Study of stress characteristics of brittle failures of rock around underground openings
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Study of stress characteristics of brittle failures of rock around underground openings
Vol. 33, Issue S1, (2012)
作者机构:
1. 中国地震局地壳应力研究所,北京,100085
2. 中国水利水电科学研究院 岩土工程研究所,北京,100048
作者简介:
基金信息:
DOI:
CLC:TU456
Online First:21 September 2012,
Published:2012
稿件说明:
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WANG Cheng-hu, SONG Cheng-ke, LIU Li-peng. Study of stress characteristics of brittle failures of rock around underground openings[J]. 2012, 33(S1).
DOI:
WANG Cheng-hu, SONG Cheng-ke, LIU Li-peng. Study of stress characteristics of brittle failures of rock around underground openings[J]. 2012, 33(S1).DOI:
Study of stress characteristics of brittle failures of rock around underground openings
borehole breakouts and spalling are all common phenomena which occur around the underground openings. In substance
these three phenomena all belong to brittle failures of intact rock mass; but they reflect different failure extents of intact rock mass under the action of high stresses. After analyzing and comparing the stress-strength criteria for rock bursts
borehole breakouts and spalling put forward by other specialists
we find that these brittle failure phenomena share the same stress requirement. The stress requirements for brittle failures can be defined with the ratio of the maximum tangential stress around an underground opening to the uniaxial compressive strength ( / ) or the ratio of the maximum principal stress to the uniaxial compressive strength ( / ); actually
both indices reflect the same stress requirements. For /
the ratio of 0.4±0.1 should be the critical stress requirement
but for /
the ratio of 0.15±0.05 should be the critical stress requirement. Large amounts of engineering cases and the mechanical analysis based on the Hoek-Brown criterion also prove the validity of these two stress requirements. Here
the two stress requirements reflect a ratio range because the complicated rock mass ratings
lithology and geotechnical conditions shall have profound impacts on the stress requirement for brittle failures.