多破裂面走滑断层错动下隧道结构响应规律研究

Study on Response Characteristics of the Tunnel Structure under Dislocation of Strike-slip Faults with Multiple Fracture Surfaces

  • 摘要: 大型活动走滑断层破碎带内的岩体位错具有明显的非线性特征,使得断层带内不同区域岩土体的破坏特征各不相同,穿越断层区隧道结构变形受力十分复杂。文章依托某穿越大型走滑断层隧道工程,通过模型试验与数值模拟研究穿越多破裂面走滑断层的隧道结构响应沿纵向的分布规律。结果表明:随着断层错动量的增加,隧道水平位移不断增加,隧道变形呈现S型分布特征,且错动引起的隧道变形主要发生在断层区域内。走滑断层错动下,隧道拱腰纵向变形反弯凹陷段与围岩挤压更为明显,凸出段与围岩存在脱离趋势。隧道结构的受力破坏主要集中于两断层错动面附近,断层上盘隧道结构相较于下盘隧道结构更易被损坏。

     

    Abstract: The rock mass dislocation in the large active strike-slip fault fracture zone exhibits significant nonlinear characteristics, resulting in varying failure features of rock and soil masses in different areas of the fault zone. This makes the deformation and stress of tunnel structure crossing fault zones increasingly complex. This paper, based on a tunnel project crossing a large strike-slip fault, uses model tests and numerical simulations to obtain the longitudinal distribution patterns of tunnel structure responses when crossing faults with multiple fracture surfaces. The results show that with the increase in fault dislocation, the horizontal displacement of the tunnel continuously increases,showing an S-shaped deformation pattern, with dislocation-induced deformation mainly occurring in the fault zone. Under strike-slip fault dislocation, the compression is more pronounced between the reverse bending concave section of longitudinal deformation curve of the tunnel arch waist and the surrounding rock, while the convex section has a tendency to detach from the surrounding rock. The stress-induced failure of the tunnel structure is mainly concentrated near the two fault dislocation surfaces, with the tunnel structure in the upper wall being more prone to failure compared to the lower wall.

     

/

返回文章
返回