摘要
根据现场测量资料分析,作者获得了如下结论:(1)潮流是烂泥形成的主要动力;(2)余流环流固定了烂泥的位置;(3)絮凝作用加速了烂泥的形成;(4)波浪力更新了烂泥。对于现行河口烂泥形成的动力机制进行了综合概述。
Based on the field measured data, the following conclusions are obtained; (1) Tidal current is an important dynamic factor of formation of muddy sediment. (2) Location of muddy sediment is fixed by the circulation of residual current. (3) Muddy sediment is quickened by flocculation. (4) Muddy sediment is renewed by wave force. In this paper the author has summarized the dynamic mechanism of formation of muddy sediment at Yellow River estutary.
出处
《海岸工程》
北大核心
1992年第2期44-52,共9页
Coastal Engineering
