[1]王文龙,李占斌,张平仓,等.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(02):83-85.
　WANG Wenlong,LI Zhanbin,ZHANG Pingcang,et al.An Analysis on Forming Condition of Debris Flows Caused by Human Activities in Shenfu-Dongsheng Coal Field[J].Research of Soil and Water Conservation,2003,10(02):83-85.
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神府东胜煤田开发中人为泥石流形成条件分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 10 期数: 2003年02期 页码: 83-85 栏目: 出版日期: 1900-01-01
Title:
An Analysis on Forming Condition of Debris Flows Caused by Human Activities in Shenfu-Dongsheng Coal Field
作者:
王文龙1,2, 李占斌1,2, 张平仓3, 刘敏4
1. 中国科学院水利部水土保持研究所;
2. 西北农林科技大学, 陕西, 杨陵712100;
3. 长江科学院, 湖北, 武汉430010;
4. 陕西省杨凌示范区水务局, 陕西, 杨陵712100
Author(s):
WANG Wenlong1,2, LI Zhanbin1,2, ZHANG Pingcang3, LIU Min4
1. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources;
2. Northwestern Sci tech University of Agricalture and Forestry, Yangling 712100, Shanxi, China;
3. Academy of Sciences Yangtze River, Wuhan 430051, Hubei, China;
4. Water Conservancy Bureau of Yangling District, Yangling 712100, Shanxi, China
关键词:
神府东胜煤田; 人为泥石流; 形成条件
Keywords:
Shenfu-Dongsheng coal field; debris flow induced by human factors; condition of forming
分类号:
P642.23
摘要:
神府东胜煤田是我国重要的能源重化工基地,自1987年大规模开发以来泥石流频繁发生,通过野外考察发现,神府东胜煤田泥石流属由人为诱发的人为泥石流.详细地分析了该区泥石流形成的三个基本条件:丰富的松散固体物质储备、陡峻的地形条件和沟床比降和高强度长历时的降雨过程,认为在流域内人为堆置的大量松散弃土弃渣物质是该区泥石流形成发育的主要因素.
Abstract:
Shenfu-Dongsheng coal field is an important base of energy resources and heavy chemical industry of our country,since the large scale development in 1987,mud rock flows occurred frequently.According to the investigation,mud rock flow in Shenfu-Dongsheng is caused by human activities.Three basic conditions that triggered mud rock in the area are analyzed,ie rich loose solid material reserve,precipitous topography condition and ditch bed than fall with high strength length and duration rainfall process,it is think that artificial pile of plenty of abandoned earth and dregs is the major factor causing mud rock flow in this area.

相似文献/References:

[1]罗婷,王文龙,李宏伟,等.开发建设中扰动地面新增水土流失研究[J].水土保持研究,2012,19(03):30.
　LUO Ting,LI Hong-wei,BAI Yun.Study on the Newly Occurred Soil and Water Loss on the Disturbed Lands in the Site of Development and Construction[J].Research of Soil and Water Conservation,2012,19(02):30.
[2]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(04):54.
　Wang Wenlong,Zhang Pingcang,Gao Xuetian.Investigation of Man-Made Mud-Rock Flow during the First and Scond Construction Phases of in Shenfu-Dongsheng Coal Mining Area[J].Research of Soil and Water Conservation,1994,1(02):54.
[3]黄雅茹,董杰,汪季,等.神府东胜煤田沉陷区三种人工林生长状况比较研究[J].水土保持研究,2013,20(02):115.
　HUANG Ya-ru,DONG Jie,WANG Ji,et al.Comparision Study on the Growth Status of Three Planted Forests in Subsidence Area in Shenfu Dongsheng Coalfield[J].Research of Soil and Water Conservation,2013,20(02):115.

备注/Memo

收稿日期:2002-10-13
基金项目:中国科学院知识创新工程(KZCX1-10-04)黄土高原土壤侵蚀与旱地农业国家重点实验室基金(10501-78)中国科学院"山地灾害滑坡泥石流"特别支持项目(9303043)陕西省科学院择优专项支持项目(B22055200)联合资助
作者简介:王文龙(1964- ),男,陕西大荔人,博士生,副研究员,曾参加或主持科研项目20多项,发表论文30余篇.

更新日期/Last Update: 1900-01-01