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High-resolution flow characterization close to the sediment-water interface in a run of the river reservoir

机译:河流水库运行过程中靠近沉积物-水界面的高分辨率流量表征

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A bistatic high-resolution acoustic profiler was used in order to characterize the lowermost boundary layer of a run of the river reservoir. The profiler allows determining the statistics of the three-dimensional flow field at a single point (sweet spot) as well as the measurement of the time averaged flow velocity profiles at 1 mm resolution around the sweet spot. Therefore, in addition to the flow statistics provided by single point acoustic Doppler profilers, mixing coefficients as well as production of turbulent kinetic energy can be calculated using a single device. Fitting of semiempirical relations to observed cospectra allowed eliminating artifacts as they result from coordinate system rotation during calculation of Reynolds stress profiles at millimeter resolution. While most parameters showed characteristics of a constant stress layer, length scales indicated anisotropy of the turbulent flow. Under these anisotropic near wall conditions, we found that the use of the commonly accepted Kolmogorov constants for the determination of dissipation rates using the inertial dissipation method is not valid any more. Instead, these constants vary with distance from the sediment water interface. We provide evidence that coefficients determined by numerical simulations are the appropriate choice also in field applications. In addition we resolved the viscous boundary layer close to the sediment-water interface in high resolution (1 mm) profiles and identified a double logarithmic layer above 1.5 cm at one location. The discrepancy of the scales as well as the double logarithmic layer suggests the existence of roughness elements upstream of the measurement sites.
机译:为了描述河流水库段的最低边界层,使用了双基地高分辨率声廓线仪。剖析器允许确定单个点(最佳点)上三维流场的统计数据,以及在最佳点周围以1毫米分辨率测量时均流速曲线。因此,除了单点声学多普勒剖面仪提供的流量统计信息外,还可以使用单个设备来计算混合系数以及湍动能的产生。将半经验关系拟合到观测到的共谱可以消除伪影,因为它们是在毫米分辨率的雷诺应力分布计算过程中由坐标系旋转产生的。尽管大多数参数都显示出恒定应力层的特征,但长度标度表明了湍流的各向异性。在这些各向异性的近壁条件下,我们发现使用惯性耗散法确定耗散率的常用公认Kolmogorov常数已不再有效。相反,这些常数随距沉积物水界面的距离而变化。我们提供的证据表明,在现场应用中,通过数值模拟确定的系数也是合适的选择。此外,我们以高分辨率(1 mm)剖面解析了靠近沉积物-水界面的粘性边界层,并在一个位置识别了1.5 cm以上的双对数层。标尺以及双对数层的差异表明在测量部位的上游存在粗糙度元素。

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