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Analysis of the impact force of debris flows on a check dam by using a coupled Eulerian-Lagrangian (CEL) method

机译:欧拉-拉格朗日耦合法分析碎石流对坝体的冲击力

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The dynamic impact force of debris flows on a check dam was investigated by using numerical analysis and an analytical investigation. The emphasis was on quantifying the magnitude and distributions of the dynamic impact force due to the moving debris flows and the static force due to the deposited material of debris flows. The behavior of debris flows on a check dam and the corresponding response of the significant factors influencing the dynamic impact force of debris flows, such as the entrainment of the soil layer, thickness of sedimentation, and flow velocity, were analyzed by using a three dimensional coupled Eulerian-Lagrangian (CEL) approach. The prediction method can adequately analyze the behavior of debris flows involving the entrainment of the soil layer. The obtained results indicate that the impact force of a debris flow with a high flow velocity cannot be predicted accurately by using the conventional static empirical model, especially when the dynamic empirical model is overestimated. The proposed method was verified by comparing the characteristics of the laboratory test results and the actual debris flows that occurred in Mt. Umyeon, South Korea in 2011.
机译:通过数值分析和分析研究,研究了泥石流对止水坝的动态冲击力。重点是量化由于移动的碎屑流引起的动态冲击力的大小和分布以及由于碎屑流的沉积材料引起的静态力的大小。利用三维空间分析了坝体上的泥石流行为以及影响泥石流动态冲击力的重要因素的相应响应,例如土层的夹带,沉积厚度和流速。欧拉-拉格朗日(CEL)耦合方法。该预测方法可以充分分析涉及土层夹带的泥石流行为。结果表明,采用传统的静态经验模型无法准确地预测高流速泥石流的冲击力,特别是当动态经验模型被高估时。通过比较实验室测试结果的特征和山中发生的实际泥石流,验证了该方法的有效性。 2011年,韩国面目市。

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