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Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows

机译:砾石河道水流双倍平均速度分布对数层的参数化

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摘要

The logarithmic layer of double-averaged (in time and space) streamwise velocity profiles obtained from field measurements made in the Swiss rivers, Venoge and Chamberonne is parameterized and discussed. Velocity measurements were made using a 3D Acoustic Doppler Velocity Profiler. Both riverbeds are hydraulically rough, composed of coarse gravel, with relative submergences (h/D_(50)) of 5.25 and 5.96, respectively. From the observations, the flow may be divided into three different layers: a roughness layer near the bed, an equivalent logarithmic layer and a surface or outer layer. It was found that a logarithmic law can describe the double-averaged profiles in the layer 0.30 < z/h < 0.75. The parameterization of the logarithmic law is discussed. Special emphasis is given to the geometric parameters roughness and zero-displacement heights and to the equivalent von Karman constant.
机译:对在瑞士河,维诺日河和钱伯纳河上进行的野外测量获得的双倍平均(在时间和空间上)的水流速度分布的对数层进行参数化和讨论。使用3D声学多普勒速度剖面仪进行速度测量。两个河床都是水力粗糙的,由粗糙的砾石组成,相对淹没度(h / D_(50))分别为5.25和5.96。根据观察结果,流可分为三个不同的层:靠近床层的粗糙层,等效的对数层和表面或外层。发现对数定律可以描述层0.30

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