TECHNICAL NOTES
Jul 1, 1997

Infiltration over Heterogenous Watershed: Influence of Rain Excess

Publication: Journal of Hydrologic Engineering
Volume 2, Issue 3

Abstract

Once the soil surface reaches saturation, rain excess is generated. This rain excess may run over and infiltrate in other areas of the watershed. In this study, we consider three scenarios of distributing rain excess/run-on to examine how it affects infiltration over a watershed. For these scenarios, we introduce simple solutions that allow the users to (1) estimate the ponded area-fraction of the watershed, and (2) determine the area-averaged infiltration. The solutions are practical because they require trivial computations. The solutions of ponding time and area-averaged infiltration account for the influence of initial water content and contain parameters with precise physical meaning. We find that area-averaged infiltration depends strongly on the distribution of rain excess at the surface. Thus we question the use of many stochastic area-averaged infiltration models that ignore the influence of rain excess.

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References

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Published In

Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 2Issue 3July 1997
Pages: 140 - 143

History

Published online: Jul 1, 1997
Published in print: Jul 1997

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Authors

Affiliations

Mahmood H. Nachabe
Water Engrg. and Mgmt. Program, Asian Inst. of Technol., P.O. Box 4, Klongluang, Pathum Thani 12120, Thailand; formerly, U.S. Dept. of Agr., Agr. Res. Services, 301 S. Howes, Fort Collins, CO 80522.
Tissa H. Illangasekare
Prof., Univ. of Colorado at Boulder, CB 428, Boulder, CO 80309-0428.
Hubert J. Morel-Seytoux
Hydrology Days Publication, 57 Selby Lane, Atherton, CA 94027.
Laj R. Ahuja, Members, ASCE,
Res. Leader, U.S. Dept. of Agr., Agr. Res. Services, 301 S. Howes, Fort Collins, CO.
Huan Ruan
Grad. Student, Univ. of Colorado at Boulder, CB 428, Boulder, CO.

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