Item talk:Q324619: Difference between revisions
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{ | { | ||
" | "DOI": { | ||
"doi": "10.5066/p9zbfxi5", | "doi": "10.5066/p9zbfxi5", | ||
"identifiers": [], | "identifiers": [], | ||
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"published": null, | "published": null, | ||
"updated": "2023-02-21T16:42:53Z" | "updated": "2023-02-21T16:42:53Z" | ||
} | } | ||
} | } |
Latest revision as of 23:29, 10 September 2024
{
"DOI": { "doi": "10.5066/p9zbfxi5", "identifiers": [], "creators": [ { "name": "Ikard, Scott J", "nameType": "Personal", "givenName": "Scott J", "familyName": "Ikard", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0002-8304-4935", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Kress, Wade", "nameType": "Personal", "givenName": "Wade", "familyName": "Kress", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0002-6833-028X", "nameIdentifierScheme": "ORCID" } ] } ], "titles": [ { "title": "Historical (1940–2006) and recent (2019–20) aquifer slug test datasets used to model transmissivity and hydraulic conductivity of the Mississippi River Valley alluvial aquifer from recent (2018–20) airborne electromagnetic (AEM) survey data" } ], "publisher": "U.S. Geological Survey", "container": {}, "publicationYear": 2022, "subjects": [ { "subject": "Geophysics, Hydrology, Water Resources" } ], "contributors": [], "dates": [ { "date": "2022", "dateType": "Issued" } ], "language": null, "types": { "ris": "DATA", "bibtex": "misc", "citeproc": "dataset", "schemaOrg": "Dataset", "resourceType": "Dataset", "resourceTypeGeneral": "Dataset" }, "relatedIdentifiers": [ { "relationType": "IsCitedBy", "relatedIdentifier": "10.1007/s10040-022-02590-6", "relatedIdentifierType": "DOI" } ], "relatedItems": [], "sizes": [], "formats": [], "version": null, "rightsList": [], "descriptions": [ { "description": "The Mississippi River Valley alluvial aquifer (\u201calluvial aquifer\u201d) is one of the most extensively developed aquifers in the United States. The alluvial aquifer is present at the land surface in parts of southeastern Missouri, northeastern Louisiana, western Mississippi, western Tennessee and Kentucky near the Mississippi River, and throughout eastern Arkansas. Historical (1940\u20132006) and recent (2019\u201320) aquifer-test datasets were compiled to model transmissivity and hydraulic conductivity of the alluvial aquifer from recent (2018\u201319) airborne electromagnetic (AEM) survey data. This data release contains the aquifer-test and geophysical data along with computer codes written in Matlab version R2014a syntax used to process the data as [...]", "descriptionType": "Abstract" } ], "geoLocations": [], "fundingReferences": [], "url": "https://www.sciencebase.gov/catalog/item/62101ac1d34e6c7e83bab22e", "contentUrl": null, "metadataVersion": 2, "schemaVersion": "http://datacite.org/schema/kernel-4", "source": "mds", "isActive": true, "state": "findable", "reason": null, "viewCount": 0, "downloadCount": 0, "referenceCount": 0, "citationCount": 1, "partCount": 0, "partOfCount": 0, "versionCount": 0, "versionOfCount": 0, "created": "2022-07-18T14:40:16Z", "registered": "2022-07-18T14:40:17Z", "published": null, "updated": "2023-02-21T16:42:53Z" }
}