The paper presents numerical simulations of water infiltration in unsaturated porous media containing coarse-textured inclusions embedded in fine-textured background material. The calculations are performed using the two-phase model for water and air flow and a simplified model known as the Richards equation. It is shown that the Richards equation cannot correctly describe flow in the presence of heterogeneities. However, its performance can be improved by introducing appropriately defined effective capillary and permeability functions, representing largescale behaviour of the heterogeneous medium
Traditionally, multiphase flow in porous media is described by the so-called extended Darcy’s Law, w...
The macroscopic behavior of air and water in porous media is often approximated using Richards’ equa...
We wish to thank our students, Y. Benarafa and S. Delau, who participated in this study at its early...
The paper presents a 2D upward infiltration experiment performed on a model porous medium consisting...
The Richards equation is widely used in hydrogeology for modelling flow in an unsaturated porous me...
Several existing equations for solving the non-linear soil-hydraulic properties are introduced and v...
The two-phase flow behaviour in porous media is determined on the basis of capillary pressure–satura...
Well-defined laboratory experiments have been conducted to determine the significance of dynamic eff...
We investigate a two-phase porous media flow model, in which dynamic effects are taken into account ...
The process of flow modeling in unsaturated porous medium is often found in many fields of sciences:...
We investigate a two-phase porous media flow model, in which dynamic effects are taken into account ...
Capillary pressure-saturation-relative permeability relations described using the van Genuchten [198...
We investigate a two-phase porous media flow model, in which dynamic effects are taken into account ...
Water infiltration into the unsaturated zone is potentially affected by air compression ahead of the...
This paper deals with two-equation models describing solute transport in highly heterogeneous porous...
Traditionally, multiphase flow in porous media is described by the so-called extended Darcy’s Law, w...
The macroscopic behavior of air and water in porous media is often approximated using Richards’ equa...
We wish to thank our students, Y. Benarafa and S. Delau, who participated in this study at its early...
The paper presents a 2D upward infiltration experiment performed on a model porous medium consisting...
The Richards equation is widely used in hydrogeology for modelling flow in an unsaturated porous me...
Several existing equations for solving the non-linear soil-hydraulic properties are introduced and v...
The two-phase flow behaviour in porous media is determined on the basis of capillary pressure–satura...
Well-defined laboratory experiments have been conducted to determine the significance of dynamic eff...
We investigate a two-phase porous media flow model, in which dynamic effects are taken into account ...
The process of flow modeling in unsaturated porous medium is often found in many fields of sciences:...
We investigate a two-phase porous media flow model, in which dynamic effects are taken into account ...
Capillary pressure-saturation-relative permeability relations described using the van Genuchten [198...
We investigate a two-phase porous media flow model, in which dynamic effects are taken into account ...
Water infiltration into the unsaturated zone is potentially affected by air compression ahead of the...
This paper deals with two-equation models describing solute transport in highly heterogeneous porous...
Traditionally, multiphase flow in porous media is described by the so-called extended Darcy’s Law, w...
The macroscopic behavior of air and water in porous media is often approximated using Richards’ equa...
We wish to thank our students, Y. Benarafa and S. Delau, who participated in this study at its early...