Abstract
Infiltration from a point trickle source in the presence of water extraction is investigated using an approximate hemispherical model. Analytic expressions for the position of the wetting front are derived. In the short-time limit the wetting front follows a simple t one third dependence. The rate of advance of the wetting front depends on a single soil parameter, closely related to the saturated water content. At larger times the effects of water extraction modify the solution to an exponential approach to a limiting radius, which is determined by the balance between the competing discharge and extraction processes. -from Authors
Original language | English |
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Pages (from-to) | 882-887 |
Number of pages | 6 |
Journal | Soil Science Society of America Journal |
Volume | 50 |
Issue number | 4 |
DOIs | |
State | Published - 1 Jan 1986 |
ASJC Scopus subject areas
- Soil Science