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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 (
) 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
was estimated from the difference between the initial
(
i) and air-dry
(
ad), multiplied by a conductance coefficient (C). The C represents the fraction of the remaining soil water (
i -
ad) that can be removed in 1 d during SSE and is a power function of soil depth. Testing the dependency of C and
(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
for different soils at different depths during SSE. Linear relationships with zero intercept were found between
and drained upper limit
(
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
dul were correlated with r2 > 0.9. Root mean square error (RMSE) between measured and estimated
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
, soil water content
ad, air-dry soil water content
dul, drained upper limit soil water content
i, initial soil water content
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