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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. The evaporation rate can be estimated for homogeneous as well as layered soils. Results obtained with the method demonstrate how the soil-water evaporation rates depend on potential evaporation, water table depth, vapor transfer, and certain soil parameters.

Estimating steady-state evaporation rates from bare soils under conditions of high water table