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Effect of vortex formation on sediment transport at dual pipe intakes

机译:双管道进气口涡流形成对沉积物输运的影响

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Vortex formation and subsequent sediment transport into the intake due to sea water withdrawal is one of the problems in coastal engineering. The effect of vortex formation on rate of sediment transport at coastal dual pipe intakes was investigated using a scaled physical model. Experiments were performed on dual pipe intakes at three common intake withdrawal directions (vertical, horizontal and with angle of 45 ° ). In eachexperiment, the class of vortex with respect to its strength was determined. Particle tracking velocimetry (PTV) was employed to measure tangential velocity of vortices. Results indicated that the rate of sediment transport was considerably affected by the strength of formed vortices. The rate of transported sediment was increased by increasing the strength of formed vortex. Moreover, amount of sediment transport was affected by angle of pipe intakes. It could be concluded that the minimum and maximum rates of sediment transport occur for inclined and horizontal intakes, respectively.
机译:涡流的形成以及随后由于海水的抽出而将沉积物运入进水口,是沿海工程中的问题之一。使用缩放的物理模型研究了涡流形成对沿海双管进水口泥沙输送速率的影响。实验是在三个常见的进气口撤回方向(垂直,水平和45°角)上进行的双管进气口实验。在每个实验中,确定相对于其强度的涡流类别。粒子跟踪测速法(PTV)用于测量涡旋切线速度。结果表明,沉积物的传输速度受形成的涡旋强度的影响很大。通过增加形成的涡流强度,增加了泥沙的输送速度。此外,输沙量受管道入口角度的影响。可以得出结论,分别在倾斜和水平进水口出现最小和最大的泥沙输送速率。

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