多孔平板后的涡流脱落与流动方向一致

M. Cicolin, S. Chellini, B. Usherwood, B. Ganapathisubramani, Ian P. Castro
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摘要

本研究探讨了在雷诺数 $Re = UD/\nu$($U$为进入速度,$\nu$为运动粘度)介于 15 000 和 70 000 之间的中等范围内,在宽度固定为 $D$ 的名义上为二维的矩形板经过时,板体孔隙率对尾流的影响。孔隙率 $\beta$ 定义为板的开口面积与总面积之比,可以确定的是,随着孔隙率的增加,尾流会从周期性的 von Kármán 甩流行为转变为不存在涡流甩流的状态。这种变化会影响作用在板上的流体力,尤其是阻力,没有涡流脱落的尾流阻力会明显降低。我们使用热线风速测量法、粒子图像测速法和力测量法对这两种状态之间的过渡进行了实验分析。通过相干性和相位测量,我们可以根据尾流两侧两个主要剪切层的速度波动来确定是否存在有规律的周期性涡流脱落。结果表明,与 $Re$ 无关,当 $\beta 0.3$ 时,湍流表现出经典的卡尔曼涡流脱落模式。在中间范围($0.2<\beta <0.3$)内,存在一个以前从未发现过的过渡机制;其特点是间歇性脱落。流动在涡旋脱落和非脱落模式之间随机交替,观察到涡旋脱落的总时间比例(间歇性)随着孔隙度的增加而减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Vortex shedding behind porous flat plates normal to the flow
This work examines the influence of body porosity on the wake past nominally two-dimensional rectangular plates of fixed width $D$ in the moderate range of Reynolds numbers $Re = UD/\nu$ (with $U$ the incoming velocity and $\nu$ the kinematic viscosity) between 15 000 and 70 000. With porosity $\beta$ defined as the ratio of open to total area of the plate, it is well established that as porosity increases, the wake shifts from the periodic von Kármán shedding behaviour to a regime where this vortex shedding is absent. This change impacts the fluid forces acting on the plate, especially the drag, which is significantly lower for a wake without vortex shedding. We analyse experimentally the transition between these two regimes using hot-wire anemometry, particle-image velocimetry and force measurements. Coherence and phase measurements are used to determine the existence of regular, periodic vortex shedding based on the velocity fluctuations in the two main shear layers on either side of the wake. Results show that, independent of $Re$ , the wake exhibits the classical Kármán vortex shedding pattern for $\beta <0.2$ but this is absent for $\beta >0.3$ . In the intermediate range, $0.2<\beta <0.3$ , there is a transitional regime that has not previously been identified; it is characterised by intermittent shedding. The flow alternates randomly between a vortex shedding and a non-shedding pattern and the total proportion of time during which vortex shedding is observed (the intermittency) decreases with increasing porosity.
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