SSSAJ Journal of Natural Resources and Life Sciences Education
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Figure 1


Fig. 1. Observed and simulated pressure head at (a) 0.4-m depth, (b) 1.0-m depth, and (c) 2.6-m depth using minimum, median, and maximum values of the saturated hydraulic conductivity, Ks, derived from laboratory analysis of vadose zone samples. A simulation with median Ks and optimized pore-connectivity parameter l values is also shown.





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