{"title":"Stabilité linéaire tridimensionnelle de l'écoulement dans un divergent en rotation","authors":"Marwan Al-Farkh, Mahmoud Hamadiche","doi":"10.1016/S1251-8069(97)86947-3","DOIUrl":null,"url":null,"abstract":"<div><p>The linear temporal three-dimensional instability of incompressible viscous flow in a rotating divergent channel is studied. The boundary between stable and unstable regions is plotted as a function of the different physical parameters of the problem. It is shown that the instability is caused by the channel rotation when the half-angle of the channel, α, is small and it is caused by the channel expansion for large α. When α is taken constant, we found that rotation has the same effect as in plane channel flow, where the basic flow is destabilized by weak rotation and stabilized by strong rotation.</p></div>","PeriodicalId":100304,"journal":{"name":"Comptes Rendus de l'Académie des Sciences - Series IIB - Mechanics-Physics-Chemistry-Astronomy","volume":"326 1","pages":"Pages 13-20"},"PeriodicalIF":0.0000,"publicationDate":"1998-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1251-8069(97)86947-3","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Comptes Rendus de l'Académie des Sciences - Series IIB - Mechanics-Physics-Chemistry-Astronomy","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1251806997869473","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 linear temporal three-dimensional instability of incompressible viscous flow in a rotating divergent channel is studied. The boundary between stable and unstable regions is plotted as a function of the different physical parameters of the problem. It is shown that the instability is caused by the channel rotation when the half-angle of the channel, α, is small and it is caused by the channel expansion for large α. When α is taken constant, we found that rotation has the same effect as in plane channel flow, where the basic flow is destabilized by weak rotation and stabilized by strong rotation.