Stress and deformation analysis of rockfill in true triaxial stress conditions based on PFC
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Stress and deformation analysis of rockfill in true triaxial stress conditions based on PFC
Vol. 33, Issue 10, (2012)
作者机构:
1. 武汉大学 水资源与水电工程科学国家重点实验室,武汉,430072
2. 武汉大学 水工岩石力学教育部重点实验室,武汉,430072
3. 中铁第四勘察设计院集团有限公司,武汉,430063
作者简介:
基金信息:
DOI:
CLC:O241
Online First:19 October 2012,
Published:2012
稿件说明:
移动端阅览
ZHOU Wei, XIE Ting-ting, MA Gang, et al. Stress and deformation analysis of rockfill in true triaxial stress conditions based on PFC[J]. 2012, 33(10).
DOI:
ZHOU Wei, XIE Ting-ting, MA Gang, et al. Stress and deformation analysis of rockfill in true triaxial stress conditions based on PFC[J]. 2012, 33(10).DOI:
Stress and deformation analysis of rockfill in true triaxial stress conditions based on PFC
Three-dimensional particle flow code(PFC)is adopted to simulate the true triaxial tests of rockfill. Not only the macro stress and deformation characteristics of the rockfill under three-dimensional stress conditions are researched
but also the micro and macro parameters are then linked with each other in order to further improve the study of rockfill. In the process of the test
the ratio of intermediate principal stress is fixed. By comparing the results of rockfill true triaxial test based on PFC and the results of true triaxial test in laboratory
we find that the PFC can suitably simulate the mechanical properties of rockfill. The PFC numerically experimental results indicate that the intermediate principal stress has a remarkable influence on the strength and deformation of rockfill under the three-dimensional stress condition. When stress ratio parameter change from 0 to 1
the intermediate principal stress surface compresses firstly and inflates later; the minor principal stress surface is always on the compression state. The intermediate principal stress is influences on the internal friction angle
the elasticity coefficient and the Poisson's ratio. In a mesoscopic view
we find that the higher confining pressure is
the higher value of b is
the greater particle coordination number is
and the smaller porosity factor is. The rockfill macroscopic stress and deformation phenomena are explained from microscopic angle.