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
2013年
z2期
3486-3492
,共7页
黎华清%甘伏平%陈玉玲%程展林%饶锡保%肖国强
黎華清%甘伏平%陳玉玲%程展林%饒錫保%肖國彊
려화청%감복평%진옥령%정전림%요석보%초국강
水利工程%金沙江下游%软弱夹层%深厚覆盖层%孔间Color-CT成像%电站坝基
水利工程%金沙江下遊%軟弱夾層%深厚覆蓋層%孔間Color-CT成像%電站壩基
수리공정%금사강하유%연약협층%심후복개층%공간Color-CT성상%전참패기
hydraulic engineering%downstream of Jinsha River%weak intercalated layers%deep overburden layer%cross-well Color-CT imaging%dam foundation of power station
深厚覆盖层是一种特殊工程地基。其结构松散、岩性不连续、成因类型及岩土体结构组成复杂、物理力学性质呈非均质性分布。深厚覆盖层中的结构面、软弱夹层呈非连续性分布,给分层带来困难,是目前尚未解决的热点工程地质问题。结合乌东德水电站坝址深厚覆盖层分层进行实测试验,依据孔间电磁波Color-CT成像结果,揭示出深厚覆盖层内保存有完好的软弱夹层地质事件证据。以孔间Color-CT成像为研究对象,采用非线性计算岩土体吸收系数,将岩土体结构面进行阈值划分,把不同结构面区域标定出来,最终通过面积、位置参数、形状等特征划分出软弱夹层区域,定位出孔间剖面内软弱夹层个体数量和空间分布。
深厚覆蓋層是一種特殊工程地基。其結構鬆散、巖性不連續、成因類型及巖土體結構組成複雜、物理力學性質呈非均質性分佈。深厚覆蓋層中的結構麵、軟弱夾層呈非連續性分佈,給分層帶來睏難,是目前尚未解決的熱點工程地質問題。結閤烏東德水電站壩阯深厚覆蓋層分層進行實測試驗,依據孔間電磁波Color-CT成像結果,揭示齣深厚覆蓋層內保存有完好的軟弱夾層地質事件證據。以孔間Color-CT成像為研究對象,採用非線性計算巖土體吸收繫數,將巖土體結構麵進行閾值劃分,把不同結構麵區域標定齣來,最終通過麵積、位置參數、形狀等特徵劃分齣軟弱夾層區域,定位齣孔間剖麵內軟弱夾層箇體數量和空間分佈。
심후복개층시일충특수공정지기。기결구송산、암성불련속、성인류형급암토체결구조성복잡、물리역학성질정비균질성분포。심후복개층중적결구면、연약협층정비련속성분포,급분층대래곤난,시목전상미해결적열점공정지질문제。결합오동덕수전참패지심후복개층분층진행실측시험,의거공간전자파Color-CT성상결과,게시출심후복개층내보존유완호적연약협층지질사건증거。이공간Color-CT성상위연구대상,채용비선성계산암토체흡수계수,장암토체결구면진행역치화분,파불동결구면구역표정출래,최종통과면적、위치삼수、형상등특정화분출연약협층구역,정위출공간부면내연약협층개체수량화공간분포。
Deep overburden layer is a special engineering foundation. It is distributed non-uniformly in loose structure,lithologic discontinuity,genetic type and rock-soil structure,physico-mechanical properties. The structure plane in deep overburden and weak intercalated layers distribute discontinuously,which make it difficult to identify those layers. It is currently an unsolved hotspot problem of engineering geology. Field experiments to identify the deep overburden layers were implemented at Wudongde hydropower station. The geological evidence is revealed that the intact weak intercalated layers are preserved in the deep overburden layer based on cross-well electromagnetic wave Color-CT imaging findings. Through the study of cross-well Color-CT images,the threshold values are selected for separating the structure planes of rock and soil mass and the regions of different structure planes are calibrated,using the nonlinear calculation of the absorption coefficients of rock and soil mass. Finally,the weak intercalated layer regions are located based on the feature parameters of area,location and shape. The quantity and spatial distribution of the weak intercalated layers in the cross-section between holes are defined.