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    强震山区地震诱发滑坡发育规律与易发性评估

    李永威 徐林荣 张亮亮 陆志强 苏娜

    李永威, 徐林荣, 张亮亮, 陆志强, 苏娜, 2023. 强震山区地震诱发滑坡发育规律与易发性评估. 地球科学, 48(5): 1960-1976. doi: 10.3799/dqkx.2022.224
    引用本文: 李永威, 徐林荣, 张亮亮, 陆志强, 苏娜, 2023. 强震山区地震诱发滑坡发育规律与易发性评估. 地球科学, 48(5): 1960-1976. doi: 10.3799/dqkx.2022.224
    Li Yongwei, Xu Linrong, Zhang Liangliang, Lu Zhiqiang, Su Na, 2023. Study on Development Patterns and Susceptibility Evaluation of Coseismic Landslides within Mountainous Regions Influenced by Strong Earthquakes. Earth Science, 48(5): 1960-1976. doi: 10.3799/dqkx.2022.224
    Citation: Li Yongwei, Xu Linrong, Zhang Liangliang, Lu Zhiqiang, Su Na, 2023. Study on Development Patterns and Susceptibility Evaluation of Coseismic Landslides within Mountainous Regions Influenced by Strong Earthquakes. Earth Science, 48(5): 1960-1976. doi: 10.3799/dqkx.2022.224

    强震山区地震诱发滑坡发育规律与易发性评估

    doi: 10.3799/dqkx.2022.224
    基金项目: 

    国家自然科学面上项目 42172322

    国家自然科学基金项目 42007419

    国家重点研发计划项目 2018YFC1505403

    湖南省自然科学基金项目 2020JJ5981

    湖南省教育厅科学研究项目优秀青年基金项目 21B0226

    中南大学研究生自主探索创新项目 2022ZZTS0646

    详细信息
      作者简介:

      李永威(1994-), 男, 博士研究生, 主要从事地质灾害评估、防治与预警预报研究工作.E-mail: yongweili@csu.edu.cn

      通讯作者:

      徐林荣, E-mail: lrxu@csu.edu.cn

    • 中图分类号: P694

    Study on Development Patterns and Susceptibility Evaluation of Coseismic Landslides within Mountainous Regions Influenced by Strong Earthquakes

    • 摘要: 强震山区地形陡峭,植被茂盛,使同震滑坡“点多面广”,难以探测,为灾害防控带来困难.滑坡易发性评估能够预测灾害空间分布.但传统评估方法存在数据源有限、数据量化标准不一等问题,难以获取准确的易发性评价结果及难以掌握复杂孕灾环境下滑坡发育特征.鉴于此,通过多源监测数据、空间分析和深度学习方法,分析同震滑坡的发育规律,探究滑坡的地震响应机制,并进行滑坡易发性区划.结果表明:地震通过影响地形地貌的应力场及岩土体结构对地震波的地震响应的作用,使同震滑坡表现不同形式的发灾效应(如锁固段效应、微地形效应和地层倾向效应等);采用基于卷积神经网络(CNN)和深度神经网络(DNN)的深度学习模型取得了良好的易发性评价结果(AUC值分别为0.901和0.865),CNN模型的预测性能优于DNN模型.两模型精度都较高,均能较为准确识别潜在的滑坡区域;极高和高滑坡易发性区域广泛分布于丹祖沟等13条沟道中,这些沟道在暴雨下更容易发生泥石流.

       

    • 图  1  九寨沟研究区位置和地质构造

      Fig.  1.  Location and geological structure of Jiuzhaigou

      图  2  九寨沟同震滑坡孕灾环境因素

      Fig.  2.  Geo-environmntal factors of coseismic landslides in Jiuzhaigou

      图  3  本文采用的深度神经网络预测模型

      Fig.  3.  Predication model based on Deep Neural Networks in this work

      图  4  本文采用的卷积神经网络预测模型

      Fig.  4.  Predication model based on convolutional neural network in this work

      图  5  熊猫海和九寨天堂附近同震滑坡遥感影像解译实例;

      a、e为震前遥感影像;b、c、f和g为震后遥感影像

      Fig.  5.  Coseismic landslides interpretation based on remote sensing images near Panda Lake and Jiuzhai Paradise

      图  6  九寨沟野外地质灾害详查照片

      Fig.  6.  The field investigation photos in Jiuzhaigou scenic spot

      图  7  同震滑坡分布和密度分析

      Fig.  7.  Distribution and density of coseismic landslides

      图  8  滑坡孕灾环境因素敏感性分析

      Fig.  8.  Sensitivity analysis of geo-environmental factors for coseismic landslides

      图  9  滑坡与孕灾环境因素的空间关系

      Fig.  9.  Relationship of geo-environmental factors and coseismic landslides

      图  10  滑坡与地层岩性空间关系

      Fig.  10.  Relationship of lithology and coseismic landslides

      图  11  九寨沟地震滑坡易发性评价结果

      a、b分别为基于卷积神经网络和深度神经网络的滑坡易发性评价结果

      Fig.  11.  Coseismic landslide susceptibility mapping in Jiuzhaigou

      图  12  基于卷积神经网络和深度神经网络的滑坡易发性评价模型ROC曲线

      Fig.  12.  ROC curve of evaluation models of landslide susceptibility based on convolutional neural network (CNN) and deep neural network (DNN)

      表  1  遥感影像和地理数据

      Table  1.   Remote sensing image and geographic information data

      数据类型 数据来源 日期 分辨率
      遥感影像 Sentinel-2A 20170729 10 m
      20170907 10 m
      Google image 20151207 0.3 m
      20170814 0.3 m
      地震数据 美国地质调查局 20170808 矢量数据
      中国地震局 20170808 矢量数据
      地质数据 中国地质调查局 震前 1∶200 000
      地形数据 美国航空航天局 20110213 12.5
      下载: 导出CSV

      表  2  同震滑坡面积占各易发性区域的百分比

      Table  2.   Percentage of coseismic landslides in the susceptibility region

      DNN CNN
      滑坡占极高易发区(%) 64.71 77.33
      滑坡占高易发区(%) 20.26 11.45
      滑坡占中等易发区(%) 6.79 5.15
      滑坡占低易发区(%) 3.70 2.74
      滑坡占稳定区(%) 4.54 3.33
      下载: 导出CSV

      表  3  2017年九寨沟地震诱发滑坡相关研究对比结果

      Table  3.   Comparison of relevant studies on landslides triggered by the 2017 Jiuzhaigou earthquake

      研究区面积(km2 同震滑坡面积(km2 滑坡数量(个) 滑坡最大面积(104m2 最小面积(m2 遥感影像数据源
      戴岚欣等(2017)Fan et al. (2018) 840 8.11 1 883 23.1 9.7 SPOT5(2.5 m)、UAV(0.2 m)、GF-1、GF-2(1 m)
      许冲等(2018) / 9.6 4 800 / / GF-1与GF-2(0.8~2 m)、Google image(0.5 m)
      Wang et al. (2018) 651.3 11.8 2 212 20.9 10 Google image(1 m)、GF-2(4 m)、Sentinel-2A(10 m)、UAV
      Wu et al. (2018) 1 275 11.8 2 122 23.1 9.7 Google image(1 m)、GF-2(4 m)、Sentinel-2A(10 m)、UAV
      Tian et al. (2019) 434 9.64 4 834 23.6 7.8 Google image(0.5 m)
      Yi et al. (2020) 546.85 / 681 20.0 80 Sentinel-2A(10 m)、GF-1(2 m)、GF-2(1 m)
      Ling et al. (2021) 1 840 14.1 5 633 23.9 15 Google image(0.5 m)、GF-2(1 m)、UAV(0.2 m)、Sentinel-2A(10 m)
      Wang and Mao (2022) 938.9 9.45 5 431 24.3 6 Google image(0.3 m)、GF-1、GF-2(2 m)、Sentinel-2A(10 m)、Planet image(3m)
      本研究 1 330 10.56 5 487 24.3 5.5 Google image(0.3 m)、Sentinel-2A(10 m)
      注:UAV为Unmanned Aerial Vehicle images无人机影像; GF⁃1和GF⁃2分别为高分1号和2号影像.
      下载: 导出CSV
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    出版历程
    • 收稿日期:  2022-09-21
    • 网络出版日期:  2023-06-06
    • 刊出日期:  2023-05-25

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