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首页> 外文期刊>International journal of geomechanics >Discrete-Element Simulation of Scaling Effect of Strain Localization in Dense Granular Materials
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Discrete-Element Simulation of Scaling Effect of Strain Localization in Dense Granular Materials

机译:致密粒状材料应变局部化尺度效应的离散元模拟

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摘要

This paper presents a discrete-element method (DEM) study of the scaling effect of strain localization in dense sand. We used disc particles and clump particles to generate specimens for biaxial compression tests, and we adopted a flexible boundary. To investigate the scaling effect, we used a fixed size of specimen composed of different size particles. Numerical simulation reveals that the obtained stress difference and volume strain at a certain strain decrease with R (ratio of specimen width and mean particle size d(50)). As long as the ratio R is larger than 30, the stress difference, volume strain, peak friction angle, and maximum dilatancy angle approach stable values. The influence of R on the shear strength and volumetric strain of the specimen made of disc particles is greater than the one made of clump particles. With the increase in R, the coordination number and average and maximum contact forces decrease gradually, and the shear band width in dense sand gradually decreases and converges to a constant. The shear band inclination does not reveal obvious variation with R, and the obtained results are close to Roscoe's formula. When R is large enough (i.e., R = 40), the obtained shear band width keeps a constant, and the influence of particle size on shear band disappears. With the decrease in d(50), the ratio of shear band width with d(50) gradually decreases; it reaches a stable value when R is large enough.
机译:本文提出了一种离散元方法(DEM)研究稠密砂土中应变局部化的比例效应。我们使用圆盘粒子和团块粒子生成用于双轴压缩测试的标本,并采用了灵活的边界。为了研究缩放效果,我们使用了由大小不同的粒子组成的固定大小的样本。数值模拟表明,在一定应变下获得的应力差和体积应变随R(试样宽度与平均粒径d(50)的比值)的减小而减小。只要比率R大于30,应力差,体积应变,峰值摩擦角和最大剪胀角都接近稳定值。 R对由圆盘状颗粒制成的试样的剪切强度和体积应变的影响要大于由团块状颗粒制成的试样。随着R的增加,配位数,平均和最大接触力逐渐减小,致密砂土中的剪切带宽度逐渐减小并收敛到一个常数。剪切带倾角没有显示出随R的明显变化,并且所得结果接近Roscoe公式。当R足够大(即,R> = 40)时,获得的剪切带宽度保持恒定,并且粒径对剪切带的影响消失。随着d(50)的减小,剪切带宽度与d(50)的比值逐渐减小。当R足够大时,它将达到稳定值。

著录项

  • 来源
    《International journal of geomechanics》 |2019年第6期|04019059.1-04019059.10|共10页
  • 作者单位

    Tongji Univ, Dept Geotech Engn, Shanghai 200092, Peoples R China|Tongji Univ, Key Lab Geotech & Underground Engn, Minist Educ, Shanghai 200092, Peoples R China;

    Tongji Univ, Dept Geotech Engn, Shanghai 200092, Peoples R China;

    Tongji Univ, Dept Geotech Engn, Shanghai 200092, Peoples R China|Tongji Univ, Key Lab Geotech & Underground Engn, Minist Educ, Shanghai 200092, Peoples R China;

    Tongji Univ, Dept Geotech Engn, Shanghai 200092, Peoples R China|Tongji Univ, Key Lab Geotech & Underground Engn, Minist Educ, Shanghai 200092, Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Dense sand; Scaling effect; Biaxial compression test; Shear band; Discrete-element simulation (DEM);

    机译:致密砂;结垢效应;双轴压缩试验;剪切带;离散元模拟(DEM);

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