Add to ORKGThe classical treatment of the water flow in the unsaturated porous medium is represented by Richards equation. In order to obtain an approximation of the solution, the problem has been treated numerically by applying the finite differences method and obtaining a non-linear system of equations where the uniqueness of the solution is ensured by Neumann boundary condition. The resolution of the system is carried out by combining Euler explicit method with Crank-Nicolson method
This paper presents a functional approach to a nonlinear model describing the complete physical proc...
Analytical solutions of differential equations describe physical problems and provide general insigh...
A numerical program has been developed to study the motion of a fluid (e.g. rainfall water) within a...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richard...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richard...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
An applied numerical unsaturated flow model was developed in the previous paper to describe the move...
Flow movement in unsaturated soil can be expressed by a partial differential equation, named Richard...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
This paper presents a functional approach to a nonlinear model describing the complete physical proc...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
Analytical solutions of differential equations describe physical problems and provide general insigh...
This paper presents a functional approach to a nonlinear model describing the complete physical proc...
Analytical solutions of differential equations describe physical problems and provide general insigh...
A numerical program has been developed to study the motion of a fluid (e.g. rainfall water) within a...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richard...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richard...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richar...
An applied numerical unsaturated flow model was developed in the previous paper to describe the move...
Flow movement in unsaturated soil can be expressed by a partial differential equation, named Richard...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
This paper presents a functional approach to a nonlinear model describing the complete physical proc...
Solutions of the linearized one-dimensional Richards equation for discrete arbitrary initial and bou...
Analytical solutions of differential equations describe physical problems and provide general insigh...
This paper presents a functional approach to a nonlinear model describing the complete physical proc...
Analytical solutions of differential equations describe physical problems and provide general insigh...
A numerical program has been developed to study the motion of a fluid (e.g. rainfall water) within a...