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磨刀门咸潮上溯对河口拦门沙地形变化的响应研究

林中源 胡晓张 邹华志 张光 陈睿智 唐琦

水资源保护2024,Vol.40Issue(5):104-111,8.
水资源保护2024,Vol.40Issue(5):104-111,8.DOI:10.3880/j.issn.1004-6933.2024.05.013

磨刀门咸潮上溯对河口拦门沙地形变化的响应研究

Study on response of saltwater intrusion to topographic changes of mouth bar in Modaomen Estuary

林中源 1胡晓张 1邹华志 1张光 2陈睿智 1唐琦3

作者信息

  • 1. 水利部珠江河口治理与保护重点实验室,广东广州 510611||珠江水利科学研究院河流海岸研究所,广东广州 510611
  • 2. 中山大学海洋科学学院,广东珠海 519082
  • 3. 珠江水利科学研究院河流海岸研究所,广东广州 510611
  • 折叠

摘要

Abstract

Using measured terrain data from 2005 and 2020 before and after topographic changes of mouth bar in the Modaomen Estuary,a FVCOM three-dimensional numerical model was used to compare and analyze the response of saltwater intrusion to topographic changes of mouth bar,and to explore the impact mechanism of mouth bar shrinkage on salt transport.The results showed that the mouth bar shrinkage resulted in increases in the salinity difference between the surface and bottom layers of each water intake in the Modaomen Waterway,increases in the degree of water stratification,and gradual decreases in the degree of stratification enhancement from downstream to upstream.The maximum potential energy anomaly of Guangchang Pump Station increased by 25.2 J/m3,while Majiao Water Lock,Pinggang Pump Station,and Zhuzhoutou Pump Station increased by 8.3,2.9,and 0.2 J/m3 respectively.The shrinkage of the mouth bar did not change the upward trend of the saltwater intrusion in the Modaomen Estuary,and the peak salinity of the half-moon tide cycle still appeared in the middle tide period after the small tide.The mouth bar has a significant hindering effect on the upstream movement of the saltwater intrusion.The maximum upstream distance of the 15 psu iso-salinity line in the bottom layer is pushed towards the land by 5.1 km,while the maximum upstream distance of the 0.5 psu iso-salinity line in the surface layer,which is more important for water intake,is pushed towards the land by 2.9 km.The significant increase of stable shear salt flux is the main reason for the saltwater intrusion after the shrinkage of mouth bar,on top of which is the influence of tidal oscillation salt flux increase.

关键词

咸潮上溯/河口拦门沙/FVCOM三维数值模型/盐通量/磨刀门

Key words

saltwater intrusion/mouth bar/FVCOM three-dimensional numerical model/salt flux/Modaomen Estuary

分类

海洋科学

引用本文复制引用

林中源,胡晓张,邹华志,张光,陈睿智,唐琦..磨刀门咸潮上溯对河口拦门沙地形变化的响应研究[J].水资源保护,2024,40(5):104-111,8.

基金项目

广东省水利科技创新项目(2023-01) (2023-01)

水利部重大科技项目(SKS-2022005) (SKS-2022005)

水资源保护

OA北大核心CSTPCDEI

1004-6933

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