The focus of this paper is two-dimensional computational modelling of water flow in unsaturated soils consisting of weakly conductive disconnected inclusions embedded in a highly conductive connected matrix. When the inclusions are small, a two-scale Richards’ equation-based model has been proposed in the literature taking the form of an equation with effective parameters governing the macroscopic flow coupled with a microscopic equation, defined at each point in the macroscopic domain, governing the flow in the inclusions. This paper is devoted to a number of advances in the numerical implementation of this model. Namely, by treating the micro-scale as a two-dimensional problem, our solution approach based on a control volume finite elemen...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
The focus of this paper is two-dimensional computational modelling of water flow in unsaturated soil...
Unsaturated water flow in soil is commonly modelled using Richards’ equation, which requires the hyd...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
International audienceThe paper deals with modelling of unsaturated water flow in soils which are co...
International audienceThe paper deals with modelling of unsaturated water flow in soils which are co...
International audienceThe paper deals with modelling of unsaturated water flow in soils which are co...
International audienceThis paper presents the experimental validation of a macroscopic model of unsa...
International audienceThis paper presents the experimental validation of a macroscopic model of unsa...
International audienceThis paper presents the experimental validation of a macroscopic model of unsa...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
The focus of this paper is two-dimensional computational modelling of water flow in unsaturated soil...
Unsaturated water flow in soil is commonly modelled using Richards’ equation, which requires the hyd...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
Many biological and geological systems can be modelled as porous media with small inclusions. Vascul...
International audienceThe paper deals with modelling of unsaturated water flow in soils which are co...
International audienceThe paper deals with modelling of unsaturated water flow in soils which are co...
International audienceThe paper deals with modelling of unsaturated water flow in soils which are co...
International audienceThis paper presents the experimental validation of a macroscopic model of unsa...
International audienceThis paper presents the experimental validation of a macroscopic model of unsa...
International audienceThis paper presents the experimental validation of a macroscopic model of unsa...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...
A two-dimensional Galerkin finite element model for water flow in variably saturated soil is present...