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盐城滨海湿地高程监测及潮滩地貌时空变化

赵永强 周良勇 武伟

海洋地质前沿2026,Vol.42Issue(5):83-95,13.
海洋地质前沿2026,Vol.42Issue(5):83-95,13.DOI:10.16028/j.1009-2722.2025.133

盐城滨海湿地高程监测及潮滩地貌时空变化

Elevation monitoring of Yancheng coastal wetland and spatiotemporal changes in tidal flat landforms

赵永强 1周良勇 2武伟3

作者信息

  • 1. 江苏盐城国家级珍禽自然保护区管理处,盐城 224057
  • 2. 中国地质调查局青岛海洋地质研究所,青岛 266237||自然资源部华东海岸带野外科学观测研究站,南京 210007
  • 3. 江苏盐城市勘查测绘院,盐城 224002
  • 折叠

摘要

Abstract

Coastal wetlands have important ecological and environmental values.The core area of the Yancheng National Natural Reserve needs urgent protection.The reserve has been subjected to erosion since 2012,and the edge of the salt marsh has been retreating and tidal flat bed has been deepening.However,there is no proven method on how to carry out seasonal and long-term monitoring on the tidal flats in the reserve,nor the systematic accumulation of data and information.The rod-type surface elevation monitoring system is a widely used wetland elevation monitoring system.Based on the characteristics of tidal flats dynamics,we improved the system and ap-plied it to the tidal flats of the coastal wetlands.Monitoring stations were established in five typical shore beaches,and erosion and siltation monitoring has been carried out seasonally for more than four years.On this basis,a data table of surface elevation changes was formed by combining the absolute elevations measured by Real-Time Kin-ematic positioning(RTK).The data table was processed in several methods,including seasonal comparisons,cu-mulative changes over the years,profile changes,slope changes,and continuous changes in site elevation.Results show that the seasonal and interannual changes in trend and rate changes reflect the amount of cumulative change;profile change and slope changes indicate morphological variation of the profile where monitoring stations situ-ated;and the continuous changes in site elevation show fluctuations in topography over time.Data from the monit-oring stations combined with beach surveys reveal the erosion history on the northern side of the reserve and the erosion-siltation changes on the southern side.The monitoring data in the north indicate that the shoreline has been eroding overall,and the cumulative values of tidal flatbed were lowered from 0.78 to 1.30 m in the four-year period of monitoring,and rates of erosion was decreased from 0.20 to 0.32 m/a.The fitting of the monitoring showed the longterm trend of continuous erosion and the mode of phase change.However,the southern tidal flat showed the dynamics of siltation,erosion,and re-silting,and in general siltation still dominated in the area.The monitoring data record the process and scale of tidal flatbed change,reveal the process of erosion of the coast,and help to verify the numerical simulation results,which is important for the management of the wetland reserve and the development of strategies against erosion.

关键词

侵蚀监测/潮滩高程/杆型地表高程系统/盐城滨海湿地

Key words

erosion monitoring/elevation of tidal flat/RSET/Yancheng coastal wetland

分类

海洋科学

引用本文复制引用

赵永强,周良勇,武伟..盐城滨海湿地高程监测及潮滩地貌时空变化[J].海洋地质前沿,2026,42(5):83-95,13.

基金项目

自然资源部华东海岸带野外科学观测研究站项目"监测杆技术在年际尺度和季节尺度上潮滩动态监测中的应用"(ORSECCZ2022102) (ORSECCZ2022102)

中国地质调查局项目(DD20189503) (DD20189503)

海洋地质前沿

1009-2722

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