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- W2011182938 abstract "Abstract The application of conventional pore structure models that predict the hydraulic-conductivity/watercontent function, K ( Θ ), from the soilwater retention data, yield K ( Θ ) expressions which in some cases deviate significantly from the actual K ( Θ ). An alternative method for the determination of K ( Θ ) is developed, in which a statistical model in a more general form with an additional unknown parameter is used, in conjunction with the one-step outflow laboratory method. Previous results were reformulated on the basis of the Brooks and Corey model to obtain the cumulative outflow data by semi-analytical formulae. The procedure suggested was applied in two different porous materials." @default.
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- W2011182938 date "1991-11-01" @default.
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- W2011182938 title "Laboratory determination of unsaturated hydraulic conductivity using a generalized-form hydraulic model" @default.
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- W2011182938 doi "https://doi.org/10.1016/0022-1694(91)90143-6" @default.
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