By a porous medium we mean a material consisting of a solid matrix with an interconnected
void. We suppose that the solid matrix is either rigid (the usual situation) or it undergoes …

This paper is concerned with the question of the beginning of convective motion in a fluid
saturated porous layer, containing a salt in solution, heated below and salted above and …

We discuss models for flow in a class of generalized Navier–Stokes equations. The work
concentrates on producing models for thermal convection, analysing these in detail, and …

We investigate the effects of anisotropic permeability and changing boundary conditions
upon the onset of penetrative convection in a porous medium of Darcy type and of Brinkman …

Modal and non-modal linear stability analyses are employed to investigate the effect of
internal and external heating on disturbance temporal growth for the Darcy–Bénard …

The effect of the Soret parameter on the convective stability of double diffusive convection
solely because of the viscous dissipation in a horizontal porous channel is studied. The …

We address the problem of initiation of convective motion in the case of a fluid saturated
porous layer, containing a salt in solution, which is heated and salted below. We amplify the …

The effect of viscous dissipation may be the sole cause of a thermoconvective instability
either in a fluid clear of solid material or in a fluid-saturated porous medium. Several recent …

We present a model for thermal convection in a horizontal layer rotating about a vertical axis,
when the fluid is an incompressible Navier–Stokes fluid of Fried–Gurtin–Musesti type. This …

We investigate nonlinear stability in a model for thermal convection in a saturated porous
material using Brinkman theory, taking into account viscous dissipation effects. There are (at …