Boundary-layer separation and adverse pressure gradient for 2-D viscous incompressible flow

被引:29
作者
Ghil, M
Liu, JG
Wang, C
Wang, SH
机构
[1] Indiana Univ, Dept Math, Bloomington, IN 47405 USA
[2] Indiana Univ, Inst Sci Comp & Appl Math, Bloomington, IN 47405 USA
[3] Ecole Normale Super, Dept Terre Atmosphere Ocean, F-75231 Paris, France
[4] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
[5] Univ Maryland, Inst Phys Sci & Technol, Dept Math, College Pk, MD 20742 USA
[6] Univ Tennessee, Dept Math, Knoxville, TN 37996 USA
基金
美国国家科学基金会;
关键词
divergence-free vector fields; structural bifurcation Navier-Stokes equations; boundary layer separation; adverse pressure gradient; driven-cavity flow;
D O I
10.1016/j.physd.2004.06.012
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
We study the detailed process of bifurcation in the flow's topological structure for a two-dimensional (2-D) incompressible flow subject to no-slip boundary conditions and its connection with boundary-layer separation. The boundary-layer separation theory of M. Ghil, T. Ma and S. Wang, based on the structural-bifurcation concept, is translated into vorticity form. The vorticity formulation of the theory shows that structural bifurcation occurs whenever a degenerate singular point for the vorticity appears on the boundary; this singular point is characterized by nonzero tangential second-order derivative and nonzero time derivative of the vorticity. Furthermore, we prove the presence of an adverse pressure gradient at the critical point, due to reversal in the direction of the pressure force with respect to the basic shear flow at this point. A numerical example of 2-D driven-cavity flow, governed by the Navier Stokes equations, is presented; boundary-layer separation occurs, the bifurcation criterion is satisfied, and an adverse pressure gradient is shown to be present. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:149 / 173
页数:25
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