Flow movement in unsaturated soil can be expressed by a partial differential equation, named Richards equation. The objective of this study is the finding of an appropriate implicit numerical solution for head based Richards equation. Some of the well known finite difference schemes (fully implicit, Crank Nicolson and Runge-Kutta) have been utilized in this study. In addition, the effects of different approximations of moisture capacity function, convergence criteria and time stepping methods were evaluated. Two different infiltration problems were solved to investigate the performance of different schemes. These problems include of vertical water flow in a wet and very dry soils. The numerical solutions of two problems were compared using ...
Scaling methods allow a single solution to Richards' equation (RE) to suffice for numerous specific ...
An applied numerical unsaturated flow model was developed in the previous paper to describe the move...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richard...
Simulation Infiltration Rate of water on two dimension of thin plate soil by using finite difference...
Simulation Infiltration Rate of water on two dimension of thin plate soil by using finite difference...
International audienceA new numerical scheme has been proposed by Ross [Ross, P.J., 2003. Modeling s...
International audienceA new numerical scheme has been proposed by Ross [Ross, P.J., 2003. Modeling s...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / PHYLEAU [TR2_IRSTEA]RIE / TRANSFEAUInternational audienceA ...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / PHYLEAU [TR2_IRSTEA]RIE / TRANSFEAUInternational audienceA ...
Analysis of water and solute movement in unsaturated-saturated soil systems would greatly benefit fr...
Warrick and Hussen developed in the nineties of the last century a method to scale Richards' equatio...
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Scaling methods allow a single solution to Richards' equation (RE) to suffice for numerous specific ...
An applied numerical unsaturated flow model was developed in the previous paper to describe the move...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richard...
Simulation Infiltration Rate of water on two dimension of thin plate soil by using finite difference...
Simulation Infiltration Rate of water on two dimension of thin plate soil by using finite difference...
International audienceA new numerical scheme has been proposed by Ross [Ross, P.J., 2003. Modeling s...
International audienceA new numerical scheme has been proposed by Ross [Ross, P.J., 2003. Modeling s...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / PHYLEAU [TR2_IRSTEA]RIE / TRANSFEAUInternational audienceA ...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / PHYLEAU [TR2_IRSTEA]RIE / TRANSFEAUInternational audienceA ...
Analysis of water and solute movement in unsaturated-saturated soil systems would greatly benefit fr...
Warrick and Hussen developed in the nineties of the last century a method to scale Richards' equatio...
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Transient water flow processes in unsaturated soils are usually modeled using the Richards equation....
Scaling methods allow a single solution to Richards' equation (RE) to suffice for numerous specific ...
An applied numerical unsaturated flow model was developed in the previous paper to describe the move...
The classical treatment of the water flow in the unsaturated porous medium is represented by Richard...