Abstract
Thermal convection in multi-component fluid has wide applications in industrial, ionospheric and geothermal systems. The effect of Coriolis force on Soret driven ferrothermohaline convection in densely packed anisotropic porous medium has been studied. A linear stability analysis is carried out using normal mode technique. It is found that stationary mode is favorable for Darcy model and oscillatory instability is studied. The porous medium is assumed to be variable and the effect of permeable parameter and vertical anisotropy are to destabilize the system. The non-buoyancy magnetization and Soret effects are found to stabilize the system in consideration with anisotropy of the system. The results are depicted graphically.
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