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contributor authorS. Shateyi
contributor authorP. Sibanda
contributor authorS. S. Motsa
date accessioned2017-05-09T00:24:29Z
date available2017-05-09T00:24:29Z
date copyrightDecember, 2007
date issued2007
identifier issn0022-1481
identifier otherJHTRAO-27828#1708_1.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/136160
description abstractThe problem of steady, laminar, magnetohydrodynamic flow past a semi-infinite vertical plate is studied. The primary purpose of this study was to characterize the effects of thermal radiative heat transfer, magnetic field strength, and Hall currents on the flow properties. The governing nonlinear coupled differential equations comprising the laws of mass, linear momentum, and energy modified to include magnetic and radiative effects were solved numerically. The effects of the Hall current, the Hartmann number, and the radiative parameter on the velocity and temperature profiles are presented graphically. Large Hall currents and radiation effects cause the fluid to heat up and the velocity to increase in the lateral direction but decrease in the tangential direction. This study showed inter alia that reducing Hall currents and increasing the strength of the magnetic field lead to a reduction in the temperature and, consequently, in the thermal boundary layer, and so confirming that heat transfer mitigation through magnetic control is possible.
publisherThe American Society of Mechanical Engineers (ASME)
titleMagnetohydrodynamic Flow Past a Vertical Plate With Radiative Heat Transfer
typeJournal Paper
journal volume129
journal issue12
journal titleJournal of Heat Transfer
identifier doi10.1115/1.2767750
journal fristpage1708
journal lastpage1713
identifier eissn1528-8943
keywordsFlow (Dynamics)
keywordsHeat
keywordsTemperature
keywordsRadiative heat transfer
keywordsFluids
keywordsMagnetic fields
keywordsVertical plates
keywordsBoundary layers
keywordsHall effect
keywordsThermal boundary layers AND Heat transfer
treeJournal of Heat Transfer:;2007:;volume( 129 ):;issue: 012
contenttypeFulltext


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