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同震崩塌滑坡的光学遥感影像多特征融合解译方法

韩征, 方振雄, 傅邦杰, 吴斌晖, 李艳鸽, 李常丽, 陈光齐. 同震崩塌滑坡的光学遥感影像多特征融合解译方法[J]. 中国地质灾害与防治学报, 2022, 33(6): 103-113. doi: 10.16031/j.cnki.issn.1003-8035.202111008
引用本文: 韩征, 方振雄, 傅邦杰, 吴斌晖, 李艳鸽, 李常丽, 陈光齐. 同震崩塌滑坡的光学遥感影像多特征融合解译方法[J]. 中国地质灾害与防治学报, 2022, 33(6): 103-113. doi: 10.16031/j.cnki.issn.1003-8035.202111008
HAN Zheng, FANG Zhenxiong, FU Bangjie, WU Binhui, LI Yange, LI Changli, CHEN Guangqi. Interpretation method for regional co-seismic collapses based on multi-feature fusion of optical remote sensing[J]. The Chinese Journal of Geological Hazard and Control, 2022, 33(6): 103-113. doi: 10.16031/j.cnki.issn.1003-8035.202111008
Citation: HAN Zheng, FANG Zhenxiong, FU Bangjie, WU Binhui, LI Yange, LI Changli, CHEN Guangqi. Interpretation method for regional co-seismic collapses based on multi-feature fusion of optical remote sensing[J]. The Chinese Journal of Geological Hazard and Control, 2022, 33(6): 103-113. doi: 10.16031/j.cnki.issn.1003-8035.202111008

同震崩塌滑坡的光学遥感影像多特征融合解译方法

  • 基金项目: 国家重点研发计划专项(2018YFC1505401);国家自然科学基金面上项目(52078493);湖南省自然科学基金优秀青年项目(2021JJ20057);湖南创新型省份建设专项经费资助项目(2020RC3002);长沙市科技计划项目(kq2106018)
详细信息
    作者简介: 韩 征(1986-),男,福建永安人,博士,教授,博士生导师,主要从事地质灾害防治与数值模拟方面的研究工作。E-mail:zheng_han@csu.edu.cn
    通讯作者: 李艳鸽(1984-),女,河南巩义人,博士,副教授,博士生导师,主要从事灾害风险评价与遥感解译方面的研究工作。E-mail:liyange@csu.edu.cn
  • 中图分类号: P642.21

Interpretation method for regional co-seismic collapses based on multi-feature fusion of optical remote sensing

More Information
  • 同震崩塌滑坡的解译及定位是震区灾后恢复工作中需要重点解决的问题,如何在灾害快速、自动解译的基础上,不断提高解译精度,是目前同震崩塌滑坡解译的研究热点之一,也是促使地质灾害早期识别向智能化、科学化发展的必要前提。文章在团队前期所提出的遥感影像局部阈值二值化方法的基础上,针对同震崩塌滑坡解译结果假阳率偏高的问题,分析了假阳性地物的光学和几何特点,提出了融合目标区域光学影像灰度特征、区域坡度信息、NDVI指数特征及解译地物主轴特征的同震崩塌滑坡多特征融合解译方法。为验证所提出模型的准确性,以2014年云南鲁甸地震龙头山镇为研究区,利用震后获取的高分一号(GF-1)卫星影像数据及数字高程模型对该同震崩塌滑坡进行了解译识别,结果表明,文中提出的方法准确解译出了同震崩塌滑坡区域,并有效去除了假阳性地物干扰,提高了解译精度。

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  • 图 1  方法流程示意图

    Figure 1. 

    图 2  全色影像局部阈值二值化初步检测流程图

    Figure 2. 

    图 3  计算主轴特征示意图

    Figure 3. 

    图 4  主轴轴向特征示意图

    Figure 4. 

    图 5  鲁甸县龙头山镇影像(影像数据来源于高分一号卫星2014年8月20日影像数据)

    Figure 5. 

    图 6  局部阈值二值化分割结果

    Figure 6. 

    图 7  融合坡度信息的判定结果

    Figure 7. 

    图 8  融合主轴轴向特征的判定结果

    Figure 8. 

    图 9  融合NDVI指数特征的判定结果

    Figure 9. 

    图 10  研究区震前影像(影像数据来源于WorldView-2卫星2011年12月6日影像数据)

    Figure 10. 

    图 11  目视解译结果示意图(红色区域为同震崩塌滑坡,蓝色区域为挖方边坡等疑似地物)

    Figure 11. 

    表 1  原始数据参数信息表

    Table 1.  Information of the input data

    原始数据谱段范围/μm空间分辨率/m
    高分一号(GF-1)
    卫星影像数据
    0.45~0.902.00
    0.45~0.528.00
    0.52~0.59
    0.63~0.69
    0.77~0.89
    数字高程模型DEM30.00
    下载: 导出CSV

    表 2  检测解译效果统计

    Table 2.  Detection and interpretation effect statistics

    识别
    阶段
    方法崩塌
    数量
    真阳率
    /%
    假阳数假阳率
    /%
    1局部阈值二值化、
    地形坡度特征(图7
    4110025156.3
    2局部阈值二值化、地形坡度特征、
    主轴轴向特征(图8
    3410018112.5
    3局部阈值二值化、地形坡度特征、
    主轴轴向特征、NDVI指数特征(图9
    16100323.1
    4目视解译(图1116
    下载: 导出CSV
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出版历程
收稿日期:  2021-11-03
修回日期:  2022-01-28
刊出日期:  2022-12-25

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