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Автор White, I.
Автор Sully, M. J.
Дата выпуска 1992
dc.description The quasi‐linear parameterization for unsaturated hydraulic conductivity K(Ψ) = K<sub>s</sub> exp (αΨ), where K is hydraulic conductivity, Ψ is soil water matric potential, K<sub>s</sub> is saturated hydraulic conductivity, and α is a porous material parameter, has been used in both stochastic and deterministic models of unsaturated water flow in porous materials. In the stochastic approach, K<sub>s</sub> is assumed lognormally distributed, but α and the volumetric soil water capacity C = dθ/dΨ, with θ volumetric soil water content, are assumed normally distributed. We point out here that α and K<sub>s</sub> are related to the same internal pore geometry of the soil. This interrelationship ensures that if K<sub>s</sub> is lognormal, then α, and possibly C, will also be lognormal. Additionally, we present preliminary field results which indicate that α is better described by a lognormal than a normal distribution. The quasi‐linear parameterization can be expected to be correct only in some integral sense. Predictions of increases in the variability of hydraulic conductivity with decreasing Ψ may therefore be prejudiced by the use of the exponential form for K(Ψ). Tests of the sensitivity of stochastic model predictions to both the parameterizations adopted for K(Ψ) and the assumed distribution functions of parameters seem warranted. Reliable experimental evidence on field variability of K(Ψ) and Ψ(θ) at substantial negative values of Ψ are also needed.
Формат application.pdf
Копирайт Published in 1992 by the American Geophysical Union.
Тема HYDROLOGY
Тема Soil moisture
Тема Hydrologic scaling
Тема Stochastic hydrology
Тема Hydrology
Тема Hydrology
Тема Hydrology
Название On the variability and use of the hydraulic conductivity alpha parameter in stochastic treatments of unsaturated flow
Тип article
DOI 10.1029/91WR02198
Electronic ISSN 1944-7973
Print ISSN 0043-1397
Журнал Water Resources Research
Том 28
Первая страница 209
Последняя страница 213
Выпуск 1
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