TECHNICAL PAPERS
Apr 5, 2009

Toward Physically Based Estimation of Surface Irrigation Infiltration

Publication: Journal of Irrigation and Drainage Engineering
Volume 135, Issue 5

Abstract

Irrigation practitioners use empirical infiltration equations. Theoretical infiltration equations are currently not capable of capturing surface irrigation infiltration behavior, particularly during initial wetting. For a coarse textured soil, an example is shown where the Green-Ampt equation can be adjusted to match field “average” infiltration conditions by altering the soil’s physical properties. For finer textured soils, a time offset is proposed for adjusting the Green-Ampt equation to account for cracking and soil consolidation upon wetting. This results in a nonzero infiltration amount at time 0, a phenomenon commonly observed for infiltration of cracking soils. Applying this concept to the Philip equation (same as Modified Kostiakov equation with a=1/2 ) suggests the addition of an offset parameter. A modification to the two-point method is presented for this equation with the aim to better fit mathematical parameter functions to infiltration data.

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References

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Published In

Go to Journal of Irrigation and Drainage Engineering
Journal of Irrigation and Drainage Engineering
Volume 135Issue 5October 2009
Pages: 588 - 596

History

Received: Jun 12, 2008
Accepted: Apr 3, 2009
Published online: Apr 5, 2009
Published in print: Oct 2009

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Authors

Affiliations

A. J. Clemmens [email protected]
Center Director, U.S. Arid Land Agricultural Research Center, 21881 N. Cardon Lane, Maricopa, AZ 85238 (corresponding author). E-mail: [email protected]
E. Bautista [email protected]
Research Hydraulic Engineer, U.S. Arid Land Agricultural Research Center, 21881 N. Cardon Lane, Maricopa, AZ 85238. E-mail: [email protected]

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