王毅, 杨建宏. 2015: 溪洛渡水电站河床坝基固结灌浆与检测评价. 工程地质学报, 23(s1): 499-503. DOI: 10.13544/j.cnki.jeg.2015.s1.076
    引用本文: 王毅, 杨建宏. 2015: 溪洛渡水电站河床坝基固结灌浆与检测评价. 工程地质学报, 23(s1): 499-503. DOI: 10.13544/j.cnki.jeg.2015.s1.076
    WANG Yi, YANG Jianhong. 2015: THE TEST AND ASSESSMENT OF CONSOLIDATION GROUTING IN RIVER BED DAM FOUNDATION OF XILUODU HYDROPOWER STATION. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 499-503. DOI: 10.13544/j.cnki.jeg.2015.s1.076
    Citation: WANG Yi, YANG Jianhong. 2015: THE TEST AND ASSESSMENT OF CONSOLIDATION GROUTING IN RIVER BED DAM FOUNDATION OF XILUODU HYDROPOWER STATION. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 499-503. DOI: 10.13544/j.cnki.jeg.2015.s1.076

    溪洛渡水电站河床坝基固结灌浆与检测评价

    THE TEST AND ASSESSMENT OF CONSOLIDATION GROUTING IN RIVER BED DAM FOUNDATION OF XILUODU HYDROPOWER STATION

    • 摘要: 金沙江溪洛渡水电站混凝土拱坝坝高285.5m, 河床坝基岩体为峨眉山玄武岩, Ⅲ1级岩体为主, 局部分布受错动带影响的Ⅲ2级岩体, 岩体声波平均速度4652ms-1, 小于4000ms-1约占28%。固结灌浆处理后, 坝基岩体的平均波速大于5200ms-1, 小于4000ms-1的比例多在5%以下, Ⅲ1级岩体平均波速达5300~5500ms-1, 波速提高约2%~5%, Ⅲ2级岩体平均波为4200~4700ms-1, 波速提高约12%~18%, 错动带平均波速3600~4200ms-1, 提高率在10%~28%左右, 岩体的透水率均小于3Lu, 钻孔变形模量平均值达到10.0~15GPa。固结灌浆对Ⅲ2级岩体和错动带等地质缺陷具有明显的改善作用, 坝基岩体的整体性和均一性得到了有效的提高。

       

      Abstract: Xiluodu hydropower station is located on the Jinshajiang River, with a 285.5m high arch dam. The bedrock of the dam foundation consists of basalt, which can be dominantly classified as Ⅲ-1 class with some local distribution of disturbed Ⅲ-2 class. The average acoustic velocity of the bedrock is originally 4652ms-1, with about 28% being slower than 4000ms-1.After consolidation grouting treatment, the average velocity is greater than 5200ms-1, with less than 5% being slower than 4000ms-1.After treatment, the average velocity of the Ⅲ-1 class bedrock has reached 5300~5500ms-1, being increased by 2%~5%; the Ⅲ-2 class 4200~4700ms-1, being increased by 12%~18%; the disturbed belt 3600~4200ms-1, being increased by 10%~28%, respectively. The rock permeability are less than 3 Lu and the average borehole deformation modulus is 10-15GPa. Consolidation grouting has dramatically improved the geological condition of the Ⅲ-2 class rock mass and the disturbed belt, which has effectively improved the integrity and homogeneity of the riverbed dam foundation.

       

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