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Local Scour at Downstream Sloped Submerged Weirs

机译:下游倾斜水下堰的局部冲刷

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摘要

This paper presents an experimental study of local scour at submerged weirs with different downstream slopes. Thirty-three tests of coarse sand (d(50) = 0.85 mm) and 24 tests of fine sand (d(50) = 0.26 mm) were carried out in a sand-recirculating flume. The tests for each sand type used four weirs with different downstream weir slopes (pi/6, pi/4, pi/3, and pi/2 to horizontal for the fine sand; pi/12, pi/6, pi/4, and pi/2 to horizontal for the coarse sand). The results show that the upstream scour depth is independent of the downstream weir slope beta. For both sand types, the downstream weir slope has no effect on the downstream scour depth when it is greater than the upstream slope of the downstream scour hole theta. For beta theta, the downstream weir surface is partly exposed to flow, resulting in a downstream scour depth at the weir surface d(w), which can be increased by the increase in either downstream scour depth or theta. In this situation, the upstream water level rises because of the reduced flow cross-section area, and the overflow jet is deflected to be approximately aligned with the downstream weir surface. For the coarse sand tests, when beta = pi/6, the effect of the rising upstream water level is predominant because beta is close to theta(a) (time-averaged value of theta). This results in larger downstream scour depths. When beta is considerably smaller than theta(a), the effect of jet deflection starts to be predominant in the coarse sand tests, generating lower downstream scour depths when U-0/U-c 2.6. Those two effects balance each other when 2.6 U-0/U-c 3.1 for beta = pi/12, resulting in the same downstream scour depths as those for a rectangular weir. For the fine sand tests, the jet deflection effect is predominant because the downstream weir slope has limited effect on the upstream water level. A conservative design method accounting for both effects is proposed for the local scour at downstream sloped submerged weirs. (C) 2018 American Society of Civil Engineers.
机译:本文对不同下游坡度的淹没堰进行了局部冲刷试验研究。在循环砂槽中进行了33次粗砂试验(d(50)= 0.85 mm)和24次细砂试验(d(50)= 0.26 mm)。每种砂的测试均使用了四个堰,这些堰具有不同的下游堰坡度(对于细砂,pi / 6,pi / 4,pi / 3和pi / 2相对于水平方向为水平; pi / 12,pi / 6,pi / 4, pi / 2为水平(对于粗砂)。结果表明,上游冲刷深度与下游堰角β无关。对于这两种类型的砂,当下游堰的坡度大于下游冲孔θ的上游坡度时,下游堰的坡度对下游冲孔深度没有影响。对于β<θ,下游堰表面部分地暴露于流动,导致在堰表面d(w)处的下游冲刷深度,该下游冲刷深度可以通过下游冲刷深度或θ的增加而增加。在这种情况下,由于水流横截面面积的减小,上游水位上升,溢流射流转向与下游堰表面大致对准。对于粗砂试验,当beta = pi / 6时,上游水位上升的影响最为明显,因为beta接近theta(a)(theta的时间平均值)。这导致较大的下游冲刷深度。当β值远小于theta(a)时,在粗砂试验中,射流偏转的影响开始占主导地位,当U-0 / U-c <2.6时,下游冲刷深度较小。当β= pi / 12时,当2.6

著录项

  • 来源
    《Journal of Hydraulic Engineering》 |2018年第8期|04018044.1-04018044.8|共8页
  • 作者单位

    Univ Auckland, Dept Civil & Environm Engn, Private Bag 92019, Auckland 1142, New Zealand;

    Univ Auckland, Dept Civil & Environm Engn, Private Bag 92019, Auckland 1142, New Zealand;

    Hohai Univ, Coll Harbor Coastal & Offshore Engn, Nanjing 210098, Jiangsu, Peoples R China;

    Univ Auckland, Dept Civil & Environm Engn, Private Bag 92019, Auckland 1142, New Zealand;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Local scour; Submerged weir; Downstream weir slope;

    机译:局部冲刷;淹没堰;下游堰坡;
  • 入库时间 2022-08-18 00:20:53

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