Finite amplitude oscillatory convection in a rotating Rivlin-Ericksen ferrofluid layer with variable viscosity
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This study explores the onset of oscillatory convection, bifurcation structure, and heat trans- port in a rotating viscoelastic ferrofluid layer, where the viscoelastic model is described by Rivlin-Ericksen (RE) constitutive equations, and the viscosity varies with applied magnetic field. Motivated by applications such as magnetic drug targeting with ferrofluid carriers in a viscoelastic bloodstream under an external magnetic field, as well as in aerospace, cool- ing, and biomedical systems, the analysis yields critical Rayleigh numbers and wavenumbers for both stationary and oscillatory modes, with the latter identified as the preferred mode. Weakly nonlinear theory is employed to analyze bifurcation behavior, leading to a complex Ginzburg–Landau amplitude equation solved numerically. Heat transport is quantified via the Nusselt number( N s ), expressed in terms of the nonlinear convection amplitude. The results reveal that the Coriolis force ( Ta n ) significantly alters the flow structure and stabilizes the system. The viscoelasticity parameter f v exhibits a twofold influence, as it does not affect the stationary onset threshold, but it significantly impacts the nature of the bifurcation, which can be either supercritical or subcritical, depending strongly on its value. Compared to the non-rotating, constant-viscosity case, the combined action of fv , M 1 , and Ta n ampli- fies convective strength and heat transfer, whereas stronger magnetic field-dependent (MFD) viscosity reduces thermal transport effciency. The evolution of heat transport is further exam- ined through isotherm plots. The formulation is validated through excellent agreement with classical limiting cases and existing results from prior studies.