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References (4)
-
J. Rubin (1967)
Numerical Method for Analyzing Hysteresis-Affected, Post-Infiltration Redistribution of Soil Moisture1Soil Science Society of America Journal, 31
-
E. Bresler, W. Kemper, R. Hanks (1969)
Infiltration, Redistribution, and Subsequent Evaporation of Water from Soil as Affected by Wetting Rate and HysteresisSoil Science Society of America Journal, 33
-
R. Hanks, S. Bowers (1962)
Numerical Solution of the Moisture Flow Equation for Infiltration into Layered Soils 1Soil Science Society of America Journal, 26
-
R. Freeze (1969)
The Mechanism of Natural Ground-Water Recharge and Discharge: 1. One-dimensional, Vertical, Unsteady, Unsaturated Flow above a Recharging or Discharging Ground-Water Flow SystemWater Resources Research, 5
- 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 Research – Wiley
Published: Oct 1, 1969