The hydrochemistry and age of the water in the Milk River aquifer, Alberta, Canada
dc.contributor.author | Swanick, Gerald Bernard. | |
dc.creator | Swanick, Gerald Bernard. | en_US |
dc.date.accessioned | 2011-11-28T14:05:13Z | |
dc.date.available | 2011-11-28T14:05:13Z | |
dc.date.issued | 1982 | en_US |
dc.identifier.uri | http://hdl.handle.net/10150/191755 | |
dc.description.abstract | The 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.iso | en | en_US |
dc.publisher | The University of Arizona. | en_US |
dc.rights | Copyright © 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 | Hydrology. | |
dc.subject | Groundwater -- Milk River Aquifer (Mont. and Alta.) | |
dc.subject | Groundwater analysis. | |
dc.subject | Hydrology -- Milk River Aquifer (Mont. and Alta.) | |
dc.subject | Radiocarbon dating. | |
dc.title | The hydrochemistry and age of the water in the Milk River aquifer, Alberta, Canada | en_US |
dc.type | Thesis-Reproduction (electronic) | en_US |
dc.type | text | en_US |
dc.contributor.chair | Davis, Stanley N. | en_US |
dc.identifier.oclc | 212893470 | en_US |
thesis.degree.grantor | University of Arizona | en_US |
thesis.degree.level | masters | en_US |
thesis.degree.discipline | Hydrology and Water Resources | en_US |
thesis.degree.discipline | Graduate College | en_US |
thesis.degree.name | M.S. | en_US |
dc.description.note | hydrology collection | en_US |
refterms.dateFOA | 2018-06-12T22:40:33Z | |
html.description.abstract | The 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. |