摘要
针对1998 年洪季北槽下段航道#255 ~#260 灯浮段出现的局部淤浅现象, 由近年来不同季节的测图资料分析研究结果表明: 这是北槽下段总的演变格局所决定; 与当时正在施工的长江口深水航道治理工程无关, 对北槽下段航道的淤浅也没有影响。
To counter the phenomenon of local siltation appeared at the section between #255~ #260 light buoys along the downstream north channel during flood period of 1998,anslyses are carried out to the mapping data of different seasons of several years.It is shown that the siltation is because of the overall evolution pattern of the downstream north channel,and has no relationship with the deepwater channel regulation project.
出处
《水运工程》
北大核心
1999年第10期48-51,共4页
Port & Waterway Engineering
关键词
长江口
北槽下段
航道淤浅
原因分析
演变格局
the Yangtze Estuary
downstream north channel
siltation at waterway
analysis of reasons