引用本文:严以新,高进,诸裕良,茅丽华,郑金海.长江口北槽优良河势机制[J].水利水运工程学报,2001,(3):8-12
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长江口北槽优良河势机制
严以新1,高进2,诸裕良1,茅丽华1,郑金海1
1. 河海大学海岸及海洋工程研究所
2. 湘潭工学院土木系
摘要:
长江口南港北槽具有稳定的分流比和相对较小的分沙比。其优良河势的机制在于,北槽与南港主槽衔接顺直,利于水流下泄;南、北槽分流口流场的水动力特征有利于南槽排泄底沙。
关键词:  分流比 分沙比 水动力 输沙 北槽 长江口
DOI:
分类号:TV143.3
基金项目:国家自然科学基金资助项目(50079003)
Mechanism of excellent regime of north channel in the Yangtze Estuary
YAN Yi xin ,GAO Jin ,ZHU Yu liang ,MAO Li hua ,ZHENG Jin hai
YAN Yi xin 1,GAO Jin 2,ZHU Yu liang 1,MAO Li hua 1,ZHENG Jin hai 1
Abstract:
The regime of the north channel in the Yangtze Estuary is excellent with a stable discharge ratio and a relatively small sand ratio.Because the north channel is favorable to dewatering,joining smoothly to the major channel of Nangang,and the hydrodynamic characteristics of the velocity field in the diversion of the north and south channels are beneficial for the south channel to desilt.
Key words:  discharge ratio,sand ratio,hydrodynamic characteristic,desilting,the north channel,the Yangtze Estuary
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