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A Study on the Formation Mechanism and Calculation Method of Surrounding Rock Pressure in Shallow-buried Loess Tunnel Considering the Influence of Vertical Joints

机译:考虑竖向节理影响的浅埋黄土隧道围岩压力形成机理及计算方法研究

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摘要

Vertical joints have significant effects on the stability of shallow-buried loess tunnel. Due to the presence of vertical joints distributed widely in loess, the formation mechanisms of surrounding rock pressure on shallow-buried loess tunnel and its computational method are far different from those in other types of soil tunnel. In this study, the distribution characteristics of surrounding rock pressure in shallow-buried loess tunnel were investigated, and discrete element software 3DEC was used to analyze the formation mechanism and development process of surrounding rock pressure in loess tunnel under the influence of joints. We correlated the stratum deformation characteristic with the frictional force caused by the mutual dislocation between joints, and revised the semi-empirical method (Chinese Code methods) in China. The results show that the measured data of radial surrounding rock pressure of shallow-buried loess tunnel are generally between 0 - 600 kPa, and 80 in the range of 0 - 200 kPa. The surrounding rock pressure increases with the burial depth, while the distribution of lateral pressure coefficient is relatively discrete. The existence of loess vertical joints (LVJs) aggravates the uneven distribution of the vertical pressure above the tunnel, and the reduction of the lateral earth pressure coefficient at rest under the influence of joints leads to an increase in pressure near the arch shoulder, these two constitute the essence of the joints action on the surrounding rock pressure. The surrounding rock pressure of the shallow-buried loess tunnel reaches the peak stress at about 0.5D from the tunnel face (D is the tunnel span), which is about 1.04 - 1.32 times of the initial stress. After the excavation of the upper step, the stress of the tunnel crown monitoring point decreased to about 60 of the initial stress. Compared with ignoring the influence of joints, the time of reaching the peak stress at the arch shoulder monitoring point is earlier, and the final stress release degree is smaller. The comparison of the analytical results (proposed method) with the numerical results and the field data exhibits good agreement, proving the proposed method's correctness.
机译:竖向节理对浅埋黄土隧道的稳定性有显著影响。由于黄土中垂直节理分布广泛,浅埋黄土隧道围岩压力的形成机理及其计算方法与其他类型土体隧道存在较大差异。本研究研究了浅埋黄土隧道围岩压力的分布特征,并利用离散元软件3DEC分析了节理作用下黄土隧道围岩压力的形成机理及发展过程。将地层变形特征与节理间相互错位引起的摩擦力相关联,对我国的半经验法(中国规范法)进行了修正。结果表明:浅埋黄土隧道径向围岩压力实测数据一般在0—600 kPa之间,0—200 kPa范围内为80%;围岩压力随埋藏深度的增加而增大,而侧向压力系数的分布相对离散。黄土竖向节理(LVJs)的存在加剧了隧道上方竖向压力分布的不均匀性,在节理作用下,静向土压力系数的降低导致拱肩附近压力增大,这两者构成了节理作用对围岩压力的本质。浅埋黄土隧道围岩压力在距隧道掌子面约0.5D处达到峰值应力(D为隧道跨度),约为初始应力的1.04—1.32倍。上台阶开挖后,隧道冠部监测点应力降低至初始应力的60%左右。与忽略关节影响相比,弓肩监测点达到峰值应力的时间更早,最终应力释放程度更小。分析结果(所提方法)与数值结果和现场数据的对比具有较好的一致性,证明了所提方法的正确性。

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