Date of Award:
5-1964
Document Type:
Dissertation
Degree Name:
Doctor of Philosophy (PhD)
Department:
Plants, Soils, and Climate
Advisor/Chair:
Sterling A. Taylor
Abstract
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.
Recommended Citation
Meeuwig, Richard O'Bannon, "Effects of Temperature on Moisture Conductivity in Unsaturated Soil" (1964). All Graduate Theses and Dissertations. 3793.
https://digitalcommons.usu.edu/etd/3793
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