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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Modelling hyperconcentrated floods in the Middle Yellow River using an improved river network model
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Modelling hyperconcentrated floods in the Middle Yellow River using an improved river network model

机译:用改进的河网模型建模中黄河中的超增长洪水

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摘要

In the section of the Middle Yellow River from Longmen to the Sanmenxia Dam, the prediction to hyperconcentrated flood processes is difficult because of the abrupt change of channel geometry along the river and the high variability of the amount of flood water and sediment load from the main river and tributaries. A river network model based on a Godunov-type FVM scheme is proposed in order to investigate the flow dynamics, sediment transport and bed evolution during hyperconcentrated floods. A quasi 2D algorithm is adopted to calculate the velocity at the junction cell, which is then used for providing the interior boundary conditions. The computation for each reach can be executed simultaneously and the solution procedure is parallelized using OpenMP. The speedup factor compared with a serial program increases linearly in theory with the number of reaches in the river network. Two flood events, featuring significant erosion and deposition respectively, were simulated to validate the model. The calculated water levels, discharges and fractional concentrations of non-uniform suspended load were in agreement with the measurements. A comparison was made between the proposed model and an existing model neglecting the momentum conservation principle at the junction, with the former showing better prediction of the peak water levels near the confluence. Numerical experiments were conducted to analyze the influences of reservoir operation and discharge capacity of the dam on flood routing and bed evolution in the river network. It is demonstrated that decreasing pool level during flood season and increasing discharge capacity are both valid measures to alleviate sedimentation in the Sanmenxia Reservoir, and the former measure is a prerequisite. Therefore, the model presented here can help to enhance the understanding of river network system subject to high sediment input and inspire better strategies on sustainable reservoir management.
机译:在龙门的中黄河到三门峡大坝的一部分中,由于沿河的渠道几何形状的突然变化以及洪水水和沉积物荷载量的高度变化,预测对多交流的洪水过程难以实现。河流和支流。提出了一种基于GODUNOV型FVM方案的河道网络模型,以研究洪水洪水洪水的流动动态,泥沙运输和床进化。采用准2D算法计算结电池的速度,然后用于提供内部边界条件。可以同时执行每个覆盖范围的计算,并且解决方案过程使用OpenMP并行化。与串行程序相比的加速因子在理论上线性增加,河流网络中的到达数量。分别模拟了两个洪水事件,具有显着的侵蚀和沉积,以验证模型。计算的水水平,排出和分数浓度的非均匀悬浮载荷与测量值一致。在拟议的模型和现有模型之间进行了比较,忽视了交界处的动量保护原理,前者显示更好地预测汇合附近的水平。进行了数值实验,分析了河北河网洪水路径床演化的储层运行和放电能力的影响。结果表明,汛期期间的池水平降低,放电容量的增加是在三门峡水库缓解沉降的有效措施,前者是先决条件。因此,这里展示的模型可以帮助提高对高沉积物投入,并激发可持续水库管理的更好策略的理解。

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