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dc.contributor.authorLassotovitch, Cheryl Rhodes.
dc.creatorLassotovitch, Cheryl Rhodesen_US
dc.date.accessioned2011-11-28T13:51:05Z
dc.date.available2011-11-28T13:51:05Z
dc.date.issued1996en_US
dc.identifier.urihttp://hdl.handle.net/10150/191327
dc.description.abstractAn evaluation of the distribution of DBCP in the aquifer was conducted within the Kings Groundwater Basin, Central San Joaquin Valley, California. The geographical distribution of DBCP coincides with locations of vineyards and orchards, and sandy soils. High DBCP concentrations are generally found above a depth of 250 feet, and DBCP is normally undetected below a depth of about 300 to 350 feet in the Kings Basin. Aquifer parameters and the direction and rate of lateral and vertical groundwater flow were analyzed for a number of subareas to determine the direction and migration rate of DBCP. The urban area pumping depressions accelerate the lateral flow of DBCP contaminated groundwater into the urban area. The geographical extent of DBCP has been observed to decrease considerably over time. The field half life of DBCP was found to be approximately six years for all factors involved in the degradation of the chemical. DBCP is expected to remain a serious groundwater contaminant that adversely affects the development of potable groundwater in the Kings Basin for one to two more decades.
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.subjectDibromochloropropane -- Environmental aspects -- California.
dc.subjectGroundwater -- Pollution -- California.
dc.subjectHydrology.
dc.titleThe Evaluation of DBCP in groundwater of the Kings Basin, Central Joaquin Valley Californiaen_US
dc.typeThesis-Reproduction (electronic)en_US
dc.typetexten_US
dc.contributor.chairMaddock, Thomasen_US
dc.contributor.chairSchmidt, Kenneth D.en_US
dc.identifier.oclc221367144en_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.dateFOA2018-07-15T00:42:02Z
html.description.abstractAn evaluation of the distribution of DBCP in the aquifer was conducted within the Kings Groundwater Basin, Central San Joaquin Valley, California. The geographical distribution of DBCP coincides with locations of vineyards and orchards, and sandy soils. High DBCP concentrations are generally found above a depth of 250 feet, and DBCP is normally undetected below a depth of about 300 to 350 feet in the Kings Basin. Aquifer parameters and the direction and rate of lateral and vertical groundwater flow were analyzed for a number of subareas to determine the direction and migration rate of DBCP. The urban area pumping depressions accelerate the lateral flow of DBCP contaminated groundwater into the urban area. The geographical extent of DBCP has been observed to decrease considerably over time. The field half life of DBCP was found to be approximately six years for all factors involved in the degradation of the chemical. DBCP is expected to remain a serious groundwater contaminant that adversely affects the development of potable groundwater in the Kings Basin for one to two more decades.


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