摘要
分析虾峙门海域实测的潮流、波浪及泥沙资料，通过研究该海区水流泥沙特性表明：由于狭道地形影响，狭道内及口门处潮流为往复流，口门外开阔海域潮流为顺时针方向的旋转流；波流作用与水体含沙量有对应关系。
The real-measured data of the current, wave and sediment of Xiazhimen Sea Area is analyzed. Based on the study of the flow & sediment characteristics of this area, it is shown that because of the influence of the narrow pass topography, the tide inside the narrow pass and at the entrance is reversing current and the tide at the open area outside the entrance is rotary current of clockwise direction. There is a corresponding relation between wave action and silt content.
出处
《水运工程》
北大核心
1997年第9期1-4,共4页
Port & Waterway Engineering
