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contributor authorRahman, M. M.
date accessioned2017-05-09T01:30:45Z
date available2017-05-09T01:30:45Z
date issued2016
identifier issn0022-1481
identifier otherht_138_12_122503.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/161716
description abstractIn this paper, we investigate the effects of secondorder slip and magnetic field on the nonlinear mixed convection stagnationpoint flow toward a vertical permeable stretching/shrinking sheet in an upper convected Maxwell (UCM) fluid with variable surface temperature. Numerical results are obtained using the bvp4c function from matlab for the reduced skinfriction coefficient, the rate of heat transfer, the velocity, and the temperature profiles. The results indicate that multiple (dual) solutions exist for a buoyancy opposing flow for certain values of the parameter space irrespective to the types of surfaces whether it is stretched or shrinked. It is found that an applied magnetic field compensates the suction velocity for the existence of the dual solutions. Depending on the parametric conditions; elastic parameter, magnetic field parameter, firstand secondorder slip parameters significantly controls the flow and heat transfer characteristics. The illustrated streamlines show that for upper branch solutions, the effects of stretching and suction are direct and obvious as the flow near the surface is seen to suck through the permeable sheet and drag away from the origin of the sheet. However, aligned but reverse flow occurs for the case of lower branch solutions when the mixed convection effect is less significant.
publisherThe American Society of Mechanical Engineers (ASME)
titleEffects of Second Order Slip and Magnetic Field on Mixed Convection Stagnation Point Flow of a Maxwellian Fluid: Multiple Solutions
typeJournal Paper
journal volume138
journal issue12
journal titleJournal of Heat Transfer
identifier doi10.1115/1.4034161
journal fristpage122503
journal lastpage122503
identifier eissn1528-8943
treeJournal of Heat Transfer:;2016:;volume( 138 ):;issue: 012
contenttypeFulltext


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