Thermally induced countercurrent flow in unsaturated rock
Axial temperature gradients were established in two sealed unsaturated rock cores and maintained until near steady distributions of temperature and moisture content were observed. Water content measurements, made at intervals along the length of the cores, indicated net moisture movement was from wa...
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| Language: | en |
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The University of Arizona.
1986
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| Online Access: | http://hdl.handle.net/10150/191920 |