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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 (
P). The K(
) and
(h) of the simulated soils were represented using van Genuchten forms (Eq. [2]).
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