正断型倾角60°隐伏地裂缝破裂扩展模拟研究

    SIMULATION STUDY ON FRACTURE PROPAGATION OF NORMAL BURIED GROUND FISSURE WITH A DIP OF 60°

    • 摘要: 地裂缝灾害属于缓变型地质灾害,而隐伏地裂缝数量众多,又具有突发性特点,其破裂扩展的影响范围与潜在灾害效应是当前急需解决的问题。基于隐伏地裂缝主要表现为正断型,在黄土地区广泛分布,开展了正断型隐伏地裂缝在黄土层中的破裂扩展物理模拟试验和数值模拟分析,研究了倾角为60°的隐伏地裂缝错动引起上覆土体中应力和地表位移的变化规律以及破裂向上扩展的平剖面特征,总结了隐伏裂缝的破裂扩展全过程。模拟结果表明,在隐伏地裂缝活动下,上覆土体主要受拉张作用发生变形破坏,并在剖面上形成一倒三角的破裂区,在上盘的破裂区范围明显大于下盘;土体中的土压力变化与预设裂缝顶端形成的土拱效应以及向上盘方向发生的倾倒变形有关;隐伏地裂缝的破裂扩展过程经历了6个阶段,即隐伏地裂缝初始活动阶段、反倾破裂产生阶段、近直立破裂产生和反倾破裂扩展阶段、近直立破裂和反倾破裂同步扩展阶段、近直立破裂与隐伏裂缝贯通阶段以及地裂缝稳定变形阶段。上述模拟结果可为地裂缝发育区的工程建设和灾害防治提供依据和参考。

       

      Abstract: Ground fissure disasters are slow-occurring geological disasters, the most common of which is the buried ground fissure, characterized by abruptness. The large influence range and potential disaster effects of buried ground fissures are urgent problems that need to be solved. The buried ground fissures are mainly normal faults that are widely distributed in areas with loess formation. A large physical test model and a discrete element model of buried ground fissures in loess formation were established to study the fracture extending mode, the variation law of stress, and surface displacement in overlying soil caused by the activity of buried ground fissures with a dip angle of 60°. The characteristics of fracture extension were analyzed, and the whole process of fracture extension was summarized. The results show that the rupture zone of the hanging wall is obviously larger than that of the footwall. Under the activity of the buried ground fissure, tensile deformation is the main form of the overlying soil, and an inverted triangle fracture zone appears. The soil pressure variation in the soil is related to the soil arch at the top of the cracks and the toppling deformation toward the direction of the hanging wall. The fracture extension process of buried ground fissures can be divided into six stages: the initial activity stage of buried ground fissures, the generation stage of reverse dip cracks, the generation stage of near-vertical fractures and reverse dip cracks extending stage, the synchronous expansion stage of near-vertical cracks and reverse dip cracks, the connection stage of near-vertical cracks and buried ground fissures, and the stable deformation stage of ground fissures. The above simulation results can provide a basis and reference for engineering construction and disaster prevention in areas with ground fissures.

       

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