Add to ORKGIn this paper, the effect of suspended particles on thermal convection of incompressible Rivlin-Ericksen elastico-viscous fluid in a porous medium is considered. For the porous medium, the Brinkman model is employed. By applying normal mode analysis method, the dispersion relation has been derived and solved analytically. It is observed that the medium permeability, suspended particles, gravity field and viscoelasticity introduce oscillatory modes. For stationary convection, it is observed that the Darcy number has stabilizing effect whereas the suspended particles and medium permeability has destabilizing effects on the system. The effects of suspended particles, Darcy number and medium permeability has also been shown graphically to depic...
The thermal instability of a Kuvshiniski viscoelastic fluid is considered to include the effects of ...
In the present note, we have considered the problem of the onset of convection in a couple-stress fl...
The stability of a horizontal fluid saturated sparsely packed porous layer heated from below and coo...
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 in an incompressible Rivlin-E...
In this paper, the double diffusive convection of Non- NewtonianWalters’B ′ viscoelastic fluid with ...
The thermosolutal stability of a layer of the Rivlin-Ericksen fluid in a porous medium is considered...
The instability of plane interface between two superposed Rivlin-Ericksen elastico-viscous fluids sa...
A layer of a Rivlin-Ericksen elastico-viscous fluid heated and soluted from below in the presence of...
Thermal instability in a horizontal layer of Oldroydian visco-elastic fluid in a porous medium is in...
Convection induced by the selective absorption of radiation in a porous medium is studied analytical...
none1noThis chapter contains a review of the thermoconvective instabilities that may occur in a flui...
On the basis of Brinkman model, the onset of double-diffusive (thermosolutal) convection with a reac...
AbstractAn incompressible Oldroydian viscoelastic fluid layer heated and soluted from below in the p...
Abstract The thermosolutal convection in Walters B ’ heterogeneous viscoelastic fluid through Brinkm...
The thermal instability of a Kuvshiniski viscoelastic fluid is considered to include the effects of ...
In the present note, we have considered the problem of the onset of convection in a couple-stress fl...
The stability of a horizontal fluid saturated sparsely packed porous layer heated from below and coo...
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 in an incompressible Rivlin-E...
In this paper, the double diffusive convection of Non- NewtonianWalters’B ′ viscoelastic fluid with ...
The thermosolutal stability of a layer of the Rivlin-Ericksen fluid in a porous medium is considered...
The instability of plane interface between two superposed Rivlin-Ericksen elastico-viscous fluids sa...
A layer of a Rivlin-Ericksen elastico-viscous fluid heated and soluted from below in the presence of...
Thermal instability in a horizontal layer of Oldroydian visco-elastic fluid in a porous medium is in...
Convection induced by the selective absorption of radiation in a porous medium is studied analytical...
none1noThis chapter contains a review of the thermoconvective instabilities that may occur in a flui...
On the basis of Brinkman model, the onset of double-diffusive (thermosolutal) convection with a reac...
AbstractAn incompressible Oldroydian viscoelastic fluid layer heated and soluted from below in the p...
Abstract The thermosolutal convection in Walters B ’ heterogeneous viscoelastic fluid through Brinkm...
The thermal instability of a Kuvshiniski viscoelastic fluid is considered to include the effects of ...
In the present note, we have considered the problem of the onset of convection in a couple-stress fl...
The stability of a horizontal fluid saturated sparsely packed porous layer heated from below and coo...