摘要
根据实测资料分析发现，射阳港拦门沙具有一年内随烘、枯水期不断南北往复摆动、而多年总体向北偏移和水深逐渐变深的变化规律：其演变是射阳河口建挡潮闸，下泄径流量及河道纳潮量变化、潮波变形和废黄河口泥沙沿岸运移所致，对船舶航行和港口建设有参考意义。
The changing pattern of the mouth bar and the cause evolution is analysed based on measured data for Sheyang Habour in this paper, which have important meaning for directting production and construction of the harbor.
出处
《海岸工程》
1998年第3期14-17,共4页
Coastal Engineering
关键词
射阳港
拦门沙
演变
港口
Sheyang Port the mouth bar evolution
