胡刘洋, 张鹏, 黄波林. 2023. 三峡库区消落带岩体劣化下危岩体长期变形破坏机理——以冠木岭为例[J]. 工程地质学报, 31(6): 1891-1900. doi: 10.13544/j.cnki.jeg.2022-0260.
    引用本文: 胡刘洋, 张鹏, 黄波林. 2023. 三峡库区消落带岩体劣化下危岩体长期变形破坏机理——以冠木岭为例[J]. 工程地质学报, 31(6): 1891-1900. doi: 10.13544/j.cnki.jeg.2022-0260.
    Hu Liuyang, Zhang Peng, Huang Bolin. 2023. Long-term deformation and failure mechanism of dangerous rock mass in water-level-fluctuation zone of Three Gorges Reservoir area: a case study of Guanmuling[J]. Journal of Engineering Geology, 31(6): 1891-1900. doi: 10.13544/j.cnki.jeg.2022-0260.
    Citation: Hu Liuyang, Zhang Peng, Huang Bolin. 2023. Long-term deformation and failure mechanism of dangerous rock mass in water-level-fluctuation zone of Three Gorges Reservoir area: a case study of Guanmuling[J]. Journal of Engineering Geology, 31(6): 1891-1900. doi: 10.13544/j.cnki.jeg.2022-0260.

    三峡库区消落带岩体劣化下危岩体长期变形破坏机理——以冠木岭为例

    LONG-TERM DEFORMATION AND FAILURE MECHANISM OF DANGEROUS ROCK MASS IN WATER-LEVEL-FLUCTUATION ZONE OF THREE GORGES RESERVOIR AREA: A CASE STUDY OF GUANMULING

    • 摘要: 三峡库区水位周期性变动导致消落带岩体劣化,加速了库区部分危岩体朝不稳定方向发展,潜在涌浪灾害威胁长江航道。本文以冠木岭危岩体为研究对象,阐述了冠木岭危岩体下部软弱层在收到上部荷载作用及库水波动影响下,岩体强度不断减弱,最终演化为倾倒滑移或基座压裂座滑的破坏模式。使用抗剪强度折减法计算了5种工况下随水位周期该危岩体的稳定性系数,结果表明:在现状自然工况下危岩体处于基本稳定状态,稳定性系数大约在1.3;在劣化工况下,强度以每个周期下降1%的速率进行折减,岩体劣化与强降雨+岩体劣化两种工况下,在20个水文周期的库水变动影响下,稳定性系数维持在1.1以上,处于基本稳定状态;库水+岩体劣化工况下稳定性系数由1.3下降到1.0,稳定性状态也从稳定状态过渡到极限平衡状态;库水+强降水+岩体劣化工况处于极限平衡-不稳定状态,在此种最不利条件下,危岩位移量达到11 m,稳定性系数下降到0.76,危岩处于不稳定状态;在经过长达20个水文周期的库水位变化后,考虑岩体劣化工况下的冠木岭危岩已处于极限平衡状态或不稳定状态,建议开展专项岩体劣化防治,提高危岩体稳定性,以保障航道安全。

       

      Abstract: The periodic fluctuation of water level in the Three Gorges reservoir area leads to the deterioration of rock mass in the water-level-fluctuation zone, which accelerates the unstable development of some dangerous rock masses in the reservoir area and threatens the Yangtze River waterway with potential surges. This paper takes Guanmuling dangerous rock mass as the research object, and expounds that under the influence of the upper load and the fluctuation of reservoir water, the strength of the weak layer in the lower part of the Guanmuling dangerous rock mass is continuously weakened, and finally evolves into the failure mode of tipping-slip or base fracturing and seat-slip. The stability coefficient of the dangerous rock mass is calculated with the shear strength reduction method under five working conditions. The results show the follows. The dangerous rock mass is basically stable under the current natural working conditions, and the final stability coefficient is 1.3. Under the deterioration condition, the strength is reduced at the rate of 1% per cycle. Under the two conditions of rock mass deterioration and heavy rainfall plus rock mass deterioration, the stability coefficient remains above 1.1 under the influence of 20 hydrological cycles' reservoir water change, which is basically stable. Under the condition of reservoir water and rock mass deterioration, the stability coefficient changes from 1.3 to 1.0, and the stability state also changes from stable state to limit equilibrium state. Reservoir water and heavy precipitation and rock mass deterioration are in the limit equilibrium to unstable state. Under the most unfavorable condition, the displacement of dangerous rock reaches 11 m, the stability coefficient drops to 0.76, and the dangerous rock is in an unstable state. After 20 hydrological cycles of periodic water level change, Guanmuling dangerous rock under rock deterioration condition is in limit equilibrium state or unstable state. It is suggested to carry out special rock deterioration prevention and control to improve the stability of dangerous rock mass and ensure the safety of waterway.

       

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