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Magnetohydrodynamic unsteady natural convective flow in a porous medium over a moving infinite cylinder

机译:Magnetohydrodynamic unsteady natural convective flow in a porous medium over a moving infinite cylinder

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摘要

The effect of the magnetic field on the unsteady natural convective one‐dimensional laminar flow of an incompressible viscous and slightly electrically conducting fluid over a vertical cylinder is investigated analytically. The cylinder is assumed to be embedded in a porous medium, and it moves with a uniform velocity along the vertically upward direction. The boundary layer flow equations are converted to a non‐dimensional form using appropriate non‐dimensional parameters, and the closed‐form solutions are obtained using the Laplace transform method. Fluid velocity depends on radial distance, time, magnetic parameter, Grashof number, permeability parameter, and Prandtl number. Graphical and tabulated results of the fluid velocity profile and shear stress based on the analytical solutions are presented and discussed. The analytical solution reveals that the unsteady fluid velocity tends to a steady state at a large time. The present study demonstrates that increased porosity leads to enhancement in the fluid velocity, whereas the transverse magnetic field resists the fluid velocity. Furthermore, the absolute value of shear stress decreases with a decrease in porosity of the medium or an increase in magnetic field effect.
机译:不稳定的磁场的影响自然对流的特色维层流不可压缩粘性的和略导电流体在一个垂直的气缸是调查分析。缸被认为是嵌入在多孔媒介,它以统一的运动速度沿垂直向上的方向。边界层流动方程转化为一个非维使用适当的形式非高尺寸参数和封闭的形式解决方案是使用拉普拉斯获得变换方法。径向距离、时间、磁参数,格拉晓夫数、渗透性参数和普朗特数。流体的速度分布和剪切应力根据分析提出了解决方案和讨论。不稳定的流体速度一般在一个大的时间稳定状态。表明,孔隙度会增加增强的流体速度,而横向磁场抵抗液体速度。剪切应力随下降而减小孔隙介质或磁场的增加场效应。

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