The mechanism of long-wave instability in a shear-thinning film flow on a porous substrate

被引:8
|
作者
Millet, S. [1 ]
Usha, R. [2 ]
Button, V [1 ,3 ]
Rousset, E. [4 ]
机构
[1] Univ Lyon, Univ Lyon 1, INSA Lyon, Lab Mecan Fluides & Acoust UMR CNRS 5509,Ecole Ce, F-69621 Lyon, France
[2] Indian Inst Technol Madras, Dept Math, Chennai 600036, Tamil Nadu, India
[3] Univ Euromediterraneenne Fes, INSA Euromediterranee, Route Meknes,BP51, Fes, Morocco
[4] Univ Lyon, CNRS, INSA Lyon, UMR5008,CETHIL, F-69621 Villeurbanne, France
关键词
LINEAR-STABILITY; POISEUILLE FLOW; FLUID-FLOW; EVOLUTION; PLANE;
D O I
10.1007/s00707-019-02376-0
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
A linear stability analysis of a thin shear-thinning film with a deformable top surface flowing down an inclined porous substrate modelled as a smooth substrate with velocity slip at the wall is examined, and the physical mechanism for the long-wave instability is analysed. Through a phenomenological model, the influence of slip velocity and the shear-thinning rheology on the wave speed of long surface waves on a non-Newtonian shear-thinning film down a substrate with velocity slip is predicted. The viscosity disturbance plays a significant role in the destabilization of the flow system. Indeed, slip at the bottom that accounts for the characteristics of the porous/rough substrate does not affect the physical mechanism of the instability. However, it is shown that slip at the bottom enhances the inertia effects which in turn destabilizes the flow system at smaller Reynolds numbers.
引用
收藏
页码:2201 / 2220
页数:20
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