长江流域资源与环境 >> 2017, Vol. 26 >> Issue (05): 698-705.doi: 10.11870/cjlyzyyhj201705006
姚振兴, 陈庆强, 杨钦川
YAO Zhen-xing, CHEN Qing-qiang, YANG Qin-chuan
摘要: 崇明岛作为我国最大的河口冲积岛,其形成发育与长江来水来沙息息相关。历史上就有崇明岛围垦筑堤的记载,近60年来崇明岛东部地区所筑大堤主要有54大堤、64大堤、68大堤、92大堤和98大堤。选取正东、东北、东南不同方向的4个断面,以大堤位置代表所筑年份海岸线位置,对崇明岛东部淤涨速率及滩地淤涨面积变化进行计算,结果表明:(1)近60年来崇明岛东部整体淤涨速率约为200 m/a,淤涨面积年均增长率为2.80 km2/a;(2)不同断面上淤涨速率存在差别,其中正东方向断面上淤涨最快;(3)不同时段崇明岛东部各断面淤涨速率存在快慢变化。各断面上,20世纪90年代的淤涨速率均最大。对比发现,20世纪50~80年代崇明岛东部淤涨速率的变化趋势,与同期长江年入海泥沙量的变化趋势基本一致;但20世纪90年代,由于围垦强度加大,两者变化趋势不一致。以海堤研究岸线变迁的工作尚不多见,此方法将为研究长时间尺度的岸线变迁提供借鉴。
中图分类号:
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