长江上游泥石流最重度危险区

CORC > 成都山地灾害与环境研究所 > 中国科学院水利部成都山地灾害与环境研究所 > 成都山地所知识仓储（2009年以前）

	长江上游泥石流最重度危险区
	韦方强; 谢洪; 钟敦伦
刊名	山地研究
	1994
卷号	12 期号:2 页码:94-98
关键词	长江上游泥石流最重度危险区
ISSN号	1000-002X
其他题名	MOST CATASTROPHIC DANGER DISTRICT OF DEBRIS FLOW IN UPPER REACHES OF CHANGJIANG RIVER
通讯作者	韦方强
合作状况	其它
中文摘要	泥石流最重度危险区内泥石流危害最严重或危害能力最强．论述了长江上游泥石流最重度危险区的泥石流形成条件，活动特征及发展趋势，总结了区内泥石流的防治现状，并提出了区内泥石流防治的原则和意见．
英文摘要	Debris flow harms the peopel’s lifes and ptoperty most seriously,or has the most destructive capability in the most catastrophic danger district of debris flow in the upper reaches of Changjiang River.The firming conditions,activty characteristics and developmental tendency ofdebris flow are discussed,the status quo of debris flow prevention is summed up,and some princi-ples and suggestions of debris flow prevention in the district are put forward. The natural danger degrees are A which is favourable to the most intense activity of debris flow of the district in most part and B which is favourable to intense activity of debris flow inlittle part. The economic developmental level is 4(low) in greater part of the district,3(middle)and 2 (subhigh)in a little part,and l(high)in little part. Debris flow gullies are dense , frequency is high,scale is great,and destructive power isstrong in the district.The favourable natural environmental conditions enliven debris flow activities. and human unreasonable economic activity stimulates debris flow occurrence further.Unified planning,puttin;the prevention first,combining prevention with control,preventingoverally, controlling major points,and combining civil engineering and biologic engineering arethe principles of debris flow control. 更多
学科主题	P642.23
收录类别	CSCD ; 北大中文核心
语种	中文
CSCD记录号	CSCD:938503
公开日期	2010-07-03
内容类型	期刊论文
源URL	[http://ir.imde.ac.cn/handle/131551/207]
专题	成都山地灾害与环境研究所_成都山地所知识仓储（2009年以前）成都山地灾害与环境研究所_山地灾害与地表过程重点实验室科技信息与传播中心
作者单位	中国科学院、水利部成都山地灾害与环境研究所
推荐引用方式 GB/T 7714	韦方强,谢洪,钟敦伦. 长江上游泥石流最重度危险区[J]. 山地研究,1994,12(2):94-98.
APA	韦方强,谢洪,&钟敦伦.(1994).长江上游泥石流最重度危险区.山地研究,12(2),94-98.
MLA	韦方强,et al."长江上游泥石流最重度危险区".山地研究 12.2(1994):94-98.