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基于CF与CF-LR模型的地质灾害易发性评价

屠水云, 张钟远, 付弘流, 徐世光, 邓明国, 何例春, 刘金宇. 基于CF与CF-LR模型的地质灾害易发性评价[J]. 中国地质灾害与防治学报, 2022, 33(2): 96-104. doi: 10.16031/j.cnki.issn.1003-8035.2022.02-12
引用本文: 屠水云, 张钟远, 付弘流, 徐世光, 邓明国, 何例春, 刘金宇. 基于CF与CF-LR模型的地质灾害易发性评价[J]. 中国地质灾害与防治学报, 2022, 33(2): 96-104. doi: 10.16031/j.cnki.issn.1003-8035.2022.02-12
TU Shuiyun, ZHANG Zhongyuan, FU Hongliu, XU Shiguang, DENG Mingguo, HE Lichun, LIU Jinyu. Geological hazard susceptibility evaluation based on CF and CF-LR model[J]. The Chinese Journal of Geological Hazard and Control, 2022, 33(2): 96-104. doi: 10.16031/j.cnki.issn.1003-8035.2022.02-12
Citation: TU Shuiyun, ZHANG Zhongyuan, FU Hongliu, XU Shiguang, DENG Mingguo, HE Lichun, LIU Jinyu. Geological hazard susceptibility evaluation based on CF and CF-LR model[J]. The Chinese Journal of Geological Hazard and Control, 2022, 33(2): 96-104. doi: 10.16031/j.cnki.issn.1003-8035.2022.02-12

基于CF与CF-LR模型的地质灾害易发性评价

详细信息
    作者简介: 屠水云(1968-),男,汉族,云南昆明人,硕士,高级工程师,研究方向为水工环地质。E-mail:414943009@qq.com
    通讯作者: 张钟远(1996-),男,侗族,贵州铜仁人,硕士研究生,研究方向为环境地质与灾害地质。E-mail:KFZZZY@163.com
  • 中图分类号: P642

Geological hazard susceptibility evaluation based on CF and CF-LR model

More Information
  • 区域地质灾害易发性评价对地质灾害防治具有重要意义。本文以贵州省沿河县为研究区,考虑海拔、坡度、坡向、地形曲率、NDVI、工程地质岩组、断层、道路、水系9个因素,通过相关性分析后作为评价因子。分别利用CF模型和CF-LR模型评价沿河县地质灾害易发性。结果表明:CF模型比CF-LR模型地质灾害易发性等级的频率比值从低易发区到极高易发区明显增大,均有效评价了沿河县地质灾害易发性;CF-LR模型比CF模型AUC值提高了0.096,CF-LR模型具有更高的评价精度。

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  • 图 1  研究区地理位置及地质灾害点分布

    Figure 1. 

    图 2  评价指标因子分级图

    Figure 2. 

    图 3  地质灾害易发性区划

    Figure 3. 

    图 4  ROC曲线

    Figure 4. 

    表 1  评价指标因子相关性系数矩阵

    Table 1.  Correlation coefficient matrix of evaluation index factors

    评价因子海拔坡度坡向地形曲率NDVI工程地质岩组断层缓冲区道路缓冲区河流缓冲区
    海拔1
    坡度−0.0091
    坡向0.0090.0591
    地形曲率0.1380.045−0.0041
    NDVI0.1540.094−0.0730.0321
    工程地质岩组−0.0040.004−0.016−0.010−0.0061
    断层缓冲区0.182−0.0020.0020.0040.0240.1041
    道路缓冲区0.1130.0810.0040.0090.0430.0070.0601
    河流缓冲区0.324−0.0420.0060.0240.0590.0750.0940.1461
    下载: 导出CSV

    表 2  评价指标因子分级、频率比、确定性系数

    Table 2.  Evaluation index factor classification, frequency ratio and certainty coefficient

    评价指
    标因子
    分级地质灾
    害频数
    分级面积
    /km2
    频率比CF评价指
    标因子
    分级地质灾
    害频数
    分级面积
    /km2
    频率比CF
    工程地
    质岩组
    坚硬岩组19908.6500.399−0.374地形
    曲率
    <−0.254842.3201.2250.194
    较坚硬岩组12433.8410.528−0.485−0.2~0.241804.5090.974−0.028
    较软岩组24354.6241.2930.239≥0.235836.6810.799−0.210
    软岩组24156.9082.9220.694道路缓
    冲区/m
    0~20010121.6081.5710.384
    软硬相间岩组51629.4871.5480.373200~4007110.0301.2150.187
    海拔/m209~40019125.5282.8920.690400~6008102.0961.4970.350
    400~60035630.0161.0610.061600~800896.1481.5900.391
    600~80046781.4361.1250.117800~1000491.3580.836−0.206
    800~100023557.5910.788−0.221≥1000931962.2700.905−0.099
    1000~12005329.8690.290−0.721河流缓
    冲区/m
    0~20018292.0501.1770.159
    1200~1408259.0680.647−0.366200~40020270.7621.4110.307
    坡度/(°)0~88360.7770.424−0.589400~60016276.5471.1050.112
    8~1644774.5341.0850.083600~80015263.6641.0870.084
    16~2447726.4151.2360.202800~100013249.4470.996−0.005
    24~3224407.5031.1250.117≥1000481131.0390.811−0.198
    32~405150.8860.633−0.380断层缓
    冲区/m
    0~30015263.9221.0860.083
    ≥40263.3950.603−0.410300~60013246.9681.0060.006
    坡向平面09.0520.000−1.000600~90013230.3451.0780.077
    17249.9941.2990.243900~120010202.0120.946−0.057
    东北19325.9201.1140.1081200~15008176.9010.864−0.143
    32390.8191.5640.381≥1500711363.3630.995−0.005
    东南14338.8930.789−0.220NDVI−0.02~0.19219.3310.784−0.225
    9253.1270.679−0.3330.1~0.225459.4781.0390.040
    西南21287.8071.3940.2980.2~0.3611008.8611.1550.142
    西7326.1640.410−0.6030.3~0.434757.6560.857−0.149
    西北11301.7340.696−0.3150.4~0.54138.1830.500−0.513
    下载: 导出CSV

    表 3  频率比大于1的属性区间

    Table 3.  Attribute intervals with frequency ratio greater than 1

    评价因子海拔/m坡度/(°)坡向地形曲率NDVI工程地质岩组断层缓冲区/m道路缓冲区/m河流缓冲区/m
    频率比大于
    1类别
    209~4008~16< −0.20.1~0.2较软质岩0~3000~2000~200
    400~60016~24东北0.2~0.3软质岩300~600200~400200~400
    600~80024~32软硬相间质岩600~900400~600400~600
    西南600~800600~800
    下载: 导出CSV

    表 4  逻辑回归系数和显著性

    Table 4.  Logistic regression coefficient and significance

    评价因子海拔坡度坡向地形曲率NDVI工程地质岩组断层缓冲区道路缓冲区河流缓冲区常量
    β3.8442.4953.4184.0851.1984.3773.2180.7342.7282.604
    sig0.0000.0030.0000.0190.0230.0000.0270.0360.1300.000
    下载: 导出CSV

    表 5  地质灾害易发性评价频率比值

    Table 5.  Frequency ratio of geological hazard susceptibility evaluation

    评价模型易发性
    等级
    分级面积
    /km2
    面积
    占比
    灾害点
    频数
    灾害
    占比
    频率比
    CF低易发区361.2650.14530.0230.159
    中易发区784.2690.316170.1310.414
    高易发区895.1970.360470.3621.003
    极高易发区442.7790.178630.4852.718
    CF-LR低易发区671.2520.27050.0380.142
    中易发区467.7580.18880.0620.327
    高易发区927.5270.373360.2770.741
    极高易发区507.1450.204810.6233.051
    下载: 导出CSV
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收稿日期:  2021-04-26
修回日期:  2021-06-03
刊出日期:  2022-04-25

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