.gph.<br> <br> The work reported here was performed at the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration. <br> Copyright 2021 All Rights Reserved
DOI: 10.5281/zenodo.5634280
title: Activity cliffs with dual-atom replacements and single-atom analogs

description: From the ChEMBL database, 852 activity cliffs (ACs) with dual-atom replacements were extracted which were formed by compounds with high-confidence activity data. Each AC captured an at least 10-fold difference in compound potency. For a subset of these ACs, analogs with corresponding single-atom replacements were identified. The dual-atom ACs and available single-atom replacement analogs were provided (SMILES representation and ChEMBL compound ID). For each AC compound and analog, targets from ChEMBL are reported (with UniProt ID). The target shared by all associated compounds represents the primary AC target
DOI: 10.5281/zenodo.5634279
title: Activity cliffs with dual-atom replacements and single-atom analogs

description: From the ChEMBL database, 852 activity cliffs (ACs) with dual-atom replacements were extracted which were formed by compounds with high-confidence activity data. Each AC captured an at least 10-fold difference in compound potency. For a subset of these ACs, analogs with corresponding single-atom replacements were identified. The dual-atom ACs and available single-atom replacement analogs were provided (SMILES representation and ChEMBL compound ID). For each AC compound and analog, targets from ChEMBL are reported (with UniProt ID). The target shared by all associated compounds represents the primary AC target
DOI: 10.5281/zenodo.5636141
title: Distribution of lemma "digital" in PD and TE projects (2016, 2019, 2021)

description: sdj
DOI: 10.5281/zenodo.5636140
title: Distribution of lemma "digital" in PD and TE projects (2016, 2019, 2021)

description: sdj
DOI: 10.5281/zenodo.5635638
title: Mindfulness publications-2021-08-20

description: The original data of mindfulness publications
DOI: 10.5281/zenodo.5635637
title: Mindfulness publications-2021-08-20

description: The original data of mindfulness publications
DOI: 10.5281/zenodo.4758045
title: Visible to Mid-Infrared Optical Constants of Orthopyroxenes: data

description: The data stored here are the input and output data of optical constant modeling of orthopyroxenes.
DOI: 10.5281/zenodo.4758044
title: Visible to Mid-Infrared Optical Constants of Orthopyroxenes: data

description: The data stored here are the input and output data of optical constant modeling of orthopyroxenes.
DOI: 10.18112/openneuro.ds003724.v1.0.0
title: In vivo T1w MRI of a TDP-43 knock-in mouse model of ALS-FTD
DOI: 10.6084/m9.figshare.14602311
title: Data from: Reef-building corals act as long-term sink for microplastic

description: Data will be uploaded after publication<br>
DOI: 10.6084/m9.figshare.14602311.v1
title: Data from: Reef-building corals act as long-term sink for microplastic

description: Data will be uploaded after publication<br>
DOI: 10.5519/qd.29xqqhc0
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (8 records)
DOI: 10.5517/ccdc.csd.cc2204hr
title: CCDC 1906763: Experimental Crystal Structure Determination

description: Related Article: Tong Zhang, Yanning Han, Meng Liang, Weixiao Bian, Yan Zhang, Xiaoting Li, Chunyu Zhang, Pengchong Xue|2019|Dyes Pigm.|171|107692|doi:10.1016/j.dyepig.2019.107692
DOI: 10.5517/ccdc.csd.cc276v9m
title: CCDC 2062160: Experimental Crystal Structure Determination

description: Related Article: Sofian Gatfaoui, Noureddine Issaoui, Silvia Antonia Brandán, Mouna Medimagh, Omar Al-Dossary, Thierry Roisnel, Houda Marouani, Aleksandr S. Kazachenko|2022|J.Mol.Struct.|1250|131720|doi:10.1016/j.molstruc.2021.131720
DOI: 10.5519/qd.cw083y03
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (744 records)
DOI: 10.17909/t9-pa2m-e521
title: TOI-712 TESS SPOC data

description: TESS data from Years 1 and 3 used in discovery paper for TOI-712 (Vach et al.)
DOI: 10.6084/m9.figshare.13027829.v4
title: Rank and Transitive Inference in chicks.xlsx

description: The data presented describe training and testing of chicks on a transitive inference task. The Excel table shows the rank (1-3), sex (1=male; 2 =female) and outcomes (number of trials to criterion of 20 correct choices - a correct choice at training being rewarded with a food item for pecking the 'higher' rank .i.e A over B, B over C etc. Testing is of non-rewarded pairs AE and BD, previously not seen before). To note chicks were held in groups of 3 or 4 individuals and ranked at Day 5 of life when first grouped together.
DOI: 10.5519/qd.diqffxpp
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (33 records)
DOI: 10.48760/vkr5-n231
title: Great Slave Lake 2019-2020 Christie Bay thermistor mooring
DOI: 10.6084/m9.figshare.16880536
title: Arrive-ten-aby

description: Arrive essential for animal laboratory
DOI: 10.48760/vrde-1494
title: Great Slave Lake 2019-2020 Christie Bay Thermistor mooring data set 2 of 2),
DOI: 10.3886/e113635v1-100400
title: Replication data for: Social Networks as Contract Enforcement: Evidence from a Lab Experiment in the Field

description: Lack of well-functioning formal institutions leads to reliance on social networks to enforce informal contracts. Social proximity and network centrality may affect cooperation. To assess the extent to which networks substitute for enforcement, we conducted high-stakes games across 34 Indian villages. We randomized subjects' partners and whether contracts were enforced to estimate how partners' relative network position differentially matters across contracting environments. While socially close pairs cooperate even without enforcement, distant pairs do not. Individuals with more central partners behave more cooperatively without enforcement. Capacity for cooperation in the absence of contract enforcement, therefore, depends on the subjects' network position.
DOI: 10.5517/ccdc.csd.cc28byyj
title: CCDC 2095908: Experimental Crystal Structure Determination

description: Related Article: Han Hao|2021|CSD Communication|||
description: Related Article: Han Hao, Laurel L. Schafer|2021|Organometallics|40|3235|doi:10.1021/acs.organomet.1c00416
DOI: 10.5517/ccdc.csd.cc28c0vj
title: CCDC 2095967: Experimental Crystal Structure Determination

description: Related Article: Elizabeth A. Stone|2021|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc28ygrg
title: CCDC 2113696: Experimental Crystal Structure Determination

description: Related Article: Martin Nieger|2021|CSD Communication|||
DOI: 10.6073/pasta/13cda54bbcb84aca68c4b8b037f8746a
title: Clear Creek Gravel Augmentations, 1996-2021

description: Clear Creek Anadromous Fish Habitat Restoration and Management Project (aka “Gravel Augmentations”), 1996-2021 The purpose of the Clear Creek Gravel Augmentation Project (the Project) is to improve habitat conditions in Lower Clear Creek for anadromous salmonid species, including spring-run, fall-run, and late fall-run Chinook salmon, and Central Valley steelhead. This programmatic effort was formally titled Lower Clear Creek Anadromous Fish Habitat Restoration and Management Project (LCCAFHRMP), though “gravel augmentations” remains the most commonly use name for the project. The Project is implemented annually to improve fish habitat by placing gravel and other desirable materials into the stream channel with the intent of restoring and maintaining the balance of sediment in Clear Creek, providing desirable creek channel attributes like floodplain connectivity, channel migration, fish habitat formation (e.g. spawning habitat), and supporting riparian community development. The Project is proposed to meet the requirements of the CVPIA 3406 (b)(12) which has identified the lack of in-stream spawning gravel as a significant factor limiting anadromous fish reproduction in Clear Creek. The Clear Creek Gravel Augmentation Project consists of adding clean (washed), size-sorted natural river gravel directly (riffle supplementation) or indirectly (talus cone, lateral berm) into the Clear Creek channel, along with other desirable materials (i.e., large wood and boulders). The project is funded by the CVPIA. Each year, the Clear Creek Technical Team chooses the top priority gravel augmentation sites for implementations.
DOI: 10.34943/e33fe79a-dfe3-46b4-8137-0ff2f8037665
title: Barkley Canyon Upper Slope Echosounder, Bioacoustic Deployed 2021-03-26

description: The ASL AZFP Echosounder 55016 was deployed on 2021-03-26 at Barkley Canyon Upper Slope. Upper Slope is a location within Barkley Canyon, which is located on the upper continental slope. This device is a Echosounder, Bioacoustic. Echosounders are used to measure acoustic backscatter as a proxy for detecting zooplankton, fish, bubbles or other particles in the water-column. An echosounder has one or more transducers which emit acoustic pulses at a particular frequency. When the pulses strike animals or other objects in the water, echoes are produced, which can be detected and converted by the transducers back into electrical signals. Software is then used to determine distances, sizes, concentrations and movements of organisms and other objects in the water. It was deployed on a profiling platform. Data from this deployment were archived and made available through Ocean Networks Canada's Oceans 2.0 digital infrastructure, with quality assurance and derived data products following established practices.
DOI: 10.25345/c5357t
title: MassIVE MSV000088299 - Evaluation of Ion Mobility Spectrometry for Improving Constitutional Assignment in Natural Products Mixtures
title: Mixtures and Pure samples of standards used for the evaluation of various MS acquisition modes.
DOI: 10.25919/r530-ka12
title: Parkes observations for project P1050 semester 2021OCTS_02

description: This is a request for observing time for the timing campaign of new pulsar discoveries from the reprocessing of the low-latitude Galactic plane section of the HTRU survey (P630). We have now completed 90 % of the survey with GPU based coherent acceleration search, template bank and fast folding algorithm pipelines, and now have discovered 92 previously unknown pulsars and 8 "class A" pulsars awaiting confirmation. Interesting science can usually only be derived from a new pulsar after confirmation and a follow-up timing campaign is carried out. One year of initial timing is the minimum timespan required to fully characterise any newly-discovered pulsars, essential for deriving pulsar parameters such as the characteristic age, magnetic field strength, spin-down rate, as well as to detect any unexpected behaviour of the pulsar which might result from emission instabilities. Pulsars on the observing list here have been confirmed in the previous and current 2021APRS semesters, the follow-up timing in OCTS2021 will produce completely new and exciting results. In addition, this timing project will allow us to measure the true Galactic plane pulsar population and the boundaries of pulsar parameter space in the galactic plane.
DOI: 10.25451/flinders.16881958
title: Hydrostratigraphic model of the Gambier Basin and South West Murray Basin

description: A three-dimensional hydrostratigraphic model of the entire regional groundwater flow system that includes the Gambier Basin and the south western Murray Basin has been produced. The domain of this model stretches from the Dundas Plateau in Victoria to the Padthaway Ridge in South Australia and includes the Lower Limestone Coast and Padthaway Prescribed Wells Areas in South Australia, as well as part of the Border Designated Area (Zones 1A/1B to 6A/B and part of Zones 7A/B). The domain of the hydrostratigraphic model was governed by the boundaries of the South East Regional Water Balance Model, which is being developed as part of a Goyder Institute for Water Research project. This groundwater flow model required a hydrostratigraphic model that covered the whole regional groundwater flow system that encompasses the Lower Limestone Coast Prescribed Wells Area. This is the first cross-border hydrostratigraphic model to be produced for this region. The hydrostratigraphic model includes five layers, Layer 1: the Quaternary Limestone Aquifer, Layer 2: the Upper Mid-Tertiary Aquifer (Gambier / Murray Group Limestone Aquifer), Layer 3: the Upper Tertiary Aquitard, Layer 4: The Lower Tertiary Aquifer (Mepunga Formation) and the Lower Tertiary Confined Aquifer (Dilwyn Sand / Renmark Group Aquifer) and Layer 5: the Pre-Cainozoic Sediments and Basement (however, the model does not include data for the base of Layer 5). <br>The model includes the following datasets: Topographic Surface: • SA/VIC State 1 second Digital Elevation Model (DEM), later updated with a version that includes lidar DEM data where available. <br>Top of Layer 2 (Top of Gambier / Murray Group Limestone): • 2,697 stratigraphic data points for the South Australian portion of the model domain. • 209 stratigraphic data points for the Victorian portion of the model domain. <br>Top of Layer 3 (Top of Aquitard): • 733 data points for the whole model domain, including Victoria. <br>Top of Layer 4 (Top of Dilwyn Sand / Renmark Group) – Layer 4 includes the Pember Mudstone and Pebble Point Formation. • 874 stratigraphic data points for the South Australian portion of the model domain. • 83 stratigraphic data points for the Victorian portion of the model domain. <br>Top of Layer 5 (Top of Basement): • 243 points for the South Australian portion of the study area. These were restricted to the Murray Basin (northern) portion of the study area. • Contours of basement outcrops in the northern part of the SA portion of the study area. • Contours derived from petroleum well and seismic data for the southern portion of the South Australian part of the study area. • 63 points on the Victorian portion of the study area. The hydrostratigraphic model was created in an ArcGIS framework and is available as an ArcGIS geodatabase. <br>The parent datasets described above are also available in ArcGIS format. This study was supported by The Goyder Institute for Water Research<br>
DOI: 10.25451/flinders.16881958.v1
title: Hydrostratigraphic model of the Gambier Basin and South West Murray Basin

description: A three-dimensional hydrostratigraphic model of the entire regional groundwater flow system that includes the Gambier Basin and the south western Murray Basin has been produced. The domain of this model stretches from the Dundas Plateau in Victoria to the Padthaway Ridge in South Australia and includes the Lower Limestone Coast and Padthaway Prescribed Wells Areas in South Australia, as well as part of the Border Designated Area (Zones 1A/1B to 6A/B and part of Zones 7A/B). The domain of the hydrostratigraphic model was governed by the boundaries of the South East Regional Water Balance Model, which is being developed as part of a Goyder Institute for Water Research project. This groundwater flow model required a hydrostratigraphic model that covered the whole regional groundwater flow system that encompasses the Lower Limestone Coast Prescribed Wells Area. This is the first cross-border hydrostratigraphic model to be produced for this region. The hydrostratigraphic model includes five layers, Layer 1: the Quaternary Limestone Aquifer, Layer 2: the Upper Mid-Tertiary Aquifer (Gambier / Murray Group Limestone Aquifer), Layer 3: the Upper Tertiary Aquitard, Layer 4: The Lower Tertiary Aquifer (Mepunga Formation) and the Lower Tertiary Confined Aquifer (Dilwyn Sand / Renmark Group Aquifer) and Layer 5: the Pre-Cainozoic Sediments and Basement (however, the model does not include data for the base of Layer 5). <br>The model includes the following datasets: Topographic Surface: • SA/VIC State 1 second Digital Elevation Model (DEM), later updated with a version that includes lidar DEM data where available. <br>Top of Layer 2 (Top of Gambier / Murray Group Limestone): • 2,697 stratigraphic data points for the South Australian portion of the model domain. • 209 stratigraphic data points for the Victorian portion of the model domain. <br>Top of Layer 3 (Top of Aquitard): • 733 data points for the whole model domain, including Victoria. <br>Top of Layer 4 (Top of Dilwyn Sand / Renmark Group) – Layer 4 includes the Pember Mudstone and Pebble Point Formation. • 874 stratigraphic data points for the South Australian portion of the model domain. • 83 stratigraphic data points for the Victorian portion of the model domain. <br>Top of Layer 5 (Top of Basement): • 243 points for the South Australian portion of the study area. These were restricted to the Murray Basin (northern) portion of the study area. • Contours of basement outcrops in the northern part of the SA portion of the study area. • Contours derived from petroleum well and seismic data for the southern portion of the South Australian part of the study area. • 63 points on the Victorian portion of the study area. The hydrostratigraphic model was created in an ArcGIS framework and is available as an ArcGIS geodatabase. <br>The parent datasets described above are also available in ArcGIS format. This study was supported by The Goyder Institute for Water Research<br>
DOI: 10.5281/zenodo.5637379
title: Isoetes engelmannii SPAdes preassembly

description: .
DOI: 10.5281/zenodo.5637378
title: Isoetes engelmannii SPAdes preassembly

description: .
DOI: 10.15784/601482
title: Locations of Adelie penguins from geolocating dive recorders 2017-2019

description: Positions of migrating, molting, and wintering Adelie penguins from Cape Royds and Cape Crozier, Ross Island as calculated from geolocation sensors (GLS) using probabilistic methods (R package SGAT)
DOI: 10.25451/flinders.16881904.v1
title: South East Regional Groundwater Flow Model- LEACHM Recharge Model

description: LEACHM Recharge Model produced as a result of the GOYDER INSTITUTE FOR WATER RESEARCH Project No.E.2.6.<br><br>The LEACHM model was used to create the recharge input files for the regional groundwater flow model developed as part of the same project.<br><br>LEACHM is a one-dimensional soil water and chemical fate and transport model (Hutson, 2003). Water flow is described either by a capacity (tipping-bucket) model or by a mechanistic (Darcy-based Richard’s) model. The mechanistic model was used in this work. It was used in a previous project to assess the risk of nitrogen and pesticide contamination in the Lower South East (Fleming and Hutson, 2014).<br><br>The GIS-linked version of the LEACHM model (LEACHG) aims to assess regional behaviour. The stand-alone LEACHM input data file consists of sections describing the simulation period, profile geometry and boundary conditions, soil, vegetation, chemical properties, irrigation and chemical management and weather. In LEACHG, each of these data components vary spatially, defined by GIS rasters based on state soil and land use maps, along with spatially interpolated weather data. In addition, features such as water table depth and land surface slope class etc. may also be applied to the model in GIS format. In LEACHG, each of the data file components are selected from a library of input data files linked to raster ID values. For example, if a land use raster cell has an ID of 23, then LEACHG will read data from a library file named Crops.023. Initially, the model reads all relevant rasters, identifies unique combinations of soil, land use and weather, and performs a single simulation of each combination for the defined time period. A complete set of LEACHM output files are generated for each simulation, identified by the raster ID values that are used to name the files. Post-processing generates rasters of any desired output variable, such as drainage from the soil profile, actual evapotranspiration or irrigation applications, produces summaries of water mass balance components both in terms of water depths and volumes, and generates input data files for the groundwater model MODFLOW.<br><br>The LEACHM code is written in the FORTRAN language. The code is continually improved and adapted to the requirements of specific projects and post-processing requirements; contact Dr John Hutson (John.Hutson@flinders.edu.au). The time period of the LEACHM model simulations can be extended, however this requires modifying the input data files and obtaining or generating the required climate and land use datasets.<br><br>All datasets used in the model development are stored with the model.<br><br><br>Location: The model domain includes the Lower Limestone Coast Prescribed Wells Area in the Lower South East of SA (South Australia), and part of the Border Designated Area, and the encompassing groundwater flow system