VZJ Journal of Natural Resources and Life Sciences Education
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Fig. 2. Errors in the directly estimated hydraulic conductivity near saturation (h < -20 cm) in three hypothetical soils. Contours represent Kestimated/Kactual as a function of soil length (L) and the rate of lower boundary pressure change ({Delta}P). The K({theta}) and {theta}(h) of the simulated soils were represented using van Genuchten forms (Eq. [2]).





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