Zhou Chao, Dong Zhihong, Zhou Chunhua, Fu Ping, Luo Sheng
Key Laboratory of Geotechnical Mechanics and Engineering of Ministry of Water Resources, Yangtze River Scientific Research Institute, Wuhan, 430010, Hubei, China.
State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, 430072, Hubei, China.
Sci Rep. 2024 Aug 5;14(1):18076. doi: 10.1038/s41598-024-69274-x.
The Qinling water conveyance tunnel has a large buried depth and high in-situ stress level, and rockburst disasters frequently occurred during excavation. In order to find out the mechanical mechanism of rockburst, the research work in this paper is as follows: (1) In-situ three-dimensional hydraulic fracturing method was used to measure the in-situ stress of the deep buried tunnel crossing the ridge. (2) Based on the measured in-situ stress results, the stress distribution characteristics of the tunnel crossing the ridge were obtained by the multiple linear regression method, and the rockburst tendency during construction was predicted. (3) A three-dimensional numerical model of tunnel excavation was established to analyze the dynamic adjustment characteristics of the surrounding rock stress and elastic strain energy during TBM excavation, and to clarify the mechanical mechanism of rockburst. The research results show that the maximum principal stress of the deep-buried tunnel crossing the ridge of Qinling is 40-66 MPa, which belongs to extremely high in-situ stress level, and medium-strong rockburst may occur during excavation. In the process of TBM excavation, the stress of the surrounding rock in the range of 2.6 times the diameter of the tunnel before and after the working face is adjusted violently, and the concentrated zones after the stress redistribution are mainly distributed in the arch roof and arch bottom, and the stress concentration coefficient can reach 2.06. The arch roof, arch waist, and arch bottom are susceptible to immediate rockburst due to stress transient unloading at the moment of excavation. After the elastic strain energy of the surrounding rock at the arch roof and the arch bottom is released and accumulated, it is easy to cause time delayed rockburst, and the depth of the rockburst pit can reach 3.5 m, which is consistent with the rockburst phenomenon in the field.
秦岭输水隧道埋深大、地应力水平高,开挖过程中岩爆灾害频发。为查明岩爆发生的力学机制,本文开展了以下研究工作:(1)采用现场三维水压致裂法测量了穿越山脊的深埋隧道地应力。(2)基于实测地应力结果,采用多元线性回归方法得到了穿越山脊隧道的应力分布特征,并对施工期间的岩爆倾向进行了预测。(3)建立了隧道开挖三维数值模型,分析了TBM开挖过程中围岩应力和弹性应变能的动态调整特征,阐明了岩爆发生的力学机制。研究结果表明,秦岭穿越山脊深埋隧道的最大主应力为40 - 66MPa,属于极高地应力水平,开挖过程中可能发生中强岩爆。在TBM开挖过程中,掌子面前后2.6倍洞径范围内的围岩应力调整剧烈,应力重分布后的集中区主要分布在拱顶和拱底,应力集中系数可达2.06。开挖瞬间,拱顶、拱腰和拱底因应力瞬间卸荷易发生即时岩爆。拱顶和拱底围岩弹性应变能释放并积累后,易引发延时岩爆,岩爆坑深度可达3.5m,与现场岩爆现象一致。