引江补汉工程高应力层状软岩变形破坏特性

    Deformation and Failure Characteristics of High-Stress Layered Soft Rock: A Case Study of the Yangtze-Han Water Diversion Project

    • 摘要: 为揭示深埋层状页岩的各向异性力学特性与破坏机制,以引江补汉工程寺坪-牛头山复向斜段志留系砂质页岩为研究对象开展研究。采用 MTS 岩石力学试验系统进行单轴压缩、三轴压缩试验,结合扫描电子显微镜观测破裂表面微观特征,分析层理倾角与围压对页岩力学参数及破坏模式的影响规律。结果表明,页岩峰值强度随层理倾角β呈"U"形分布,最大值出现于β=0°,最小值集中在β=40°~55°;围压增大可提升弹性模量并削弱强度各向异性,其中压缩强度各向异性度随围压升高持续降低,弹性模量各向异性度在围压超5MPa后趋于稳定。破坏模式受层理倾角与围压协同调控,单轴压缩下以沿层理剪切为主,高围压下转变为"沿层理剪切+穿层理张拉"复合模式;内摩擦角与黏聚力随层理倾角同样呈"U"形分布,在β=45°~55°区间达最小值。该研究明确了层状页岩力学特性的关键影响因素与演化规律,为深埋层状页岩隧道围岩变形破坏预判及支护方案优化提供了可靠的试验依据。

       

      Abstract: To reveal the anisotropic mechanical properties and failure mechanisms of deeply buried layered shale, a study was conducted on the Silurian shale section of the Siiping-Niutoushan duplex in the the Yangtze-Han water diversion project. The MTS rock mechanics test system was used to conduct uniaxial compression and triaxial compression tests. Combined with the observation of the microscopic characteristics of the fracture surface by scanning electron microscopy, the influence laws of bedding dip angle and confining pressure on the mechanical parameters and failure mode of shale were analyzed. The results showed that the peak strength of shale presented a "U" shape distribution with the bedding dip angle β, with the maximum value occurring at β=0° and the minimum value concentrated in the range of β=40°-55°; increasing the confining pressure could enhance the elastic modulus and weaken the anisotropy of strength. Among them, the anisotropy degree of compressive strength decreased continuously with the increase of confining pressure, and the anisotropy degree of elastic modulus stabilized after the confining pressure exceeded 5 MPa. The failure mode was jointly regulated by the bedding dip angle and confining pressure. Under uniaxial compression, it was mainly shear along the bedding, and under high confining pressure, it transformed into a "shear along bedding+transverse bedding tension" composite mode. The internal friction angle and cohesion also presented a "U" shape distribution, reaching the minimum value in the range of β=45°-55°. This study clarified the key influencing factors and evolution laws of the mechanical properties of layered shale, providing a reliable experimental basis for the prediction of deformation and failure of surrounding rock in deep-buried layered shale tunnels and the optimization of support schemes.

       

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