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On Exchange Principle in Magnetohydrodynamic Triply Diffusive Convection with Viscosity Variations
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Linear stability of a triply diffusive fluid layer heated from below, which is kept under the effect of uniform vertical magnetic field, has been studied by considering variable viscosity. A sufficient condition for the occurrence of stationary convection is derived. These results are uniformly valid for quite general nature of the bounding surfaces.
Keywords
Triply Diffusive Convection, Variable Viscosity, Concentration Rayleigh Number, Stationary Convection, Chandrasekhar Number.
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