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长江口南港北槽水域水文特征分析

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长江口水域滩槽相间汊道众多,河势水情变化复杂.为分析径潮流作用下长江口南港北槽水域水文的变化,进一步提高对长江口南港北槽水域的认识,基于 2018-2022 年长江口水域各实测站点洪枯季水文测量资料,对各水文特征值进行统计对比分析.研究结果表明:径潮流变化对长江口南港北槽水域各水文特征影响不尽相同,水域涨落潮流同时受到径流和潮流的耦合作用影响.径潮流在南港北槽水域影响作用的临界点大约在北槽上口门水域,临界位置跟随径潮流变化而摆动,盐水楔和最大浑浊带的位置也随着径潮流变化而上下摆动,并且此种摆动也会造成回淤分布的变化.
Hydrographic characteristics for south channel and north passage of Yangtze River estuary
The waters of the Yangtze River estuary are characterised by a large number of channels and complex changes in river conditions.To analyse the changes in hydrology of the south channels and north passage of the Yangtze River estuary under the action of runoff currents,and further improve the understanding of the south channels and north passage of the Yangtze River estuary,statistical comparative analyses are conducted on the hydrological characteristics based on the hydrographic data of the flood and dry season at each measured station in the Yangtze River estuary from 2018 to 2022.The research results show that the impact of runoff and tidal current changes on the hydrological features of the south channels and north passage of the Yangtze River estuary are different,and the upward and downward flows of the waters are influenced by the coupling effect of runoff and tidal current at the same time.The critical point of the influence of the runoff tide in the south channels and north passage is around the upper mouth of the north passage.The critical position oscillates with the change of the runoff and tide,and the position of the salt water wedge and the maximum turbidity zone also oscillates up and down with the change of the runoff and tide.This oscillation also causes the change of the silt return distribution.

Yangtze estuaryrunoff and tidehydrology

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交通运输部长江口航道管理局, 上海 200003

上海河口海岸科学研究中心, 上海 201201

长江口 径潮流 水文

2024

水运工程
中交水运规划设计院有限公司

水运工程

CSTPCD
影响因子:0.428
ISSN:1002-4972
年,卷(期):2024.(2)
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