王猛, 石安池, 周家文, 范刚, 严鸿川, 李海波. 2021: 高地应力大型地下洞群围岩变形破坏响应特征分析. 工程地质学报, 29(S1): 18-27. DOI: 10.13544/j.cnki.jeg.2021-0469
    引用本文: 王猛, 石安池, 周家文, 范刚, 严鸿川, 李海波. 2021: 高地应力大型地下洞群围岩变形破坏响应特征分析. 工程地质学报, 29(S1): 18-27. DOI: 10.13544/j.cnki.jeg.2021-0469
    WANG Meng, SHI Anchi, ZHOU Jiawen, FAN Gang, YAN Hongchuan, LI Haibo. 2021: RESPONSE CHARACTERISTIC ANALYSIS OF THE DEFORMATION AND FAILURE OF SURROUNDING ROCK MASS IN A LARGE UNDERGROUND POWERHOUSE UNDER HIGH IN-SITU STRESS. JOURNAL OF ENGINEERING GEOLOGY, 29(S1): 18-27. DOI: 10.13544/j.cnki.jeg.2021-0469
    Citation: WANG Meng, SHI Anchi, ZHOU Jiawen, FAN Gang, YAN Hongchuan, LI Haibo. 2021: RESPONSE CHARACTERISTIC ANALYSIS OF THE DEFORMATION AND FAILURE OF SURROUNDING ROCK MASS IN A LARGE UNDERGROUND POWERHOUSE UNDER HIGH IN-SITU STRESS. JOURNAL OF ENGINEERING GEOLOGY, 29(S1): 18-27. DOI: 10.13544/j.cnki.jeg.2021-0469

    高地应力大型地下洞群围岩变形破坏响应特征分析

    RESPONSE CHARACTERISTIC ANALYSIS OF THE DEFORMATION AND FAILURE OF SURROUNDING ROCK MASS IN A LARGE UNDERGROUND POWERHOUSE UNDER HIGH IN-SITU STRESS

    • 摘要: 我国西南地区的水电工程多拥有尺寸规模庞大的地下厂房洞室群,受高地应力及复杂地质条件影响,洞群施工期间围岩变形破坏问题十分突出。文章以白鹤滩水电站右岸地下洞室群为工程案例,基于多点变位计连续监测成果,从量值、空间分布和时间演化3个方面分析了主副厂房围岩变形响应规律。并基于现场调查情况,对地下洞群施工期多种围岩破坏现象的响应特征进行了分析。最后结合初始地应力状态、岩体特性等影响因素,对上述围岩变形破坏的作用机制进行了探讨。研究结果表明,厂区方向与厂房轴线近似垂直的第二主应力对厂房应力调整起控制作用,开挖后在厂房上游拱肩和下游墙脚处产生应力集中,应力集中区内发生片帮、围岩破裂及喷护混凝土开裂等应力主导型破坏;高地应力环境下开挖使围岩强烈卸荷,导致厂房围岩变形整体较大并具有时间效应,拱圈及边墙局部围岩变形随开挖持续增长、收敛性较差。

       

      Abstract: The hydropower station in southwest China usually has large-scale underground powerhouse. Subjected to high in situ stress and complex geological condition, the construction of these powerhouses often encounters deformation and failure of surrounding rock mass. This paper takes the Baihetan right bank underground powerhouse as a case study, which is large-scale and under high in situ stress. Via site monitoring and field investigation, we analyzed the response characteristics of deformation and failure of surrounding rock mass in the underground powerhouse. With the factors including in situ stress and rock mass property, we discussed the mechanism of deformation and failure of surrounding rock mass. The results show that the second principal stress with a direction approximately perpendicular to the powerhouse axis plays a dominant role in the stress adjustment of the main powerhouse. When the main powerhouse was excavated, stress concentration zones formed at the upstream spandrel and the foot of downstream sidewall. In these two areas, stress-dominated failures occurred, such as spalling, surrounding rock mass fracture and shotcrete cracking. The underground excavation under high in situ stress causes strong unloading of surrounding rock mass, which leads to the large deformation with time effect. In the parts of arch and sidewalls, the surrounding rock mass deformation increased continuously as the stratified excavation progressed.

       

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