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arXiv 2304.03499physics.flu-dyn

各向异性且非均匀多孔层位于流体层下方的非等温平面库埃特流的线性稳定性分析

Linear stability analysis of non-isothermal plane Couette flow in an anisotropic and inhomogeneous porous layer underlying a fluid layer

Nandita Barman, Anjali Aleria, Premananda Bera

AI总结:

本文对流体层下方各向异性非均匀多孔层中的平面库埃特流进行线性稳定性分析,利用 Darcy 模型和 Chebyshev 配点法求解,发现非均匀性、深度比等参数显著影响系统稳定性及中性曲线模态特征。

摘要:

本文对位于流体层下方的多孔层中的平面库埃特流进行了线性稳定性分析,其中多孔层是各向异性且非均匀的。平面库埃特流由上板的均匀运动引起,而由于上下板之间维持温差,从而产生了对流。所考虑的流体是牛顿流体且不可压缩。使用 Darcy 模型描述多孔层中的流动,并在交界面处使用 Beavers-Joseph 条件。采用 Chebyshev 配点法求解广义特征值问题。本文研究了多孔介质的各向异性和非均匀性,以及流体层与多孔层厚度比(即深度比 $(\hat{d})$)、Reynolds 数 $(Re)$ 和 Darcy 数 $(δ)$ 的影响。分析主要针对水进行;然而,通过改变 Prandtl 数 ($Pr$),也研究了各向异性和非均匀性对不同流体的影响。根据参数值的不同,得到了中性曲线的单峰(多孔模式或流体模式)、双峰(多孔模式和流体模式)以及三峰(多孔模式、流体模式和多孔模式)特性。非均匀参数或深度比的增加,或者各向异性参数、Reynolds 数、Prandtl 数和 Darcy 数的减小,会提高系统的不稳定性。对于 $δ=0.002$、$Pr=6.9$ 和 $Re=10$,无论各向异性和非均匀参数如何,当 $\hat{d}<0.07$ 时总是观察到多孔模式占主导,当 $\hat{d}>0.21$ 时则流体模式占主导。借助能量收支分析,对不稳定性类型进行了分类,并验证了从线性稳定性分析中获得的模式类型。此外,还可视化了二次流模式以理解流动动力学。

英文摘要:

This paper carries out a linear stability analysis of a plane Couette flow in a porous layer underlying a fluid layer where the porous layer is anisotropic and inhomogeneous. The plane Couette flow is induced due to the uniform movement of the upper plate and convection arises due to the maintenance of the temperature difference between the upper plate and the lower plate. The fluid considered is Newtonian and incompressible. Darcy model is used to narrate the flow in the porous layer and at the interface, the Beavers-Joseph condition is used. The Chebyshev collocation method is used to solve the generalized eigenvalue problem. Here, the effect of anisotropy and inhomogeneity of the porous medium, along with the ratio of the thickness of fluid to porous layer, i.e., depth ratio $(\hat{d})$, Reynolds number $(Re)$ and Darcy number $(δ)$ are studied. The analysis is carried out majorly for water; however, the impact of anisotropy and inhomogeneity on different fluids by varying Prandtl number ($Pr$) is also studied. Depending on the value of parameters, the unimodal (porous mode or fluid mode), bimodal (porous mode and fluid mode) and also trimodal (porous mode, fluid mode and porous mode) nature of the neutral curve is obtained. The increasing value of the inhomogeneity parameter, depth ratio or decreasing value of the anisotropy parameter, Reynolds number, Prandtl number and Darcy number raises the system instability. For $δ=0.002$, $Pr=6.9$ and $Re=10$, dominating nature of porous mode is always observed for $\hat{d}<0.07$, and fluid mode for $\hat{d}>0.21$ irrespective of anisotropy and inhomogeneity parameter. With the help of energy budget analysis, the types of instability are categorized and also the types of mode obtained from linear stability analysis are verified. Secondary flow patterns are also visualized to understand the flow dynamics.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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