The linear and weakly nonlinear stability analysis of the quiescent state in a viscoelastic fluid subject to vertical solute concentration and temperature gradients is investigated. The non-Newtonian behavior of the viscoelastic fluid is characterized using the Oldroyd model. Analytical expressions for the critical Rayleigh numbers and corresponding wave numbers for the onset of stationary or oscillatory convection subject to cross diffusion effects is determined. A stability diagram clearly demarcates non-overlapping regions of finger and diffusive instabilities. A Lorenz system is obtained in the case of the weakly nonlinear stability analysis. The effect of Dufour and Soret parameters on the heat and mass transports are determined and di...
The linear stability of a viscoelastic fluid saturated densely packed horizontal porous layer heated...
This paper deals linear and weak nonlinear stability analysis of double-diffusive convection in an a...
The stability of the conduction regime of natural convection in a porous vertical slab saturated wit...
The triple diffusive convection in an Oldroyd-B fluid-saturated porous layer is investigated by perf...
The nonlinear stability of stationary and oscillatory double-diffusive convection in an Oldroyd-B fl...
International audienceA linear stability analysis of a plane Couette flow in the presence of an unst...
The onset and stability of a triple cross-diffusive viscoelastic fluid layer is investigated. The rh...
Based oil a modified Darcy-Brinkman-Oldroyd model, linear and nonlinear thermal stability analyses o...
Following the insight of P. Kolodner (J. Non-Newtonian Fluid Mech. 75 (1998) 167)on DNA solutions, a...
The stability of a binary viscoelastic fluid-saturated porous layer which is heated from below is st...
The stability of a binary viscoelastic fluid-saturated porous layer which is heated from below is st...
The onset and stability of a triple cross-diffusive viscoelastic fluid layer is investigated. The rh...
The onset and stability of a triple cross-diffusive viscoelastic fluid layer is investigated. The rh...
AbstractWe report theoretical and numerical results on thermal convection of a magnetic fluid in a v...
We report theoretical and numerical results on thermal convection of a magnetic fluid in a viscoelas...
The linear stability of a viscoelastic fluid saturated densely packed horizontal porous layer heated...
This paper deals linear and weak nonlinear stability analysis of double-diffusive convection in an a...
The stability of the conduction regime of natural convection in a porous vertical slab saturated wit...
The triple diffusive convection in an Oldroyd-B fluid-saturated porous layer is investigated by perf...
The nonlinear stability of stationary and oscillatory double-diffusive convection in an Oldroyd-B fl...
International audienceA linear stability analysis of a plane Couette flow in the presence of an unst...
The onset and stability of a triple cross-diffusive viscoelastic fluid layer is investigated. The rh...
Based oil a modified Darcy-Brinkman-Oldroyd model, linear and nonlinear thermal stability analyses o...
Following the insight of P. Kolodner (J. Non-Newtonian Fluid Mech. 75 (1998) 167)on DNA solutions, a...
The stability of a binary viscoelastic fluid-saturated porous layer which is heated from below is st...
The stability of a binary viscoelastic fluid-saturated porous layer which is heated from below is st...
The onset and stability of a triple cross-diffusive viscoelastic fluid layer is investigated. The rh...
The onset and stability of a triple cross-diffusive viscoelastic fluid layer is investigated. The rh...
AbstractWe report theoretical and numerical results on thermal convection of a magnetic fluid in a v...
We report theoretical and numerical results on thermal convection of a magnetic fluid in a viscoelas...
The linear stability of a viscoelastic fluid saturated densely packed horizontal porous layer heated...
This paper deals linear and weak nonlinear stability analysis of double-diffusive convection in an a...
The stability of the conduction regime of natural convection in a porous vertical slab saturated wit...