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淤泥质海岸形态的演变及形成机制

Development and mechanism of transitional coast

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【作者】 王艳红张忍顺吴德安燕守广沈永明刘永学陈宏友

【Author】 WANG Yanhong1, ZHANG Renshun1, WU Dean1, YAN Shouguang1, SHEN Yongmin1, LIU Yongxue1, CHEN Hongyou2(1. Institute of Ocean & Tidalflat, Nanjing Normal University, Nanjing 210097, China; 2.Bureau of Agricultural Resources Development of Jiangsu Province, Nanjing 210093, China)

【机构】 南京师范大学海洋与滩涂研究所江苏省农业资源开发局 江苏 南京 210097江苏 南京 210097江苏 南京 210093

【摘要】 在淤长型和侵蚀型岸段之间,存在着一种由淤积到侵蚀的过渡型岸段。通过剖面测量、粒度分析和地质调查,认为过渡型岸段具有上部淤积下部冲刷、冲刷逐渐向上部扩展、潮滩表层沉积物不断粗化、淤积带逐渐变窄最后过渡到全剖面侵蚀的基本特征和发展趋势。

【Abstract】 In the muddy coast that makes up 92% of Jiangsu coastline, there are not only seriously eroding segments such as the Abandoned Huanghe River Mouth but also quickly prograding ones. Between the two kinds of coasts, there is a transitional coast from prograding to eroding. Measurements of coastal profiles, particle size analyses and geological investigations, indicate that the transitional coasts has some essential characteristics and developing tendencies as follows: prograding is found on the upper parts and eroding on the lower parts; erosion expands landward and the prograding area becomes narrower and narrower; and the whole profile will be eroded at last.

【基金】 教育部"海岸滩涂演变规律及可持续利用模式研究"重点项目资助(000171)
  • 【文献出处】 海洋工程 ,The Ocean Engineering , 编辑部邮箱 ,2003年02期
  • 【分类号】P737.1
  • 【被引频次】71
  • 【下载频次】1095
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