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首页> 外文期刊>Journal of Hydraulic Engineering >Hydraulic and Contraction Scour Analysis of a Meandering Channel: James River Bridges near Mitchell, South Dakota
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Hydraulic and Contraction Scour Analysis of a Meandering Channel: James River Bridges near Mitchell, South Dakota

机译:弯曲河道的水力和收缩冲刷分析:南达科他州米切尔附近的詹姆斯河大桥

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摘要

The two-dimensional (2D) depth-averaged river model Finite-Element Surface-Water Modeling System (FESWMS) was used to simulate the hydraulic conditions at a contracted bridge site. The site studied was the James River bridges near Mitchell, South Dakota. The parallel bridges are located in a crossing between the two bends of a meander. The floodplain alignment relative to the channel and skewed bridges produces complex 2D flow patterns that cannot be predicted accurately by using a one-dimensional (ID) river model. The 2D model was validated by using flow measurements collected by the USGS during three high-flow events with return periods ranging from 25 to 100 years. The validated model was used to examine the site characteristics that influence the concentrated flow on the right side of the main channel and the exchange of flow between the main channel and floodplains. The rating curves derived from the 2D model and the results of soil erosion tests were used to evaluate live-bed and clear-water contraction scour at the bridge site. The scour analysis was conducted by using the equations in Hydraulic Engineering Circular No. 18 (HEC-18) and a method that accounts for the soil erodibility by using a curve of measured erosion rate versus shear stress. The study found that channel meandering, the no-flow boundary condition imposed by the walls of the river valley and skewed roadway embankment, and the dense trees along the left bank are the three main factors that create the unique hydraulic conditions at the bridge site. It is shown that using a 2D flow model could improve the estimation of contraction scour by providing more accurate information on the hydraulic parameters. The predicted scour depth was very sensitive to the critical shear stress and slope of the curve of erosion rate versus shear stress. Therefore, design should incorporate uncertainty in soil properties. It is also shown that an unsteady-flow approach to scour would produce a more realistic curve of predicted scour depth versus time. However, the cumulative effects of multiple flood events must be evaluated if time-dependent scour is used in design.
机译:二维(2D)深度平均的河流模型有限元地表水建模系统(FESWMS)被用来模拟收缩桥梁现场的水力条件。研究的地点是南达科他州米切尔附近的詹姆斯河大桥。平行桥位于曲折的两个弯曲之间的交叉处。相对于河道和斜桥的洪泛区对齐会产生复杂的2D流模式,这些流模式无法使用一维(ID)河模型进行准确预测。通过使用USGS在三个高流量事件期间收集的流量测量值对2D模型进行了验证,其返回时间范围为25至100年。经过验证的模型用于检查影响主河道右侧集中水流以及主河道与洪泛区之间水流交换的站点特征。从二维模型得出的等级曲线和水土流失测试的结果用于评估桥梁工地的活床和清水收缩冲刷。冲刷分析是通过使用《水利工程通告》第18号(HEC-18)中的方程式以及通过使用测得的侵蚀速率与剪切应力之间的关系曲线解决土壤侵蚀性的方法进行的。研究发现,河道蜿蜒曲折,河谷墙和偏斜的路堤施加的无水流边界条件以及沿左岸的茂密树木是在桥梁工地创造独特水力条件的三个主要因素。结果表明,使用二维流模型可以通过提供有关水力参数的更准确信息来改善收缩冲刷的估算。预测的冲刷深度对临界剪应力和侵蚀速率与剪应力的关系曲线的斜率非常敏感。因此,设计应考虑土壤特性的不确定性。还表明,采用非恒定流方式进行冲刷会产生更实际的预测冲刷深度与时间的曲线。但是,如果在设计中使用了与时间有关的冲刷,则必须评估多个洪水事件的累积影响。

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