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    锁固段边坡模型破坏前兆特征

    朱星 唐垚

    朱星, 唐垚, 2022. 锁固段边坡模型破坏前兆特征. 地球科学, 47(6): 1957-1968. doi: 10.3799/dqkx.2021.204
    引用本文: 朱星, 唐垚, 2022. 锁固段边坡模型破坏前兆特征. 地球科学, 47(6): 1957-1968. doi: 10.3799/dqkx.2021.204
    Zhu Xing, Tang Yao, 2022. Failure Precursory Characteristics of Slope Model with Locked Section. Earth Science, 47(6): 1957-1968. doi: 10.3799/dqkx.2021.204
    Citation: Zhu Xing, Tang Yao, 2022. Failure Precursory Characteristics of Slope Model with Locked Section. Earth Science, 47(6): 1957-1968. doi: 10.3799/dqkx.2021.204

    锁固段边坡模型破坏前兆特征

    doi: 10.3799/dqkx.2021.204
    基金项目: 

    国家自然科学基金重大专项资助 41941019

    国家自然科学基金面上项目 41877254

    第二次青藏高原综合科学考察研究资助 2019QZKK0201

    详细信息
      作者简介:

      朱星(1984-),男,博士,副教授,博士生导师,主要从事于岩土(地质)工程监测预警研究. ORCID:0000-0002-0602-7823.E-mail:zhuxing_84@qq.com

      通讯作者:

      唐垚,E-mail:960511411@qq.com

    • 中图分类号: P694

    Failure Precursory Characteristics of Slope Model with Locked Section

    • 摘要: 为探究花岗岩锁固段边坡模型损伤破坏过程中的微震信号能量、频率分布特征及临界慢化现象,开展了花岗岩锁固段边坡模型的破坏试验研究,利用单轴加载系统对不同岩桥角度的花岗岩锁固段边坡模型进行加载,采用应变片、微震(microseismic,MS)监测系统对其加载全过程进行同步观测.试验结果表明:(1)岩桥角对边坡模型的破坏形式产生影响,当岩桥角为70°和90°时破坏形式以拉张破坏为主;当岩桥角为110°时为拉压混合破坏;当岩桥角为130°时为压剪破坏,前缘蠕滑段为锁固型边坡变形最大的部位.(2)在加载过程中,当存在微小损伤破裂时,主要以高频、低能的微震信号为主,当产生大尺度损伤破裂时会伴随着低频、高能的微震信号.(3)在锁固段边坡模型处于临界破坏状态时会出现明显的临界慢化现象,表现为微震信号的方差、自相关系数产生突增现象,且突增点所对应的时间均达到失稳时间的80%,具有较好的时效性,可将微震信号的方差、自相关系数的突增作为边坡模型的失稳破坏前兆信息.(4)能量比方法与临界慢化理论形成联合预测判据,可克服单一判据的缺点,提高预测的准确性.该研究可为突发型的岩质边坡监测预警提供可用的参考价值.

       

    • 图  1  “三段式”滑坡示意图

      黄润秋等(2017)黄达等(2018)

      Fig.  1.  Sketch of "Three sections" landslide

      图  2  锁固段边坡模型

      α为后缘裂缝与顶部的夹角;β分为70°、90°、110°和130°;γ为前缘裂缝与坡面的夹角

      Fig.  2.  Geometric parameter model of locked section slope model

      图  3  加载系统及数据采集系统

      Fig.  3.  Loading system and data acquisition system

      图  4  锁固段边坡模型变形特征

      a.70°锁固段边坡模型; b.90°锁固段边坡模型; c.110°锁固段边坡模型; d.130°锁固段边坡模型

      Fig.  4.  Deformation characteristics of locked section slope model

      图  5  70°模型各频段频率分布特征

      Fig.  5.  Frequency distribution characteristics of each frequency band of the 70° model

      图  6  各频段信号及能量贡献率

      Fig.  6.  Signal and energy contribution of each frequency band

      图  7  瞬时能量比

      Fig.  7.  Instantaneous energy ratio

      图  8  边坡模型破坏的临界慢化特征

      Fig.  8.  Critical slowing characteristics of slope model failure

      图  9  联合前兆特征

      Fig.  9.  Joint precursor characteristics

      表  1  小波变换结果

      Table  1.   Wavelet transform result

      频段号 变换后信号 频宽(Hz)
      1
      2
      3
      4
      5
      6
      7
      8
      a7
      d7
      d6
      d5
      d4
      d3
      d2
      d1
      0~3.906 3
      3.906 3~7.812 6
      7.812 6~15.625 2
      15.625 2~31.250 4
      31.250 4~62.500 8
      62.500 8~125.001 6
      125.001 6~250.003 2
      250.003 2~500.000 0
      下载: 导出CSV
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    • 收稿日期:  2021-10-01
    • 刊出日期:  2022-06-25

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