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dc.contributor.authorSwanick, Gerald Bernard.
dc.creatorSwanick, Gerald Bernard.en_US
dc.date.accessioned2011-11-28T14:05:13Z
dc.date.available2011-11-28T14:05:13Z
dc.date.issued1982en_US
dc.identifier.urihttp://hdl.handle.net/10150/191755
dc.description.abstractThe Milk River aquifer system in Alberta, Canada, was studied to develop age-dating techniques for old ground water. A steadystate flow model used to calculate hydrodynamic ages of the ground water and ¹⁴C concentrations in the water were used to calculate ages for comparison. The results were compared with ³⁶Cl-predicted ages of the same aquifer. The ages predicted with the flow model showed a progression of increasing age from zero at the Milk River sandstone outcrop near the United States—Canadian border to 500,000 years near Taber, a town about 60 miles northwest of the outcrop. A sensitivity analysis on the input parameters to the flow model indicated that the predicted age of the water is most sensitive to changes in sandstone porosity and the vertical permeability of the shales and clays overlying and underlying the sandstone aquifer.
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.subjectHydrology.
dc.subjectGroundwater -- Milk River Aquifer (Mont. and Alta.)
dc.subjectGroundwater analysis.
dc.subjectHydrology -- Milk River Aquifer (Mont. and Alta.)
dc.subjectRadiocarbon dating.
dc.titleThe hydrochemistry and age of the water in the Milk River aquifer, Alberta, Canadaen_US
dc.typeThesis-Reproduction (electronic)en_US
dc.typetexten_US
dc.contributor.chairDavis, Stanley N.en_US
dc.identifier.oclc212893470en_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.dateFOA2018-06-12T22:40:33Z
html.description.abstractThe Milk River aquifer system in Alberta, Canada, was studied to develop age-dating techniques for old ground water. A steadystate flow model used to calculate hydrodynamic ages of the ground water and ¹⁴C concentrations in the water were used to calculate ages for comparison. The results were compared with ³⁶Cl-predicted ages of the same aquifer. The ages predicted with the flow model showed a progression of increasing age from zero at the Milk River sandstone outcrop near the United States—Canadian border to 500,000 years near Taber, a town about 60 miles northwest of the outcrop. A sensitivity analysis on the input parameters to the flow model indicated that the predicted age of the water is most sensitive to changes in sandstone porosity and the vertical permeability of the shales and clays overlying and underlying the sandstone aquifer.


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