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Effects of Temperature on Moisture Conductivity in Unsaturated SoilMeeuwig, Richard O'Bannon 01 May 1964 (has links)
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 potential gradient.
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