吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (4): 1193-1203.doi: 10.13278/j.cnki.jjuese.20200114
魏伟, 骆蓓菁, 丁玲
Wei Wei, Luo Beijing, Ding Ling
摘要: 由于人类活动的不断加剧和入海泥沙的日益减少,我国部分河口潮滩湿地已面临严重的侵蚀退化风险,给沿岸城市发展带来巨大威胁,实现河口潮滩湿地的科学管理和合理利用极为紧迫。本研究利用1990—2017年多期长江口深水航道北导堤工程与横沙岛成陆-促淤工程前后区域海图地形数据,使用ArcGIS地理配准、等深线数字化、数字高程模型建立和叠加分析等功能分析长江口横沙岛潮滩湿地地貌、等深线形态与地形冲刷-淤积厚度的时空变化过程。研究结果表明,长江口深水航道北导堤工程与横沙岛成陆-促淤工程的实施,改变了横沙岛潮滩湿地周边水域的水文泥沙动力条件,使得地貌冲淤时空特征发生变化:1)深水航道北导堤工程与横沙岛成陆-促淤工程的实施极大地推动了特征等深线的向外延伸,其中0、2和5 m等深线包络面积年均最大增长率(2009—2013年)分别是工程前(1990—1998年)的42.13、280.73和235.65倍,0~1、1~2、2~3、3~4及4~5 m等深线包络体积整体呈现1990—1998年、1998—2009年、2009—2013年增加,2013—2017年较为明显减少,潮滩湿地"长高不长大"的趋势;2)冲刷-淤积频率特征表现为工程前微淤(1990—1998年)、工程后微淤(1998—2009年)、淤积增加明显(2009—2013年)及微冲(2013—2017年),长江入海泥沙通量的减少对2 m等深线以深区域的潮滩发育可能产生一定影响。
中图分类号:
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