深部巷道围岩的分区破裂机制及“深部”界定探讨  被引量:74

ON MECHANISM OF ZONAL DISINTEGRATION WITHIN ROCK MASS AROUND DEEP TUNNEL AND DEFINITION OF “DEEP ROCK ENGINEERING"

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作  者:王明洋[1] 宋华[1] 郑大亮[1] 陈士林[1] 

机构地区:[1]解放军理工大学工程兵工程学院,江苏南京210007

出  处:《岩石力学与工程学报》2006年第9期1771-1776,共6页Chinese Journal of Rock Mechanics and Engineering

基  金:国家自然科学基金重大项目(50490275);教育部新世纪优秀人才支持计划

摘  要:通过分析巷道围岩的应力状态和变形破坏多阶段、多水平的性状,揭示巷道围岩最大支撑压力区的体积变形状态及其后果,得出深部围岩区域破裂现象的发生条件、岩体的初始压力和围岩全过程变形状态,尤其是围岩峰值后状态下材料的残留强度关系。根据分区破裂现象的出现条件,提出界定浅部及深部工程活动的标准:浅部工程——坑道最大支撑压力区不破坏的深度;深部工程——坑道最大支撑压力区发生破坏的深度。By analysing the stress state, deformation and failure of rock mass around tunnels at a variety of stages and at multi-level of stresses, the volumetric deformation state and its consequences are exhibited for the maximum supporting pressure zone. The relationships are derived between the condition for the occurrence of zonal disintegration phenomenon in deep rocks and the initial rock stresses, the total deformation process of rocks, and in special, the residual strengths of rocks at post-peak stresses. According to the condition for the occurrence of zonal disintegration phenomenon, a criterion is proposed for defining the shallow and the deep rock engineering, the shallow rock engineering corresponds to the depth to which the rock mass within the maximum supporting pressure zone does not fail: and the reverse is true for the deep rock engineering.

关 键 词:岩石力学 应力状态 深部巷道围岩 区域破裂现象 

分 类 号:TU45[建筑科学—岩土工程]

 

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