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A field study of transport and mixing in a river using an Acoustic Doppler Velocity Profiler

机译:声速度分析器的河流运输与混合的田间研究

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A 3-D Acoustic Doppler Velocity Profiler (ADVP) is used for measuring closely spaced profiles across the river Poisine (on a straight river reach with mean water depth h ≈ 0.5 m, width B ≈ 12m, flat gravel bed with estimated D_(50) ≈ 6 cm). The mean streamwise velocity profiles show logarithmic profiles all across the half section, decreasing towards the bank. Most of the three turbulence intensities profiles between the center (y/B = 0.5) and y/B = 0.24 agree relatively well with laboratory profiles. Closer to the bank (y/B < 0.24) strong deviations in the profile form indicate "side-wall" effects. A cumulant discard method is applied and conditional statistics and conditional sampling are used to compare the experimental relative covariance contributions from the four quadrants. In the center (y/B = 0.5), all quadrant distributions correspond to those observed in laboratory open-channel flow. Near the bank (y/B = 0.04), significant differences between the results for different depths occur in all planes. Thus, the flow near the bank cannot be considered two-dimensional.
机译:3-D声学多普勒速度分析器(ADVP)用于测量河流泊滨的紧密间隔的曲线(在平均水深H≈0.5M,宽度B≈12M,扁平砾石床,估计D_(50 )≈6cm)。平均流动速度配置文件显示半部分的对数型材,朝向银行减少。中心(Y / B = 0.5)和Y / B = 0.24之间的三个三种湍流强度曲线与实验室型材相对较好。靠近堤岸(Y / B <0.24)轮廓形式的强偏差表明“侧壁”效果。应用累积丢弃方法,使用条件统计和条件采样来比较四象限的实验相对协方差贡献。在中心(Y / B = 0.5)中,所有象限分布对应于在实验室开放式流动中观察到的象限分布。靠近银行(Y / B = 0.04),在所有平面中发生不同深度的结果之间的显着差异。因此,银行附近的流不能被认为是二维的。

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