Temperature as an indicator of flow in fractured rocks near Oracle, Arizona
Knowledge of flow patterns in fractured rocks is important in understanding hydrology and contaminant transport. Methods of locating flow zones based on geophysical measurements are unreliable because of a lack of correlation between fracture density and hydraulic conductivity. In this work, analysi...
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| Language: | en |
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The University of Arizona.
1989
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| Online Access: | http://hdl.handle.net/10150/192014 |