AbstractA general set of boundary conditions at fluid-permeable interfaces between dissimilar fluid-filled porous matrices is established starting from an extended Hamilton–Rayleigh principle. These conditions do include friction and inertial effects. Once linearized, they encompass boundary conditions relative to volume Darcy–Brinkman and to surface Saffman–Beavers–Joseph dissipation effects
The analysis and simulation of the dynamics of a moving boundary between immiscible fluids in a poro...
We derive boundary conditions at the interface of a homogeneous and isotropic porous medium and an o...
A new approach to the modelling of wetting fronts in porous media on the Darcy scale is developed, b...
AbstractA general set of boundary conditions at fluid-permeable interfaces between dissimilar fluid-...
International audienceA general set of boundary conditions at fluid-permeable interfaces between dis...
AbstractThe presence of interfaces (such as cracks, membranes and bi-material boundaries) in hydrate...
International audienceThis work addresses the macroscopic modeling of flow near porous media boundar...
The single-domain, Darcy-Brinkman model is applied to some analytically tractable flows through adja...
In soil chemistry or marine microbiology (for example when dealing with marine aggregates), one ofte...
AbstractSecond gradient theories have been developed in mechanics for treating different phenomena a...
For liquid-porous material interactions (LPMI), three variational principles are developed in Biot's...
We consider certain computational aspects of upscaling fluid flows through deformable porous media. ...
This chapter presents a model developed by the author, in publications dated from 2002 to 2016, on f...
International audienceSecond gradient theories have been developed in mechanics for treating differe...
Le changement d’échelle des écoulements diphasiques immiscibles dans des milieux poreux très perméab...
The analysis and simulation of the dynamics of a moving boundary between immiscible fluids in a poro...
We derive boundary conditions at the interface of a homogeneous and isotropic porous medium and an o...
A new approach to the modelling of wetting fronts in porous media on the Darcy scale is developed, b...
AbstractA general set of boundary conditions at fluid-permeable interfaces between dissimilar fluid-...
International audienceA general set of boundary conditions at fluid-permeable interfaces between dis...
AbstractThe presence of interfaces (such as cracks, membranes and bi-material boundaries) in hydrate...
International audienceThis work addresses the macroscopic modeling of flow near porous media boundar...
The single-domain, Darcy-Brinkman model is applied to some analytically tractable flows through adja...
In soil chemistry or marine microbiology (for example when dealing with marine aggregates), one ofte...
AbstractSecond gradient theories have been developed in mechanics for treating different phenomena a...
For liquid-porous material interactions (LPMI), three variational principles are developed in Biot's...
We consider certain computational aspects of upscaling fluid flows through deformable porous media. ...
This chapter presents a model developed by the author, in publications dated from 2002 to 2016, on f...
International audienceSecond gradient theories have been developed in mechanics for treating differe...
Le changement d’échelle des écoulements diphasiques immiscibles dans des milieux poreux très perméab...
The analysis and simulation of the dynamics of a moving boundary between immiscible fluids in a poro...
We derive boundary conditions at the interface of a homogeneous and isotropic porous medium and an o...
A new approach to the modelling of wetting fronts in porous media on the Darcy scale is developed, b...