Estimating steady-state evaporation rates from bare soils under conditions of high water table
Open-File Report
By: C.D. Ripple, J. Rubin, and T. E. A. Van Hylckama
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Abstract
A procedure that combines meteorological and soil equations of water transfer makes it possible to estimate approximately the steady-state evaporation from bare soils under conditions of high water table. Field data required include soil-water retention curves, water table depth and a record of air temperature, air humidity and wind velocity at one elevation. The procedure takes into account the relevant atmospheric factors and the soil's capability to conduct 'water in liquid and vapor forms. It neglects the effects of thermal transfer (except in the vapor case) and of salt accumulation. Homogeneous as well as layered soils can be treated. Results obtained with the method demonstrate how the soil evaporation rates·depend on potential evaporation, water table depth, vapor transfer and certain soil parameters.
Suggested Citation
Ripple, C., Rubin, J., Van Hylckama, T.E., 1970, Estimating steady-state evaporation rates from bare soils under conditions of high water table: Open-File Report, vii, 62 p., https://doi.org/10.3133/70047724.
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Unnumbered Series |
| Title | Estimating steady-state evaporation rates from bare soils under conditions of high water table |
| Series title | Open-File Report |
| DOI | 10.3133/70047724 |
| Year Published | 1970 |
| Language | English |
| Publisher | U.S. Government Printing Office |
| Publisher location | Washington, DC |
| Contributing office(s) | Water Resources Division |
| Description | vii, 62 p. |