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Onset of surface-tension-driven convection in superposed layers of fluid and saturated porous medium

机译:流体和饱和多孔介质叠加层中表面张力驱动的对流的发生

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摘要

The onset of surface-tension-driven convection is studied in a two-layer system comprising an incompressible fluid-saturated porous layer over which lies a layer of the same fluid. The lower rigid surface of the porous layer is either perfectly heat conducting or insulating, while the upper heat insulating fluid boundary is free and at which the surface tension effects are allowed for. At the contact surface between the fluid-saturated porous medium and the adjacent bulk fluid, both Beavers-Joseph and the Jones conditions are employed. The resulting eigenvalue problem is solved exactly. Besides, analytical expression for the critical Marangoni number is obtained for insulating boundaries by using regular perturbation technique. The effect of variation of different physical parameters on the onset of Marangoni convection is investigated in detail. It is found that the parameter ζ, the ratio of the thickness of the fluid layer to that of the porous layer, has a profound effect on the stability of the system.
机译:在两层系统中研究了表面张力驱动的对流的发生,该系统包括不可压缩的流体饱和多孔层,该流体层上铺有一层相同的流体。多孔层的下部刚性表面是完全导热的或绝热的,而上部绝热流体的边界是自由的,并且允许表面张力作用。在流体饱和的多孔介质与相邻的块状流体之间的接触表面上,采用了比弗斯-约瑟夫(Beavers-Joseph)和琼斯(Jones)条件。由此产生的特征值问题得到了精确解决。此外,通过使用常规的扰动技术,获得了用于绝缘边界的临界Marangoni数的解析表达式。详细研究了不同物理参数的变化对马兰戈尼对流爆发的影响。发现参数ζ,即流体层的厚度与多孔层的厚度之比,对系统的稳定性有深远的影响。

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