Department of Mechanical Engineering, University of the Philippines Diliman, Magsaysay Avenue, Diliman, Quezon City, Metro Manila 1101, Philippines.
Graduate School of Engineering Science, Osaka University, 1-3 Machikaneyama, Toyonaka, Osaka 560-8531, Japan.
Chaos. 2023 Jun 1;33(6). doi: 10.1063/5.0133492.
We identify the presence of three homoclinic bifurcations that are associated with edge states in a system that is governed by the full Navier-Stokes equation. In plane Couette flow with a streamwise period slightly longer than the minimal unit, we describe a rich bifurcation scenario that is related to new time-periodic solutions and the Nagata steady solution [M. Nagata, J. Fluid Mech. 217, 519-527 (1990)]. In this computational domain, the vigorous time-periodic solution (PO3) with comparable fluctuation amplitude to turbulence and the lower branch of the Nagata steady solution are considered as edge states at different ranges of Reynolds number. These edge states can help in understanding the mechanism of subcritical transition to turbulence in wall-bounded shear flows. At the Reynolds numbers at which the homoclinic bifurcations occur, we find the creation (or destruction) of the time-periodic solutions. At a higher Reynolds number, we observe the edge state switching from the lower-branch Nagata steady solution to PO3 at the creation of this vigorous cycle due to the homoclinic bifurcation. Consequently, the formation of the boundary separating the basins of attraction of the laminar attractor and the time-periodic/chaotic attractor also switches to the respective stable manifolds of the edge states, providing a change in the behavior of a typical amplitude of perturbation toward triggering the transition to turbulence.
我们确定了在由完整纳维-斯托克斯方程控制的系统中存在三种与边缘态相关的同宿分叉。在流向周期略长于最小单元的平面 Couette 流中,我们描述了一个丰富的分岔情景,该情景与新的时变解和 Nagata 定常解有关[M. Nagata, J. Fluid Mech. 217, 519-527 (1990)]。在这个计算域中,具有与湍流相当的波动幅度的剧烈时变解(PO3)和 Nagata 定常解的下分支被视为不同雷诺数范围的边缘态。这些边缘态有助于理解壁面剪切流中超临界向湍流的转迁机制。在同宿分岔发生的雷诺数下,我们发现了时变解的产生(或破坏)。在更高的雷诺数下,由于同宿分岔,我们观察到边缘态从 Nagata 定常解的下分支切换到 PO3,这是由于这个剧烈周期的产生。因此,分隔层流吸引子和时变/混沌吸引子的边界的形成也切换到边缘态的相应稳定流形,导致典型扰动幅度的行为发生变化,从而引发向湍流的转迁。