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dc.contributor.advisorYeh, T.C. Jimen
dc.contributor.authorZimmerlund, Benjamin Wayne
dc.creatorZimmerlund, Benjamin Wayneen
dc.date.accessioned2018-02-28T22:20:02Z
dc.date.available2018-02-28T22:20:02Z
dc.date.issued2008
dc.identifier.urihttp://hdl.handle.net/10150/626931
dc.description.abstractThe City of Tucson plans to construct a groundwater recharge and recovery facility in southern Avra Valley to infiltrate Central Arizona Project (CAP) water. The Southern Avra Valley Recharge and Recovery Project (SA VSARP) will initially recharge up to 60,000 acre-feet of CAP water per year. Characterization of the vadose zone is important in understanding the behavior of recharged water. Using grain-size distribution data from well cuttings, three lithologic units are defined and a 2-D vertical cross-section is developed in the area of predominant recharge. Soil samples representing each defined lithologic unit are laboratory tested for saturated and unsaturated flow parameters. Soil moisture retention data is fit to the van Genuchten equation to obtain unsaturated flow model parameters. A 1-D unsaturated flow model is developed using VSAFT2 to simulate infiltration of CAP water through the vadose zone.
dc.language.isoen_USen
dc.publisherThe University of Arizona.en
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
dc.titleVadose zone characterization pertaining to artificial groundwater recharge, Southern Avra Valley, Arizonaen_US
dc.typetexten
dc.typeThesis-Reproduction (electronic)en
thesis.degree.grantorUniversity of Arizonaen
thesis.degree.levelmastersen
dc.contributor.committeememberYeh, T.C. Jimen
thesis.degree.disciplineGraduate Collegeen
thesis.degree.disciplineHydrology and Water Resourcesen
thesis.degree.nameM.S.en
dc.description.noteDigitized from paper copies provided by the Department of Hydrology & Atmospheric Sciences.en
refterms.dateFOA2018-06-23T13:46:46Z
html.description.abstractThe City of Tucson plans to construct a groundwater recharge and recovery facility in southern Avra Valley to infiltrate Central Arizona Project (CAP) water. The Southern Avra Valley Recharge and Recovery Project (SA VSARP) will initially recharge up to 60,000 acre-feet of CAP water per year. Characterization of the vadose zone is important in understanding the behavior of recharged water. Using grain-size distribution data from well cuttings, three lithologic units are defined and a 2-D vertical cross-section is developed in the area of predominant recharge. Soil samples representing each defined lithologic unit are laboratory tested for saturated and unsaturated flow parameters. Soil moisture retention data is fit to the van Genuchten equation to obtain unsaturated flow model parameters. A 1-D unsaturated flow model is developed using VSAFT2 to simulate infiltration of CAP water through the vadose zone.


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