Research on crustal stress measurement and inversion of stress disturbed area of a tunnel
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Research on crustal stress measurement and inversion of stress disturbed area of a tunnel
Vol. 29, Issue 11, (2008)
作者机构:
1. 中国科学院武汉岩土力学研究所,武汉,430071
2. 重庆大学 西南资源开发及环境灾害控制工程教育部重点实验室,重庆,400030
作者简介:
基金信息:
DOI:
CLC:U451
Online First:07 August 2013,
Published:2008
稿件说明:
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BAI Shi-wei, HAN Chang-rui, GU Yi-lei, et al. Research on crustal stress measurement and inversion of stress disturbed area of a tunnel[J]. 2008, 29(11).
DOI:
BAI Shi-wei, HAN Chang-rui, GU Yi-lei, et al. Research on crustal stress measurement and inversion of stress disturbed area of a tunnel[J]. 2008, 29(11).DOI:
Research on crustal stress measurement and inversion of stress disturbed area of a tunnel
Through investigation and in-situ measurement of crustal stress in tunnel location
rather large tectonic stress is ascertained in the tunnel region at first. Because of core sample break
only stress of disturbed area is measured in the tunnel. In the process of 3-dimension numerical modeling
the course of vertical erosion by the Wujiang River is modeled in order to reflect the effect of topographic form on crustal stress. And using the method of pilot calculation to adjust coefficient of horizontal pressure
then appropriate initial stress is determined. Making calculated results coincide with the data measured in-situ
the rational coefficient and crustal stress is obtained. Numerical calculation covers the shortage of in-situ measurement. The research results show that crustal stress of tunnel axis varies with embedded depth and topographic features; and the section K42 is of very high stress. The results provide a scientific foundation for analyzing excavation