Record Details

Modeling effect of initial soil moisture on sorptivity and infiltration

ScholarsArchive at Oregon State University

Field Value
Title Modeling effect of initial soil moisture on sorptivity and infiltration
Names Stewart, Ryan D. (creator)
Rupp, David E. (creator)
Abou Najm, Majdi R. (creator)
Selker, John S. (creator)
Date Issued 2013-10-28 (iso8601)
Note This is the publisher’s final pdf. The published article is copyrighted by the American Geophysical Union and can be found at: http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)1944-7973.
Abstract A soil’s capillarity, associated with the parameter sorptivity, is a dominant control on
infiltration, particularly at the onset of rainfall or irrigation. Many mathematical models
used to estimate sorptivity are only valid for dry soils. This paper examines how sorptivity
and its capillary component (as wetting front potential) change with initial degree of
saturation. We capture these effects with a simple modification to the classic Green-Ampt
model of sorptivity. The modified model has practical applications, including (1) accurately
describing the relative sorptivity of a soil at various water contents and (2) allowing for
quantification of a soil’s saturated hydraulic conductivity from sorptivity measurements,
given estimates of the soil’s characteristic curve and initial water content. The latter
application is particularly useful in soils of low permeability, where the time required to
estimate hydraulic conductivity through steady-state methods can be impractical.
Genre Article
Topic infiltration
Identifier Stewart, R. D., D. E. Rupp, M. R. Abou Najm, and J. S. Selker (2013), Modeling effect of initial soil moisture on sorptivity and infiltration, Water Resources Research, 49, 7037–7047. doi:10.1002/wrcr.20508

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