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2017-2022年深圳海水入侵变化趋势及影响因素

陈北辰 李晴岚 王正阳 张洪岩 李文博 程靖清 王晓

海洋地质前沿2024,Vol.40Issue(1):55-64,10.
海洋地质前沿2024,Vol.40Issue(1):55-64,10.DOI:10.16028/j.1009-2722.2023.003

2017-2022年深圳海水入侵变化趋势及影响因素

Analysis on the change trend and influencing factors of seawater intrusion in Shenzhen from 2017 to 2022

陈北辰 1李晴岚 2王正阳 3张洪岩 3李文博 3程靖清 3王晓4

作者信息

  • 1. 中国科学院深圳先进技术研究院,深圳 518055||深圳市自然资源与不动产评估发展研究中心,深圳 518040||中国地质大学(武汉)海洋学院,武汉 430074||中海石油(中国)有限公司深圳分公司,深圳 518054
  • 2. 中国科学院深圳先进技术研究院,深圳 518055
  • 3. 深圳市自然资源与不动产评估发展研究中心,深圳 518040
  • 4. 中国地质大学(武汉)海洋学院,武汉 430074
  • 折叠

摘要

Abstract

Based on the data of 25 monitoring wells on seawater intrusion in Shenzhen,from 2017 to 2022,and using Cl-concentration as the evaluation index,the spatial distribution and variation trend of seawater intrusion in Shenzhen were analyzed.Results show that the buried groundwater layer in Shenzhen is relatively shallow,and the change of water level elevation was relatively stable.Seawater intrusion was detected mainly in the Shajing area of Bao'an,the central area of Nanshan,the Yantian Free Trade Zone,and the mouth of the Kwai Chung River in Dapeng.Meanwhile,the factors including regional geology,rock and soil types,resistivity geophysical pro-specting,rainfall changes,and human activities were considered,and results show that the exploitation of ground-water is an important factor causing seawater intrusion.The Quaternary faults are potential channels for seawater intrusion.The land reclamation area is vulnerable to seawater intrusion.The correlation between rainfall and sea-water intrusion is small.This study provided a reference for the disaster prevention of seawater intrusion in Shen-zhen.

关键词

海水入侵/地下水/氯离子浓度/降雨量/深圳市

Key words

seawater intrusion/groundwater/chloride concentration/rainfall/Shenzhen

分类

海洋科学

引用本文复制引用

陈北辰,李晴岚,王正阳,张洪岩,李文博,程靖清,王晓..2017-2022年深圳海水入侵变化趋势及影响因素[J].海洋地质前沿,2024,40(1):55-64,10.

基金项目

深圳市基础研究面上项目"登陆粤港澳大湾区台风降雨时空分布特征及机理研究"(JCYJ20210324101006016) (JCYJ20210324101006016)

深圳市国际合作研究项目"粤港澳湾区复杂地形条件下热带气旋近地面风场形成机制及预报研究"(GJHZ20210705141403010) (GJHZ20210705141403010)

海洋地质前沿

OA北大核心CSTPCD

1009-2722

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