[1]吕学军,倪化勇,徐如阁,等.四川峨边县蒋沟矿渣侵蚀泥石流成因与特征[J].水土保持研究,2011,18(03):83-87.
　LÜ,Xue-jun,NI Hua-yong,et al.Formation and Characteristics of Mine-slag Debris Flows from Jianggou Ravine in Ebian County, Sichuan Province[J].Research of Soil and Water Conservation,2011,18(03):83-87.
点击复制

四川峨边县蒋沟矿渣侵蚀泥石流成因与特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 18 期数: 2011年03期 页码: 83-87 栏目: 出版日期: 2011-06-20
Title:
Formation and Characteristics of Mine-slag Debris Flows from Jianggou Ravine in Ebian County, Sichuan Province
作者:
吕学军1, 倪化勇2, 徐如阁2, 巴仁基2
1. 滨州学院 建筑与城乡规划系, 山东 滨州 256603;
2. 成都地质矿产研究所, 成都 610081
Author(s):
LÜ Xue-jun1, NI Hua-yong2, XU Ru-ge2, BA Ren-ji2
1. Department of Architecture & Urban Planning, Binzhou University, Binzhou, Shandong 256603, China;
2. Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, China
关键词:
泥石流; 矿渣; 侵蚀; 蒋沟
Keywords:
debris flow; mine slag; erosion; Jianggou Ravine
分类号:
P642.23
摘要:
四川峨边县蒋沟是一条典型的矿渣型泥石流沟，在侵蚀作用下时常发生泥石流并造成严重危害。该文采用调查、测绘和综合研究相结合的方法，论述了蒋沟矿渣侵蚀泥石流的成因和特征。形成条件方面，矿渣侵蚀类泥石流具有物源集中和机械组成固定性特征；发生过程呈现出降雨-侵蚀-崩滑-搬运复合型和循环性，侵蚀成为泥石流形成和发生的关键环节；泥石流特征则主要表现为堆积物成分单一，堆积比降小，暴发频率高和地貌塑造作用强等方面。最后，针对成因和特征，提出了以水土分离、固床和护坡等工程措施为主，以矿山植被恢复措施为辅的防治建议。
Abstract:
Jianggou Ravine is a typical mine-slag debris flow-induced gully,where debris flow with an incision process frequently occurred and caused serious damages.In this paper,on the basis of field investigation,survey and comprehensive research,the formation and characteristics are discussed and corresponding prevention countermeasures are put forward.In terms of debris flow forming condition,mine-slag debris flow-induced in Jianggou Ravine is representative for mass concentricity and grain-composition fixity.A complex and circle process,namely rainfall-erosion-collapse or landslide-engulfment,existed during debris flow occurrence and erosion is the key process.As characteristics are concerned,debris flows induced by mine slag are typicality in simple deposition,smaller deposition obliquity,high frequency and intense evolvement in landform.In accordance with such forming condition and occurrence characteristics,corresponding countermeasures are put forward at the end of this paper,including main engineering controls such as separating method between water and soil,gull-bed fixing method,slope blocking method and accessorial vegetation recovering method.

参考文献/References:

[1] 张丽萍,唐克丽.矿山泥石流[M].北京:地质出版社,2001.
[2] 倪化勇,郑万模,巴仁基,等.基于水动力条件的矿渣型泥石流形成与特征:以石棉县后沟为例[J].山地学报,2010,28(4):470-478.
[3] 王文龙,李占斌,张平仓.神府东胜煤田开发中人为泥石流形成条件分析[J].水土保持研究,2003,10(2):83-85.
[4] 王文龙,张平仓,高学田.神府东胜矿区一、二期工程与人为泥石流[J].水土保持研究,1994,1(4):54-59.
[5] 徐友宁,何芳,陈华清.西北地区矿山泥石流及分布特征[J].山地学报,2007,25(6):729-736.
[6] 张锐波,张丽萍.矿山泥石流形成的理论动态分析:以神府东胜矿区为例[J].中国地质灾害与防治学报,2003,14(3):86-90.
[7] 张丽萍,唐克丽,张平仓.矿山泥石流形成的固体物质补给特点研究:以神府东胜矿区为例[J].中国地质灾害与防治学报,1999,10(1):61-66.
[8] 徐友宁,李育敬,陈社斌,等.潼关金矿区矿渣型泥石流灾害特征及防治对策[J].山地学报,2006,24(6):667-671.
[9] 陈华清,徐友宁,张江华.小秦岭大湖峪矿渣型泥石流的物源特征及其危险度评价[J].地质通报,2008,27(8):1292-1298.
[10] 邓龙胜,范文,熊炜.矿渣型泥石流发育特征及危险性评价[J].工程地质学报,2005,17(3):415-420.
[11] 陈廷方,崔鹏,刘岁海,等.矿产资源开发与泥石流灾害及其防治对策[J].工程地质学报,2005,13(2):179-182.
[12] 李智毅,王裕云.工程地质概论[M].北京：中国地质大学出版社,1994.

相似文献/References:

[1]王高峰,唐川,王洪德,等.初咱磨子沟泥石流特征及危险性评价研究[J].水土保持研究,2012,19(04):234.
　WANG Gao-feng,TANG Chuan,WANG Hong-de,et al.Characteristics and Hazard Assessment of Debris Flows in Chuzanmozigou Catchment[J].Research of Soil and Water Conservation,2012,19(03):234.
[2]田冰,王裕宜.基于功率谱分析的蒋家沟泥石流侵蚀输沙量准周期的探讨[J].水土保持研究,2012,19(04):244.
　TIAN Bing,WANG Yu-yi.Power Spectral Analysis on Periodicity of Sediment Transport in Debris Flow in Jiangjiagou Watershed[J].Research of Soil and Water Conservation,2012,19(03):244.
[3]胡桂胜,陈宁生,邓虎.基于GIS的西藏林芝地区泥石流易发与危险区分析[J].水土保持研究,2012,19(03):195.
　HU Gui-sheng,CHEN Ning-sheng,DENG Hu.Analysis of Debris Flow-prone and Dangerous Area in Nyingchi of Tibet Based on GIS[J].Research of Soil and Water Conservation,2012,19(03):195.
[4]李朝安,胡卸文,李冠奇,等.四川省“8·13”特大泥石流灾害成生机理与防治原则[J].水土保持研究,2012,19(02):257.
　LI Chao-an,HU Xie-wen,LI Guan-qi,et al.Formation Mechanism of the ’8·13’ Catastrophic Debris Flow in Sichuan and the Principles of Controlling[J].Research of Soil and Water Conservation,2012,19(03):257.
[5]张黎勇.皖南山区山体滑坡、泥石流的成因及其防治[J].水土保持研究,1997,4(01):171.
　Zhang Liyong.The Cause and Prevention of Slideslope, Debris Flow in the Hilly Areas of Southern Anhui Province[J].Research of Soil and Water Conservation,1997,4(03):171.
[6]李树德.中国滑坡、泥石流灾害的时空分布特点[J].水土保持研究,1999,6(04):33.
　Li Shude.The Temporal and Spacial Distribution of Landslide and Debris Flow Disasters in China[J].Research of Soil and Water Conservation,1999,6(03):33.
[7]吴正华.北京泥石流灾害及其降水触发条件[J].水土保持研究,2001,8(01):67.
　WU Zhenghua.The Mud-rock Flow Disaster and Their Touch off Condition by Rainfall in Beijing Area[J].Research of Soil and Water Conservation,2001,8(03):67.
[8]崔之久,冯金良.东川蒋家沟泥石流沉积亚相组合特征[J].水土保持研究,2001,8(02):2.
　CUI Zhi-jiu,FENG Jin-liang.Combination Features of Depositional Sub-facies of Debris-flowon the Jiangjiagou Valley, Yunnan Province[J].Research of Soil and Water Conservation,2001,8(03):2.
[9]冯金良,崔之久,李庆辰.太行山区下瓦岔泥石流灾害实录[J].水土保持研究,2001,8(02):41.
　FENG Jin-liang,CUI Zhi-jiu,LI Qing-chen.The Record of Xiawacha Debris-flow in Taihang Mountains[J].Research of Soil and Water Conservation,2001,8(03):41.
[10]李永化,张小咏,崔之久.陇南山地泥石流期、气候期与构造期的耦合[J].水土保持研究,2003,10(02):96.
　LI Yonghua,ZHANG Xiaoyong,CUI Zhijiu.Coupling of Debris Flow Period, Climate Period and Tectonic Period in the Mountainous Area of Longnan[J].Research of Soil and Water Conservation,2003,10(03):96.

备注/Memo

收稿日期:2010-11-11;改回日期:2010-11-30。
基金项目:国土资源调查项目（121201814019）;滨州学院青年人才创新工程科研基金项目（BZXYQNLG200503）
作者简介:吕学军（1967- ），男，山东滨州人，讲师，理学硕士，主要从事地质灾害环境影响评价研究。E-mail：xjlv_210@163.com

更新日期/Last Update: 1900-01-01