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Experimental study of air-water turbulent flow structures on stepped spillways

机译:阶梯溢洪道上空气水湍流结构的试验研究

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Stepped chute flows are characterized by intense turbulence and strong flow aeration, but most studies did not investigate the turbulence characteristics. In this study, highly turbulent air-water flows skimming down a large-size stepped chute were systematically investigated. An experimental study of detailed air-water flow properties measurements were introduced in different types of flow regimes on a stepped chute (θ = 21.8°, h = 0.04 m, l = 0.10 m) model to investigate the location and the flow depth at inception point of air entrainment and velocity profiles distributions. Detailed velocity and turbulence intensity measurements in flow direction were performed by use of a phase detection conductivity probe which was designed, developed and calibrated by writers. The results showed that the turbulence characteristics vary in different regions. The study showed further that the turbulence intensity increases rapidly close to the step bottom at the viscous sub layer and maximized for 0.4 ≤ y/dc ≤ 0.5 at intermediate region then decreases gradually in the upper region. It is hypothesized that the high turbulence levels in the intermediate region were caused by the continuous deformations and modification of the air-water interfacial structure.
机译:阶梯状斜槽气流的特征是强烈的湍流和强劲的气流,但大多数研究并未研究湍流特性。在这项研究中,系统地研究了从大型阶梯式溜槽上掠过的高度湍流的空气水流。在阶梯式溜槽(θ= 21.8°,h = 0.04 m,l = 0.10 m)模型上,在不同类型的流态下进行了详细的空气-水流动特性测量的实验研究,以研究位置和流动深度在空气夹带和速度剖面分布的起始点。通过使用由作者设计,开发和校准的相位检测电导率探头,可以对流向进行详细的速度和湍流强度测量。结果表明,湍流特性在不同区域有所不同。研究进一步表明,湍流强度在粘性子层的台阶底部附近迅速增加,并在0.4≤处最大。 y / dc≤在中间区域的0.5,然后在上部区域逐渐减小。假设中间区域的湍流水平较高是由于空气-水界面结构的连续变形和变型引起的。

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