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dc.contributor.advisorJohnson, Roy A.en_US
dc.contributor.authorRipich, Marcella A.
dc.creatorRipich, Marcella A.en_US
dc.date.accessioned2013-04-03T13:35:14Z
dc.date.available2013-04-03T13:35:14Z
dc.date.issued2000en_US
dc.identifier.urihttp://hdl.handle.net/10150/278744
dc.description.abstractRillito Creek, near Tucson, Arizona is like many ephemeral streams in the Southwest in that flows within the creek are an important source of recharge to the regional groundwater system. Increasing demands on groundwater resources in the area have prompted proposals for artificial recharge along the 20-km-long channel. The U.S. Geological Survey, along with the Arizona Department of Water Resources, is developing a regional groundwater-flow model to determine recharge effectiveness. This study provides the geometry and a detailed characterization of recent alluvium and basin-fill deposits. The approach used to determine the geometry and physical and hydraulic properties of the deposits included the integration of surface and borehole geological data and geophysical data. Data were derived from electromagnetic, resistivity and seismic-refraction surveys, pre-existing geologic logs and analysis of cores and cuttings for grain-size distribution, particle and bulk density, porosity, saturated hydraulic conductivity and volumetric water content. A fine-grained layer in the lower reach of Rillito Creek may impede infiltration and decrease recharge rates in this area.
dc.language.isoen_USen_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.subjectGeology.en_US
dc.subjectGeophysics.en_US
dc.subjectHydrology.en_US
dc.titleDelineation of subsurface deposits through the integration of geological, geophysical and hydrological data, Rillito Creek, Tucson, Arizonaen_US
dc.typetexten_US
dc.typeThesis-Reproduction (electronic)en_US
thesis.degree.grantorUniversity of Arizonaen_US
thesis.degree.levelmastersen_US
dc.identifier.proquest1402028en_US
thesis.degree.disciplineGraduate Collegeen_US
thesis.degree.disciplineEarth sciencesen_US
thesis.degree.nameM.S.en_US
dc.identifier.bibrecord.b41166024en_US
refterms.dateFOA2018-06-28T01:40:50Z
html.description.abstractRillito Creek, near Tucson, Arizona is like many ephemeral streams in the Southwest in that flows within the creek are an important source of recharge to the regional groundwater system. Increasing demands on groundwater resources in the area have prompted proposals for artificial recharge along the 20-km-long channel. The U.S. Geological Survey, along with the Arizona Department of Water Resources, is developing a regional groundwater-flow model to determine recharge effectiveness. This study provides the geometry and a detailed characterization of recent alluvium and basin-fill deposits. The approach used to determine the geometry and physical and hydraulic properties of the deposits included the integration of surface and borehole geological data and geophysical data. Data were derived from electromagnetic, resistivity and seismic-refraction surveys, pre-existing geologic logs and analysis of cores and cuttings for grain-size distribution, particle and bulk density, porosity, saturated hydraulic conductivity and volumetric water content. A fine-grained layer in the lower reach of Rillito Creek may impede infiltration and decrease recharge rates in this area.


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