{"title":"Stability of buoyant-Couette flow in a vertical porous slot","authors":"B. M. Shankar, I. S. Shivakumara","doi":"arxiv-2312.04270","DOIUrl":null,"url":null,"abstract":"The stability of two-dimensional buoyancy-driven convection in a vertical\nporous slot, wherein a plane Couette flow is additionally present, is studied.\nThis complex fluid flow scenario is examined under the influence of Robin-type\nboundary conditions, which are applied to perturbations in both velocity and\ntemperature. The inclusion of a time-derivative velocity term within the Darcy\nmomentum equation notably introduces intricacies to the study. The stability of\nthe basic natural convection flow is primarily governed by several key\nparameters namely, the P\\'eclet number, the Prandtl-Darcy number, the Biot\nnumber and a non-negative parameter that dictates the nature of the vertical\nboundaries. Through numerical analysis, the stability eigenvalue problem is\nsolved for a variety of combinations of boundary conditions. The outcomes of\nthis analysis reveal the critical threshold values that signify the onset of\ninstability. Furthermore, a detailed examination of the stability of the system\nhas provided insights into both its commonalities and distinctions under\ndifferent conditions. It is observed that, except for the scenario featuring\nimpermeable-isothermal boundaries, the underlying base flow exhibits\ninstability when subjected to various other configurations of perturbed\nvelocity and temperature boundary conditions. This underscores the notion that\nthe presence of Couette flow alone does not suffice to induce instability\nwithin the system. The plots depicting neutral stability curves show either\nbi-modal or uni-modal characteristics, contingent upon specific parameter\nvalues that influence the onset of instability.","PeriodicalId":501275,"journal":{"name":"arXiv - PHYS - Mathematical Physics","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2023-12-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Mathematical Physics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2312.04270","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
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.