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Water repellency has a great influence on water infiltration into soil. Currently, there is no modified correlation model that is applicable to the water infiltration of water-repellent soils (WRS). In order to better construct a model suitable for water
Youzhen Xiang, Bei Zhang
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A Modified Green-Ampt Infiltration Model for Muddy Water
Journal of HydrologyLiangjun Fei, Yun Zhong
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Solutions to Green-Ampt Infiltration Equation
Journal of the Irrigation and Drainage Division, 1976The simple method of solving the Green-Ampt one-dimensional infiltration equations developed from Darcy's law are proposed for practical applications. The explicit solution is an approximation obtained by employing a power series expansion of the logarithmic term. The maximum error resulting from applying this simple explicit solution is 8%.
Ruh-Ming Li +2 more
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DEVELOPMENT OF A CRUST FACTOR FOR A GREEN AMPT MODEL
Transactions of the ASAE, 1990ABSTRACT The formation of a soil crust has been shown to cause a major decrease in infiltration and needs to be accounted for in infiltration models. In response to this need, a procedure based on such properties and wetted front depth was developed for incorporating the steady state crust conductivity into the hydraulic conductivity term of the Green ...
null W. J. Rawls +3 more
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Use of the Green‐Ampt Equation with Variable Conductivity
Soil Science Society of America Journal, 1976Abstract A comparison with Phillp's two‐term equation, derived from a series solution involving t 1/2 , indicates that the hydraulic conductivity in the Green‐Ampt equation of vertical infiltration varies with time when the soil water content of the transmission zone is ...
L. R. Ahuja, G. Y. Tsuji
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Approximate Form of Green‐Ampt Infiltration Equation
Journal of Irrigation and Drainage Engineering, 1994We develop an approximation of the Green‐Ampt infiltration equation by using the first two terms of a Taylor‐series expansion of the equation. The resulting approximate equation is in the form of the Philip's equation, with an added term to account for the error in the approximation.
Jeffry J. Stone +2 more
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Exploring the parameter space of the Green–Ampt model
Advances in Water Resources, 2013This study systematically investigates the entire parameter space of the Green–Ampt model for water infiltration and allows for arbitrary constant hydraulic head boundary conditions, any column inclination, hydrophilic and hydrophobic porous media, and a nonzero initial cumulative infiltration.
Markus Hilpert, Roland Glantz
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The Green–Ampt limit with reference to infiltration coefficients
Water Resources Research, 2012Recent progress with an analytic nonlinear model has provided the exact infiltration coefficients for realistic soil behaviors with nonsingular hydraulic functions, as well as their exact delta‐function diffusivity limits. After some correction and reinterpretation of the approximate analytical method, the exactly solvable model validates some ...
D. Triadis, P. Broadbridge
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Applications of the Green-Ampt Method across Scales
World Environmental and Water Resources Congress 2014, 2014The Green-Ampt method has been widely used for simulating infiltration and rainfall-runoff processes in various hydrologic models across spatial scales ranging from small laboratory scales to large field and watershed scales. A fundamental question is this: how do such spatial scales affect the applicability of the Green-Ampt method?
Xuefeng Chu, Noah Habtezion
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Drainage to a water table analysed by the Green-Ampt approach
Journal of Hydrology, 1976By means of the Green-Ampt analysis, it is shown that the drainage from an initially saturated column of porous material after the water table is suddenly lowered to a given level from the surface on which infiltration is maintained at a rate q during the drainage, may be described to a good approximation by the equation: 1-Q′Q′∞=exp[-(F0-q)tQ′∞]
E.G. Youngs, S. Aggelides
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