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    动水驱动型滑坡的状态仿射迁移学习方法

    刘勇 李星瑞 詹伟文 李炳辰 郭敬楷 钟梁

    刘勇, 李星瑞, 詹伟文, 李炳辰, 郭敬楷, 钟梁, 2023. 动水驱动型滑坡的状态仿射迁移学习方法. 地球科学, 48(5): 1793-1806. doi: 10.3799/dqkx.2022.439
    引用本文: 刘勇, 李星瑞, 詹伟文, 李炳辰, 郭敬楷, 钟梁, 2023. 动水驱动型滑坡的状态仿射迁移学习方法. 地球科学, 48(5): 1793-1806. doi: 10.3799/dqkx.2022.439
    Liu Yong, Li Xingrui, Zhan Weiwen, Li Bingchen, Guo Jingkai, Zhong Liang, 2023. State Affine Transfer Learning Method for Hydrodynamic Pressure-Driven Landslide. Earth Science, 48(5): 1793-1806. doi: 10.3799/dqkx.2022.439
    Citation: Liu Yong, Li Xingrui, Zhan Weiwen, Li Bingchen, Guo Jingkai, Zhong Liang, 2023. State Affine Transfer Learning Method for Hydrodynamic Pressure-Driven Landslide. Earth Science, 48(5): 1793-1806. doi: 10.3799/dqkx.2022.439

    动水驱动型滑坡的状态仿射迁移学习方法

    doi: 10.3799/dqkx.2022.439
    基金项目: 

    国家自然科学基金重大项目 KZ21W30023

    国家自然科学基金面上项目 41772376

    详细信息
      作者简介:

      刘勇(1979-),男,博士,副教授,主要从事滑坡灾害、信息处理方面的研究工作.ORCID:0000-0001-6892-4320.E-mail:yongliu@cug.edu.cn

      通讯作者:

      钟梁, E-mail:zhongliang@cug.edu.cn

    • 中图分类号: P694

    State Affine Transfer Learning Method for Hydrodynamic Pressure-Driven Landslide

    • 摘要: 三峡库区的动水驱动型滑坡具有阶梯式变形特征,在监测数据不足的情况下,难以准确、合理地完成滑坡分析与预测预报等相关研究.针对监测数据不足的情况,设计了一种状态仿射迁移学习方法(State affine transfer learning method,SATLM),通过学习相似滑坡的知识完成对数据量不足的滑坡状态分析.为验证SATLM对滑坡状态分析的有效性,设计了一种状态相似分析方法,完成对库区多个滑坡的知识学习后实现对另一个数据量不足的滑坡地表位移预测.结果表明,完成状态仿射迁移后,本方法与BPNN和SVM相比,万州塘角1号滑坡地表位移预测的平均绝对误差和均方根误差都实现了较大降低.白家包滑坡、白水河滑坡、八字门滑坡知识的成功迁移,证明了SATLM在相似动水驱动型滑坡的知识迁移上具有较好效果.

       

    • 图  1  基本迁移学习模型示意

      Fig.  1.  Schematic diagram of basic transfer learning model

      图  2  状态仿射迁移学习方法流程

      Fig.  2.  The flowchart of state affine transfer learning method

      图  3  状态仿射迁移示意

      Fig.  3.  State affine transfer diagram

      图  4  白家包滑坡、白水河滑坡、八字门滑坡、万州塘角1号滑坡位置关系

      Fig.  4.  The locations of Baijiabao landslide, Baishuihe landslide, Bazimen landslide, Wanzhou Tangjiao No.1 landslide

      图  5  白家包滑坡(a)、白水河滑坡(b)、八字门滑坡(c)、万州塘角1号滑坡(d)剖面图(Long et al., 2022)

      Fig.  5.  The cross-section of Baijiabao landslide (a), Baishuihe landslide (b), Bazimen landslide (c), Wanzhou Tangjiao No.1 landslide (d) (Long et al., 2022)

      图  6  白家包滑坡(a)、白水河滑坡(b)、八字门滑坡(c)、万州塘角1号滑坡(d)GPS监测点分布图(Long et al., 2022)

      Fig.  6.  The locations of GPS monioring sites of (a) Baijiabao landslide, (b) Baishuihe landslide, (c) Bazimen landslide, (d) Wanzhou Tangjiao No.1 landslide (Long et al., 2022)

      图  7  白家包滑坡(a)、白水河滑坡(b)、八字门滑坡(c)、万州塘角1号滑坡(d)累积地表位移、库水位、降雨量关系(Li et al., 2021)

      Fig.  7.  Relationship between the cumulative displacement, reservoir water level and precipitation of Baijiabao landslide (a), Baishuihe landslide (b), Bazimen landslide (c), Wanzhou Tangjiao No.1 landslide (d) (Li et al., 2021)

      图  8  万州塘角1号滑坡地表位移预测对比

      Fig.  8.  The comparison of prediction results of Wanzhou Tangjiao No.1 landslide

      表  1  滑坡地表位移与影响因子灰色关联度统计

      Table  1.   Grey correlation degree statistics of landslide displacements and influence factors

      监测点
      名称
      Rt‒2 Rt‒1 Rt Kt‒2 Kt‒1 Kt Wt‒2 Wt‒1
      源域 ZG323 0.74 0.76 0.75 0.74 0.76 0.76 0.84 0.88
      ZG324 0.73 0.76 0.74 0.75 0.76 0.75 0.85 0.88
      ZG325 0.73 0.75 0.74 0.74 0.76 0.75 0.84 0.88
      ZG326 0.73 0.75 0.73 0.74 0.76 0.75 0.84 0.88
      ZG93 0.75 0.75 0.76 0.72 0.74 0.75 0.77 0.80
      ZG110 0.73 0.72 0.71 0.75 0.71 0.69 0.70 0.67
      ZG111 0.67 0.73 0.72 0.72 0.72 0.67 0.65 0.61
      目标域 WZ13-09 0.67 0.66 0.73 0.81 0.81 0.81 0.75 0.75
      下载: 导出CSV

      表  2  滑坡状态的分类情况

      Table  2.   Classification of landslide state

      ZG323 ZG324 ZG325 ZG326
      突变状态时间段 2009.06
      2010.07
      2011.06
      2012.06
      2013.06
      2009.06
      2010.07
      2011.06
      2012.06
      2013.06
      2009.06
      2010.07
      2011.06
      2012.06
      2013.06
      2009.06
      2010.07
      2011.06
      2012.06
      2013.06
      蠕变状态时间段 2008.03~2009.05
      2009.10~2010.06
      2010.10~2011.05
      2011.10~2012.05
      2012.10~2013.05
      2013.10~2013.12
      2008.03~2009.05
      2009.10~2010.06
      2010.10~2011.05
      2011.10~2012.05
      2012.10~2013.05
      2013.10~2013.12
      2008.03~2009.05
      2009.10~2010.06
      2010.10~2011.05
      2011.10~2012.05
      2012.10~2013.05
      2013.10~2013.12
      2008.03~2009.05
      2009.11~2010.06
      2010.11~2011.05
      2011.10~2012.05
      2012.10~2013.05
      2013.10~2013.12
      ZG93 ZG110 ZG111 WZ13-09
      突变状态时间段 2010.07
      2011.07
      2012.06
      2013.07
      2009.06
      2010.07
      2011.06
      2012.07
      2013.06
      2008.09
      2009.06
      2010.07
      2011.06
      2012.07
      2013.06
      2012.04
      2013.05
      蠕变状态时间段 2010.03~2010.06
      2010.12~2011.06
      2011.10~2012.05
      2012.11~2013.06
      2013.10~2013.12
      2008.03~2009.05
      2009.10~2010.06
      2010.10~2011.05
      2011.10~2012.06
      2012.10~2013.05
      2013.09~2013.12
      2008.03~2008.08
      2008.12~2009.05
      2009.10~2010.06
      2010.10~2011.05
      2011.10~2012.06
      2012.10~2013.05
      2013.09~2013.12
      2011.03~2012.03
      2012.07~2013.04
      2013.08~2014.05
      下载: 导出CSV

      表  3  3种方法预测结果的RMSE值和MAE值

      Table  3.   The RMSE and MAE values of three methods

      RMSE MAE
      SSAM 2.5 1.9
      BPNN 8.3 5.4
      SVM 8.5 5.1
      下载: 导出CSV
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    • 收稿日期:  2022-07-29
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