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.
Cite this article:
Jyoti Prakash, Rajeev Kumar, Vinod Kumar. On Exchange Principle in Magnetohydrodynamic Triply Diffusive Convection with viscosity variations. Research J. Engineering and Tech. 6(1): Jan.-Mar. 2015 page 01-05. doi: 10.5958/2321-581X.2015.00001.X