流体颗粒悬浮液嵌入非达西多孔介质中拉伸表面的磁流体边界层流动和传热数值解

B.J. Gireesha , B. Mahanthesh , P.T. Manjunatha , R.S.R. Gorla
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引用次数: 75

摘要

本文研究了非达西多孔介质中导电尘埃流体在非定常拉伸表面上的边界层流动和传热问题。采用基于Darcy-Forchheimer的模型描述了多孔介质中的流动。流场和温度场的不稳定性是由于拉伸速度和表面温度随时间的变化而引起的。同时考虑了热辐射、粘性耗散和热源/汇不均匀等因素的影响。通过适当的相似变换,将控制流动和传热的相关时变方程简化为一组非线性常微分方程。利用四五阶龙格-库塔-费贝格法对变换后的方程进行数值积分。通过几个图分析了不同物理参数对两相速度和温度分布的影响。作为本研究的特殊情况,所得到的数值结果与先前发表的结果相比较,结果很好地吻合。研究发现,在洁净流体中悬浮细尘颗粒可以减小热边界层厚度。因此,在涉及冷却过程的工程和科学应用中,含尘流体是优选的。
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Numerical solution for hydromagnetic boundary layer flow and heat transfer past a stretching surface embedded in non-Darcy porous medium with fluid-particle suspension

This paper investigates the problem of MHD boundary layer flow and heat transfer of an electrically conducting dusty fluid over an unsteady stretching surface through a non-Darcy porous medium. The flow in porous medium is described by employing the Darcy–Forchheimer based model. The unsteadiness in the flow and temperature fields are because of time-dependent stretching velocity and surface temperature. The effect of thermal radiation, viscous dissipation and non-uniform heat source/sink are also taken into account. The pertinent time-dependent equations, governing the flow and heat transfer are reduced into a set of non-linear ordinary differential equations with the aid of suitable similarity transformations. The transformed equations are numerically integrated using fourth–fifth order Runge–Kutta–Fehlberg method. The effects of various physical parameters on the velocity and temperature profiles of both phases are analyzed through several plots. Obtained numerical results are compared and found to be in good agreement with previously published results as special cases of the present investigation. It is found that, by suspending fine dust particles in the clean fluid reduces the thermal boundary layer thickness. Therefore, the dusty fluids are preferable in engineering and scientific applications, involving cooling processes.

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