Item talk:Q250613
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Review: Regional land subsidence accompanying groundwater extraction", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70034646", "url": "https://pubs.usgs.gov/publication/70034646" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70034646 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1007/s10040-011-0775-5", "url": "https://doi.org/10.1007/s10040-011-0775-5" }, { "@type": "PropertyValue", "propertyID": "ISSN", "value": "14312174" } ], "journal": { "@type": "Periodical", "name": "Hydrogeology Journal", "volumeNumber": "19", "issueNumber": "8" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Hydrogeology Journal" } ], "datePublished": "2011", "dateModified": "2019-09-06", "abstract": "The extraction of groundwater can generate land subsidence by causing the compaction of susceptible aquifer systems, typically unconsolidated alluvial or basin-fill aquifer systems comprising aquifers and aquitards. Various ground-based and remotely sensed methods are used to measure and map subsidence. Many areas of subsidence caused by groundwater pumping have been identified and monitored, and corrective measures to slow or halt subsidence have been devised. Two principal means are used to mitigate subsidence caused by groundwater withdrawal\u2014reduction of groundwater withdrawal, and artificial recharge. Analysis and simulation of aquifer-system compaction follow from the basic relations between head, stress, compressibility, and groundwater flow and are addressed primarily using two approaches\u2014one based on conventional groundwater flow theory and one based on linear poroelasticity theory. Research and development to improve the assessment and analysis of aquifer-system compaction, the accompanying subsidence and potential ground ruptures are needed in the topic areas of the hydromechanical behavior of aquitards, the role of horizontal deformation, the application of differential synthetic aperture radar interferometry, and the regional-scale simulation of coupled groundwater flow and aquifer-system deformation to support resource management and hazard mitigation measures.", "description": "28 p.", "publisher": { "@type": "Organization", "name": "Springer" }, "author": [ { "@type": "Person", "name": "Galloway, Devin L. dlgallow@usgs.gov", "givenName": "Devin L.", "familyName": "Galloway", "email": "dlgallow@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0003-0904-5355", "url": "https://orcid.org/0000-0003-0904-5355" }, "affiliation": [ { "@type": "Organization", "name": "Office of the Associate Director for Water", "url": "https://www.usgs.gov/mission-areas/water-resources" }, { "@type": "Organization", "name": "WMA - Earth System Processes Division", "url": "https://www.usgs.gov/mission-areas/water-resources" }, { "@type": "Organization", "name": "Southwest Regional Director's Office", "url": "https://www.usgs.gov/regions/southwest" }, { "@type": "Organization", "name": "Office of the Chief Scientist for Water", "url": "https://www.usgs.gov/associate-chief-information-officer" }, { "@type": "Organization", "name": "Ohio-Kentucky-Indiana Water Science Center", "url": "https://www.usgs.govhttps://www.usgs.gov/centers/oki-water" } ] }, { "@type": "Person", "name": "Burbey, Thomas J.", "givenName": "Thomas J.", "familyName": "Burbey" } ], "funder": [ { "@type": "Organization", "name": "Ohio-Kentucky-Indiana Water Science Center", "url": "https://www.usgs.govhttps://www.usgs.gov/centers/oki-water" } ] }, "OpenAlex": { "abstract_inverted_index": null, "apc_list": { "value": 2690, "currency": "EUR", "value_usd": 3390, "provenance": "doaj" }, "apc_paid": null, "authorships": [ { "author_position": "first", "author": { "id": "https://openalex.org/A5014636714", "display_name": "Devin L. 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