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潮汐河道河床活动性时空变化研究

黄春华 吴尧 卢陈 高时友

泥沙研究2023,Vol.48Issue(6):44-50,7.
泥沙研究2023,Vol.48Issue(6):44-50,7.DOI:10.16239/j.cnki.0468-155x.2023.06.007

潮汐河道河床活动性时空变化研究

Study on temporal and spatial variations of bed activity in tidal rivers:A case of Shenzhen River

黄春华 1吴尧 2卢陈 1高时友1

作者信息

  • 1. 珠江水利委员会珠江水利科学研究院,广东广州 510611||水利部珠江河口治理与保护重点实验室,广东广州 510611
  • 2. 珠江水利委员会珠江水利科学研究院,广东广州 510611||水利部珠江河口治理与保护重点实验室,广东广州 510611||河海大学水文水资源与水利工程科学国家重点实验室,江苏南京 210098
  • 折叠

摘要

Abstract

The evolution of erosion and deposition in tidal rivers is related to river regulation and smooth navigation,it is of great significance to study the riverbed activity and its variation in temporal and spatial.Taken the Shenzhen River,a typical tidal-dominant river,as an example,the variation characteristics of water and sediment relationship in different river reaches during flood and dry seasons are comparative analyzed,and the dominant discharges in different seasons are calculated by the Makayev method,the impacts of river runoff and tidal current on the dominant discharge are also discussed to further explore the temporal and spatial variations of riverbed activity.The results show that the periodic flood-ebb tidal current plays a substantive role on the riverbed evolution,there exists a cluster of dominant discharge with basically equivalent bed forming effect.The dominant discharge at Shenzhenhekou station in the lower reach ranges from 200 to 280 m3/s,and it is greater in the wet season than that in the dry season.However,the dominant discharge at Luohu station in the upper reach is about 40~60 m3/s,with small difference in different seasons.The characteristics of scouring in flood season and silting in dry season are in good relationship with the variation of dominant discharge,the riverbed activity in the upper and lower reaches of the Shenzhen River presents significant spatial differences.

关键词

造床流量/涨落潮流/洪冲枯淤/潮汐河道

Key words

dominant discharge/flood and ebb current/seasonal changes/tidal river

分类

建筑与水利

引用本文复制引用

黄春华,吴尧,卢陈,高时友..潮汐河道河床活动性时空变化研究[J].泥沙研究,2023,48(6):44-50,7.

基金项目

国家自然科学基金青年基金项目(42006157) (42006157)

水文水资源与水利工程科学国家重点实验室"一带一路"水与可持续发展科技基金(2020492111) (2020492111)

泥沙研究

OA北大核心CSCDCSTPCD

0468-155X

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