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三眼峪特大泥石流沟流域分区特征
引用本文:黎志恒,朱立峰,胡向德,于国强,贾贵义,李瑞冬.三眼峪特大泥石流沟流域分区特征[J].西北地质,2011,44(3):38-43.
作者姓名:黎志恒  朱立峰  胡向德  于国强  贾贵义  李瑞冬
作者单位:1. 甘肃省地质环境监测院,兰州,730020
2. 中国地质调查局西安地质调查中心,西安,710054
基金项目:国土资源大调查计划项目"西北黄土高原区地质灾害详细调查",国土资源大调查项目"甘肃省白龙江流域主要城镇环境工程地质勘查",国家自然科学基金项目
摘    要:三眼峪“8.8”特大泥石流属典型的沟谷型泥石流,整个沟域具有明显的形成区、流通区及堆积区。通过野外调查,竹塔沟-桥子沟以上的大、小眼峪上游沟脑为雨洪产流汇流区域,产流区与罐子坪-峪支沟一线之间为主要的固体物源区,大、小眼峪口至三眼峪口之间以过流为主,峪口至白龙江之间为堆积区。通过分析三眼峪流域分区特征和泥石流在不同分区的沿程冲淤变化,以期为建立三眼峪泥石流监测预警体系提供依据。

关 键 词:泥石流沟  流域  分区特征  冲淤特征

Basin Zoning Characteristics of Sanyanyu Extremely Big Debris Flow Gully
LI Zhi-heng,ZHU Li-feng,HU Xiang-de,YU Guo-qiang,JIA Gui-yi,LI Rui-dong.Basin Zoning Characteristics of Sanyanyu Extremely Big Debris Flow Gully[J].Northwestern Geology,2011,44(3):38-43.
Authors:LI Zhi-heng  ZHU Li-feng  HU Xiang-de  YU Guo-qiang  JIA Gui-yi  LI Rui-dong
Institution:LI Zhi-heng1,ZHU Li-feng2,HU Xiang-de1,YU Guo-qiang2,JIA Gui-yi1,LI Rui-dong1(1.Gansu Institute of Geological Environment Monitoring,Lanzhou 730020,2.Xi'an Centre of Geological Survey,CGS,Xi'an 710054,China)
Abstract:8.8 extremely big debris flow in Sanyanyu belongs to typical gully debris flow with obvious forming zone,transportation zone and accumulation zone.Based on site investigation,it is found that the gully head of upstream Dayanyu and Xiaoyanyu,situating at the up streams of Zhuta gully and Qiaozi gully,is the forming and accumulation zone of flood.It is also noted that the area between the forming zone and Guanziping-Yuzhi gully is the main solid source area.Area between Dayanyu-Xiaoyanyu and Sanyanyu is domin...
Keywords:debris flow gully  basin  zoning charateristics  erosion and siltation charateristics  
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