Abstract
The thermosolutal convection in a layer of electrically conducting Oldroyd fluid heated and soluted from below in porous medium is considered to include the effect of a uniform vertical magnetic field. The magnetic field and stable solute gradient are found to have stabilizing effects whereas the medium permeability is shown to have a destabilizing effect. For stationary convection, the Oldroyd fluid behaves like a Newtonian fluid. The sufficient conditions for the nonexistence of overstability are obtained.
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