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This paper introduces a finite‐element collocation technique for solving the equation governing two‐dimensional flow in a variably saturated porous medium. The scheme uses a mass‐conserving formulation of Richards' equation as the basis for the finite‐difference time‐stepping method. Collocation in tensor‐product spaces of Hermite cubics yields a computationally efficient finite‐element approximation of the spatial derivatives. A Newton‐like iteration gives a temporally stable implicit scheme. The paper examines two sample problems, including an initial boundary‐value problem involving subsurface irrigation.
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Allen et al. (1986) studied this question.
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