Transient MHD Radiative Fluid Flow over an Inclined Porous Plate with Thermal and Mass Diffusion: An EFDM Numerical Approach

Abstract

This research aims to delve into the transient MHD flow over a porous plate having an inclination, with heat and mass diffusion by taking the radiative phenomenon into consideration. The flow controlling equations of continuity, momentum, energy, and concentration are developed using the boundary layer approximations. The radiative flux is described using a differential approximation. The governing time-dependent equations are brought into a conversion to create a system of non-dimensional partial differential equations (PDEs). Numerical schemes approaching the explicit finite difference method (EFDM) are employed to discretize and reckon the equations in dimensional agreement. Stability and convergence checking are prepared to ensure the converging restrictions of pertinent parameters. The profiles of velocity, concentration, and temperature have been illustrated graphically and discussed comprehensively.

A Numerical Investigation of Hydro-Magnetic Mixed Convection Flow of Viscous Dissipative Fluid in a Channel Filled with Porous Material

“…The MHD convection flow of Casson fluid in micro-channels including porous material was discussed by Gireesha and Sindhu [22]. When Noor et al [23] used network simulation method solutions to analyze time-dependent hydro-magnetic radiative fluid flow over an inclined porous plate with heat and mass permeability, they found that the fluid momentum tended to rise or fall gradually towards the plate and then diminish or grow slowly away from the plate. The temperature of the fluid has been reported to exhibit the same tendency.…”

Significance of Viscous Dissipation on Hydromagnetic Oscillatory Flow Affected by Nanoparticles Through a Boundary Layer Regime

“…The MHD convection flow of Casson fluid in micro-channels including porous material was discussed by Gireesha and Sindhu (2020). When Alam et al (2021) used network simulation method solutions to analyze time-dependent hydro-magnetic radiative fluid flow over an inclined porous plate with heat and mass permeability, they found that the fluid momentum tended to rise or fall gradually towards the plate and then diminish or grow slowly away from the plate. The temperature of the fluid has been reported to exhibit the same tendency.…”