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颗粒破碎的三维离散元模拟研究

张科芬 张升 滕继东 盛岱超

岩土力学2017,Vol.38Issue(7):2119-2127,9.
岩土力学2017,Vol.38Issue(7):2119-2127,9.DOI:10.16285/j.rsm.2017.07.036

颗粒破碎的三维离散元模拟研究

3D numerical simulation of particle breakage using discrete element method

张科芬 1张升 2滕继东 1盛岱超2

作者信息

  • 1. 中南大学土木工程学院,湖南长沙410075
  • 2. 中南大学高速铁路建造技术国家工程实验室,湖南长沙410075
  • 折叠

摘要

Abstract

Discrete element method (DEM),such as particle flow code (PFC),has become one of the current highlights to investigate the particle breakage process in the geotechnical field.In this study,based on the point load crushing criterion considering the local stress concentration,a three-dimensional (3D) particle crushing model was established.Particually,the particle balance among particles before and after crushing is ensured by the Apollo filling and expansion method,and a size effect factor is used to characterize strength of particles with different sizes.Then,numerical simulations were performed on three types of sand with different degrees of breakage,namely silica sand,calcareous sand and Sacramento River sand.The comparisons of numerical and experimental results show that the established model can well describe compressive properties of granular materials with different degrees of breakage.Comparing with the failure criterion rooted in Mohr-Coulomb theory on the basis of mean stress,the criterion in the established model shows a better manner in reflecting the real fragmentation phenomena under the same loading condition.At the same time,the established model reveals the influence of crushing on the anisotropic dissipation and gradation evolution of granular materials.

关键词

颗粒破碎/离散元法/多代子颗粒/破碎准则

Key words

particle breakage/discrete element method/multi-generations of particles/crushing criterion

分类

建筑与水利

引用本文复制引用

张科芬,张升,滕继东,盛岱超..颗粒破碎的三维离散元模拟研究[J].岩土力学,2017,38(7):2119-2127,9.

基金项目

国家重点基础研究发展计划(973)项目(No.2014CB047001) (973)

国家自然科学基金项目(No.41340012,No.51508578).This work was supported by the National Basic Research Program of China (973 Program) (2014CB047001) and the National Natural Science Foundation of China (41340012,51508578). (No.41340012,No.51508578)

岩土力学

OA北大核心CSCDCSTPCD

1000-7598

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