干旱区研究 ›› 2019, Vol. 36 ›› Issue (3): 761-770.doi: 10.13866/j.azr.2019.03.28

• 生态与环境 • 上一篇    下一篇

泥石流易发性评价模型的构建——以白龙江流域石门乡羊汤河段为例

王高峰, 杨强, 田运涛, 叶振南, 陈宗良, 高幼龙, 郭宁, 邓兵   

  1. 中国地质调查局水文地质环境地质调查中心,河北 保定 071051
  • 收稿日期:2018-05-26 修回日期:2018-07-04 发布日期:2025-10-18
  • 通讯作者: 田运涛. E-mail: tytao@163.com
  • 作者简介:王高峰(1984-),高级工程师,工学硕士,主要从事地质灾害调查与GIS评价研究. E-mail:wgf_cgcs303@163.com
  • 基金资助:
    中国地质调查局地质调查项目(DD20160281,12120115053701)资助

Establishment of Assessment Model for Debris Flow Susceptibility:A Case Study Along the Yangtang River Reach in Shimen Township in the Bailong River Basin

WANG Gao-feng, YANG Qing, TIAN Yun-tao, YE Zhen-nan, CHEN Zong-liang, GAO You-long, GUO Ning, DENG Bing   

  1. Center for Hydrogeology and Environmental Geology Survey,China Geology Survey,Baoding 071051,Hebei,China
  • Received:2018-05-26 Revised:2018-07-04 Online:2025-10-18

摘要: 以白龙江流域石门乡至羊汤河段为例,采用松散物质面密度、地层岩性、构造断裂密度、地震密度、坡向、土壤可蚀性、土地利用类型、坡长坡度、沟床比降、流域沟壑密度及年均降雨量等11项评价因子的归一化值,在GIS平台下运用层次分析法建立泥石流易发性评价模型,将研究区泥石流易发性评价栅格图划分为4个等级。研究表明:泥石流中高易发区域占整个研究区面积的51.04%,区内发育的泥石流流域面积占中高易发区面积的68.71%,其分布特点具有沿大型活动性断裂呈带状分布,在次级断裂和小型褶皱密集区集中发育;沿易崩易滑地层呈片状展布,在沟壑密集带分区块集中发育;在坡面侵蚀强的区域多为泥石流高易发区,呈串珠状连片分布。利用研究区泥石流数据库对评价结果进行检验,检验曲线表明分区效果良好,检验曲线下面积即AUC值为62.13%,说明易发性评价结果较为可靠。

关键词: 泥石流, 易发性评价, AHP层次分析法, 模型构建, 白龙江流域

Abstract: In this study,the hierarchy analysis,GIS means and normalized values of 9 evaluation factors,such as loose material surface density,stratigraphic lithology,tectonic fracture density,seismic density,slope aspect,soil erodibility,land use type,slope length and gradient,gully bed slope and gully density,and average annual rainfall,were used.The purposes of the study was to develop an assessment model for debris flow susceptibility along the Yangtang river reach in Shimen Township in the Bailong River Basin.Finally,the grid diagram of assessing debris flow susceptibility in the study area was divided into 4 grades.The results showed that the proportion of the areas with high debris flow susceptibility accounted for 51.04% of the whole study area,and the areas with mid-high debris flow susceptibility accounted for 68.71%.The debris flows were distributed along the large active fault zones,especially in the zones with intensive secondary fractures and small folds.They were also distributed along the slidable strata,especially in the zones with dense gullies.Debris flow occurred easily on the slopes with high soil erosion.The results were tested by the database of debris flow in the study area.

Key words: debris flow, susceptibility assessment, analytic hierarchy process, model development, Bailong River Basin