岩石力学与工程学报
巖石力學與工程學報
암석역학여공정학보
CHINESE JOURNAL OF ROCK MECHANICS AND ENGINEERING
2014年
11期
2291-2300
,共10页
李志鹏%徐光黎%董家兴%李志刚%王金生%陈春文
李誌鵬%徐光黎%董傢興%李誌剛%王金生%陳春文
리지붕%서광려%동가흥%리지강%왕금생%진춘문
地下工程%地下厂房洞室群%高地应力%低强度应力比%变形特征%破坏特征%猴子岩水电站
地下工程%地下廠房洞室群%高地應力%低彊度應力比%變形特徵%破壞特徵%猴子巖水電站
지하공정%지하엄방동실군%고지응력%저강도응력비%변형특정%파배특정%후자암수전참
underground engineering%underground caverns%high geostress%low strength-to-stress ratio%deformation characteristics%failure characteristics%Houziyan hydropower station
猴子岩水电站地下厂房洞室群具有高地应力、低强度应力比的特点,在施工过程中出现严重的变形破坏现象。结合地质、监测、检测及施工资料对施工期围岩的变形与破坏特征进行分析,分析结果表明:主厂房、主变室及尾调室围岩位移大于50 mm的测点分别占17.2%,27.3%和9.4%,三大洞室围岩变形处于较大水平,远超其他电站同期水平。最大位移出现在III 1类围岩处,表明高地应力条件下,较完整硬岩产生的卸荷回弹变形较大,岩石本身破坏产生的变形所占比重增加。围岩变形深度为5~15 m,最大可达23 m,相对较大;围岩变形与开挖卸荷关系密切,呈“阶跃式”发展。围岩变形破坏以应力重分布起主导作用的应力驱动型为主,由结构面不利组合控制的重力驱动型不再占主导地位。研究猴子岩地下厂房洞室群围岩变形破坏机制对其施工及运营安全具有重要的工程意义。
猴子巖水電站地下廠房洞室群具有高地應力、低彊度應力比的特點,在施工過程中齣現嚴重的變形破壞現象。結閤地質、鑑測、檢測及施工資料對施工期圍巖的變形與破壞特徵進行分析,分析結果錶明:主廠房、主變室及尾調室圍巖位移大于50 mm的測點分彆佔17.2%,27.3%和9.4%,三大洞室圍巖變形處于較大水平,遠超其他電站同期水平。最大位移齣現在III 1類圍巖處,錶明高地應力條件下,較完整硬巖產生的卸荷迴彈變形較大,巖石本身破壞產生的變形所佔比重增加。圍巖變形深度為5~15 m,最大可達23 m,相對較大;圍巖變形與開挖卸荷關繫密切,呈“階躍式”髮展。圍巖變形破壞以應力重分佈起主導作用的應力驅動型為主,由結構麵不利組閤控製的重力驅動型不再佔主導地位。研究猴子巖地下廠房洞室群圍巖變形破壞機製對其施工及運營安全具有重要的工程意義。
후자암수전참지하엄방동실군구유고지응력、저강도응력비적특점,재시공과정중출현엄중적변형파배현상。결합지질、감측、검측급시공자료대시공기위암적변형여파배특정진행분석,분석결과표명:주엄방、주변실급미조실위암위이대우50 mm적측점분별점17.2%,27.3%화9.4%,삼대동실위암변형처우교대수평,원초기타전참동기수평。최대위이출현재III 1류위암처,표명고지응력조건하,교완정경암산생적사하회탄변형교대,암석본신파배산생적변형소점비중증가。위암변형심도위5~15 m,최대가체23 m,상대교대;위암변형여개알사하관계밀절,정“계약식”발전。위암변형파배이응력중분포기주도작용적응력구동형위주,유결구면불리조합공제적중력구동형불재점주도지위。연구후자암지하엄방동실군위암변형파배궤제대기시공급운영안전구유중요적공정의의。
The surrounding rock mass of the underground caverns at Houziyan hydropower station is under high ground stresses and has a low strength-to-stress ratio,leading to severe rock deformations and failures in the process of construction. The deformation and fracture characteristics of the surrounding rock mass were analyzed according to the geological conditions,the data from monitoring and geophysical detection,and the construction process. The proportions of the measured points with the displacements greater than 50 mm in three main caverns are 17.2%,27.3% and 9.4% respectively. The deformations of the surrounding rock mass of the underground caverns are much greater than the ones of the underground caverns at other stations in the same period. The largest displacement is in the rock of category III 1 ,which indicates that the deformation of rebound of the relatively complete and hard rock due to unloading under high ground stress are quite large. The depths of surrounding rock deformation reache 5 to 15 m,even up to 23 m. The deformation of surrounding rock was found to be closely related to the excavation with a stepped process of development. The deformation of the surrounding rock is largely stress driven with the stress redistribution playing the dominant role and the one to be gravity driven controlled by the adverse combination of structural planes played less roles.