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Study on the Influence of Water–Rock Interaction on the Stability of Schist Slope

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  • Qian-Cheng Sun

    (Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, China Three Gorges University, Yichang 443002, China
    National Field Observation and Research Station of Landslides in Three Gorges Reservoir Area of Yangtze River, China Three Gorges University, Yichang 443002, China)

  • Can Wei

    (Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, China Three Gorges University, Yichang 443002, China)

  • Xi-Man Sha

    (Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, China Three Gorges University, Yichang 443002, China)

  • Bing-Hao Zhou

    (Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, China Three Gorges University, Yichang 443002, China)

  • Guo-Dong Zhang

    (National Field Observation and Research Station of Landslides in Three Gorges Reservoir Area of Yangtze River, China Three Gorges University, Yichang 443002, China)

  • Zhi-Hua Xu

    (Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, China Three Gorges University, Yichang 443002, China
    National Field Observation and Research Station of Landslides in Three Gorges Reservoir Area of Yangtze River, China Three Gorges University, Yichang 443002, China)

  • Ling Cao

    (Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, China Three Gorges University, Yichang 443002, China)

Abstract

(1) The studies on the influence of rainfall on slope stability mainly focus on rainfall characteristics and the variation of strength parameters. Few studies pay attention to the micro structure changes of rock mass under long-term rainfall conditions, and the influence of failure mode. (2) Based on nuclear magnetic resonance (NMR) and electron microscopic imaging (Emmi) technology, the micro structure changes and macro deformation characteristics of the schist, under long-term immersion in different liquids are analyzed. (3) After soaking in the deionized water, the uniaxial compression strength of the intact specimen is slightly lower than that of the untreated specimens, but the test process in the elastic compression stage is considerably prolonged, and the failure modes show both shear and slip at the same time. While after soaking in acid solution, the fracture of rock samples with initial cracks can be obviously reduced and healed, which is consistent with the change of micro pore structure. The uniaxial strength and modulus of the intact samples are significantly lower, and only slip failure mode occurred. (4) It shows that water–rock interaction is an important factor influencing the stability of slope besides the external rainfall force, which affects the structural characteristics and mechanical properties of rock.

Suggested Citation

  • Qian-Cheng Sun & Can Wei & Xi-Man Sha & Bing-Hao Zhou & Guo-Dong Zhang & Zhi-Hua Xu & Ling Cao, 2020. "Study on the Influence of Water–Rock Interaction on the Stability of Schist Slope," Sustainability, MDPI, vol. 12(17), pages 1-14, September.
    • Handle: RePEc:gam:jsusta:v:12:y:2020:i:17:p:7141-:d:407371
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    References listed on IDEAS

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    1. Zhi-Hua Xu & Guang-Liang Feng & Qian-Cheng Sun & Guo-Dong Zhang & Yu-Ming He, 2020. "A Modified Model for Predicting the Strength of Drying-Wetting Cycled Sandstone Based on the P-Wave Velocity," Sustainability, MDPI, vol. 12(14), pages 1-17, July.
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