Research on Characteristics of Brittleness to Ductility Transition of Stratification in Continental Shale
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摘要: 针对深部页岩气盖层脆-延转化压力与层理倾角关系不明确的问题,从岩石物理力学性质倾角出发,通过室内岩石单轴、三轴压缩试验进行探究,并基于Hoek-Brown破坏准则,引入层理损伤来预测脆-延转化临界压力。结果表明:1)围压的增大抑制了层理面对力学性质的控制作用;2)随着围压的增大,泥页岩的破坏模式逐渐统一为单一裂缝的剪切破坏;3)层理面对脆-延转化压力起着一定的控制作用,平行层理和垂直层理方向的脆-延转化压力明显高于其他方向的压力。Abstract: In view of the problem that the relation between pressure of brittleness to ductility transition on deep shale gas caprock and dip angles of stratification were indefinite, uniaxial and triaxial compression tests of rock were conducted from the perspective of physical and mechanical properties of rock. Based on Hoek-Brown Failure Criterion, stratification damage was introduced to predict the critical pressure of brittleness to ductility transition. The results showed that: to increase confining pressure could restrained the effect of stratification on mechanical properties of rock; with the increase of confining pressure, the failure mode of shale gradually tended to shear failure with a single fracture;stratification surfaces played a certain role in controlling the pressure of brittleness to ductility transition, and the pressure of brittleness to ductility transition in parallel and vertical stratification directions was significantly higher than that of rock at other dip angle directions with stratification.
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