诱导下岩体裂隙扩展规律研究存在问题及对策

    Problems and countermeasures in the study of fracture propagation laws of rock mass under induction

    • 摘要: 大部分地下工程的失稳都是岩体在长期的“诱导”作用下裂隙扩展、贯通从而改变岩体本身的强度特征导致的结果,因此,研究岩体中裂隙的扩展演化规律,对进一步揭示岩体工程失稳、岩石破坏现象的机理和本质具有重要意义。本文从物理实验、数值模拟和力学理论三个方面介绍了目前对于裂隙岩体扩展的研究现状,并结合地下工程的演化过程和工程需求分析了目前裂隙扩展研究中存在的问题,提出了更适应工程问题需求的研究思路:以相似材料、3D打印和声发射技术为手段,首先通过小试样压缩实验确定适用于声发射技术监测的相似材料成分及配比范围,然后采用3D打印的方法制作成交叉裂隙的拉、剪实验试件并开展拉、剪蠕变试验,研究裂隙扩展致裂规律,裂隙岩体拉、剪蠕变声发射特征及破坏的前兆特征,分析岩体强度随蠕变时间的变化规律,在此基础上建立裂隙岩体的大型相似材料模型,研究开挖诱导下随裂隙参数、时间等因素的预测模型和岩体冒落触发时间与裂隙参数、开挖空间的关系模型,揭示裂隙岩体冒落演化机制,预测岩体冒落时间和范围,为地下工程长期稳定性和岩体冒落调控提供理论支撑。

       

      Abstract: The instability observed in most underground engineering projects is typically attributed to the expansion and penetration of fractures in the rock mass due to long-term “induction” effects, which alter the inherent strength characteristics of the rock mass. Consequently, the study of the spatiotemporal evolution patterns of fractures in rock masses is deemed crucial for elucidating the mechanisms and essence of rock instability and failure phenomena. In this paper, the current research status on the expansion of fractures in rock masses is introduced from three aspects: physical experiments, numerical simulations, and mechanical theory. Moreover, the issues present in current fracture propagation research are analyzed in conjunction with the evolution process of underground engineering and its requirements. To address these issues and better align with engineering requirements, a novel research approach has been proposed: methods involving similar materials, 3D printing, and acoustic emission are proposed. The composition and mixing ratio range of similar materials suitable for acoustic emission monitoring are determined through compression experiments on small samples, and then 3D printing techniques are employed to fabricate specimens with intersecting fractures for tensile and shear tests. Creep experiments are conducted to investigate the propagation patterns of fractures and their associated failure precursors through acoustic emission. Additionally, the changes in rock mass strength over time due to creep are analyzed. On this basis, a large-scale similar material model of fractured rock masses is established to investigate predictive models for excavation-induced changes in fracture parameters over time. Furthermore, the relationship between the initiation time of rock mass collapse, fracture parameters, and excavation space is explored. The evolution mechanism of fractured rock mass collapse is aimed to be revealed, along with the prediction of the timing and extent of collapse. The theoretical support provided by these findings is intended to contribute to the long-term stability and collapse control of underground engineering projects.

       

    /

    返回文章
    返回