含泥化夹层岩质边坡地震响应特征振动台试验及数值模拟
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作者单位:

1.云南省交通综合行政执法局质监支队;2.西安工业大学建筑工程学院;3.长安大学公路学院

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中图分类号:

TU416.1+4

基金项目:

基金项目:基于冰楔-渗流耦合作用的寒区黄土斜坡失稳机制研究,国家自然科学基金面上项目(批准号:42372323)


Shaking Table Test and Numerical Simulation of Seismic Response Characteristics of Rock Slope with Muddy Interlayer
Author:
Affiliation:

1.Quality Supervision Detachment of Yunnan Provincial Transportation Comprehensive Administrative Law Enforcement Bureau;2.School of Civil&3.Architecture Engineering, Xi'4.'5.an Technological University;6.School of Highway, Chang’an University

Fund Project:

Study on the instability mechanism of loess slopes in cold regions based on the coupling effect of ice wedge and seepage

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    摘要:

    为研究含泥化夹层岩质边坡的地震宏观破坏过程及动力响应特征,揭示泥化夹层对边坡稳定性的影响,设计凹凸两种坡型的相似边坡模型,开展振动台试验,采用有限元分析进行数值建模分析,将二者得出的结果进行对比。结果表明:试验模型边坡的宏观变形破坏过程为:①泥化夹层错动,裂缝产生;②泥化夹层滑移,裂缝扩展;③坡体崩塌破坏。地震荷载对边坡稳定性有着决定性因素,随着地震加速度幅值的增大,边坡破坏越严重。泥化夹层在试验中率先出现张拉裂缝,是边坡的薄弱部位,也是地震荷载下诱发边坡失稳的重要原因。两种边坡的地震加速度响应特征为:随着地震荷载的增大,两种边坡的PGA放大系数先明显增大再缓慢减小;二者PGA放大系数曲线趋势基本一致,在第三层夹层附近及坡肩处数值明显大于其他测点;凹型边坡PGA放大系数整体稍大于凸型边坡,折线趋势更曲折,呈现出的放大效应更加复杂。数值模拟在地震加速度幅值为0.6g时边坡失稳破坏。凹凸两种坡型边坡的破坏模式略有不同,凹型边坡破坏模式为:坡肩崩塌,变坡点附近滑移破坏;凸型边坡破坏模式为:变坡线崩塌破坏。凸型边坡的抗震稳定性略好于凹型边坡。

    Abstract:

    In order to study the seismic macro-failure process and dynamic response characteristics of rock slope with muddy interlayer,and reveal the influence of muddy interlayer on slope stability, a similar slope model with concave and convex slope types was designed,shaking table test was carried out,and finite element analysis was used for numerical modeling analysis,and the results obtained by the two models were compared.The results show that:The macroscopic deformation and failure process of the model slope is as follows:①Mud interlayer dislocates and cracks occur;②Mud interlayer slips and cracks expand;③Slope collapse.The earthquake has a decisive factor on the stability of the slope.With the increase of the earthquake load,the peak acceleration of the slope increases and the damage becomes more serious.In the testthe clay interlayer is the first to appear tensile crack,which is the weak part of the slope and the important reason for the slope instability induced by earthquake load.The seismic acceleration response characteristics of the two slopes are as follows: with the increase of seismic load, the PGA amplification coefficient of the two slopes first significantly increases and then slowly decreases.The curve trend of PGA amplification coefficient is basically the same. The values near the third layer interlayer and at the slope shoulder are significantly higher than other measurement points.The PGA amplification factor of concave slope is slightly larger than that of convex slope,and the trend of broken line is more tortuous,showing more complicated amplification effect. Numerical simulation of slope instability and failure under seismic acceleration amplitude of 0.6g.The failure modes of concave and convex slopes are slightly different.The failure modes of concave slopes are:slope shoulder collapse,sliding failure near the changing slope point;The failure mode of convex slope is:slope line collapse failure.The seismic stability of convex slope is slightly better than that of concave slope.

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  • 收稿日期:2023-09-07
  • 最后修改日期:2024-03-16
  • 录用日期:2024-04-17
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