A layer of compressible, rotating, elastico-viscous fluid of related density heated & soluted from below is considered in the presence of vertical magnetic field to include the effect of Hall currents. Dispersion relation governing the effect of visco-elasticity, salinity gradient, rotation, magnetic field and Hall currents is derived. For the case of stationary convection, the Rivlin-Erickson ...

Elastrco-vrscous fluids, m particular the model characterrzed by Walters [l] (hqmd B’), exhibit a close resemblance to real fluids hke olls and certam hrgh polymer solutrons One of the important aspects of any fluid 1s the behavror of its unsteady boundary layers A large number of papers concernmg the time-dependent flows of elastrco-viscous hqmd B' have appeared m the literature, for example, ...