A linear stability analysis was performed for three models of flow in unsaturated porous media to determine the conditions for growth of small perturbations. The models considered include the conventional Richards equation (RE), a sharp front Richards equation (SFRE) and an extended Richards equation (RRE). The first two models are based on the use of an equilibrium capillary pressure-saturation function, while the third model is derived using a dynamic capillary pressure-saturation function represented by a relaxation coefficient. A traveling wave solution was formulated for each of the governing equations and used as the basic solution of each model. The stability analysis was based on imposing a small perturbation to the basic solution. ...
The paper theoretically investigates the stability properties of the dam–break wave of a fluid with ...
We consider gravitational instability of a saline boundary layer formed by evaporation induced upwar...
Several experiments have evidenced the occurrence of saturation overshoots for flows in homogeneous ...
A linear stability analysis was performed for three models of flow in unsaturated porous media to de...
Stability analysis of gravity-driven unsaturated flow is examined for the general case of Darcian fl...
Several alternative mathematical models for describing water flow in unsaturated porous media are pr...
Several alternative mathematical models for describing water flow in unsaturated porous media are pr...
The Richards equation is a mathematical model for unsaturated flow through porous media. This paper ...
The formation of preferential flow paths during infiltration of water into homogeneous, dry soil is ...
The author investigates the stability of an external gravity wave progressing horizontally in an inv...
The coupled equations for flow in unsaturated soil as proposed by Beliaev and Hassanizadeh [6] are d...
Linear stability analysis is applied to the Richards equation by perturbing the pressure field. An a...
none2noWe analyse the linear stability of self-similar shallow, two-dimensional and axisymmetric gra...
Gravity-driven fingering has been observed during downward infiltration of water into dry sand. More...
Gravity-driven fingering has been observed during downward infiltration of water into dry sand. More...
The paper theoretically investigates the stability properties of the dam–break wave of a fluid with ...
We consider gravitational instability of a saline boundary layer formed by evaporation induced upwar...
Several experiments have evidenced the occurrence of saturation overshoots for flows in homogeneous ...
A linear stability analysis was performed for three models of flow in unsaturated porous media to de...
Stability analysis of gravity-driven unsaturated flow is examined for the general case of Darcian fl...
Several alternative mathematical models for describing water flow in unsaturated porous media are pr...
Several alternative mathematical models for describing water flow in unsaturated porous media are pr...
The Richards equation is a mathematical model for unsaturated flow through porous media. This paper ...
The formation of preferential flow paths during infiltration of water into homogeneous, dry soil is ...
The author investigates the stability of an external gravity wave progressing horizontally in an inv...
The coupled equations for flow in unsaturated soil as proposed by Beliaev and Hassanizadeh [6] are d...
Linear stability analysis is applied to the Richards equation by perturbing the pressure field. An a...
none2noWe analyse the linear stability of self-similar shallow, two-dimensional and axisymmetric gra...
Gravity-driven fingering has been observed during downward infiltration of water into dry sand. More...
Gravity-driven fingering has been observed during downward infiltration of water into dry sand. More...
The paper theoretically investigates the stability properties of the dam–break wave of a fluid with ...
We consider gravitational instability of a saline boundary layer formed by evaporation induced upwar...
Several experiments have evidenced the occurrence of saturation overshoots for flows in homogeneous ...