2023
DOI: 10.37934/arfmts.102.1.7384
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MHD Mixed Convective Non-Newtonian Stagnation Point Flow Over an Inclined Stretching Sheet: Numerical Simulation

Abstract: This paper includes numerical simulation upon MHD mixed convective heat transfer properties of stagnation point flow across an angled stretched sheet. Boundary value problem is solved using similarity transformation approach with shooting technique. The impact of different corporeal constraints like mixed convection parameter, thermal radiation parameter, chemical reaction parameter, Brownian motion and thermophoresis, Casson parameter upon velocity and temp profile as well as skin-friction coefficient , Nusse… Show more

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Cited by 4 publications
(1 citation statement)
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“…They develop a plate without any inclination from any axis. The fluid flows over an inclined sheet were reported for the MHD model [8][9][10][11][12] are with these controlling factors: when the fluid state is unsteady [8], with the Newtonian heating effect [9], the fluid model considers the free convection flow [10], the fluid is bounded by the slip condition [11], with the presence of porous medium [11,13], or when the stagnation point is existed in the fluid flow [12]. The boundary layer flow bounded by an inclined sheet observes the characteristics of the fluid flow when the sheet can be displaced by a certain angle by the same origin point, instead of the static sheet.…”
Section: Introductionmentioning
confidence: 99%
“…They develop a plate without any inclination from any axis. The fluid flows over an inclined sheet were reported for the MHD model [8][9][10][11][12] are with these controlling factors: when the fluid state is unsteady [8], with the Newtonian heating effect [9], the fluid model considers the free convection flow [10], the fluid is bounded by the slip condition [11], with the presence of porous medium [11,13], or when the stagnation point is existed in the fluid flow [12]. The boundary layer flow bounded by an inclined sheet observes the characteristics of the fluid flow when the sheet can be displaced by a certain angle by the same origin point, instead of the static sheet.…”
Section: Introductionmentioning
confidence: 99%