Item talk:Q237238
From geokb
{
"USGS Publications Warehouse": {
"@context": "https://schema.org",
"@type": "Article",
"additionalType": "Journal Article",
"name": "A multiple-tracer approach to understanding regional groundwaterflow in the Snake Valley area of the eastern Great Basin, USA",
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"value": "70193132",
"url": "https://pubs.usgs.gov/publication/70193132"
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"value": 70193132
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"propertyID": "DOI",
"value": "10.1016/j.apgeochem.2014.02.010",
"url": "https://doi.org/10.1016/j.apgeochem.2014.02.010"
}
],
"journal": {
"@type": "Periodical",
"name": "Applied Geochemistry",
"volumeNumber": "45",
"issueNumber": null
},
"inLanguage": "en",
"isPartOf": [
{
"@type": "CreativeWorkSeries",
"name": "Applied Geochemistry"
}
],
"datePublished": "2014",
"dateModified": "2017-10-31",
"abstract": "Groundwater in Snake Valley and surrounding basins in the eastern Great Basin province of the western\nUnited States is being targeted for large-scale groundwater extraction and export. Concern about declining\ngroundwater levels and spring flows in western Utah as a result of the proposed groundwater withdrawals\nhas led to efforts that have improved the understanding of this regional groundwater flow system. In this\nstudy, environmental tracers (del2H, del18O, 3H, 14C, 3He, 4He, 20Ne, 40Ar, 84Kr, and 129Xe) and major ions from\n142 sites were evaluated to investigate groundwater recharge and flow-path characteristics. With few\nexceptions, del2H and del18O show that most valley groundwater has similar ratios to mountain springs,\nindicating recharge is dominated by relatively high-altitude precipitation. The spatial distribution of 3H,\nterrigenic helium (4Heterr), and 3H/3He ages shows that modern groundwater (<60 yr) in valley aquifers\nis found only in the western third of the study area. Pleistocene and late-Holocene groundwater is found\nin the eastern parts of the study area. The age of Pleistocene groundwater is supported by minimum\nadjusted radiocarbon ages of up to 32 ka. Noble gas recharge temperatures (NGTs) are generally\n1\u201311 degrees C in Snake and southern Spring Valleys and >11 degrees C to the east of Snake Valley and indicate a\nhydraulic discontinuity between Snake and Tule Valleys across the northern Confusion Range. The\ncombination of NGTs and 4Heterr shows that the majority of Snake Valley groundwater discharges as\nsprings, evapotranspiration, and well withdrawals within Snake Valley rather than continuing\nnortheastward to discharge at either Fish Springs or the Great Salt Lake Playa. The refined understanding\nof groundwater recharge and flow paths acquired from this multi-tracer investigation has broad\nimplications for interbasin subsurface flow estimates and future groundwater development.",
"description": "17 p.",
"publisher": {
"@type": "Organization",
"name": "Elsevier"
},
"author": [
{
"@type": "Person",
"name": "Gardner, Philip M. pgardner@usgs.gov",
"givenName": "Philip M.",
"familyName": "Gardner",
"email": "pgardner@usgs.gov",
"identifier": {
"@type": "PropertyValue",
"propertyID": "ORCID",
"value": "0000-0003-3005-3587",
"url": "https://orcid.org/0000-0003-3005-3587"
},
"affiliation": [
{
"@type": "Organization",
"name": "Nevada Water Science Center",
"url": "https://www.usgs.gov/centers/nevada-water-science-center"
},
{
"@type": "Organization",
"name": "Utah Water Science Center",
"url": "https://www.usgs.gov/centers/utah-water-science-center"
}
]
}
],
"funder": [
{
"@type": "Organization",
"name": "Utah Water Science Center",
"url": "https://www.usgs.gov/centers/utah-water-science-center"
}
],
"spatialCoverage": [
{
"@type": "Place",
"additionalType": "country",
"name": "United States",
"url": "https://geonames.org/4074035"
},
{
"@type": "Place",
"additionalType": "state",
"name": "Nevada"
},
{
"@type": "Place",
"additionalType": "state",
"name": "Utah"
},
{
"@type": "Place",
"additionalType": "unknown",
"name": "Great Basin",
"url": "https://geonames.org/4965706"
},
{
"@type": "Place",
"additionalType": "unknown",
"name": "Snake Valley",
"url": "https://geonames.org/4822655"
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