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首页> 外文期刊>International Journal of Heat and Mass Transfer >Darcy-Benard-Marangoni convection in porous media
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Darcy-Benard-Marangoni convection in porous media

机译:多孔介质中的Darcy-Benard-Marangoni对流

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The onset of coupled Darcy-Benard-Marangoni convection in a liquid saturated porous layer of high permeability of practical importance is investigated by employing the Brinkman-Forchheimer- Lapwood-extended Darcy flow model with fluid viscosity different from effective viscosity. The lower boundary is taken to be rigid and insulating to temperature perturbations, while the upper surface is open to atmosphere and subject to a general thermal condition. The critical eigenvalues are obtained numerically, in general, using Galerkin method. However, closed form solution is also obtained using regular perturbation technique for insulated boundaries. Besides, the eigenvalue problem is solved exactly for pure Darcy-Marangoni convection. The numerical and analytical results are found to be in excellent agreement with each other. It is observed that the effect of buoyancy is destabilizing, while an increase in the permeability parameter is to delay the onset of convection. The Biot number and the ratio of effective viscosity to fluid viscosity are found to increase the critical conditions. Some known results are recovered as special cases.
机译:通过使用流体粘度不同于有效粘度的Brinkman-Forchheimer-Lapwood扩展Darcy流动模型,研究了在具有实际重要性的高渗透性液体饱和多孔层中达西-贝纳德-马朗戈尼耦合对流的开始。下边界被认为是刚性的并且对温度扰动是绝缘的,而上表面对大气开放并且经受一般的热条件。通常,使用Galerkin方法以数值方式获得临界特征值。但是,也可以使用规则的扰动技术来获得封闭边界的封闭形式解。此外,对于纯达西-马朗戈尼对流,本征值问题得到了精确解决。发现数值和分析结果彼此非常吻合。观察到浮力的作用是不稳定的,而渗透率参数的增加是为了延迟对流的发生。发现比奥数和有效粘度与流体粘度之比增加了临界条件。一些特殊情况会恢复一些已知结果。

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