欢迎访问《高校地质学报》官方网站,今天是
分享到:

高校地质学报 ›› 2024, Vol. 30 ›› Issue (06): 714-725.DOI: 10.16108/j.issn1006-7493.2023074

• • 上一篇    下一篇

龙游石窟3 号洞室三维地质建模与顶板裂缝演化的数值模拟研究

张德宇1, 2,周 剑1, 2*,张路青3, 4,杨志法3, 4,傅 燕5,李紫怡1, 2   

  1. 1. 北京工业大学 城市建设学部,北京 100124;
    2. 北京工业大学 城市与工程安全减灾教育部重点实验室,北京 100124;
    3. 中国科学院地质与地球物理研究所 中国科学院页岩气与地质工程重点实验室,北京 100029;
    4. 中国科学院地球科学研究院,北京 100029;5. 浙江省龙游石窟研究所,衢州 324000
  • 出版日期:2024-12-20 发布日期:2024-12-20

Three-dimensional Geological Modeling and Numerical Study on Roof Crack Evolution in No. 3 Cave of Longyou Grottoes

ZHANG Deyu1,2,ZHOU Jian1,2*,ZHANG Luqing3,4,YANG Zhifa3,4,FU Yan5,LI Ziyi1,2   

  1. 1. Beijing University of Technology, Department of Urban Construction, Beijing 100124, China;
    2. Beijing University of Technology, Key Laboratory of Urban and Engineering Safety and Disaster Reduction, Ministry of Education, Beijing 100124, China;
    3. Institute of Geology and Geophysics, Chinese Academy of Sciences, Key Laboratory of Shale Gas and Geological Engineering, Chinese Academy of Sciences, Beijing 100029, China;
    4. Institute of Earth Sciences, Chinese Academy of Sciences, Beijing 100029, China;
    5. Zhejiang Longyou Grottoes Research Institute, Quzhou 324000, China
  • Online:2024-12-20 Published:2024-12-20

摘要: 龙游石窟古地下洞室群是中国重点保护的不可移动的文物,具有上千年的历史,但其岩体强度呈现劣化趋势。近20年内多次现场调查发现3号洞室顶板围岩中的裂缝快速发展,顶板岩层较薄位置出现局部掉块。为进一步分析龙游石窟3号洞室顶板裂缝的演化和扩展规律,该研究中采用三维激光扫描技术获取了该洞室轮廓点云数据,结合岩体结构信息建立了几何模型和地质模型,借鉴强度折减法对龙游石窟3号洞室顶板的裂缝发展过程开展了数值模拟和分析。研究结果表明:高精度三维激光扫描点云数据结合地质调查能够准确构建龙游石窟3号洞室的三维地质模型,基于高精度网格模型的数值模拟的结果能够准确反映3号洞室顶板裂缝的演化和扩展规律。龙游石窟3号洞室顶板的裂缝主要产生在洞口和岩柱的周围,扩展形态以环状为主。随着岩体强度折减系数增大,顶板围岩的拉应力集中区分布在已有裂缝尖端以及多条裂缝中间的区域,拉裂缝的纵向扩展主要集中于洞室顶板最外侧围岩内。顶板岩体位移场的变化呈现空间非均匀性特征,3-1号岩柱北侧裂缝集中区最大位移为6 mm,而3-3号岩柱北侧裂缝集中区最大位移达到12.14 mm。该研究首次获得了龙游石窟3号洞室顶板裂缝分布、形态和发展趋势,与现场调查数据基本一致,可为洞室围岩的力学行分析和石窟的长期保护提供参考。

关键词: 龙游石窟, 三维地质模型, 洞室顶板裂缝演化, 强度折减法

Abstract: The ancient underground caverns in Longyou Grottoes are immovable cultural relics under the key protection in China, with a history of thousands of years, but their rock mass strength shows a trend of deterioration. In the recent 20 years, many field investigations found that cracks in the surrounding rock of the roof of No.3 cavern developed rapidly, and local blocks fell off at the thin roof rock. In order to further analyze the evolution and expansion of cracks in the roof of No.3 cave in Longyou Grottoes, high-precision three-dimensional point cloud data of the cave contour were obtained by using three-dimensional laser scanning technology. Also highprecision geometric and geological models were established combined with rock mass structure information. The development process of cracks in the roof of No. 3 cave in Longyou Grottoes was numerically simulated and analyzed by using the strength reduction method. The research results show that, based on high-precision 3D laser scanning point cloud data combined with a geological survey, the 3D geological model of Longyou Cave 3 is constructed. The results of numerical simulation on this high-precision grid model can accurately reflect the evolution and expansion law of the roof crack of Cave 3. The cracks in the roof of No.3 cave in Longyou Grottoes were mainly generated around the entrance and rock column, and the expansion form is mainly annular. With the increase in the strength reduction
coefficient of rock mass, the tensile stress concentration area of the roof surrounding rock is distributed at the tip of existing cracks and in the middle of multiple cracks, and the longitudinal expansion of tensile cracks mainly appear in the outermost surrounding rock of the tunnel roof. Variations of the displacement field of the roof rock body show the characteristics of spatial heterogeneity. The maximum displacement in the fracture concentration area on the northern side of No. 3-1 rock pillar is 6mm, while the maximum displacement in the fracture concentration area on the northern side of No.3-3 rock pillar is 12.14 mm. This study obtained the distribution, shape and development trend of cracks in the roof of Longyou Grottoes No.3 for the first time, which is generally consistent with the field survey data. Therefore, this study can provide a reference for the mechanical analysis and prediction of the surrounding rock of the cave and the long-term protection of the grottoes.

Key words: Longyou grottoes, 3D geological model, crack evolution in cavern roof, strength reduction method

中图分类号: