›› 2017, Vol. 38 ›› Issue (8): 2358-2367.doi: 10.16285/j.rsm.2017.08.025

• 岩土工程研究 • 上一篇    下一篇

基于离散元模拟和微震监测的白鹤滩水电站左岸岩质边坡稳定性分析

徐奴文1,李 韬1,戴 峰1,李 彪1,樊义林2,徐 剑2   

  1. 1. 四川大学 水利水电学院 水力学与山区河流开发保护国家重点实验室,四川 成都 610065;2. 中国长江三峡集团公司,北京 100038
  • 收稿日期:2015-09-18 出版日期:2017-08-11 发布日期:2018-06-05
  • 作者简介:徐奴文,男,1981年生,博士,副研究员,主要从事岩土工程灾害机理与微震监测方面的教学与研究工作
  • 基金资助:

    国家自然科学基金面上项目(No. 51679158);国家重点基础研究发展计划(973计划)(No. 2015CB057903)。

Stability analysis on the left bank slope of Baihetan hydropower station based on discrete element simulation and microseismic monitoring

XU Nu-wen1, LI Tao1, DAI Feng1, LI Biao1, FAN Yi-lin2, XU Jian2   

  1. 1. State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu, Sichuan 610065, China; 2. China Three Gorges Corporation, Beijing, 100038, China
  • Received:2015-09-18 Online:2017-08-11 Published:2018-06-05
  • Supported by:

    This work supported by the General Program of National Natural Science Foundation of China (51679158) and the National Program on Key Basic Research Project of China (No. 2015CB057903).

摘要: 西南地区水电站复杂高陡边坡的开挖稳定性一直是水电工程建设的关键技术问题之一。在研究金沙江白鹤滩水电站左岸边坡地形地貌、工程地质特性、地应力实测资料等基础上,利用通用离散元程序UDEC建立左岸顺层边坡离散元模型,进行开挖卸荷过程坝基边坡的稳定性分析,获得边坡开挖过程应力场、位移场、塑性区分布规律,揭示了顺层岩质边坡变形失稳机制。同时,结合左岸边坡开挖卸荷和应力调整过程微震活动特征,识别和圈定了左岸边坡深部岩体潜在损伤区域和滑裂面。综合研究结果表明,左岸边坡变形主要受构造应力、地质条件和开挖卸荷等综合因素影响,其中软弱结构面LS3318、LS3319、LS331、LS337、F17等对坝基边坡开挖变形起决定性作用。研究成果可为左岸边坡开挖和支护施工提供参考,同时也为类似顺层岩质边坡工程开挖支护提供研究思路。

关键词: 岩质边坡, 数值模拟, 离散元, 微震监测, 稳定性

Abstract: In southwestern of China, the stability problem of the complex high slopes subjected to excavation has become one of the key technical problems in the hydropower project construction. Based on the geomorphic conditions, characteristics of geologic framework and stress measurement data of the left bank slope of Baihetan hydropower station, by using the discrete element analysis procedure UDEC, a calculation model was established to study the stability of the left bank slope during excavation unloading. The principal stress field, deformation field and plastic yielded zones distribution law were studied under the condition of excavation, then the deformation mechanism of the left bank bedding rock slope has been declared. Meanwhile, the potential damage zone and critical sliding surface in deep rock mass were identified and delineated, by combination with the microseismic activity at the left bank slope during the periods of excavation and stress redistribution. The comprehensive studies indicated that the deformation of the left bank slope is mainly affected by multiple factors, such as tectonic stress, geological structure and unloading. The weak structure planes, such as LS3318, LS3319, LS331, LS337 and F17, play a decisive role in the excavation deformation of the left bank slope. The research results can provide valuable references for excavation and reinforcement of similar bedding rock slope projects.

Key words: rock slope, numerical simulation, distinct element, microseismic monitoring, stability

中图分类号: 

  • TU 457

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