DOI: 10.1515/cppm-2026-0241 ISSN: 1934-2659

Hall current, ion-slip and chemical reaction effects on unsteady MHD Casson fluid flow past an isothermal vertical plate in a rotating system with ramped mass diffusion and entropy generation analysis

Shashi Kumar Cherupally, G. Naga Malleswari, Phani Yedlapalli

Abstract

An exact analytical solution is developed for unsteady magnetohydrodynamic (MHD) flow of a Casson fluid past an impulsively started isothermal vertical plate in a rotating system, incorporating Hall current, ion-slip current, first-order chemical reaction, ramped wall concentration, and viscous dissipation. The coupled momentum, energy and species equations are reduced via a complex-velocity formulation and solved exactly by the Laplace transform; the inverse transform is evaluated numerically using the Gaver–Stehfest algorithm (degree 22), whose convergence is demonstrated to 6–7 significant figures and whose accuracy is confirmed against an independent finite-difference solution of the governing PDEs, with maximum absolute deviation of 1.7 × 10 −6 in the primary velocity over the domain tested. A previously undocumented physical mechanism is identified: secondary (cross) flow persists even in the absence of rotation ( R  = 0) whenever Hall current is present ( m  ≠ 0), and vanishes only when both R  = 0 and m  = 0 jointly, showing that Hall current alone, not only Coriolis rotation, generates transverse flow in this configuration. The local entropy generation number Ns and Bejan number Be are derived explicitly and evaluated: near the wall, heat-transfer irreversibility dominates (Be ≈ 0.67–0.92 for Br = 0.2–1.0), while fluid-friction irreversibility takes over within one boundary-layer unit as Br increases. A quantitative Casson-versus-Newtonian comparison ( β  = 0.5 vs. β  → ∞) shows the yield-stress effect thickens the boundary layer by 58.5 % and, contrary to simple-diffusion intuition, increases the magnitude of the wall velocity gradient by 13.4 % at t  = 0.5, since buoyancy and Lorentz/Coriolis forcing prevent the thicker layer from simply flattening the near-wall slope. These results provide the first quantitatively validated entropy-generation and Bejan-number analysis for this parameter combination and clarify a Hall-current-driven transport mechanism not previously isolated in the literature.

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