A general approximation for the solution to the one‐dimensional Richards equation is presented. It applies to arbitrary soil properties and boundary conditions but only uniform initial conditions at current stage. The result is very accurate (within 2%) when the diffusivity is constant, suggesting that the present general formulation is reliable, since the approximation becomes increasingly accurate as the soil‐water diffusivity approaches a delta function.Griffith Sciences, Griffith School of EnvironmentFull Tex
Unsaturated flow processes are subject to either atmosphere control or soil control, often switching...
International audienceA new numerical scheme has been proposed by Ross [Ross, P.J., 2003. Modeling s...
Richards equation describes water transport in soils, but requires as input, soil material property ...
A general approximation for the solution to the one- dimensional Richards equation is presented. It ...
Analytical solutions of differential equations describe physical problems and provide general insigh...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
Abstract We apply a series expansion technique to estimate the water content distribution and front ...
A general approximation for the solution of the one-dimensional nonlinear diffusion equation is pres...
A useful insight of physical mechanisms related to the complex hydrological problems can be provided...
Abstract. A general approximation for the solution of the one-dimensional nonlinear diffusion equati...
The modified Richards equation (MRE) is presented by using a rotated coordinate system to accommodat...
The Richards equation is widely used as a model for the flow of water in unsaturated soils. For mode...
Scaling methods allow a single solution to Richards' equation (RE) to suffice for numerous specific ...
Unsaturated flow processes are subject to either atmosphere control or soil control, often switching...
International audienceA new numerical scheme has been proposed by Ross [Ross, P.J., 2003. Modeling s...
Richards equation describes water transport in soils, but requires as input, soil material property ...
A general approximation for the solution to the one- dimensional Richards equation is presented. It ...
Analytical solutions of differential equations describe physical problems and provide general insigh...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
Abstract We apply a series expansion technique to estimate the water content distribution and front ...
A general approximation for the solution of the one-dimensional nonlinear diffusion equation is pres...
A useful insight of physical mechanisms related to the complex hydrological problems can be provided...
Abstract. A general approximation for the solution of the one-dimensional nonlinear diffusion equati...
The modified Richards equation (MRE) is presented by using a rotated coordinate system to accommodat...
The Richards equation is widely used as a model for the flow of water in unsaturated soils. For mode...
Scaling methods allow a single solution to Richards' equation (RE) to suffice for numerous specific ...
Unsaturated flow processes are subject to either atmosphere control or soil control, often switching...
International audienceA new numerical scheme has been proposed by Ross [Ross, P.J., 2003. Modeling s...
Richards equation describes water transport in soils, but requires as input, soil material property ...