Microscopic mechanism of subgrade vibration compaction based on discrete element method

IF 1 4区 数学 Q1 MATHEMATICS Electronic Research Archive Pub Date : 2023-01-01 DOI:10.3934/era.2023358
Xin Gao, Hao Liu, Zhou Fang, Yang Zhang
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Abstract

The discrete element is an important tool for vibration compaction simulation from the microscopic viewpoint. The irregular particle model was established by the disc filling method, and the linear contact model with anti-rolling was selected to reflect the contact characteristics between the particles, so as to establish the simulation model of subgrade vibratory compaction. Based on this model, the stress characteristics of the area below the center of the vibrating wheel and the surface area of the soil were studied, and the principle of vibratory compaction was discussed. The results show that the distribution of vertical stresses below the center of drum basically presents a decreasing trend in the depth range during vibration, with the stress amplitude of the lower structure increasing and the stress magnitude of the upper structure decreasing. The distribution of horizontal stresses in the area below the center of the vibrating wheel is similar to the stress distribution in the splitting test. The soil at the surface has an obvious pushing and squeezing effect, and the transmission distance of horizontal stresses is larger than that of vertical stresses. The soil at the surface is pushed and the horizontal stresses are transmitted at a greater distance than the vertical stresses, which, together with a certain degree of shear effect, causes a certain uplift deformation of the soil around the vibrating wheel. In general, the vibration compaction process is relatively consistent with the theory of repeated loading and the theory of alternating shear strain.

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基于离散元法的路基振动压实细观机理
& lt; abstract>从微观角度看,离散元是振动压实模拟的重要工具。采用圆盘填充法建立不规则颗粒模型,选择具有抗滚动的线性接触模型来反映颗粒之间的接触特性,从而建立路基振动压实仿真模型。在此基础上,研究了振动轮中心以下区域和土体表面积的应力特性,并对振动压实原理进行了探讨。结果表明:在振动深度范围内,鼓心以下垂直应力分布基本呈减小趋势,下部结构应力幅值增大,上部结构应力幅值减小;振动轮中心以下区域的水平应力分布与劈裂试验时的应力分布相似。地表土体具有明显的推挤作用,且水平应力的传递距离大于垂直应力的传递距离。表面土体受到推力作用,水平应力传递距离大于垂直应力,加之一定程度的剪切效应,使振动轮周围土体产生一定的上扬变形。总体而言,振动压实过程相对符合重复加载理论和交变剪切应变理论。& lt; / abstract>
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1.30
自引率
12.50%
发文量
170
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