测绘通报 ›› 2025, Vol. 0 ›› Issue (6): 103-108,122.doi: 10.13474/j.cnki.11-2246.2025.0618

• 学术研究 • 上一篇    

黄河三角洲海岸线变化与地面沉降监测分析

高浩亮1,2, 李德伟1, 李朋朋1, 李晓红3, 狄桂栓3   

  1. 1. 山东建筑大学测绘地理信息学院, 山东 济南 250101;
    2. 高青县自然资源局, 山东 淄博 256300;
    3. 山东省国土测绘院, 山东 济南 250102
  • 收稿日期:2024-11-12 发布日期:2025-07-04
  • 通讯作者: 李德伟。E-mail:lidewei20@sdjzu.edu.cn
  • 作者简介:高浩亮(1993—),男,硕士生,主要研究方向为卫星大地测量。E-mail:gaohaoliang001@163.com
  • 基金资助:
    国家自然科学基金(42304001);山东省自然科学基金(ZR2021QD155)

Monitoring and analysis of coastline change and land subsidence in the Yellow River Delta

GAO Haoliang1,2, LI Dewei1, LI Pengpeng1, LI Xiaohong3, DI Guishuan3   

  1. 1. School of Surveying and Geo-informatics, Shandong Jianzhu University, Jinan 250101, China;
    2. Gaoqing County Bureau of Natural Resources, Zibo 256300, China;
    3. Shandong Provincial Institute of Land Surveying and Mapping, Jinan 250102, China
  • Received:2024-11-12 Published:2025-07-04

摘要: 针对黄河三角洲海岸线附近地面沉降严重和海岸线侵蚀隐患加剧的问题,本文提出了一种以DS-InSAR和一般高潮线法为基础,结合垂直断面法的海岸线变化与地面沉降综合监测和分析框架,开展了2020—2024年黄河三角洲海岸线变化与地面沉降监测分析。结果表明,黄河三角洲地面沉降集中分布于东部沿海,形成4处显著沉降漏斗(ABCD),最大沉降速率为-350mm/a。由于人工岸线的围垦与加固,A区海岸线基本稳定。B区临近黄河入海口,海岸线淤进蚀退变化剧烈,海岸线最内侧距沉降中心约4km。C区海岸线整体淤进蚀退幅度为0.91km,距沉降中心约8km。D区海岸线呈缓慢蚀退趋势,海岸线最内侧距堤坝约0.15km,距沉降中心约9km。研究结果对海岸综合治理具有参考价值。

关键词: 黄河三角洲, 海岸线变化, 地面沉降, DS-InSAR, 一般高潮线

Abstract: In response to the severe land subsidence and escalating coastal erosion risks near the coastline of the Yellow River Delta, this paper proposes an integrated monitoring and analyzing framework of coastline change and land subsidence based on DS-InSAR and general high tide line method, combined with the vertical section method. The paper carries out the monitoring and analysis of coastline change and land subsidence in the Yellow River Delta from 2020 to 2024. The results show that land subsidence in the Yellow River Delta is concentrated along the eastern coast, forming four significant subsidence funnels (A,B,C,D), with a maximum subsidence rate of -350 mm/a. Due to the reclamation and stabilization of the artificial coastline, the coastline is basically stable in zone A. Zone B is close to the estuary of the Yellow River, with dramatic changes in the siltation, erosion and recession of the coastline, and the innermost part of the coastline is about 4 km away from the center of the subsidence. The overall siltation and erosion of the coastline in zone C is 0.91 km, about 8 km from the center of subsidence. The coastline of zone D is slowly eroding, with the innermost part of the coastline about 0.15 km from the dyke and 9 km from the center of subsidence. The results of the study have a reference value for the comprehensive management of the coastline.

Key words: Yellow River Delta, coastline change, land subsidence, DS-InSAR, general high tide line

中图分类号: