人民长江

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地形因子对沟谷泥石流发育的影响——以都汶高速“7.10”群发泥石流为例

黄成,张友谊,眭静,叶小兵,袁亚东   

  • 出版日期:2019-08-28 发布日期:2019-08-28

Influence of topographic factors on valley debris flow development: case of “7.10” cluster debris flows in Duwen Expressway

HUANG Cheng,ZHANG Youyi,SUI Jing, YE Xiaobing,YUAN Yadong   

  • Online:2019-08-28 Published:2019-08-28

摘要: 2013年7月10日,都汶高速公路沿线32条沟暴发不同程度的泥石流灾害(简称“7·10”灾害),造成都汶高速公路中断及岷江堵塞。以“7·10”灾害为背景,运用ArcGIS提取了研究区泥石流沟的关键地形因子(包括流域面积、主沟沟道长度、沟道纵比降以及沟谷斜坡坡度等),并结合计算模型分析了地形因子对泥石流发育的影响。研究结果表明: “7·10”群发性泥石流的发生符合临界值模型G=S(A/A0)0.03J0.12;泥石流沟的地形因子G越大,地形条件就越好,当G>0.45时,易发生泥石流。因此,用综合地形因子G来衡量泥石流的易发性,可为都汶高速沿线泥石流沟的危险性评价与预警预报提供科学依据。

关键词: 地形因子, 群发性泥石流, 斜坡坡度, 流域面积, 纵比降, 都汶高速

Abstract: On July 10, 2013, different levels of debris flow disasters occurred in 32 gullies along the Duwen Expressway (Referred to as "7?10" disaster), causing the interruption of the Duwen Expressway and the blockage of the Minjiang River. Based on the “7?10” disaster, this paper used ArcGIS to extract the key topographic factors of debris flow gullies in the study area (such as the basin area A, the main gully channel length L, the longitudinal gradient J, and the gully slope S, etc.). Combined with the calculation model, the influence of topographic factors on the development of debris flow was analyzed. The result indicated that the occurrence of “7?10” cluster debris flow was consistent with a threshold model that we put forward. The larger the topographical factor G of the debris flow gully was, the better the topographic conditions in the debris flow gullies were, and debris flow was prone to occur when G>0.45. Therefore, the comprehensive topographic factor G was suggested to measure the susceptibility of debris flow. It can provide a scientific basis for the risk assessment and early warning of debris flow gullies along the Duwen Expressway.

Key words: topographic factor, mass debris flows, gradient of slope, basin area, longitudinal gradient, Duwen Expressway