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LABORATORY MEASUREMENT OF SUSPENDED SEDIMENT CONCENTRATION IN SURF ZONE WITH CT CONCENTRATION METER

机译:用CT浓度计实验室测量地带悬浮泥沙浓度。

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摘要

Organized eddies generated by wave breaking have an important role on sediment transport in surf zones. In order to clarify the characteristics of intermittent sediment clouds generated by vertically-oriented eddies, the Computed Tomography (CT) technique was applied for a laboratory experiment to capture instantaneous two-dimensional distributions of suspended sediment concentration in a near-bottom horizontal plane. The Extended Bayesian Method with a smoothing filter as the prior information model was applied to obtain the optimum solution of the distribution. A specification test showed that concentration distribution was reproduced fairly well. Successive images of concentration distribution due to wave breaking were obtained and movements of sediment clouds were investigated. Concentration at the center of the measuring area was simultaneously measured for verification by a conventional optical forward-transmission-type sedimentmeter. It was found that horizontal distribution of suspended sediment concentration in a surf zone is quite inhomogeneous and the high concentration regions are formed as they indicate separated sediment clouds. Distinctive patterns of sediment clouds were observed in a relatively small number of trials. The length scale of the clouds was found to be in the order of the water depth. The primary cause of sediment cloud formation can be considered sediment pickup by intermittent eddies generated by wave breaking.
机译:波浪破碎产生的有组织的涡流对冲浪区的泥沙输送具有重要作用。为了阐明垂直方向涡流产生的间歇性泥沙云的特征,计算机断层扫描(CT)技术被用于实验室实验,以捕获近底水平面中悬浮泥沙浓度的瞬时二维分布。应用以平滑滤波器为先验信息模型的扩展贝叶斯方法来获得分布的最优解。规格测试表明浓度分布再现良好。获得了由于波浪破碎引起的浓度分布的连续图像,并研究了沉积物云的运动。同时测量在测量区域中心的浓度,以通过常规的光学正向透射型沉降计进行验证。发现海浪区悬浮泥沙浓度的水平分布非常不均匀,并且高浓度区域形成,因为它们表示分离的泥沙云。在相对较少的试验中观察到沉积物云的独特模式。发现云的长度尺度为水深的顺序。沉积物云形成的主要原因可以认为是波浪破碎产生的间歇性涡流吸收了沉积物。

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