龙游牛场1号洞顶板开裂机制及长期抗拉强度反演分析

    ROOF CRACKING MECHANISM AND LONG-TERM TENSILE STRENGTH INVERSION ANALYSIS OF NIUCHANG NO.1 CAVERN IN LONGYOU, CHINA

    • 摘要: 龙游古洞室群(小南海石室)是国家重点文物保护单位,具有重要的工程科学价值。近20 a来洞室顶板裂缝发展快速,对洞室稳定性构成威胁,深入开展顶板开裂机制和长期强度的研究是必要的。牛场1号洞是龙游古洞室群的重要组成部分,洞室几何条件相对简单,是开展顶板开裂机制分析和长期强度反演的很好实例。基于现场调查,作者首先获取了牛场1号洞顶板的裂缝分布,然后利用三维激光扫描数据建立了洞室高精度FLAC三维数值模型,并对洞室应力场进行了精细模拟。理论分析及数值模拟结果表明:牛场1号洞顶板的拉应力集中区与主要裂缝分布有着很好的一致性,应力集中是顶板裂缝启动与扩展的驱动因素;顶板分层加大了直接顶的拉应力集中程度,不仅降低了顶板抗弯强度,还可能影响着裂缝的数量和分布特征;0.35 MPa以上的拉应力区就可以引起顶板开裂的启动,可以将该值作为洞室围岩百年尺度的长期抗拉强度参考值。研究成果可为龙游古洞室群保护区的洞室长期稳定性评价和旅游安全规划提供依据。

       

      Abstract: The Longyou grottoes(Xiaonanhai Stone Room), as key protected cultural relics in China, hold significant value in engineering science. Over the past two decades, roof cracks within the caverns have developed rapidly, posing a substantial threat to their stability. Therefore, comprehensive research on the mechanism of roof cracking and long-term strength in the Longyou Grottoes Reserve is imperative. Niuchang No. 1 ancient cavern, located adjacent to the Longyou Grottoes, offers relatively simple geometric conditions that serve as an exemplary case for analyzing both roof cracking mechanisms and long-term strength inversion. Based on field investigation, the roof crack distribution of Niuchang No. 1 cavern was initially obtained. Subsequently, using three-dimensional laser scanning data, a high-precision three-dimensional numerical model of the cavern was established and its stress field was simulated. The results of theoretical analysis and numerical simulation showed that the tensile stress concentration area of the roof of Niuchang No. 1 cavern is in good agreement with the distribution of the main cracks, with stress concentration acting as a driving factor for both initiation and expansion of these cracks. The layering of roof rock mass increases the tensile stress concentration of the immediate roof, which not only reduces the bending strength of the roof but also affects the number and distribution characteristics of cracks. The tensile stress zone above 0.35 MPa can cause the initiation of roof cracking, and this value can be used as the long-term tensile strength reference value of surrounding rock at the centennial scale. The research findings can offer valuable insights into the mechanism of long-term stability and tourism safety planning of caverns in the Longyou Grottoes Reserve.

       

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