中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Current changes of sediment yields in the upper Yangtze River and its two biggest tributaries, China

文献类型:会议论文

作者Xinbao Zhang1,2; Anban Wen1
出版日期2004
会议日期MAY, 2001
会议地点Xian
关键词sediment yield Jialing River Jinsha River Upper Yangtze River
卷号41
期号3-4
DOI10.1016/j.gloplacha.2004.01.008
页码221-227
国家PEOPLES R CHINA
英文摘要The sediment yield of the Upper Yangtze River (Yichan) showed no visible trend in change, while its two largest tributaries showed different variations in sediment yield: with a decrease in Jialing River and an increase in the Jinsha River during the period from the 1950s to the 1990s. The lack of obvious change in sediment yield in the Upper Yangtze River (Yichan) during the cited period may be due to the offsetting consequences of the sediment yield changes in the two biggest tributaries during this period. It was apparent that the current decreasing trend in sediment yield in the Jialing River was due to the effects of revegetation, soil conservation and water conservancy efforts on reducing river sediment. Land degradation, engineering and channel activities were responsible for the increase in trend in sediment yield of the Jinsha River. (C) 2004 Elsevier B.V. All rights reserved.
产权排序1
会议录GLOBAL AND PLANETARY CHANGE
会议录出版者ELSEVIER SCIENCE BV
会议录出版地AMSTERDAM
语种英语
电子版国际标准刊号1872-6364
ISSN号0921-8181
WOS记录号WOS:000223432200009
源URL[http://ir.imde.ac.cn/handle/131551/33525]  
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_山地表生过程与生态调控重点实验室
科技与合作处
通讯作者Xinbao Zhang
作者单位1.State Key Lab of Loess and Quaternary Geology, Institute for Earth Environments, Chinese Academy of Sciences, 10 Fenghui South Road, Xi’an High-Tech Zone, Xi’an, Shaanxi, China
2.Chengdu Institute of Mountain Hazards and Environment, CAS, PO Box 417, Chengdu, China;
推荐引用方式
GB/T 7714
Xinbao Zhang,Anban Wen. Current changes of sediment yields in the upper Yangtze River and its two biggest tributaries, China[C]. 见:. Xian. MAY, 2001.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。