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江苏南京地质灾害风险评价

刘宝生, 陈刚, 程刚建. 江苏南京地质灾害风险评价[J]. 中国地质灾害与防治学报, 2023, 34(4): 97-104. doi: 10.16031/j.cnki.issn.1003-8035.202205048
引用本文: 刘宝生, 陈刚, 程刚建. 江苏南京地质灾害风险评价[J]. 中国地质灾害与防治学报, 2023, 34(4): 97-104. doi: 10.16031/j.cnki.issn.1003-8035.202205048
LIU Baosheng, CHEN Gang, CHENG Gangjian. Risk assessment of geological disasters in Nanjing, Jiangsu Province[J]. The Chinese Journal of Geological Hazard and Control, 2023, 34(4): 97-104. doi: 10.16031/j.cnki.issn.1003-8035.202205048
Citation: LIU Baosheng, CHEN Gang, CHENG Gangjian. Risk assessment of geological disasters in Nanjing, Jiangsu Province[J]. The Chinese Journal of Geological Hazard and Control, 2023, 34(4): 97-104. doi: 10.16031/j.cnki.issn.1003-8035.202205048

江苏南京地质灾害风险评价

详细信息
    作者简介: 刘宝生(1991-),男,安徽合肥人,硕士,工程师,主要从事地灾防治和GIS应用研究。E-mail:lbsnju@126.com
  • 中图分类号: P694

Risk assessment of geological disasters in Nanjing, Jiangsu Province

  • 地质灾害风险评价是地质灾害风险管控的支撑与依据,对于科学防治地质灾害具有重要意义。以江苏南京为研究区,选取历史灾害点密度等影响因子开展易发性评价,以降雨量作为诱发因素开展危险性评价,结合承灾体易损性,分析划定地质灾害高、中、低三类风险区。结果表明:高风险区主要集中在沿江的老山、幕府山、紫金山、栖霞山以及青龙山等部分人员聚居的山前坡麓一带,面积51.3 km2,占比0.8%;中风险区主要集中在低山丘陵中人员较集中的区域,面积371.9 km2,占比5.6%;低风险区分布较广,位于其余低山丘陵岗地,面积1740.1 km2,占比26.4%。研究成果可有效支撑当地地质灾害防灾减灾以及国土空间规划应用。

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  • 图 1  降雨量与历史地灾点数量关系

    Figure 1. 

    图 2  地质灾害易发性评价指标体系

    Figure 2. 

    图 3  评价因子分级及易发性等级

    Figure 3. 

    图 4  评价结果ROC检验曲线

    Figure 4. 

    图 5  不同重现期降雨强度下地质灾害危险性分级

    Figure 5. 

    图 6  地质灾害综合易损性以及风险评价

    Figure 6. 

    表 1  地质灾害风险等级矩阵分析

    Table 1.  Analysis of geological hazard risk level matrix

    风险性危险性
    极高


    极高极高极高
    极高
    下载: 导出CSV

    表 2  评价因子信息量

    Table 2.  Information value of evaluation factors

    评价因子子类区间信息量值
    灾害点密度/(个·km−20−5.86
    (0,2]2.51
    (2,4]3.10
    >44.12
    坡度/(°)[0,10)−0.97
    [10,25)1.97
    [25,40)3.31
    [40,50)4.87
    [50,90]5.32
    地形起伏度/m<20−2.16
    [20,40)2.86
    [40,90)3.47
    [90,120)5.24
    [120,140]6.85
    >1407.13
    工程地质岩组老黏性土−1.43
    一般黏性土−3.71
    岩浆岩类坚硬岩1.33
    碎屑岩类软~极软岩2.64
    碳酸盐岩类坚硬岩3.10
    碳酸盐岩类较坚硬岩2.40
    碎屑岩类较坚硬岩2.39
    碎屑岩类坚硬岩1.08
    距断层距离/m<202.50
    [20,200)2.48
    [200,500)1.78
    [500,1000]0.90
    >1000−0.56
    距道路距离/m<100−0.19
    [100,200]0.06
    (200,300]0.53
    (300,400]0.65
    (400,500]0.59
    >500−2.19
    下载: 导出CSV

    表 3  地质灾害易发性分区评价判断矩阵

    Table 3.  Judgment matrix for assessing susceptibility zonation of geological hazards

    地质灾害易发性
    分区评价
    地质环境条件诱发因素地质灾害现状权重
    地质环境条件1330.5936
    诱发因素1/3120.2493
    地质灾害现状1/31/210.1571
    判断矩阵一致性比例:0.0516;对总目标的权重:1.0000;
    最大特征根:3.0536
    下载: 导出CSV

    表 4  地质环境条件判断矩阵

    Table 4.  Judgment matrix for geological environmental conditions

    地质环境条件坡度工程地质岩组地形起伏度距断层距离权重
    坡度1111/20.2071
    工程地质岩组11120.2929
    地形起伏度11120.2929
    距断层距离21/21/210.2071
    判断矩阵一致性比例:0.0923;对总目标的权重:0.5936;
    最大特征根:4.2463
    下载: 导出CSV

    表 5  层次分析法计算各因子权重

    Table 5.  Calculation of factor weights using analytic hierarchy process (AHP)

    影响因子权重
    历史灾害点密度0.17
    坡度0.12
    地形起伏度0.17
    工程地质岩组0.17
    距断层距离0.12
    距道路距离0.25
    下载: 导出CSV

    表 6  研究区不同重现期降雨量

    Table 6.  Precipitation distribution in different recurrence period in the study area

    年均及不同重现期降雨量/mm
    年最大日降雨量均值101
    P=10%157.92
    P=5%182.22
    P=2%212.84
    P=1%235.22
    下载: 导出CSV
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出版历程
收稿日期:  2022-05-30
修回日期:  2022-09-08
刊出日期:  2023-08-25

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