1) Nanhuizui tidal flat
南汇嘴潮滩
1.
Analysis on Recent Topography evolution of Nanhuizui tidal flat in Yangtze Estuary;
长江河口南汇嘴潮滩近期演变分析
2) Nanhuizui tideland
南汇嘴岸滩
1.
Nanhuizui tideland is a transitional zone situated in a special area between the Yangtze estuary and Hangzhou Bay.
南汇嘴岸滩位于长江口和杭州湾的交汇地带，是长江口与杭州湾两股水流涨潮分流和落潮合流的缓流地区，涨潮水流携带大量泥沙上滩，在缓流区落淤，促使滩地淤涨发育，成为上海陆缘岸滩淤涨速度最快的滩涂，也是上海陆缘最大的后备土地资源地。
3) Jinhui tidal flat
金汇潮滩
1.
Based on the data extracted from bathymetric maps and data obtained through hydrological and sediment surveys,this paper mainly deals with the evolution of siltation and erosion of the Jinhui tidal flat in the north of Hangzhou Bay.
11世纪中叶,杭州湾北岸自修筑了第一条海塘进入人工控制后,金汇潮滩处于淤涨中。
4) Nanhui east shoal
南汇东滩
1.
Analysis of the causes of freshwater resource in Nanhui east shoal in the Yangtze River estuary;
长江口南汇东滩近岸淡水资源的成因探讨
2.
Study on Utilization of Freshwater Resource on Nanhui East Shoal in Changjiang Estuary;
长江口南汇东滩近岸水域淡水资源开发利用研究
3.
In order to understand the rule of the fresh water on the Nanhui east shoal, we have monitored the salinity over a year.
经过南汇东滩为期1 a的水体盐度监测,了解了当地淡水资源的年度分布规律。
5) Nanhui nearshore
南汇边滩
1.
Nanhui nearshore is situated in a special area of the Yangtze Estuary, Hangzhou Bay and sea interactions.
南汇边滩是长江口、杭州湾以及外海三者交互作用的特殊地带。
2.
This paper takes Nanhui nearshore which is an intersectant area of Changjiang Estuary and Hangzhou Bay as a study object.
本文以长江口与杭州湾交汇地带的南汇边滩为研究对象，在充分借鉴前人研究的基础上，采用水文学、泥沙运动力学和数理统计等方法，对长江口与杭州湾水沙交换的动力机制和输移特征以及南汇边滩的水动力、泥沙输移进行了深入系统的研究。
6) Nanhui Spit
南汇嘴
1.
Researches on characteristics and dynamic mechanism of short-term scouring and silting changes of the tidal flat on Nanhui Spit in the Changjiang Estuary in China
长江口南汇嘴潮滩短期冲淤演变及其动力机制研究
补充资料：迎潮送潮辞·送潮
【诗文】：
潮西来兮又东下，日染中流兮红洒洒。汀葭苍兮屿蓼枯，
风骚牢兮愁烟孤。大几望兮微将晦翳，睨瀛溶兮敛然而退。
爱长波兮数数，一幅巾兮无缨可濯。帆生尘兮楫有衣，
怅潮之还兮吾犹未归。
【注释】：
【出处】：
全唐诗：卷621-22
潮西来兮又东下，日染中流兮红洒洒。汀葭苍兮屿蓼枯，
风骚牢兮愁烟孤。大几望兮微将晦翳，睨瀛溶兮敛然而退。
爱长波兮数数，一幅巾兮无缨可濯。帆生尘兮楫有衣，
怅潮之还兮吾犹未归。
【注释】：
【出处】：
全唐诗：卷621-22
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条