Abstract
The subject under consideration finds manifold applications across various disciplines, including biological, industrial, and environmental sectors. Therefore, this study aims to analytically investigate the onset of convective instability in a dusty ferromagnetic fluid layer, influenced by magnetic field-dependent viscosity and fluid-permeable magnetically active boundaries, when subjected to a uniform transverse magnetic field. The eigenvalue problem is formulated through the utilization of linear stability theory followed by normal mode analysis. To address this problem, a single-term Galerkin method is employed, followed by a numerical calculation of the critical magnetic Rayleigh number. It is investigated numerically and graphically that (Nc)Free ≤ (Nc)permeable ≤ (Nc)Rigid. It has been observed that as the dust particle parameter h1 increase, the critical Rayleigh number decreases, indicating the destabilizing nature of h1 On the other hand, the viscosity parameter δ and magnetic susceptibility χ and permeability parameter Das demonstrate a stabilizing effect on the system. Initially, measure of nonlinearity of magnetization M3 exhibits a destabilizing effect, but beyond a certain threshold, it switches to a stabilizing effect within the system.