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黄河流域甘肃段地质灾害发育特征

郭富赟, 宋晓玲, 刘明霞. 黄河流域甘肃段地质灾害发育特征[J]. 中国地质灾害与防治学报, 2021, 32(5): 130-136. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-16
引用本文: 郭富赟, 宋晓玲, 刘明霞. 黄河流域甘肃段地质灾害发育特征[J]. 中国地质灾害与防治学报, 2021, 32(5): 130-136. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-16
GUO Fuyun, SONG Xiaoling, LIU Mingxia. The development characteristics of geological hazards in Gansu segment of the Yellow River basin[J]. The Chinese Journal of Geological Hazard and Control, 2021, 32(5): 130-136. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-16
Citation: GUO Fuyun, SONG Xiaoling, LIU Mingxia. The development characteristics of geological hazards in Gansu segment of the Yellow River basin[J]. The Chinese Journal of Geological Hazard and Control, 2021, 32(5): 130-136. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-16

黄河流域甘肃段地质灾害发育特征

  • 基金项目: 甘肃省科技重大专项-社会发展类(19ZD2FA002);甘肃省自然资源厅地质灾害调查(20200305)
详细信息
    作者简介: 郭富赟(1970-),男,甘肃景泰人,博士,教授级高级工程师,主要从事水工环地质和地质灾害防治方面的研究工作。E-mail:fyg51913@163.com
  • 中图分类号: P694

The development characteristics of geological hazards in Gansu segment of the Yellow River basin

  • 黄河流域甘肃段是甘肃省地质灾害最为集中的区域。截止2019年底,查明地质灾害点共12829处,占全省灾害总量的70.83%。按照水系分布划分,以渭河流域、泾河流域、黄河干流流域最为发育,其他水系次之。依据空间分布特征,划分为永登—靖远等北部泥石流灾害为主的区段、中部崩塌滑坡泥石流集中区段、南部崩塌滑坡泥石流为主的区段和玛曲—碌曲地质灾害轻微发育区段。依据时间分布特征,具有2—5月冻融期、7—9月主汛期两个高发时段。地质灾害具有小灾巨损、群发巨损和链式巨损等致灾特征。单体灾害易形成巨大损失,降雨、地震引发的群发性地质灾害往往损失巨大,同时崩滑流阻断河道形成的堰塞湖风险也常有发生。

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  • 图 1  地质灾害年内分布特征(2013—2019年平均值)

    Figure 1. 

    图 2  地质灾害多年分布特征(天水,1961—2018)

    Figure 2. 

    图 3  黄河流域甘肃段地质灾害点分布图

    Figure 3. 

    表 1  黄河流域不同水系地质灾害分布数量一览表

    Table 1.  List of distribution quantity of geological hazards in different water systems in the Yellow River basin

    水系名称滑坡崩塌泥石流地裂缝地面塌陷合计
    湟水河流域187297106293
    黄河干流流域195230056587192923
    洮河流域144487910032444
    渭河流域26762391004833930
    泾河流域249318838281213165
    北洛河流域558110074
    合计880785129431765212829
    下载: 导出CSV

    表 2  黄河流域不同水系地质灾害人员伤亡及经济损失一览表

    Table 2.  List of casualties and property losses caused by geological disasters in different water systems in the Yellow River basin

    水系名称受灾人口/人人员伤亡/人直接经济损失/万元
    黄河干流流域1131217718.34
    洮河流域58891124442.00
    渭河流域29474760419777.20
    泾河流域44481617337.70
    合计306215108469275.24
    下载: 导出CSV

    表 3  地震引发崩塌、滑坡数量表

    Table 3.  Quantity of collapse and landslide caused by earthquake

    名称震级烈度区域引发加剧灾害
    海原地震8.06~11陇东南区域大型657滑坡处,中小型上万处
    漳县岷县地震6.66~8岷县漳县289处滑坡,崩塌1000多处
    临洮地震4.56临洮辛店镇
    通渭地震5.56~7通渭县一带大于500 m3的滑坡337处
    永登祁山地震5.96~7永登景泰大小黄土滑坡150多处
    下载: 导出CSV

    表 4  黄河流域甘肃段不同水系地质灾害点面积比统计表

    Table 4.  Statistical table of area ratio of geological hazard of different water systems in Gansu section of the Yellow River basin

    水系滑坡崩塌泥石流地裂缝地面塌陷总面积比/
    (10−3个·km−2
    渭河水系102.779.1838.550.310.12150.90
    泾河水系80.536.0712.332.620.68102.19
    洮河水系59.83.6137.7100.12101.28
    湟水河水系49.317.6518.7401.5877.33
    黄河干流水系35.365.4310.231.580.3452.94
    北洛河水系24.133.514.830032.47
    下载: 导出CSV
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出版历程
收稿日期:  2020-08-25
修回日期:  2021-05-28
刊出日期:  2021-10-25

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