SSSAJ Journal of Natural Resources and Life Sciences Education
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Soil Science Society of America Journal 67:377-386 (2003)
© 2003 Soil Science Society of America

DIVISION S-1—SOIL PHYSICS

Modeling Soil Water Redistribution during Second-Stage Evaporation

A. A. Suleiman*,a and J. T. Ritchieb

a Center for Atomoshperic Sciences, Hampton University, Hampton, VA 23668
b Department of Crop and Soil Sciences, Plant and Soil Sciences Building, Michigan State University, East Lansing, MI 48824-1325

* Corresponding author (ayman.suleiman{at}hamptonu.edu)

Calculating the dynamics of soil water content ({theta}) near the surface and modeling soil water evaporation (Es) are critical for many agricultural management strategies. This study was performed to develop a model to simulate soil water redistribution during second-stage evaporation (SSE). In this model, the daily change of {theta} was estimated from the difference between the initial {theta} ({theta}i) and air-dry {theta} ({theta}ad), multiplied by a conductance coefficient (C). The C represents the fraction of the remaining soil water ({theta}i - {theta}ad) that can be removed in 1 d during SSE and is a power function of soil depth. Testing the dependency of C and {alpha} (the slope of cumulative evaporation [Ec] vs. square root of time [t1/2]) on soil characteristics was done using theoretical and laboratory data. Then the whole model was evaluated in laboratory and field conditions by measuring {theta} for different soils at different depths during SSE. Linear relationships with zero intercept were found between {alpha} and drained upper limit {theta} ({theta}dul) with slope and r2 = 1.19 and 0.69 and 1.39 and 0.95 for laboratory and theoretical data, respectively. Conductance coefficient and {theta}dul were correlated with r2 > 0.9. Root mean square error (RMSE) between measured and estimated {theta} in the field was highest (0.014 cm3 cm-3) at depths of 3 and 6 cm and lowest (0.005 cm3 cm-3) at the 9-cm depth. The model gave reasonable estimates of both water redistribution and Es during SSE and is expected to work well for soils for which the diffusivity theory holds.

Abbreviations: C, conductance coefficient • DOY, day of year • DSSAT, Decision Support System for Agrotechnology Transfer • Ec, cumulative evaporation • Es, soil water evaporation • PVC, polyvinyl chloride • SSE, second-stage evaporation • {theta}, soil water content • {theta}ad, air-dry soil water content • {theta}dul, drained upper limit soil water content • {theta}i, initial soil water content




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