Date of Award:
5-1953
Document Type:
Thesis
Degree Name:
Master of Science (MS)
Department:
Plants, Soils, and Climate
Department name when degree awarded
Soil Physics
Committee Chair(s)
S. A. Taylor
Committee
S. A. Taylor
Committee
D. W. Thorne
Committee
P. J. Hart
Abstract
The isothermal movement of liquid water in saturated soil has been intensively studied, and a sound theoretical basis has been intensively studied, and a sound theoretical basis has been developed. Considerably less is known about the flow of water in unsaturated soils, but a general theory based on Darcy’s law of flow is beginning to develop. A good theoretical basis exists for the vapor diffusion under isothermal conditions. Inconsistent data and theories are found in the literature concerning the movement of water in both the vapor and liquid phases, under the influence of thermal fields.
Checksum
07d8d7799fc842fab67c268d18098f0e
Recommended Citation
Gavazza, Luigi, "The Influence of Temperature Gradients on Soil Moisture Flow" (1953). All Graduate Theses and Dissertations, Spring 1920 to Summer 2023. 2710.
https://digitalcommons.usu.edu/etd/2710
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