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dc.contributor.authorDumeyer, John.
dc.creatorDumeyer, John.en_US
dc.date.accessioned2011-11-28T13:58:18Z
dc.date.available2011-11-28T13:58:18Z
dc.date.issued1971en_US
dc.identifier.urihttp://hdl.handle.net/10150/191551
dc.description.abstractThe Rio Grande Valley from South Fork to Del Norte, south-central Colorado, comprises a distinct hydrologic system with reasonably well-defined boundaries. The valley, located on the east flank of the San Juan Mountains, contains a twelve and one-half mile reach of the Rio Grande and has an area of 19,400 acres. A hydrologic budget developed for the alluvial aquifer of the valley for the period April 1, 1970, to March 31, 1971, indicates an inflow of 75,000 acre-feet, no storage Change, and an outflow to the Rio Grande of 25,000 acre-feet with a standard deviation of 5,000 acre-feet. The alluvial aquifer responds rapidly to a springtime recharge pulse and the water table rises from a minimum level at the end of Mardi to a maximum in early July. A hydrologic budget for this period in 1970 indicates a Change of storage of 23,000 acre-feet and a storage coefficient of 0.26.
dc.language.isoenen_US
dc.publisherThe University of Arizona.en_US
dc.rightsCopyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.en_US
dc.subject.lcshHydrology.en_US
dc.subject.lcshWater resources development -- Colorado.en_US
dc.titleGeohydrology of the Rio Grande Valley from South Fork to Del Norte, Colorado,en_US
dc.typeThesis-Reproduction (electronic)en_US
dc.typetexten_US
dc.contributor.chairWright, Jerome J.en_US
dc.identifier.oclc213296839en_US
thesis.degree.grantorUniversity of Arizonaen_US
thesis.degree.levelmastersen_US
thesis.degree.disciplineHydrology and Water Resourcesen_US
thesis.degree.disciplineGraduate Collegeen_US
thesis.degree.nameM.S.en_US
dc.description.notehydrology collectionen_US
refterms.dateFOA2018-04-26T00:46:36Z
html.description.abstractThe Rio Grande Valley from South Fork to Del Norte, south-central Colorado, comprises a distinct hydrologic system with reasonably well-defined boundaries. The valley, located on the east flank of the San Juan Mountains, contains a twelve and one-half mile reach of the Rio Grande and has an area of 19,400 acres. A hydrologic budget developed for the alluvial aquifer of the valley for the period April 1, 1970, to March 31, 1971, indicates an inflow of 75,000 acre-feet, no storage Change, and an outflow to the Rio Grande of 25,000 acre-feet with a standard deviation of 5,000 acre-feet. The alluvial aquifer responds rapidly to a springtime recharge pulse and the water table rises from a minimum level at the end of Mardi to a maximum in early July. A hydrologic budget for this period in 1970 indicates a Change of storage of 23,000 acre-feet and a storage coefficient of 0.26.


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