Effects of Temperature on Moisture Conductivity in Unsaturated Soil
Water moves in soil in response to potential gradients. The basic equation for this movement is the generalized flow equation: v = - KV0 in which v is volume of water passing through a unit area in unit time, K is the conductivity coefficient, V is the gradient operator (vector), and V 0 is the pote...
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| Format: | Others |
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DigitalCommons@USU
1964
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| Online Access: | https://digitalcommons.usu.edu/etd/3793 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=4803&context=etd |