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Analytical approach to heat and mass transfer in MHD free convection from amoving permeable vertical surface

机译:MHD在自由对流中从可渗透垂直面移动的传热传质的解析方法

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An analytical study is performed on heat and mass transfer in MHD-free convection from a moving permeable vertical surface and the results are compared with previous works on this phenomenon to test the validity. The coupled equations of boundary layer are transformed from their non-linear form to ordinary form using similarity transformation and then are solved by a newly developed method, homotopy analysis method. Having different base functions, homotopy analysis method provides us with great freedom in choosing the solution of a nonlinear problem. Solving the boundry layer equations, the effects of different parameters such as magnetic field strength parameter (M), Prandtl number (Pr), Schmidt number (Sc), buoyancy ratio and suction/blowing parameter (f_w) on velocity, temperature, and concentration profiles are taken into consideration. Obtained results show that increment of magnetic field strength parameter (M) leads to decrease in velocity profile.
机译:对无MHD对流从移动的可渗透垂直表面进行传热和传质进行了分析研究,并将结果与​​该现象的先前工作进行了比较,以检验其有效性。使用相似变换将边界层的耦合方程从其非线性形式转换为普通形式,然后通过新开发的同伦分析方法进行求解。同质分析方法具有不同的基本函数,为我们提供了选择非线性问题解的极大自由。求解边界层方程,磁场强度参数(M),普朗特数(Pr),施密特数(Sc),浮力比和吸气/吹气参数(f_w)等不同参数对速度,温度和浓度的影响配置文件被考虑在内。所得结果表明,磁场强度参数(M)的增加导致速度分布减小。

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