A general approximation for the solution to the one-dimensional Richards equation is presented. It applies to arbitrary soil properties and boundary conditions but only uniform initial conditions at current stage. The result is very accurate (within 2%) when the diffusivity is constant, suggesting that the present general formulation is reliable, since the approximation becomes increasingly accurate as the soil-water diffusivity approaches a delta function.
CITATION STYLE
Parlange, J. Y., Barry, D. A., Parlange, M. B., Hogarth, W. L., Haverkamp, R., Ross, P. J., … Steenhuis, T. S. (1997). New approximate analytical technique to solve Richards equation for arbitrary surface boundary conditions. Water Resources Research, 33(4), 903–906. https://doi.org/10.1029/96WR03846
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