引用本文:
【打印本页】   【下载PDF全文】   【View/Add Comment】  【Download reader】  【 Close 】
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被：浏览 1598次   下载 1764次 本文二维码信息
码上扫一扫！
分享到： 微信 更多
字体:加大+|默认|缩小-
长江口悬沙及其运移
张志忠1, 徐志刚1
杭州大学河口与港湾研究室
摘要:
关键词:  
DOI：
分类号:
基金项目:
SUSPENDED SEDIMENTS AND ITS TKANSPORT IN THE AREA OF CHANGJIANG RIVER ESTUARY
Abstract:
The annual discharge of suspended sediments is approximately 500 mil. tons. of the suspended sediments, most are fine grained, with the size ranging from 17 μ to 4.7 μ, and a mean value of 8.6 μ. The entrainment of the suspended sediments along the Changjiang River estuary is south-east ward. The exchange of sediments between the channels is also discussed in this article.
Key words:  
Copyright ©  Editorial Office for Marine Sciences Copyright©2008 All Rights Reserved
Supervised by: Chinese Academy of Sciences (CAS)   Sponsored by: Institute of Oceanology, CAS
Address: 7 Nanhai Road, Qingdao, China.  Postcode: 266071  Tel: 0532-82898755  E-mail: bjb@qdio.ac.cn
Technical support: Beijing E-Tiller Co.,Ltd.