后向台阶与边界层过渡中横流不稳定性的相互作用。

Jenna L. Eppink, R. Wlezien, R. King, Meelan Choudhari
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引用次数: 18

摘要

在低速流动中,研究了带压力梯度的掠板模型,以确定后向台阶对静止横流主导流动转捩的影响。对边界层流动进行了详细的热线测量,以研究由于阶跃高度为局部无扰动边界层厚度的49%而导致的上游转移。后向台阶情况下,初始平稳横流幅值的增大导致过渡锋上游运动。阶跃使平稳横流不稳定性的增长局部增加,但过渡阶段的平稳横流幅值足够低(<0.04Ue),因此平稳横流不是过渡的唯一原因。台阶下游的非定常速度谱在80 ~ 1500 hz范围内具有丰富的非定常扰动。根据相速度和波角确定了三种不同的扰动,即高度斜向扰动(可能类似于行横流),类似于tollmien - schlicht波的扰动和剪切层不稳定性。定常横流扰动引起非定常扰动的调制,导致非定常扰动幅值出现空间集中的峰值。这种非定常扰动的调制被认为是过渡锋上游运动并增加定常横流幅值的原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Interaction of a Backward-Facing Step and Crossflow Instabilities in Boundary-Layer Transition.
A swept flat plate model with an imposed pressure gradient was experimentally investigated in a low-speed flow to determine the effect of a backward-facing step on transition in a stationary crossflow-dominated flow. Detailed hotwire measurements of boundary-layer flow were performed to investigate the upstream shift in transition due to a step height of 49% of the local unperturbed boundary-layer thickness. Increasing the initial stationary crossflow amplitude caused an upstream movement of the transition front for the backward-facing step case. The step caused a local increase in the growth of the stationary crossflow instabilities, but the stationary crossflow amplitude at transition was sufficiently low (<0.04Ue ) so that stationary crossflow was not solely responsible for transition. The unsteady velocity spectra downstream of the step were rich with unsteady disturbances in the 80- to 1500-Hz range. Three distinct families of disturbances were identified based on phase speed and wave angle, namely, a highly oblique disturbance (possibly traveling-crossflow-like), a Tollmien-Schlichting-wave-like disturbance, and a shear-layer instability. The stationary crossflow disturbances caused a modulation of the unsteady disturbances, resulting in spatially concentrated peaks in unsteady disturbance amplitude. This modulation of the unsteady disturbances is believed to be the reason for the upstream movement of the transition front with increasing stationary crossflow amplitude.
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