基于逻辑回归的四川青川县区域滑坡灾害预警模型

方然可, 刘艳辉, 苏永超, 黄志全. 基于逻辑回归的四川青川县区域滑坡灾害预警模型[J]. 水文地质工程地质, 2021, 48(1): 181-187. doi: 10.16030/j.cnki.issn.1000-3665.201911034
引用本文: 方然可, 刘艳辉, 苏永超, 黄志全. 基于逻辑回归的四川青川县区域滑坡灾害预警模型[J]. 水文地质工程地质, 2021, 48(1): 181-187. doi: 10.16030/j.cnki.issn.1000-3665.201911034
FANG Ranke, LIU Yanhui, SU Yongchao, HUANG Zhiquan. A early warning model of regional landslide in Qingchuan County, Sichuan Province based on logistic regression[J]. Hydrogeology & Engineering Geology, 2021, 48(1): 181-187. doi: 10.16030/j.cnki.issn.1000-3665.201911034
Citation: FANG Ranke, LIU Yanhui, SU Yongchao, HUANG Zhiquan. A early warning model of regional landslide in Qingchuan County, Sichuan Province based on logistic regression[J]. Hydrogeology & Engineering Geology, 2021, 48(1): 181-187. doi: 10.16030/j.cnki.issn.1000-3665.201911034

基于逻辑回归的四川青川县区域滑坡灾害预警模型

  • 基金项目: 国家重点研发计划(2018YFC1505503);国家自然科学基金项目(42077440;41202217);国家科技支撑计划子课题(2015BAK10B021)
详细信息
    作者简介: 方然可(1996-),男,硕士研究生,主要从事地质灾害预警相关研究工作。E-mail: 1361853780@qq.com
    通讯作者: 刘艳辉(1978-),女,博士,教授级高级工程师,主要从事地质灾害预警与防治等方面的研究工作。E-mail: liuyh@cigem.cn
  • 中图分类号: P642.22

A early warning model of regional landslide in Qingchuan County, Sichuan Province based on logistic regression

More Information
  • 四川省青川县滑坡灾害群发,点多面广,区域滑坡灾害预警是有效防灾减灾的重要手段,预警模型是成功预警的核心。由于研究区滑坡诱发机理复杂、调查监测大数据及分析方法不足等原因,传统区域地质灾害预警模型存在预警精度有限、精细化不足等问题。文章在青川县地质灾害调查监测和降水监测成果集成整理与数据清洗基础上,构建了青川县区域滑坡灾害训练样本集,样本集包括地质环境、降雨等27个输入特征属性和1个输出特征属性,涵盖了青川县近9年(2010—2018年)全部样本,数量达1 826个(其中,正样本613个,负样本1 213个)。基于逻辑回归算法,对样本集进行5折交叉验证学习训练,采用贝叶斯优化算法进行模型优化,采用精确度、ROC曲线和AUC值等指标校验模型准确度和模型泛化能力。其中,ROC曲线也称为“受试者工作特征”曲线;AUC值表示ROC曲线下的面积。校验结果显示,基于逻辑回归算法的模型训练结果准确率和泛化能力均较好(准确率94.3%,AUC为0.980)。开展区域滑坡实际预警时,按训练样本特征属性格式,输入研究区各预警单元27个特征属性,调用预先学习训练好的模型,输出滑坡灾害发生概率,根据输出概率分段确定滑坡灾害预警等级。当输出概率P≥40%且P<60%时,发布黄色预警;当输出概率P≥60%且P<80%时,发布橙色预警;当输出概率P≥80%时,发布红色预警。

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  • 图 1  青川县区域滑坡灾害预警训练样本集

    Figure 1. 

    图 2  Sigmoid函数

    Figure 2. 

    图 3  逻辑回归模型学习曲线和ROC曲线

    Figure 3. 

    表 1  训练样本输入特征及参数

    Table 1.  Input characteristics and parameters of the training samples

    序号 输入特征 输入特征参数
    1 坡度/(°) ①0~10;②10~20;③20~30; ④30~40;⑤≥40
    2 坡向/(°) ①0~90;②90~180;③180~270; ④270~360
    3 高程/m ①0~800;②800~1200;1200~1600;
    ④1600~2000;⑤≥2000
    4 地貌类型 ①中低山;②中山;③高中山
    5 地层岩性 ①松散堆积层;②软弱-半坚硬薄-中层状岩组;③半坚硬-坚硬薄-中层状岩组;④坚硬-半坚硬中-厚层状岩组;
    ⑤未知岩性
    6 距断裂距离/m ①0~500;②500~1000;③1000~1500; ④1500~2000;⑤≥2000
    7 年雨量/mm ①0~500;②500~800;③800~1000;
    ④1000~1200;⑤≥1200
    8 距房屋距离/m ①0~200;②≥200
    9 距道路距离/m ①0~200;②≥200
    10 距沟谷距离/m ①0~200;②≥200
    11 网格单元历史灾点数/个 ①0;②1;③2;④3~4;⑤5~7
    12 当日雨量/mm ①<10;②10~25;③25~50; ④50~100;⑤>100
    13 前1日雨量/mm ①<10;②10~25;③25~50; ④50~100;⑤>100
    14 前2日雨量/mm ①<10;②10~25;③25~50; ④50~100;⑤>100
    ... ... ...
    27 前15日雨量/mm ①<10;②10~25;③25~50; ④50~100;⑤>100
    下载: 导出CSV

    表 2  不同阈值下的Logistic回归分类结果混淆矩阵

    Table 2.  Confuse matrix of the result of the logistic regression classification under different thresholds

    阈值 实际值
    滑坡 非滑坡
    0.25 预测值 滑坡 468 58 准确率:0.890
    非滑坡 25 910 准确率:0.973
    召回率:0.949 召回率:0.940 总精度:0.943
    0.5 预测值 滑坡 451 26 准确率:0.945
    非滑坡 42 942 准确率:0.957
    召回率:0.915 召回率:0.973 总精度:0.953
    0.75 预测值 滑坡 423 15 准确率:0.966
    非滑坡 70 953 准确率:0.932
    召回率:0.858 召回率:0.985 总精度:0.942
    下载: 导出CSV

    表 3  Logistic回归模型分类

    Table 3.  Logistic regression model classification report

    精确率 召回率 f1得分
    0 0.949 0.975 0.957
    1 0.950 0.883 0.915
    准确率 0.943
    宏平均 0.944 0.929 0.936
    加权平均 0.943 0.943 0.942
    下载: 导出CSV

    表 4  预警等级划分

    Table 4.  Early warning level division

    预警等级 风险等级 概率P
    红色预警 风险很高 [80%, 100%]
    橙色预警 风险高 [60%, 80%)
    黄色预警 风险较高 [40%, 60%)
    下载: 导出CSV
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出版历程
收稿日期:  2019-11-12
修回日期:  2020-01-12
刊出日期:  2021-01-15

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