Stability of buoyant-Couette flow in a vertical porous slot

B. M. Shankar, I. S. Shivakumara
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Abstract

The stability of two-dimensional buoyancy-driven convection in a vertical porous slot, wherein a plane Couette flow is additionally present, is studied. This complex fluid flow scenario is examined under the influence of Robin-type boundary conditions, which are applied to perturbations in both velocity and temperature. The inclusion of a time-derivative velocity term within the Darcy momentum equation notably introduces intricacies to the study. The stability of the basic natural convection flow is primarily governed by several key parameters namely, the P\'eclet number, the Prandtl-Darcy number, the Biot number and a non-negative parameter that dictates the nature of the vertical boundaries. Through numerical analysis, the stability eigenvalue problem is solved for a variety of combinations of boundary conditions. The outcomes of this analysis reveal the critical threshold values that signify the onset of instability. Furthermore, a detailed examination of the stability of the system has provided insights into both its commonalities and distinctions under different conditions. It is observed that, except for the scenario featuring impermeable-isothermal boundaries, the underlying base flow exhibits instability when subjected to various other configurations of perturbed velocity and temperature boundary conditions. This underscores the notion that the presence of Couette flow alone does not suffice to induce instability within the system. The plots depicting neutral stability curves show either bi-modal or uni-modal characteristics, contingent upon specific parameter values that influence the onset of instability.
垂直多孔槽中浮力-库埃特流动的稳定性
研究了垂直多孔槽中二维浮力驱动对流的稳定性,其中还存在平面库埃特流。这种复杂的流体流动情况是在罗宾型边界条件的影响下进行研究的,罗宾型边界条件适用于速度和温度的扰动。在达西动量方程中加入时间衍生速度项,为研究带来了复杂性。基本自然对流的稳定性主要受几个关键参数的制约,即 P\'eclet 数、普朗特-达西数、Biot 数和一个决定垂直边界性质的非负参数。通过数值分析,解决了各种边界条件组合下的稳定性特征值问题。分析结果揭示了标志着不稳定性开始的临界阈值。此外,通过对系统稳定性的详细研究,还深入了解了系统在不同条件下的共性和差异。研究发现,除了以不渗透等温边界为特征的情况外,底层基流在受到其他各种扰动速度和温度边界条件配置时都表现出不稳定性。这强调了一个概念,即仅仅存在库埃特流不足以引起系统的不稳定性。描述中性稳定性曲线的曲线图显示出双模态或单模态特征,这取决于影响不稳定性发生的特定参数值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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