The thermosolutal stability of a layer of the Rivlin-Ericksen fluid in a porous medium is considered under varying gravity conditions. It is found that for stationary convection, medium permeability and suspended particles have a destabilizing/stabilizing effect when gravity increases/decreases. The stable solute gradient has a stabilizing effect on the system
The stability of convection in a horizontal porous layer which is saturated with fluid and induced b...
The effect of time-periodic vertical gravity modulation on the onset of thermosolutal convection in ...
AbstractAn incompressible Oldroydian viscoelastic fluid layer heated and soluted from below in the p...
In this paper, the effect of suspended particles on thermal convection of incompressible Rivlin-Eric...
In this paper, the effect of suspended particles on thermal convection of incompressible Rivlin-Eric...
A layer of a Rivlin-Ericksen elastico-viscous fluid heated and soluted from below in the presence of...
The instability of plane interface between two superposed Rivlin-Ericksen elastico-viscous fluids sa...
The effect of a non-uniform basic temperature gradient on the onset of convection driven by surface ...
The problem of double- diffusive hydro magnetic instability of Walter’s (Model B’) visco-elastic flu...
The effects of a non-uniform temperature gradient and magnetic field on the onset of convection driv...
ABSTRACT: Free convection and mass transfer flow of a viscous incompressible fluid past a uniformly...
In the present note, we have considered the problem of the onset of convection in a couple-stress fl...
The problem treated is that of convection in a fluid saturated porous layer, heated internally and w...
Abstract: An attempt has been made to investigate the thermosolutal convection of a heterogeneous Ri...
Steady thermosolutocapillary instabilities in a horizontal thin fluid layer with deformable free sur...
The stability of convection in a horizontal porous layer which is saturated with fluid and induced b...
The effect of time-periodic vertical gravity modulation on the onset of thermosolutal convection in ...
AbstractAn incompressible Oldroydian viscoelastic fluid layer heated and soluted from below in the p...
In this paper, the effect of suspended particles on thermal convection of incompressible Rivlin-Eric...
In this paper, the effect of suspended particles on thermal convection of incompressible Rivlin-Eric...
A layer of a Rivlin-Ericksen elastico-viscous fluid heated and soluted from below in the presence of...
The instability of plane interface between two superposed Rivlin-Ericksen elastico-viscous fluids sa...
The effect of a non-uniform basic temperature gradient on the onset of convection driven by surface ...
The problem of double- diffusive hydro magnetic instability of Walter’s (Model B’) visco-elastic flu...
The effects of a non-uniform temperature gradient and magnetic field on the onset of convection driv...
ABSTRACT: Free convection and mass transfer flow of a viscous incompressible fluid past a uniformly...
In the present note, we have considered the problem of the onset of convection in a couple-stress fl...
The problem treated is that of convection in a fluid saturated porous layer, heated internally and w...
Abstract: An attempt has been made to investigate the thermosolutal convection of a heterogeneous Ri...
Steady thermosolutocapillary instabilities in a horizontal thin fluid layer with deformable free sur...
The stability of convection in a horizontal porous layer which is saturated with fluid and induced b...
The effect of time-periodic vertical gravity modulation on the onset of thermosolutal convection in ...
AbstractAn incompressible Oldroydian viscoelastic fluid layer heated and soluted from below in the p...