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Numerical modeling of landslide generated impulsive waves using coupled DDA-SPH method

机译:耦合DDA-SPH法的滑坡产生脉冲波的数值模拟

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Slope failures on the margins of dam reservoir can generated large impulsive waves. Impulsive waves with considerable wave amplitude is able to cause serious damage to the dam body, shoreline properties and lives. Thus, the study of the slope failures, impulsive wave generation and their consequences are of paramount importance for hazard prevention and reduction. Previous numerical studies had made great efforts focusing on the fluid phase, but lacking of the consideration of solid impact. However, as the nature of the two phase problem for landslide generated waves, consideration of fluid and solid interaction is of great significant. In this study, the coupled DDA (Discontinuous Deformation Analysis)-SPH (Smoothed Particle Hydrodynamics) method was used to take the solid fluid interaction into account. In specific, the SPH method was employed to represent the fluid motion by solving the full Navier-Stokes equations, and the landslide movement of a block system was reproduced by the DDA method. Additionally, the coupled scheme of the DDA and SPH method was highlighted to explain the implementation of solid and fluid interaction. As a test case, the study considered a wedge sliding along an inclined plane and interacting with the water matrix. The corresponding experimental results by Heinrich was adopted to evaluate the accuracy and performance of the coupled method in terms of the landslide movement, and wave profiles at typical instants. It is concluded that for the more common practical engineering cases of landslide generated waves, the coupled DDA-SPH method is adequate to describe the phenomena with promise accuracy due to the consideration of solid and fluid interaction.
机译:坝水库边缘的斜率故障可以产生大的冲动波浪。具有相当大波幅幅度的脉冲波能够对坝体,海岸线性质和生命造成严重损害。因此,对斜坡故障,脉冲波产生及其后果的研究对危害预防和减少至关重要。以前的数值研究使重点努力关注流体阶段,但缺乏对固体影响的考虑。然而,随着山体滑坡产生波的两个相位问题的性质,对流体和固体相互作用的考虑非常显着。在该研究中,使用偶联的DDA(不连续变形分析)-SPH(平滑粒子流体动力学)方法将固体流体相互作用考虑。具体而言,采用SPH方法来表示通过求解全部Navier-Stokes方程来表示流体运动,并且通过DDA方法再现块系统的滑坡运动。另外,突出显示DDA和SPH方法的耦合方案以解释固体和流体相互作用的实现。作为测试用例,研究认为沿倾斜平面滑动并与水基质相互作用的楔形物。采用了海因里奇的相应实验结果来评估耦合方法在旧滑坡运动方面的准确性和性能,以及典型时刻的波形曲线。结论是,对于山滑坡产生的山体内工程案例更常见,耦合的DDA-SPH方法足以描述具有承诺准确性的现象,因为考虑到固体和流体相互作用。

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