赵建军, 解明礼, 李涛, 谭盛宇, 巨能攀, 步凡. 2017: 饱水条件下千枚岩软化效应试验分析. 工程地质学报, 25(6): 1449-1454. DOI: 10.13544/j.cnki.jeg.2017.06.007
    引用本文: 赵建军, 解明礼, 李涛, 谭盛宇, 巨能攀, 步凡. 2017: 饱水条件下千枚岩软化效应试验分析. 工程地质学报, 25(6): 1449-1454. DOI: 10.13544/j.cnki.jeg.2017.06.007
    ZHAO Jianjun, XIE Mingli, LI Tao, TAN Shengyu, JU Nengpan, BU Fan. 2017: SOFTENING EFFECT OF PHYLLITE WITH WATER SATURATION. JOURNAL OF ENGINEERING GEOLOGY, 25(6): 1449-1454. DOI: 10.13544/j.cnki.jeg.2017.06.007
    Citation: ZHAO Jianjun, XIE Mingli, LI Tao, TAN Shengyu, JU Nengpan, BU Fan. 2017: SOFTENING EFFECT OF PHYLLITE WITH WATER SATURATION. JOURNAL OF ENGINEERING GEOLOGY, 25(6): 1449-1454. DOI: 10.13544/j.cnki.jeg.2017.06.007

    饱水条件下千枚岩软化效应试验分析

    SOFTENING EFFECT OF PHYLLITE WITH WATER SATURATION

    • 摘要: 水岩作用是造成水库岸边坡岩体强度劣化的主要因素,尤其对于千枚岩这类特殊性岩体,遇水时强度劣化现象尤为明显。本文以某边坡千枚岩为研究对象,设计了在不同饱水条件下的岩石常规三轴压缩试验,并综合分析试验结果随饱水时间变化规律。研究结果表明:千枚岩与水作用反应强烈,前60d岩石力学参数随饱水时间增加呈近线性降低,至70d逐渐趋于稳定,岩石变形逐渐由弹性变形为主演变为塑性变形为主;各参数劣化规律具有明显的时效性与非均匀性,随饱水时间增长,总体衰减幅度呈先增加后减小,最终趋于平稳的趋势;根据破裂面的剪切破坏模式,得出岩石饱水是一种从微观到宏观的累计损伤过程。该研究成果对于研究水库岸边坡岩体力学性质变化规律具有一定的参考价值。

       

      Abstract: Water-rock interaction is a main factor that weakens the rock mass strength of reservoir bank slope. Weaken strength for phyllite is especially obvious physical reacting with water. Taking the phyllite of a slope as example, this paper designs conventional triaxial compression tests under different saturated conditions and studies strength change law with saturated time. Results are obtained as follows:(1)the interaction between phyllite and water is strong. The rock strength parameters gradually decrease with the increase of water saturation time. For the first 60 days, the rock mass parameters linearly decrease with saturated time and tend to stable at 70 days. The mechanism gradually evolves elastic deformation to plastic deformation.(2)Weaken law of parameters shows obvious heterogeneity. The weaken degree is first large and then small, and finally tends to be stable.(3)According to shear failure mode, rock saturation is a cumulative process that from micro to macro. To sum up, the results of this paper have a certain reference value for studying the change law of mechanical property for rock mass of reservoir bank slopes.

       

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