Abstract We apply a series expansion technique to estimate the water content distribution and front position in finite boundary conditions. We derive an approximate analytical solution of the Richards equation (RE) for the horizontal infiltration problem. The solution is suitable for arbitrary hydraulic diffusivity in water infiltration. Compared with the finite element method, two examples in power law diffusivity and van Genuchten model are shown to test the accuracy of present approximation
Several authors have now used the Backlund transformation to linearize Richard's equation and so obt...
AbstractThe infiltration problem is one of the most interesting issues considered by geotechnical an...
Recently, Salvucci [1996] produced an interesting series so-lution for fixed surface moisture conten...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
A general approximation for the solution to the one‐dimensional Richards equation is presented. It a...
A general approximation for the solution to the one- dimensional Richards equation is presented. It ...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
New formulae giving the position of the wetting front and the surface water content during horizonta...
We attempt to generate new solutions for the moisture content form of the one-dimensional Richards\u...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
A useful insight of physical mechanisms related to the complex hydrological problems can be provided...
In the field of soil hydrology, the Richards equation is commonly used to model water flow in unsatu...
Perturbation methods are applied to study an initial-boundary-value problem for Richards' equation, ...
Warrick and Hussen developed in the nineties of the last century a method to scale Richards' equatio...
In this paper, an infiltration problem is considered. The problem involves time-independent flow fro...
Several authors have now used the Backlund transformation to linearize Richard's equation and so obt...
AbstractThe infiltration problem is one of the most interesting issues considered by geotechnical an...
Recently, Salvucci [1996] produced an interesting series so-lution for fixed surface moisture conten...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
A general approximation for the solution to the one‐dimensional Richards equation is presented. It a...
A general approximation for the solution to the one- dimensional Richards equation is presented. It ...
This paper aims to describe a compilation of solutions of the linearized one-dimensional Richards eq...
New formulae giving the position of the wetting front and the surface water content during horizonta...
We attempt to generate new solutions for the moisture content form of the one-dimensional Richards\u...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
A useful insight of physical mechanisms related to the complex hydrological problems can be provided...
In the field of soil hydrology, the Richards equation is commonly used to model water flow in unsatu...
Perturbation methods are applied to study an initial-boundary-value problem for Richards' equation, ...
Warrick and Hussen developed in the nineties of the last century a method to scale Richards' equatio...
In this paper, an infiltration problem is considered. The problem involves time-independent flow fro...
Several authors have now used the Backlund transformation to linearize Richard's equation and so obt...
AbstractThe infiltration problem is one of the most interesting issues considered by geotechnical an...
Recently, Salvucci [1996] produced an interesting series so-lution for fixed surface moisture conten...