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Numerical Simulation of Failure Behavior of Granular Debris Flows Based on Flume Model Tests

机译:基于水槽模型试验的颗粒泥石流破坏行为数值模拟

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摘要

In this study, the failure behaviors of debris flows were studied by flume model tests with artificial rainfall and numerical simulations (PFC3D). Model tests revealed that grain sizes distribution had profound effects on failure mode, and the failure in slope of medium sand started with cracks at crest and took the form of retrogressive toe sliding failure. With the increase of fine particles in soil, the failure mode of the slopes changed to fluidized flow. The discrete element method PFC3D can overcome the hypothesis of the traditional continuous medium mechanic and consider the simple characteristics of particle. Thus, a numerical simulations model considering liquid-solid coupled method has been developed to simulate the debris flow. Comparing the experimental results, the numerical simulation result indicated that the failure mode of the failure of medium sand slope was retrogressive toe sliding, and the failure of fine sand slope was fluidized sliding. The simulation result is consistent with the model test and theoretical analysis, and grain sizes distribution caused different failure behavior of granular debris flows. This research should be a guide to explore the theory of debris flow and to improve the prevention and reduction of debris flow.
机译:本研究通过人工降雨的水槽模型试验和数值模拟(PFC 3D )研究了泥石流的破坏行为。模型试验表明,晶粒尺寸分布对破坏模式有深远的影响,中砂边坡的破坏始于波峰处的裂纹,并以趾向后滑动破坏的形式出现。随着土壤中细颗粒的增加,边坡的破坏模式变为流化流。离散元法PFC 3D 可以克服传统连续介质力学的假设,并考虑颗粒的简单特性。因此,开发了一种考虑液固耦合方法的数值模拟模型来模拟泥石流。对比实验结果,数值模拟结果表明,中型砂质边坡破坏的破坏模式为后退趾滑,细砂型边坡破坏为流化滑动。仿真结果与模型试验和理论分析相吻合,晶粒尺寸分布导致颗粒状碎屑流的破坏行为不同。该研究应为探索泥石流理论,提高对泥石流的预防和减少提供指导。

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