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- W277870087 abstract "The paper presents relations between drainage porosity (n d ) and the saturated hydraulic conductivity (K s ). The undisturbed soil samples were characterised by the saturated hydraulic conductivity, water retention curve (WRC) and estimated sum of the soil macro and mesopores known as the drainage porosity. The latter sum was estimated from the pF curves as a difference between the total porosity ( t ) and the field capacity (FC). Two equations describing these relationships were proposed and the coefficients of the power function of Ahuja et al. [1, 2] were modified. The equations proposed were tested on the original data set and on the independent selected UNSODA data set [23] and compared with other previously published pedotransfer functions (PTFs). The results of the comparative analysis have shown that for 0.03 < d <0.30 m 3 × m -3 , the equation proposed in this paper provides a more accurate assessment of the saturated hydraulic conductivity. It has been also shown that the relation derived is universal and does not depend on the soil texture." @default.
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- W277870087 date "2007-01-01" @default.
- W277870087 modified "2023-09-27" @default.
- W277870087 title "ESTIMATION OF SATURATED HYDRAULIC CONDUCTIVITY ON THE BASIS OF DRAINAGE POROSITY" @default.
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