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大理岩破坏阶段Biot系数研究

胡大伟 周辉 谢守益 张凯 邵建富 冯夏庭

岩土力学2009,Vol.30Issue(12):3727-3732,6.
岩土力学2009,Vol.30Issue(12):3727-3732,6.

大理岩破坏阶段Biot系数研究

Study of Biot's coefficients of marble during plastic deformation phase

胡大伟 1周辉 2谢守益 1张凯 2邵建富 1冯夏庭1

作者信息

  • 1. 中国科学院武汉岩土力学研究所,岩土力学和工程国家重点实验室,武汉,430071
  • 2. 法国里尔科技大学,里尔力学实验室,法国,里尔,59655
  • 折叠

摘要

Abstract

The concept of effective stress is mostly used in hydro-mechanic coupling study, while it is difficult to determine the values of Biot's coefficients. A test system is developed to study the evolution of Biot's coefficients in cracked rock materials induced by deviatoric stress. In the plastic deformation phase of triaxial compression test, some loading-unloading cycles of axial stress were carried out at different levels of axial strains. After injection and squeeze water into/out of the specimen at the end of axial stress unloading process, the deformation is recorded during the loading-unloading cycle of pore pressure. The Biot's coefficients in axial and lateral directions are calculated based on the method proposed by Shao. The evolution of axial and lateral Biot's coefficients at different levels of axial strains is presented in a series of confining stresses; it is found that: 1)the property of Biot's coefficients is anisotropic, it is reasoned that the cracks in the specimen are grown along the direction of maximum normal stress; 2)the axial and lateral Biot's coefficients are increased when axial strain increases, the increasing of axial strain leads to the propagation of cracks, consequently causes the Biot's coefficients augment; 3)the values of axial and lateral Biot's coefficients under low confining stress are greater than the one under high confining stress, the reason is that the failure style is changed with confining stress.

关键词

Biot系数/塑性变形/裂纹/流固耦合

Key words

Biot coefficient/ plastic deformation/ crack/ hydro-mechanic coupling

分类

建筑与水利

引用本文复制引用

胡大伟,周辉,谢守益,张凯,邵建富,冯夏庭..大理岩破坏阶段Biot系数研究[J].岩土力学,2009,30(12):3727-3732,6.

基金项目

国家自然科学基金委员会、二滩水电开发有限责任公司雅砻江水电开发联合研究基金项目(No. 50579091 ()

50539090),国家自然科学基金项目资助(No. 10772190). (No. 10772190)

岩土力学

OA北大核心CSCDCSTPCD

1000-7598

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