孙琪皓, 马凤山, 刘港, 等. 2021. G109国道拉萨-羊八井段喀努纳危岩体变形破坏模式及稳定性分析[J]. 工程地质学报, 29(2): 495-507. doi: 10.13544/j.cnki.jeg.2019-093.
    引用本文: 孙琪皓, 马凤山, 刘港, 等. 2021. G109国道拉萨-羊八井段喀努纳危岩体变形破坏模式及稳定性分析[J]. 工程地质学报, 29(2): 495-507. doi: 10.13544/j.cnki.jeg.2019-093.
    Sun Qihao, Ma Fengshan, Liu Gang, et al. 2021. Deformation failure mode and stability analysis of Kanuna unstable rock mass in Lhasa-Yangbajing section of G109 national highway[J]. Journal of Engineering Geology, 29(2): 495-507. doi: 10.13544/j.cnki.jeg.2019-093.
    Citation: Sun Qihao, Ma Fengshan, Liu Gang, et al. 2021. Deformation failure mode and stability analysis of Kanuna unstable rock mass in Lhasa-Yangbajing section of G109 national highway[J]. Journal of Engineering Geology, 29(2): 495-507. doi: 10.13544/j.cnki.jeg.2019-093.

    G109国道拉萨—羊八井段喀努纳危岩体变形破坏模式及稳定性分析

    DEFORMATION FAILURE MODE AND STABILITY ANALYSIS OF KANUNA UNSTABLE ROCK MASS IN LHASA-YANGBAJING SECTION OF G109 NATIONAL HIGHWAY

    • 摘要: 喀努纳危岩体发育于青藏铁路、G109国道和京藏高速公路的交汇路段,对交通工程施工建设和安全运营造成极大威胁。为了评价喀努纳危岩体的稳定程度,同时查明潜在崩塌的失稳条件和主控因素,深入系统地分析了危岩体的地质背景、发育特征及潜在变形破坏机理。利用块体理论和离散元方法,分别研究了自重条件和地震荷载作用下危岩体的稳定性及动力响应。研究表明,危岩体纵向上可以分为上部坡顶整体崩塌源、中部基岩裂隙带和下部块石堆积区,出露有4组优势结构面。通过计算得出,在自重条件下,危岩块体处于基本稳定状态;在地震荷载作用下,危岩体将会以剪切滑动、断裂坠落方式失稳;短时强震加剧了喀努纳危岩体内部损伤的累积。最后,文章给出了针对性防治和监测预警的建议。

       

      Abstract: The unstable rock mass develop in the intersection section of Qinghai-Tibet Railway, G109 National Highway and Beijing-Tibet Expressway, which pose a great threat to the construction and safe operation of traffic engineering. The geological background, development characteristics and deformation failure mechanism of the unstable rock mass are systematically analyzed in order to find out the instability conditions, the main controlling factors and to evaluate the stability. Using block theory and discrete element method, the stability and dynamic response of dangerous rock mass under dead weight condition and seismic load are studied respectively. The study shows that the unstable rock mass can be divided into three parts: the integral collapse source at the top, the fissure zone in the middle and the accumulation area of the block stone in the lower. and there are four groups of dominant structural planes. The calculation results show that the dangerous rock block is basically stable under the condition of dead weight. The unstable modes of dangerous rock mass under the action of seismic load are shear sliding, fracture and fall. Short-time violent earthquakes intensified the accumulation of internal damage in the unstable rock mass. To ensure safety, it is suggested to carry out targeted prevention and control, monitoring and early warning.

       

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