Laboratory Study on the Turbulent Boundary Layers Over Wind-Waves Roughness

T. Bhirawa, Kévin, Jh Lee, J. Monty
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Abstract

A laboratory study of turbulent boundary layers over wind-generated waves using Particle Image Velocimetry (PIV) in a wind-wave flume at the University of Melbourne is presented. The experiments are taken at two different wind speeds of 5.5 and 8.5 m/s at a fetch length of 3.5 m. Two types of multi-camera measurement are specifically tailored to capture the flow behaviours. The first is a measurement with high spatial resolution, with aims of characterizing the mean velocity, surface drag and Reynolds stresses over the non-stationary surface. The second type is a large field-of-view measurement, designed to capture the large-scale turbulent motions which are directly associated with the surface-wave topography. Although the turbulent flow is developed over a non-stationary surface (i.e. wind-generated waves), it embodies similarities in both integral parameters and Reynolds stress behaviours to the turbulent flows over stationary rough surfaces. This observation could open a possibility to develop an important turbulence model as well as drag prediction over wind-generated waves, which could be closely related to stationary rough-wall boundary layers.
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湍流边界层对风浪粗糙度的室内研究
在墨尔本大学的风浪水槽中,利用粒子图像测速技术(PIV)对风浪上的湍流边界层进行了实验室研究。实验在5.5和8.5 m/s两种不同风速下进行,取风长度为3.5 m。两种类型的多相机测量是专门为捕捉流动行为而定制的。第一种是高空间分辨率的测量,目的是表征非静止表面上的平均速度、表面阻力和雷诺应力。第二种是大视场测量,旨在捕捉与表面波地形直接相关的大规模湍流运动。虽然紊流是在非平稳表面(即风浪)上发展的,但它在积分参数和雷诺应力行为上与静止粗糙表面上的紊流有相似之处。这一观测结果可能为开发一种重要的湍流模型以及风力产生的波浪的阻力预测提供可能性,这可能与静止的粗糙壁边界层密切相关。
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