炭质泥岩路堑边坡湿化变形模拟分析
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U213.1+3

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国家自然科学基金资助项目(51378082,51674041);湖南省研究生科研创新项目(CX20200839)


Simulation analysis of wetting deformation of carbonaceous mudstone cutting slope
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    摘要:

    为探究炭质泥岩路堑边坡湿化前、后的变形规律,通过三轴压缩试验确定邓肯?张 EB 模型的参数,并利 用 FLAC3D软件模拟了不同坡高、坡比的炭质泥岩路堑边坡的湿化变形。研究结果表明:坡比为 1︰1.5、坡高为 16 m 的二级炭质泥岩路堑边坡的干态、湿态的最大水平位移、竖向位移均发生在一级、二级边坡坡顶。湿化后的 最大水平位移、竖直位移均增大;在坡比相同时,随着坡高增加,边坡水平和竖直方向的湿化变形均增大,竖直 方向湿化变形约为水平方向湿化变形的 5~10 倍;在坡高相同时,对于坡比的增加,边坡水平与竖直方向的湿化 变形规律不明显。

    Abstract:

    To explore the wetting deformation laws of carbonaceous mudstone cutting slopes, the parameters of Duncan-Chang EB model were determine by carrying out triaxial compression tests. The wetting deformation of carbonaceous mudstone cutting slopes with different slope heights and slope ratios were simulated by FLAC3D. The simulation results indicate that the maximum horizontal displacement and vertical displacement of 16 m secondary carbonaceous mudstone cutting slope with a slope ratio of 1:1.5 per level in dry and wet occurred on the top of the firstly slope and the secondary slope, respectively. Both the maximum horizontal and vertical displacement after humidification increased. When the slope ratio remains constant, the horizontal and vertical wetting deformation of the slope increase with the increase of the slope height. The vertical wetting deformation is about 5~10 times of the horizontal wetting deformation. At the same slope height, the change of the horizontal and vertical slope wetting deformation is not obvious with the increase of the slope ratio.

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刘新喜,邓子君,李盛南,等.炭质泥岩路堑边坡湿化变形模拟分析[J].交通科学与工程,2021,37(1):1-6.
LIU Xin-xi, DENG Zi-jun, LI Sheng-nan, et al. Simulation analysis of wetting deformation of carbonaceous mudstone cutting slope[J]. Journal of Transport Science and Engineering,2021,37(1):1-6.

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  • 在线发布日期: 2022-06-06
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