岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2014年
9期
2673-2684
,共12页
岩石力学%厚壁筒%三维解析模型%深部岩体%分区破裂化
巖石力學%厚壁筒%三維解析模型%深部巖體%分區破裂化
암석역학%후벽통%삼유해석모형%심부암체%분구파열화
rock mechanics%thick-walled cylinder%3D analytical model%deep rock mass%zonal disintegration
为研究深部洞室围岩的分区破裂化机制,建立了厚壁筒三维线弹性解析模型。逐步减小厚壁筒均布内压,模拟洞室静力开挖。逐步增加厚壁筒轴向均布压力,模拟洞室开挖导致洞室轴向应力集中。逐步增加厚壁筒外周非均布压力系数,模拟洞室开挖导致洞室水平应力的重分布和集中效应。根据弹性力学知识和边界条件,确定洞室开挖引起的弹性应力场、应变场及位移场。从拉压域、应变梯度及径向压拉蓄能等3个方面入手,分别研究了内压静力卸荷、水平应力重分布、围压均匀部分及轴压对深部洞室围岩分区破裂的作用机制。结果表明:径向弹性拉伸能和径向弹性压缩能的相对变化反映了围岩能量释放速率和释放量。水平应力重分布和轴压是围岩出现分区破裂现象的主要因素,但两者作用机制不同。该模型可为研究高地应力深部洞室围岩破坏提供一个较统一的理论工具,也为深部工程设计提供了理论依据。
為研究深部洞室圍巖的分區破裂化機製,建立瞭厚壁筒三維線彈性解析模型。逐步減小厚壁筒均佈內壓,模擬洞室靜力開挖。逐步增加厚壁筒軸嚮均佈壓力,模擬洞室開挖導緻洞室軸嚮應力集中。逐步增加厚壁筒外週非均佈壓力繫數,模擬洞室開挖導緻洞室水平應力的重分佈和集中效應。根據彈性力學知識和邊界條件,確定洞室開挖引起的彈性應力場、應變場及位移場。從拉壓域、應變梯度及徑嚮壓拉蓄能等3箇方麵入手,分彆研究瞭內壓靜力卸荷、水平應力重分佈、圍壓均勻部分及軸壓對深部洞室圍巖分區破裂的作用機製。結果錶明:徑嚮彈性拉伸能和徑嚮彈性壓縮能的相對變化反映瞭圍巖能量釋放速率和釋放量。水平應力重分佈和軸壓是圍巖齣現分區破裂現象的主要因素,但兩者作用機製不同。該模型可為研究高地應力深部洞室圍巖破壞提供一箇較統一的理論工具,也為深部工程設計提供瞭理論依據。
위연구심부동실위암적분구파열화궤제,건립료후벽통삼유선탄성해석모형。축보감소후벽통균포내압,모의동실정력개알。축보증가후벽통축향균포압력,모의동실개알도치동실축향응력집중。축보증가후벽통외주비균포압력계수,모의동실개알도치동실수평응력적중분포화집중효응。근거탄성역학지식화변계조건,학정동실개알인기적탄성응력장、응변장급위이장。종랍압역、응변제도급경향압랍축능등3개방면입수,분별연구료내압정력사하、수평응력중분포、위압균균부분급축압대심부동실위암분구파렬적작용궤제。결과표명:경향탄성랍신능화경향탄성압축능적상대변화반영료위암능량석방속솔화석방량。수평응력중분포화축압시위암출현분구파렬현상적주요인소,단량자작용궤제불동。해모형가위연구고지응력심부동실위암파배제공일개교통일적이론공구,야위심부공정설계제공료이론의거。
In order to investigate the zonal disintergration of surrounding rock in deep tunnel, a 3D linear elastic model is built based on linear elastic theory of thick-walled cylinder. The internal wall of model is subjected to decreasing uniform pressure to simulate the processes of cavern static excavation. The end of model is subjected to increasing uniform pressure to simulate the stress concentration effect which causes by cavern static excavation. The external wall of model is subjected to increasing pressure to simulate the stress concentration effect and stress redistribution which caused by cavern static excavation. Based on the elasticity theory and boundary conditions, the stress field, strain field and displacement field around circular opening induced by excavation are determined. We address the following features of the model: tension-compression region, strain gradient, elastic energy of compression and tension from decreasing uniform internal pressure, increasing stress redistribution and increasing uniform external pressure and axial pressure. The results show that the relative change between elastic energy of tension and elastic energy of compression would like to reflect energy release rate and quantity during the processes of cavern static excavation. The stress redistribution and axial pressure are the main factors leading to zonal disintegration. The model provides theoretical basis to study failure of surrounding rock in deep tunnel.