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A Mathematical Model for Forecasting the Dam-Break Flood Routing Process of a Landslide Dam

机译:滑坡大坝溃决洪水过程的数学模型

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摘要

Once a landslide dam bursts, its reservoir discharges quickly in a flood which will cause catastrophic damage to life and property downstream. For a specific landslide dam, the peak flow rate and the evolution of downstream flood are influenced by the shape and size of the dike breach when dam-break occurs. According to the general nature of landslide dams and field observations of dike-breach development patterns, a dike-breach propagation mode has been determined. By combining an improved empirical equation with knowledge of the dike-breach propagation mode, a mathematical model for forecasting dam-break flood routing has been developed and is presented here. Sensitivity analysis was then carried out based on the computed results for peak flow rate and the flood evolution curve under different parameters. The computed results showed that the width coefficient and the depth coefficient had similar effects on the dam-break flood but that the impact of the depth coefficient was more significant than that of the width coefficient. Finally, the proposed model was used to calculate the flood evolution for the Tangjiashan landslide dam. The computed results showed that the error between the simulated result and the measured data was less than 5%.
机译:一旦滑坡坝破裂,其水库就会在洪水中迅速泄洪,这将对下游的生命和财产造成灾难性的破坏。对于特定的滑坡坝,当溃坝发生时,峰值流速和下游洪水的演变受堤坝的形状和大小的影响。根据滑坡坝的一般性质和堤防发展模式的野外观察,确定了堤防扩展方式。通过将改进的经验方程式与堤防越界传播模式的知识相结合,已开发了预测溃坝洪水路线的数学模型,并在此进行了介绍。然后根据计算结果对不同参数下的峰值流量和洪水演进曲线进行敏感性分析。计算结果表明,宽度系数和深度系数对溃坝洪水的影响相似,但深度系数的影响比宽度系数的影响更大。最后,该模型被用于计算唐家山滑坡坝的洪水演变。计算结果表明,仿真结果与实测数据的误差小于5%。

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  • 来源
    《Mathematical Problems in Engineering》 |2012年第6期|139642.1-139642.16|共16页
  • 作者单位

    State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu 610065, China;

    State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu 610065, China;

    State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu 610065, China,Key Laboratory of Mountain Hazards and Earth Surface Process, CAS, Chengdu 610044, China;

    State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu 610065, China;

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