Horton Infiltration Equation Revisited
Publication: Journal of Irrigation and Drainage Engineering
Volume 118, Issue 5
Abstract
The original Horton equation is valid only if the rate of rainfall is always higher than the infiltration capacity of the soil throughout a rainfall-infiltration process. This technical note presents a modified Horton equation that expresses the soil infiltration capacity as a function of the amount of water that has already infiltrated into the soil. The modified equation is derived mathematically by combining the original and the integrated forms of the Horton equation. Therefore, the original Horton parameters are maintained in the modified equation. The modified and the original equations will give the same results when the assumptions of the original equation are valid. The advantage of the modified equation is that it can be used regardless of whether the rate of rainfall is greater than or less than the infiltration capacity. The technical note also includes expressions for the ponding time, and the amount of infiltration until ponding occurs.
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References
1.
Bras, R. L. (1990). Hydrology, an introduction to hydrologic science. Addison‐Wesley Publishing Co., Reading, Mass.
2.
Horton, R. E. (1940). “An approach toward a physical interpretation of infiltration capacity.” Soil Sci. Soc. Am. J., 5, 399–417.
3.
Huber, W. C., Heaney, J. P., and Nix. S. J. (1981). “Stormwater management model.” User's manual, Version III, National Environmental Research Center, U.S. Environmental Protection Agency, Cincinnati, Ohio.
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Copyright © 1992 ASCE.
History
Published online: Sep 1, 1992
Published in print: Sep 1992
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