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Unsteady Magnetohydrodynamic Heat Transfer in a Semi-Infinite Porous Medium with Thermal Radiation Flux: Analytical and Numerical Study

机译:具有热辐射通量的半无限多孔介质中的非稳态磁流体动力传热:分析和数值研究

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摘要

The unsteady, buoyancy-induced, hydromagnetic, thermal convection flow in a semi-infinite porous regime adjacent to an infinite hot vertical plate moving with constant velocity, is studied in the presence of significant thermal radiation. The momentum and energy conservation equations are normalized and then solved using both the Laplace transform technique and Network Numerical Simulation. Excellent agreement is obtained between both analytical and numerical methods. An increase in Hartmann number (M~2) strongly decelerates the flow and for very high strength magnetic fields (M~2 = 20), the flow is reversed after a short time interval. The classical velocity overshoot is also detected close to the plate surface for low to intermediate values of M~2 at both small and large times; however this overshoot vanishes for larger strengths of the transverse magnetic field (M~2 = 10). An increase in radiation-conduction parameter (K_r) significantly increases temperature throughout the porous regime at both small and larger times, adjacent to the plate, but decreases the shear stress magnitudes at the plate. Temperature gradient is reduced at the plate surface for all times, with a rise in radiation-conduction parameter (K_r). Shear stress is reduced considerably with an increase in Darcian drag parameter (K_p).
机译:在存在大量热辐射的情况下,研究了在无限无限热垂直板附近以恒定速度运动的半无限多孔状态下的非稳态浮力诱导的水磁热对流。对动量和能量守恒方程进行归一化,然后使用拉普拉斯变换技术和网络数值模拟求解。在分析和数值方法之间都获得了极好的一致性。 Hartmann数(M〜2)的增加会极大地降低流量,并且对于非常高强度的磁场(M〜2 = 20),流量会在较短的时间间隔后反转。在较小和较大的时间,对于低到中等的M〜2值,还可以在板表面附近检测到经典的速度过冲。但是,对于较大的横向磁场强度(M〜2 = 10),此过冲消失。辐射传导参数(K_r)的增加会在较小和较大的时间内(与板相邻)在整个多孔状态下显着提高温度,但会减小板处的剪应力大小。随着辐射传导参数(K_r)的增加,板表面的温度梯度一直降低。剪切应力随着Darcian阻力参数(K_p)的增加而大大降低。

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  • 来源
    《Advances in numerical analysis》 |2011年第1期|p.304124.1-304124.17|共17页
  • 作者单位

    Department of Engineering and Mathematics, Sheaf Building,Sheffield Hallam University, Sheffield SI 1WB, UK;

    Thermal Engineering and Fluids Department, Technical University of Cartagena,Campus Muralla del Mar, 30202 Cartagena, Spain;

    Department of Mathematics, Narajole Raj College, P.O. Narajole, Midnapore 721 211, WB, India;

    Institute for Advanced Studies, Tehran 14456-63543, Iran;

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