罗平平, 王兰甫, 高献伟, 张芳. 2011: 降雨入渗下高填强夯矿渣边坡滑坡机理研究. 工程地质学报, 19(6): 844-851.
    引用本文: 罗平平, 王兰甫, 高献伟, 张芳. 2011: 降雨入渗下高填强夯矿渣边坡滑坡机理研究. 工程地质学报, 19(6): 844-851.
    LUO Pingping, WANG Lanfu, GAO Xianwei, ZHANG Fang. 2011: LANDSLIDE MECHANISM OF DYNAMICALLY COMPACTED SLAG SLOPE UNDER RAINFALL INFILTRATION. JOURNAL OF ENGINEERING GEOLOGY, 19(6): 844-851.
    Citation: LUO Pingping, WANG Lanfu, GAO Xianwei, ZHANG Fang. 2011: LANDSLIDE MECHANISM OF DYNAMICALLY COMPACTED SLAG SLOPE UNDER RAINFALL INFILTRATION. JOURNAL OF ENGINEERING GEOLOGY, 19(6): 844-851.

    降雨入渗下高填强夯矿渣边坡滑坡机理研究

    LANDSLIDE MECHANISM OF DYNAMICALLY COMPACTED SLAG SLOPE UNDER RAINFALL INFILTRATION

    • 摘要: 义马煤业集团股份有限公司所属综能公司在建场地中部有一20m高矿渣边坡,矿渣为三叠系砂岩、泥岩,堆积至今已有10~50a。该边坡整体属软质岩石,多全风化土状和强风化状,砂岩碎块手刻可碎,结构疏松、分选性差、粒间结合力弱、透水性强。虽经强夯处理,但在2010年雨季期间在边坡中下部仍出现多处滑塌。为研究该高填强夯矿渣边坡在降雨入渗下的变形特征和滑坡机理,借助于弹塑性力学有限元和非饱和渗流力学等理论,建立了高填矿渣边坡的位移场-非饱和渗流场耦合数值模型,详细分析了降雨入渗条件下边坡的位移场、渗流压力分布、体积含水量和安全系数等特点。研究结果表明:随着降雨的持续进行,高填强夯矿渣边坡安全系数大幅降低; 强夯后边坡渗透性降低,渗流正压集中于坡顶一定深度范围内,且随着降雨的持续进行,渗流正压逐渐增加至稳定,负压值基本保持不变,但负压区逐渐缩小,表明负压对强夯矿渣边坡的影响有限,重点是做好该类边坡坡顶一定深度范围内的排水措施,以消减渗流正压; 正压区体积含水量上升至饱和状态; 持续降雨条件下坡脚出现剪切破坏,导致边坡中下部出现滑塌。其研究成果对于矿山矸石山边坡、尾矿坝、高填碎石土路基等渣土混合边坡稳定性研究有重要借鉴意义。

       

      Abstract: A 20m high slope lies in construction site of an energy company.The mine slag was stacked 10 to 50 years ago and wholly belongs to Triassic soft sandstone and mudstone.The slag shows weathered earthy and strong weathering state.The sandstone fragments can be promptly crushed by hand.The mine slag shows loose structure,poor sorting,weak adhesion and strong permeability.The slag composing the slope was treated with dynamic compaction.But,many positions of the slag slope still slid and collapsed during the rainy season in 2010.The landslide sites were located in the lower slope.This paper examines the landslide mechanism and deformation characteristics of the dynamically compacted slope highly filled with slag under rainfall infiltration.It uses elastic-plastic mechanics finite element method,unsaturated fluid mechanics and other theories.The corresponding numerical model for displacement-unsaturated seepage coupling is set up.Based on the numerical model,displacement field,seepage pressure distribution,volume water content and safety factor are studied in detailed.The numerical results indicate: (a)with continuous rainfall,the slope safety factor significantly reduces; (b)because of the lower permeability after dynamic compaction,seepage positive pressure focuses on the top of the slope within a certain depth and gradually increases and tends to stabilize under continuous rainfall.But the maximum negative seepage pressure value basically keeps stable and negative pressure zone shows diminishing.This shows negative pressure has a limited impact on slope filled with slag after dynamic compaction.Emphasis is to take good drainage measures within a certain depth range at the top of slope to reduce seepage positive pressure; (c)vol.water content gradually increases to saturated status; (d)shear failure occurs at the toe of slope under continuous rainfall,leading to collapse in the lower part of slope.The research results have an important reference value for studying on stability of slag-soil mixed slope,such as gangue hill,tailing dam,roadbed primed with gravel,et al.

       

    /

    返回文章
    返回