王吉亮, 许琦, 肖云华, 白伟, 曾立, 宋涛, 魏雨军. 2015: 乌东德水电站泄洪洞进口边坡特殊岩体工程地质性状及稳定性研究. 工程地质学报, 23(s1): 465-471. DOI: 10.13544/j.cnki.jeg.2015.s1.071
    引用本文: 王吉亮, 许琦, 肖云华, 白伟, 曾立, 宋涛, 魏雨军. 2015: 乌东德水电站泄洪洞进口边坡特殊岩体工程地质性状及稳定性研究. 工程地质学报, 23(s1): 465-471. DOI: 10.13544/j.cnki.jeg.2015.s1.071
    WANG Jiliang, XU Qi, XIAO Yunhua, BAI Wei, ZENG Li, SONG Tao, WEI Yujun. 2015: STUDY OF ENGINEERING GEOLOGICAL FEATURES OF SPECIAL ROCK MASS AND ITS STABILITY OF SPILLWAY CUT SLOPE AT WUDONGDE HYDROPOWER STATION. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 465-471. DOI: 10.13544/j.cnki.jeg.2015.s1.071
    Citation: WANG Jiliang, XU Qi, XIAO Yunhua, BAI Wei, ZENG Li, SONG Tao, WEI Yujun. 2015: STUDY OF ENGINEERING GEOLOGICAL FEATURES OF SPECIAL ROCK MASS AND ITS STABILITY OF SPILLWAY CUT SLOPE AT WUDONGDE HYDROPOWER STATION. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 465-471. DOI: 10.13544/j.cnki.jeg.2015.s1.071

    乌东德水电站泄洪洞进口边坡特殊岩体工程地质性状及稳定性研究

    STUDY OF ENGINEERING GEOLOGICAL FEATURES OF SPECIAL ROCK MASS AND ITS STABILITY OF SPILLWAY CUT SLOPE AT WUDONGDE HYDROPOWER STATION

    • 摘要: 金沙江乌东德水电站左岸泄洪洞进口正面坡最大坡高150m, 边坡结构为反向坡。边坡主要位于中元古界会理群因民组第二段第一亚段(Pt22-1y)薄层状陡倾大理岩化白云岩地层中, 层面附绢云母薄膜, 层间劈理发育。岩体完整性较差, 岩体质量主要为Ⅳ级。本文通过岩石及充填物镜鉴、室内及现场物理力学试验等手段相结合的方法对该段岩体的岩性特征、结构特征、物理力学特性进行研究。以此为基础, 分析与评价由该岩体构成的边坡的稳定性与变形破坏模式, 为支护设计提供依据。通过变形监测成果分析, 说明边坡支护措施的有效性与及时支护的必要性。本文对由特殊地质体构成的边坡的稳定性研究工作具有重要的借鉴作用。

       

      Abstract: The slope of spillway of Wudongde Hydropower Station is a toppling rock slope with a height of 150m. The slope is composed of thin layered meta-dolomite rock mass from Mesoproterozoic YinMin Formation, cleavage develops between the layers and attach sericite film along bedding plane. Rock mass integrity is poor, and rock mass quality is mainly IV level. In view of this, this paper studies the rock mass from the view of engineering geology based on the combination of mineral chemical analysis and field physico-mechanical test, such as lithology characteristics, structure characteristics and mechanical property. This paper analyzes the deformation model and evaluates the stability of the slope according to the results, and provides a basis for the design. Monitoring results illustrate the effectiveness of the support measures and the importance of timely support. The research has important value to the stability analysis of slope composed of special geological body.

       

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