Item talk:Q326939
From geokb
{
"DOI": { "doi": "10.5066/p9yrt884", "identifiers": [], "creators": [ { "name": "Pace, Michael D", "nameType": "Personal", "givenName": "Michael D", "familyName": "Pace", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0003-2770-5724", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Minsley, Burke J", "nameType": "Personal", "givenName": "Burke J", "familyName": "Minsley", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0003-1689-1306", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Moulton, Craig W", "nameType": "Personal", "givenName": "Craig W", "familyName": "Moulton", "affiliation": [ "United States Geological Survey" ], "nameIdentifiers": [] }, { "name": "Reitman, James", "nameType": "Personal", "givenName": "James", "familyName": "Reitman", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0003-3551-9884", "nameIdentifierScheme": "ORCID" } ] } ], "titles": [ { "title": "Ground-based electromagnetic survey, Shellmound, Mississippi, October 2018" } ], "publisher": "U.S. Geological Survey", "container": {}, "publicationYear": 2020, "subjects": [ { "subject": "Environmental Health, Geophysics, Hydrology, Water Quality, Water Resources" } ], "contributors": [], "dates": [ { "date": "2020", "dateType": "Issued" } ], "language": null, "types": { "ris": "DATA", "bibtex": "misc", "citeproc": "dataset", "schemaOrg": "Dataset", "resourceType": "Dataset", "resourceTypeGeneral": "Dataset" }, "relatedIdentifiers": [], "relatedItems": [], "sizes": [], "formats": [], "version": null, "rightsList": [], "descriptions": [ { "description": "Shallow soil characteristics were mapped near Shellmound, Mississippi, using the DualEM 421 electromagnetic sensor in October 2018. Data were acquired by towing the DualEM sensor on a wheeled cart behind an all-terrain vehicle (ATV), with the sensor at a height of 0.432 meters (m) above the ground surface. Approximately 175 line-kilometers of data were acquired over an area of nearly four square-kilometers, with 25 m separation between survey lines. Data were manually edited for noise sources such as powerlines or other buried structures and averaged to regular output soundings every 5 m along survey lines. The processed data were inverted to recover models of electrical resistivity structure as a function of depth at each sounding location using a spatially constrained inversion. This data release contains the raw and processed data, as well as inverted resistivity models. Model results show typical depth of investigation from about 4 - 6 m, with spatial variability in mapped electrical resistivity characteristic of fluvial deposition of sediments in channels and scroll bar features adjacent to the Tallahatchie River and nearby abandoned meander channels.", "descriptionType": "Abstract" } ], "geoLocations": [], "fundingReferences": [], "url": "https://www.sciencebase.gov/catalog/item/5ada594fe4b0e2c2dd297b0a", "contentUrl": null, "metadataVersion": 1, "schemaVersion": "http://datacite.org/schema/kernel-4", "source": "mds", "isActive": true, "state": "findable", "reason": null, "viewCount": 0, "downloadCount": 0, "referenceCount": 0, "citationCount": 0, "partCount": 0, "partOfCount": 0, "versionCount": 0, "versionOfCount": 0, "created": "2020-02-25T15:45:22Z", "registered": "2020-02-25T15:45:24Z", "published": null, "updated": "2022-01-22T02:16:43Z" }
}