渗流破坏过程中颗粒运动的DEM模拟

Lin Zhong
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摘要

离散元法(DEM)是一种在单个粒子处发生粒子流动的计算方法。广泛应用于海岸工程、矿山、土木工程等领域。具体来说,当小颗粒被水带走时,由于土壤的自重,孔隙会增加和塌陷,从而导致土壤的其他部分变形。由于管道的不断发展,将细小的土壤颗粒从入口带走,因此入口不断膨胀。一旦上层土壤失去了下层的支撑,上层颗粒就会在入渗作用下崩塌。因此,随着上述现象的持续发展,水的数量和流量将会增加。同时,这将增加渗流破坏的速度。实际上,粒子运动规律包括了粒子在不同条件下的生长、聚集、扩散和结晶,可以应用于其他领域,如纺织科学中材料表面粗糙度的研究,电子工程中晶体的起源和潜在的自旋等。本文的研究可以为上述方向提供进一步的理论基础和框架,为广大学者开展后续研究工作铺平道路。本文采用电子离散元法(EDEM)建模来模拟滑动过程中颗粒的运动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
DEM Modelling of Particle Movement During Seepage Failure
The Discrete Element Method (DEM) is a calculation method by which a particle flow at a single particle occurs. It is widely used in many fields such as coastal engineering, mining and civil engineering. Specifically, when small particles are taken away by water, pores will increase and collapse due to the soil's own weight, which will cause other parts of the soil to deform. Due to the continuous development of piping, small soil particles are taken away from the entrance, so the entrance is constantly expanding. Once the upper layer of soil loses the support below, the upper layer of particles will collapse under infiltration. Therefore, as the above phenomenon continues to develop, the amount and flow of water will increase. At the same time, this will increase the rate of seepage destruction. In fact, the law of particle motion includes the growth, aggregation, diffusion and crystallization of particles under different conditions, which can be applied to other fields, such as the research of material surface roughness in textile science, the crystal origin and potential self-rotation in electronic engineering, etc. The research of this paper can provide a further theoretical basis and framework for the above direction, and pave the way for the majority of scholars to carry out the follow-up research work. In this article, EDEM (Electronic Discrete Element Method) modeling is used to simulate the movement of particles during the slip.
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