长江科学院院报 ›› 2012, Vol. 29 ›› Issue (12): 73-77.DOI: 10.3969/j.issn.1001-5485.2012.12.015

• 岩土工程 • 上一篇    下一篇

复杂地质条件下洞室围岩初始地应力场研究

冯树荣1, 蒋中明2, 赵海斌1   

  1. 1.中国水电顾问集团 中南勘测设计研究院,长沙 410014;2.长沙理工大学 水利工程学院,长沙 410004
  • 收稿日期:2011-11-04 修回日期:2012-02-21 出版日期:2012-12-01 发布日期:2012-12-18
  • 通讯作者: 蒋中明(1969-),男,重庆璧山人,教授,博士,主要从事水工岩土工程教学及科研工作
  • 作者简介:冯树荣(1963-),男,江苏江都人,教授级高级工程师,博士,主要从事岩土工程及水电工程设计研究工作
  • 基金资助:

    中国水电顾问集团科技计划项目(2010680)

Initial Geostress Field of the Surrounding Rock of Underground Cavern Under Complex Geological Condition

FENG Shu-rong1, JIANG Zhong-ming2, ZHAO Hai-bin1    

  1. 1.Hydro China Zhongnan Engineering Corporation, Changsha 410014, China; 2.School of Hydraulic Engineering, Changsha University of Science & Technology, Changsha 410004, China
  • Received:2011-11-04 Revised:2012-02-21 Online:2012-12-01 Published:2012-12-18

摘要: 初始地应力场的确定是地下洞室稳定性评价的基础。在对现场实测地应力资料分析的基础上,研究了断层等地质构造对初始地应力场分布的影响机理,指出岩体变形模量比是影响应力的关键因素之一。研究了能反映断层引起应力释放效应的初始地应力场反演分析的变刚度方法。考虑与不考虑断层影响情况下的某工程初始地应力场的计算结果和实测结果对比表明,考虑断层影响的结果与实测结果更接近,从而证明了断层应力释放效应作用及基于岩体变刚度的初始地应力反分析方法的合理性。

关键词: 地下洞室, 初始地应力场, 变刚度, 构造应力释放效应

Abstract: The determination of initial geo-stress of rock mass is the basis of stability assessment for underground cavern. By analyzing the in-situ measurements of geo-stress, we investigated the effect of geological structure such as fault on the initial geostress distribution, and found that the deformation modulus ratio of the surrounding rock mass is one of the most important factors affecting the initial geo-stress. We also presented a back analysis method in consideration of  the variable stiffness which reflects the stress release induced by faults. The calculation results of initial geostress involving and not involving the effect of fault effect are compared with the measured values, and it's found that the result considering the fault effect is more consistent with the measured result, which verifies the rationality of this method. 

Key words: underground cavern, initial geo-stress field, variable stiffness, tectonic stress release effect of fault

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