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Morphodynamic processes downstream of man-made structural interventions: Experimental investigation of the role of turbulent flow structures in the prediction of scour downstream of a rigid bed

机译:人为结构干预的下游流体动力学过程:湍流结构在预测刚性床下游冲刷中的作用的实验研究

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Experimental program was conducted to analyze scour - caused by a horizontal jet downstream of a rigid bed - and the flow velocity and turbulence characteristics within the scour hole. The experimental program was motivated by the fact that the knowledge of flow field, including turbulent characteristics, is fundamental to correctly simulate the bed-load transport and the temporal evolution of the scour hole and, thus, to define protective measures of scouring. In this paper some results of experiments - carried out to understand the role of flow turbulence in the prediction of scouring process and sediment movement - are reported. The analysis is conducted on the basis of detailed measurements of flow velocity at various sections in the scour hole region. Both a 2D LDA anemometer and an acoustic velocimeter profiler (DOP2000) were used to conduct the velocity measurements. The results show that the flow is characterized by alternating high-low speed fluid regions which lead to the formation of vertical turbulent coherent structures. The turbulent intensity assumes significant values along longitudinal planes (i.e. parallel to the flow direction) in the near-bank zones. Maps documenting the correlations between the vertical and the longitudinal turbulent intensities are shown. With the aid of the experimental data, a relationship between the bed shear stress and the volume of sand eroded is defined. The quadrant analysis is applied for the qualitative description of the turbulent events. Analysis indicates that the major turbulent activity occurs in the deepest region of the scour hole. It seems that sweep and ejection events, which correspond to positive production of the turbulent energy, play an important role in erosion and transport of the sediment particles.
机译:进行了实验程序来分析冲刷(由刚性床下游的水平射流引起)以及冲刷孔内的流速和湍流特性。实验程序的动机是这样的事实,即流场的知识(包括湍流特性)是正确模拟床层载荷传输和冲刷孔的时间演变并因此确定冲刷保护措施的基础。在本文中,报告了一些实验结果,这些实验是为了了解流动湍流在预测冲刷过程和泥沙运动中的作用而进行的。该分析是基于对冲孔区域各个部分的流速的详细测量进行的。二维LDA风速计和声速计轮廓仪(DOP2000)均用于进行速度测量。结果表明,流动的特征是交替出现高低速流体区域,从而导致垂直湍流相干结构的形成。在近岸区域中,湍流强度沿纵向平面(即,平行于流动方向)具有显着的值。显示了记录垂直和纵向湍流强度之间相关性的地图。借助实验数据,确定了床层剪切应力与被侵蚀的砂粒之间的关系。象限分析用于湍流事件的定性描述。分析表明,主要的湍流活动发生在冲刷孔的最深区域。似乎与湍流能量的正产生相对应的扫掠和喷射事件在沉积物颗粒的侵蚀和运输中起着重要作用。

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