文章摘要
刘思杰, 王 凯, 蔡 浩.白鹤滩水电站左岸地下厂房围岩破坏研究Journal of Water Resources and Water Engineering[J].,2017,28(5):232-236
白鹤滩水电站左岸地下厂房围岩破坏研究
Study on damage mechanism of surrounding rock at the underground powerhouse of Baihetan hydropower station
  
DOI:10.11705/j.issn.1672-643X.2017.05.38
中文关键词: 片帮破坏  地应力  围岩开裂  围岩破坏  地下厂房  白鹤滩水电站
英文关键词: rib spalling  geostress  cracking of surrounding rock  damage of surrounding rock  underground powerhouse  Baihetan hydropower station
基金项目:国家自然科学基金项目(51374149)
Author NameAffiliation
LIU Sijie1, WANG Kai2, CAI Hao3 1.重庆交通大学 河海学院 重庆 400074 2.中国长江电力股份有限公司湖北 宜昌 443002 3.中国电建集团华东勘测设计研究院有限公司 浙江 杭州 311122 
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中文摘要:
      为了研究白鹤滩水电站左岸地下厂房围岩变形破坏问题,通过对厂房的现场调查,对其基本破坏类型进行归纳:片帮剥落、围岩外鼓、围岩开裂,并存在渗漏、异类物质析出等现象。同时结合数值模拟,对开挖期间围岩破坏机理进行分析。结果表明:在开挖作用下,左岸地下厂房应力进行二次分布,并在上游顶拱、拱肩及边墙部位围岩形成多个应力集中区,超过围岩片帮破坏临界界值,最终发生片帮等多种破坏。主厂房上游存在多个长大裂隙,其力学参数低,承载能力弱,在开挖作用下诱发主厂房上游发生诸如围岩外鼓折断、裂隙开裂、渗水、钙类物质析出等多种围岩破坏,并导致其临近区域应力异常增大,甚至出现片帮破坏。在后期开挖过程中应密切关注主厂房上游围岩稳定性。
英文摘要:
      In order to study the deformation and damage of the surrounding rock of the left bank underground powerhouse of Baihetan Hydropower Station, through the field investigation of the main powerhouse,the primary destruction types are classified as rib spalling,bellying of surrounding; creepage and the precipitating of calcium. A calculation model was established to study the damage mechanism of the left bank underground powerhouse during excavation unloading. The result indicated that the geostress of the left bank underground powerhouse redistributes under the influence of the excavation, which results in several stress concentration at the roof of arch, spandrel and the sidewall of upside main powerhouse where the major principal stress exceeded critical value, leading to various damages of the surrounding rock. There were many long cracks with poor mechanical properties and weak carrying capacity, which will trigger bellying of surrounding, creepage and the precipitating of calcium in the upstream of the main powerhouse under excavation. And the cracks will induce abnormal increase of geostress in close region and rib spalling of the surrounding rock. The stability of the surrounding rock of the upstream should be paid close attention.
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