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李协生. 渔子溪一级水电站地下厂房围岩应力和变形的分析探讨[J]. 岩土工程学报, 1980, 2(2): 34-48.
引用本文: 李协生. 渔子溪一级水电站地下厂房围岩应力和变形的分析探讨[J]. 岩土工程学报, 1980, 2(2): 34-48.
Li Xie-sheng. Analysis and Discussion on Stress and Deformation of the Surrounding Rock in the Underground Hydroelectric Power Plant of the Fishermans' Creek I[J]. Chinese Journal of Geotechnical Engineering, 1980, 2(2): 34-48.
Citation: Li Xie-sheng. Analysis and Discussion on Stress and Deformation of the Surrounding Rock in the Underground Hydroelectric Power Plant of the Fishermans' Creek I[J]. Chinese Journal of Geotechnical Engineering, 1980, 2(2): 34-48.

渔子溪一级水电站地下厂房围岩应力和变形的分析探讨

Analysis and Discussion on Stress and Deformation of the Surrounding Rock in the Underground Hydroelectric Power Plant of the Fishermans' Creek I

  • 摘要: 本电站地下厂房的地质条件比较复杂。施工过程中,建筑物的围岩发生较明显的变形,多处混凝土衬护出现较密集的裂缝,引起关心和重视。为了监测和研究围岩的整体稳定性和建筑物结构的受力情况,按装了内部原型观测和外部裂缝观测设备。为了研究地下洞室的永久运行安全性,还进行了岩石力学和有限单元分析计算工作。综合分析表明,产生围岩变形和混凝土衬护裂缝的主要原因是岩体内地应力大,及开挖后侧向应力解除所致。边墙经采取适当的加固措施而趋于稳定。对中间岩柱的分析表明.应力分布不均一,应力增长尚不过大,且局限于较小的范围内;剪应力也不太大。因此,可以认为岩柱仍然是稳定的。今后还要继续加强原型观测和研究工作。

     

    Abstract: The severe deformation and cracking due to complex geological conditions in linings in the construction of this underground hydroelectric power plant has caused considerable concern. To monitor and investigate the stability of the surrounding rock and the behavior of reinforced concrete construction, field instrumentation has been set up and utilized, crack monitoring system was established. For the permanent stability of the underground caverns, further rock mechanics analysis and finite element analysis have been made. By synthesizing these findings, it has been shown tentatively that the "Earth Crust" stress is large and excavation induces stress redistribution in the surrounding rock. The stability of side walls has become stable by adopting some justifiable strengthening measures. Analysis shows also that the stress distribution is non-uniform, the excessive stress is increased not large and is localized in a relatively small zone in the rock pillar, and the shearing stress is not excessive. Therefore the rock pillar is still stable. Further investigations and field measurements are still under way.

     

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