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Frequency pattern of turbulent flow and sediment entrainment over ripples using image processing

机译:使用图像处理的湍流和夹杂物在波纹上的夹带频率模式

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River channel change and bed scourings are source of major environmental problem for fish and aquatic habitat. The bed form such as ripples and dunes is the result of an interaction between turbulent flow structure and sediment particles at the bed. The structure of turbulent flow over ripples is important to understand initiation of sediment entrainment and its transport. The focus of this study is the measurement and analysis of the dominant bursting events and the flow structure over ripples in the bed of a channel. Two types of ripples with sinusoidal and triangular forms were tested in this study. The velocities of flow over the ripples were measured in three dimensions using an Acoustic Doppler Velocimeter with a sampling rate of 50 Hz. These velocities were measured at different points within the flow depth from the bed and at different longitudinal positions along the flume. A CCD camera was used to capture 1500 sequential images from the bed and to monitor sediment movement at different positions along the bed. Application of image processing technique enabled us to compute the number of entrained and deposited particles over the ripples. From a quadrant decomposition of instantaneous velocity fluctuations close to the bed, it was found that bursting events downstream of the second ripple, in Quadrants 1 and 3, were dominant whereas upstream of the ripple, Quadrants 2 and 4 were dominant. More importantly consideration of these results indicates that the normalized occurrence probabilities of sweep events along the channel are in phase with the bed forms whereas those of ejection events are out of phase with the bed form. Therefore entrainment would be expected to occur upstream and deposition occurs downstream of the ripple. These expectations were confirmed by measurement of entrained and deposited sediment particles from the bed. These above information can be used in practical application for rivers where restoration is required.
机译:河道变化和河床冲刷是鱼类和水生生境的主要环境问题的根源。诸如波纹和沙丘之类的床形是湍流结构与床处沉积物颗粒相互作用的结果。湍流在涟漪上的流动结构对于理解沉积物夹带的开始及其传输非常重要。这项研究的重点是测量和分析主要爆发事件以及河床波纹中的流动结构。在这项研究中测试了两种正弦和三角形形式的波纹。使用声学多普勒测速仪以50 Hz的采样率在三个维度上测量了波纹上的流速。这些速度是在离床的流深范围内的不同点处以及沿水槽的不同纵向位置处测得的。 CCD摄像机用于从床中捕获1500个连续图像,并监视沿床不同位置的沉积物运动。图像处理技术的应用使我们能够计算出波纹上夹带和沉积颗粒的数量。从靠近床层的瞬时速度波动的象限分解中发现,在象限1和3中,第二个波纹下游的爆发事件占主导,而在象素上游,象限2和4则占主导地位。更重要的是,对这些结果的考虑表明,沿通道的扫掠事件的归一化发生概率与床形同相,而喷射事件的归一化概率与床形异相。因此,预期会在波纹的上游发生夹带而在波纹的下游发生沉积。通过测量床中夹带的和沉积的沉积物颗粒,证实了这些期望。以上这些信息可用于需要修复的河流的实际应用中。

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