Extension of classical stability theory to viscous planar wall-bounded shear flows

被引:7
|
作者
Lee, Harry [1 ]
Wang, Shixiao [2 ]
机构
[1] Univ Michigan, Dept Math, Ann Arbor, MI 48109 USA
[2] Univ Auckland, Dept Math, Auckland 1142, New Zealand
关键词
instability control; boundary layer stability; vortex dynamics; NONLINEAR STABILITY; ENERGY-DISSIPATION; LAYER;
D O I
10.1017/jfm.2019.629
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
A viscous extension of Arnold's inviscid theory for planar parallel non-inflectional shear flows is developed and a viscous Arnold's identity is obtained. Special forms of the viscous Arnold's identity have been revealed that are closely related to the perturbation's enstrophy identity derived by Synge (Proceedings of the Fifth International Congress for Applied Mechanics, 1938, pp. 326-332, John Wiley) (see also Fraternale et al., Phys. Rev. E, vol. 97, 2018, 063102). Firstly, an alternative derivation of the perturbation's enstrophy identity for strictly parallel shear flows is acquired based on the viscous Arnold's identity. The alternative derivation induces a weight function. Thereby, a novel weighted perturbation's enstrophy identity is established, which extends the previously known enstrophy identity to include general streamwise translation-invariant shear flows. Finally, the validity of the enstrophy identity for parallel shear flows is rigorously examined and established under global nonlinear dynamics imposed with two classes of wall boundary conditions. As an application of the enstrophy identity, we quantitatively investigate the mechanism of linear instability/stability within the normal modal framework. The investigation reveals a subtle interaction between a critical layer and its adjacent boundary layer, which determines the stability nature of the disturbance. As an implementation of the relaxed wall boundary conditions imposed for the enstrophy identity, a control scheme is proposed that transitions the wall settings from the no-slip condition to the free-slip condition, through which a flow is stabilized quickly in an early stage of the transition.
引用
收藏
页码:1134 / 1162
页数:29
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