摘要
本文报道了九龙江口口门浅滩地貌、沉积特征和水文泥沙特性，探讨了九龙江口口门浅滩特别是厦门海沧进港航道（即鸡屿北水道）口门浅滩的形成与演变。结果表明，厦门海沧进港航道口门浅滩是在江流、海潮、成淡水交汇等多种因素综合作用和影响下形成的，其冲淤演变过程与鸡屿河口沙坝不断淤积扩大有着直接的关系。
Based on the comprehensive environmental data of Xiamen Harbour and Jiulong River Estuary, this paper briefly describes the formation and evolution of the Jiulong Rlver estuarine shoal, especially those of the estuarine shoal in the channel to the Haichang port of Xiamen. The result shows that the estuarine shoal was formed by the comprehensive effects of such factors as the river runoff, tidal waves, and the convergence of saline and fresh water etc. And the progress of its alluviation and evolution relates directly to the continuous silting up and expansion of the estuarlne sand bar at the Jiyu Islet.
出处
《台湾海峡》
CAS
CSCD
1994年第4期317-322,共6页
Journal of Oceanography In Taiwan Strait
关键词
河口浅滩
冲淤演变
福建
Estuarine shoal, scouring-silting evolution, Fujian
