The use of temperature as a ground-water tracer in glacial outwash
A twenty-four hour, divergent-flow thermal tracer experiment was conducted to determine the usefulness of heat as a ground-water tracer. Bromide was used also in the experiment, as a means of comparing the thermal tracer to a conservative chemical species. Observations of pore-fluid temperature and...
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| Language: | en |
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The University of Arizona.
1987
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| Online Access: | http://hdl.handle.net/10150/191954 |