A numeric method for estimating infiltration, redistribution, drainage, and evaporation of water from soil

A numeric method for estimating infiltration, redistribution, drainage, and evaporation of water... A general numeric method is described for estimating one‐dimensional infiltration, redistribution, evaporation, and drainage of water from soil. The type of flow is determined by the water flux at the surface of soil or the bottom boundary. The method provides for hysteresis in the water content‐pressure head relation. Comparison with measurement made on soil columns for infiltration, redistribution, and evaporation were made. Good agreement was obtained between measured and computed values. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Water Resources Research Wiley

A numeric method for estimating infiltration, redistribution, drainage, and evaporation of water from soil

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Publisher
Wiley
Copyright
Copyright © 1969 by the American Geophysical Union.
ISSN
0043-1397
eISSN
1944-7973
DOI
10.1029/WR005i005p01064
Publisher site
See Article on Publisher Site

Abstract

A general numeric method is described for estimating one‐dimensional infiltration, redistribution, evaporation, and drainage of water from soil. The type of flow is determined by the water flux at the surface of soil or the bottom boundary. The method provides for hysteresis in the water content‐pressure head relation. Comparison with measurement made on soil columns for infiltration, redistribution, and evaporation were made. Good agreement was obtained between measured and computed values.

Journal

Water Resources ResearchWiley

Published: Oct 1, 1969

References

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