岩土力学 ›› 2026, Vol. 47 ›› Issue (5): 1750-1764.doi: 10.16285/j.rsm.2025.0388CSTR: 32223.14.j.rsm.2025.0388

• 岩土工程研究 • 上一篇    下一篇

基于非接触测量的危岩体三维非连续变形分析模型构建与失稳破坏机制研究

刘国阳1,张森1,叶唐进2,薄雾3, 4,杨灿3,康家硕1   

  1. 1. 沈阳工业大学 建筑与土木工程学院,辽宁 沈阳 110870;2. 四川建筑职业技术大学 铁道工程系,四川 成都 610399; 3. 西藏大学 工学院,西藏 拉萨 850000;4. 西藏自治区高原重大基础设施智慧建造与韧性安全技术创新中心,西藏 拉萨 850000
  • 收稿日期:2025-04-15 接受日期:2025-07-15 出版日期:2026-05-11 发布日期:2026-05-12
  • 通讯作者: 叶唐进,男,1981年生,博士,教授,主要从事青藏高原工程地质与灾害地质研究。E-mail: yetangjin@dlut.edu.cn
  • 作者简介:刘国阳,男,1989年生,博士,副教授,主要从事岩质边坡稳定性研究。E-mail: liugyang@163.com
  • 基金资助:
    国家自然科学基金项目(No. 42007241);西藏自治区重点研发计划项目(No. XZ202501ZY0150);辽宁省自然科学基金项目(No. 2023- MSLH-259);辽宁省教育厅高校基本科研项目(No. LJ232410142029)。

Three-dimensional discontinuous deformation analysis model for hazardous rock masses based on non-contact measurements and their instability and failure mechanisms

LIU Guo-yang1, ZHANG Sen1, YE Tang-jin2, BO Wu3, 4, YANG Can3, KANG Jia-shuo1   

  1. 1. School of Architecture and Civil Engineering, Shenyang University of Technology, Shenyang, Liaoning 110870, China; 2. Department of Railway Engineering, Sichuan University of Architectural Technology, Chengdu, Sichuan 610399, China; 3. School of Engineering, Xizang University, Lhasa, Xizang 850000, China; 4. Plateau Major Infrastructure Smart Construction and Resilience Safety Technology Innovation Center of Xizang Autonomous Region, Lhasa, Xizang 850000, China
  • Received:2025-04-15 Accepted:2025-07-15 Online:2026-05-11 Published:2026-05-12
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (42007241), the Key Research and Development Plan of Xiang Autonomous Region (XZ202501ZY0150), the Natural Science Foundation of Liaoning Province (2023-MSLH-259) and the Basic Scientific Research Project of Colleges and Universities of Liaoning Province Education Department (LJ232410142029).

摘要: 危岩体失稳破坏及其诱发的地质灾害已成为基础设施建设和运营的主要威胁之一。以西藏自治区G318国道沿线某岩质边坡为研究背景,分析研究区域内危岩体潜在风险,确定拟研究危岩体主控结构面信息。基于无人机(unmanned aerial vehicle,简称UAV)摄影测量技术采集边坡影像数据并生成密集点云,构建数字地表模型。利用三维激光扫描仪获取危岩体高精度点云数据并生成三角化模型,基于点云数据坐标信息识别和解译岩体次级结构面几何信息。建立兼顾建模效率与计算可行性的边坡及危岩体三维非连续变形分析(discontinuous deformation analysis,简称DDA)数值模型,结合危岩体失稳破坏过程和监测块体位移及动能时程曲线,定量分析危岩体稳定性及其破坏后的运动学成灾机制。结果表明,危岩体I在时间≤ 1.0 s时以滑动模式发生失稳,随后演变为滑动与转动的混合模式,其后缘与坡面之间形成张拉裂缝,前缘与基岩之间发生剪切破坏。危岩体II的块体II-4剧烈滑动引发岩崩灾害(最大冲击合动能达259.186 MJ),块体II-1、II-2和II-3则表现出因错动与裂缝扩展的连锁破坏效应。危岩体I的失稳直接触发危岩体II的崩塌,而危岩体II又反作用于危岩体I岩崩演化行为,两者崩塌块体相互作用合并形成大方量的块体系统,显著增强了岩崩的总体体积和冲击破坏能力。通过融合无人机摄影和三维激光扫描的非接触测量技术,提高了三维DDA的建模精度和效率;对危岩体失稳破坏及岩崩冲击碰撞过程研究,揭示了危岩体崩塌后的动力学相互作用机制,为危岩体灾害安全防控提供了理论依据和技术参考。

关键词: 危岩体, 失稳破坏, 三维非连续变形分析(DDA), 无人机摄影(UAV), 三维激光扫描

Abstract: The instability and failure of hazardous rock masses, along with the resulting geological disasters, pose significant threats to infrastructure construction and operation. This study focuses on a rock slope along the G318 National Highway in the Xizang Autonomous Region as its research background, analyzing the potential risks of hazardous rock masses in the area and identifying the characteristics of the primary controlling structural planes. Using unmanned aerial vehicle (UAV) photogrammetry, slope imagery is acquired and a dense point cloud is generated to construct a digital surface model. UAV photogrammetry is employed to acquire slope imagery and generate a dense point cloud for constructing a digital surface model. A three-dimensional laser scanner is utilized to obtain high-precision point cloud data of hazardous rock mass and create a triangulated surface model. The geometric information of secondary structural planes within the rock mass is identified and interpreted using the coordinate data from the point cloud. A three-dimensional discontinuous deformation analysis (DDA) numerical model of the slope and hazardous rock masses is developed, optimizing modeling efficiency and computational feasibility. The stability of hazardous rock masses and the spatial kinematic disaster mechanisms post-failure are quantitatively analyzed by integrating the failure process with time-history curves of block displacement and kinetic energy. The results indicate that the hazardous rock mass I initially fails in a sliding mode when time≤1.0 s, subsequently evolving into a combined sliding and rotational mode. Tensile cracks develop between the rear edge and the slope, while shear failure occurs at the interface between the rock mass and the bedrock. The violent sliding of block II-4 in hazardous rock mass II triggers a rockfall disaster, with the maximum combined kinetic energy of impact reaching 259.186 MJ. Meanwhile, blocks II-1, II-2, and II-3 exhibit cascading failure effects due to dislocation and crack propagation. The instability of hazardous rock mass I directly triggers the failure of hazardous rock mass II, which subsequently influences the motion and evolution of mass I, leading to mutual interaction and merging of collapse blocks. This results in the formation of a large-scale block system, significantly increasing the overall volume and impact potential of the rockfall. Integrating UAV photogrammetry and three-dimensional laser scanning as non-contact measurement technologies notably enhances the modeling accuracy and efficiency of the three-dimensional DDA method. This research elucidates the dynamic interaction mechanisms involved in hazardous rock mass collapse and provides a theoretical foundation and technical reference for preventing and mitigating hazardous rock mass disasters.

Key words: hazardous rock mass, instability and failure, three-dimensional discontinuous deformation analysis (DDA), unmanned aerial vehicle (UAV) photogrammetry, three-dimensional laser scanning

中图分类号: P 642.3
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