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Reactive Solute Diffusion in Boundary Layer Flow through a Porous Medium over a Permeable Flat Plate with Power-Law Variation in Surface Concentration

机译:边界层中的反应性溶质扩散在可渗透的平板上流过多孔介质,具有表面浓度的功率律变化

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摘要

The solute diffusion in boundary layer flow of an incompressible fluid through a porous medium over a porous flat plate with first-order chemical reaction and with variable surface concentration is studied. The reaction rate of the solute is also takenasvariable. The self-similar ordinary differential equations are obtained from the governing partial differential equations using similarity transformations, and then those self-similar equations are solved by shooting technique using forth-order Runge-Kutta method. The analysis shows that the velocity increases with the increase of permeability of the porous medium, whereas the concentration decreases. The thicknesses of momentum and solute boundary layers reduce for suction, and the effect of blowing is opposite. For the inverse variation of wall concentration along the surface, mass absorption at the surface is found in all cases, and in direct variation mass transfer is found. For increase of both the Schmidt number and the reaction rate parameter, the concentration as well as the solute boundary layer thickness decreases.
机译:研究了通过多孔介质在多孔平板上具有一流的化学反应和可变表面浓度的粗介质的边界层中的溶质扩散。溶质的反应速率也占用。使用相似性转换从控制局部微分方程获得自相似的常微分方程,然后通过使用射击runge-kutta方法通过拍摄技术来解决这些自我相似的等式。分析表明,随着多孔介质的渗透性的增加,速度增加,而浓度降低。动量和溶质边界层的厚度减少了吸力,吹出的效果相反。为了沿着表面的壁浓度的逆变化,在所有情况下发现表面的质量吸收,并且发现了直接变化的传质。为了增加施密特数和反应速率参数,浓度以及溶质边界层厚度降低。

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