摘要
本文通过长江口航道淤泥的室内波浪试验研究,认为影响波长变化的主要因素有相对泥床厚度、泥床含沙浓度及相对(传播距离)波长等。在本试验范围内,波浪在泥床上传播时的波长变化一般在±5％以内;但在相对泥床厚度、泥床含沙浓度及相对(传播距离)波长均较大时,波浪被急剧衰减,波长也随之迅速减小。
Through tests that were conducted in a flume by using silt from the navigation channel of the Yangtze river mouth, the paper shows that the main affective factors of wave length are relative silt bed depth (D,/D),volume ratio of silt content in the bed (Sr) and relative wave length (L/l), etc.
In this experiment, change of wave length with wave flume propagating on the silt bed is mostly within ±5 %, but wave length will also promptly decrease along when depth of the relative silt bed, volume ration of silt content and relative wave length are all quite large.
出处
《热带海洋》
CSCD
1991年第3期91-95,共5页
关键词
波长
变化
泥床
波浪
Wave length change, Relative silt bed depth, Volume ratio of silt content in the bed, Relative wave length, Wave decay, Effective water depth
