In this paper, the length scales included both in rate-dependent single phase materials and in coupled problems such as saturated and partially saturated porous media where the viscous terms are introduced naturally by the fluid mass balance equations, are discussed. The viscous effects in the two problems are quite different and the internal length scales hence have different expressions. Also the wave speeds have different relationships with the wave number
Seismic waves propagating in porous rocks saturated with two immiscible fluids can be strongly atten...
A theory of wave propagation in isotropic poroelastic media saturated by two immiscible Newtonian fl...
International audience[1] In porous rocks saturated in patches by two immiscible fluids, seismic com...
In this paper, the length scales included both in rate-dependent single phase materials and in coupl...
In this paper, a length scale included in multiphase materials such as saturated and partially satur...
The paper analyses the interaction between two internal length scales during dynamic strain localiza...
Following the work by Zhang et al. [Mech. Cohes.-Frict. Mater. Struct. 4 (1999) 443] we discuss some...
Wave propagation in saturated porous media is investigated in the framework of two models, a theoret...
The (THM) coupling effects on the dynamic wave propagation and strain localization in a fully satura...
This paper is devoted to the analysis of the fluid-solid interaction in dynamic strain localisation ...
It is well known that both rate dependent and gradient-dependent constitutive models introduce inter...
The mixture theory of fluid-saturated porous media involves three types of couplings: mechanical, th...
Wave propagation in saturated porous media involves complicated couplings between the solid skeleton...
The dynamic interaction between a rigid porous structure (porosity f) and its saturating fluid is st...
The displacement of two fluids in a porous medium can be affected by a viscous fingering instability...
Seismic waves propagating in porous rocks saturated with two immiscible fluids can be strongly atten...
A theory of wave propagation in isotropic poroelastic media saturated by two immiscible Newtonian fl...
International audience[1] In porous rocks saturated in patches by two immiscible fluids, seismic com...
In this paper, the length scales included both in rate-dependent single phase materials and in coupl...
In this paper, a length scale included in multiphase materials such as saturated and partially satur...
The paper analyses the interaction between two internal length scales during dynamic strain localiza...
Following the work by Zhang et al. [Mech. Cohes.-Frict. Mater. Struct. 4 (1999) 443] we discuss some...
Wave propagation in saturated porous media is investigated in the framework of two models, a theoret...
The (THM) coupling effects on the dynamic wave propagation and strain localization in a fully satura...
This paper is devoted to the analysis of the fluid-solid interaction in dynamic strain localisation ...
It is well known that both rate dependent and gradient-dependent constitutive models introduce inter...
The mixture theory of fluid-saturated porous media involves three types of couplings: mechanical, th...
Wave propagation in saturated porous media involves complicated couplings between the solid skeleton...
The dynamic interaction between a rigid porous structure (porosity f) and its saturating fluid is st...
The displacement of two fluids in a porous medium can be affected by a viscous fingering instability...
Seismic waves propagating in porous rocks saturated with two immiscible fluids can be strongly atten...
A theory of wave propagation in isotropic poroelastic media saturated by two immiscible Newtonian fl...
International audience[1] In porous rocks saturated in patches by two immiscible fluids, seismic com...