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An Experimental Investigation of Acceleration-Skewed Oscillatory Flow Over Vortex Ripples

机译:涡旋涟漪加速偏斜振荡流动的实验研究

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A full-scale experimental study of acceleration-skewed oscillatory flow over vortex ripples, which is an approximation of wave-driven flow over a rippled seabed, was conducted in an oscillatory water tunnel. Three acceleration-skewed-flow tests and a reference sinusoidal-flow tests were involved in this study. In each test, two-dimensional vortex ripples were generated from a coarse-sand movable bed, and the flow field was measured with a particle image velocimetry. The dominant feature of phase-averaged flow is the generation of onshore (offshore) coherent vortices during the onshore (offshore) half-cycle. The acceleration skewness expedites the offshore-onshore flow reversal and therefore speeds up the ejection of offshore vortex, while the opposite occurs for the onshore vortex. The ripple-averaged flow is similar to the acceleration-skewed turbulent oscillatory flow over a flat bed in terms of leading Fourier harmonics, boundary layer thickness, and cycle-averaged flow, suggesting a possible analogy between the two. From the aspect of flow turbulence, acceleration skewness elongates the offshore accelerating quarter, so the turbulence embedded in the offshore vortex can be better developed. This, together with a quick ejection process, allows the offshore vortex to carry a significant amount of residual turbulence to the onshore-side ripple flank, which may even enhance the production of turbulence within the onshore half-cycle. Some results on pressure field and form drag are also presented in this paper.
机译:在振动水隧道中进行了对涡流波纹的加速偏斜振荡流量的全规模实验研究,这是波纹海底上的波浪驱动的近似。本研究涉及三种加速偏斜流动测试和参考正弦流试验。在每个测试中,从粗砂可移动床中产生二维涡旋涟漪,用颗粒图像速度测量流场。相位平均流量的主导特征是在陆上(海上)半周期期间的陆上(海上)相干涡流的产生。加速度偏斜加快了海上陆上流动逆转,因此加速了海上涡旋的喷射,而陆上涡旋相反。纹波平均流量类似于在领先的傅立叶谐波,边界层厚度和循环平均流程方面通过平板均匀的加速偏斜湍流振荡流流,这表明两者之间可能的类比。从流动湍流的方面,加速偏振伸长近海加速季,因此可以更好地开发嵌入在海上涡旋中的湍流。这与快速喷射过程一起允许离岸涡旋将大量的残余湍流携带到坐骨侧纹波侧面,这甚至可以增强陆上半循环内的湍流的产生。在本文还提出了压力场的一些结果和形成拖动。

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