Abstract
AbstractThe effects of wall velocity and radiating Coriolis force (CF) on convective flow over a moving porous vertical plate in a rotating fluid due to a magnetic field and viscous dissipation have been investigated. Assume that the resiliency impact emerges from a combination of concentration and temperature. Utilizing the convenient affinity renovations, the nonlinear partial differential equations are renewed into ordinary differential equations, which are solved numerically by a resourceful shooting technique using the Range–Kutta–Fehlberg scheme. The results are inspected and illustrated graphically for a choice of stream factors on the speed, warmth, and concentration profiles, as well as the shear and couple pressures and the rates of heat and mass exchange at the plate. It can be noted that the reading of the CF reveals that the temperature and concentration fields show opposing tendencies to the velocity profiles. The heat and concentration fields decrease with increasing wall velocity, but the velocity profiles react in the opposite direction. The goal of this review is to determine the impacts of Coriolis and wall velocity causes in terms of geography, which are the deflection of airplanes, winds, missiles, and currents in the ocean. Moreover, the effects of Coriolis power are given more attention in practical designs and applications of rotating systems imposed through flow.
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