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ABSTRACT
Water flow from a point source is analyzed using a linearized form of the moisture flow equation. Time-dependence is assumed with the results simplifying to those of previous investigators for steady-state conditions. Discrete time-distributed inputs such as might occur for trickle or high frequency irrigation is amenable to the solution. Numerical simulations include (i) the advance of a wetting front during infiltration, (ii) moisture variation resulting from a cyclic input as during irrigation, and (iii) the matric flux potential field for a two-source problem.
1 Arizona Agri. Exp. Sta. Paper no. 2174. Support was from the Western Regional Project W-68.
2 Associate Professor, Department of Soils, Water and Engineering, The Univ. of Arizona, Tucson 85721.
Received for publication September 18, 1973. Accepted for publication December 14, 1973.
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