摘要
本文首先建立了一个一维水流、二维泥沙数学模型,以长江口南港北槽为实际背景,研究了径流和潮流共同作用下,泥沙输运的规律;讨论了泥沙近底边界条件,认为非恒定情况下泥沙底边界条件应考虑沉降效应。分析了径流和潮流的不同组合,对长江口泥沙输运的影响。同时,对长江口实施整治工程后航道的变化进行了预测。
A one dimensional, vertical grid unsteady model is
developed to study sediment transport in combined tide runoff flows around the Yangtze
estuary. The model uses reference concentration as the bottom boundary condition for
suspended sediment. It is suggested that the bottom boundary condition in unsteady flow
should take the effect of sediment settling into consideration. The respective influences of
runoff and tide have been carefully analysed. Finally, the topographic variation of waterway
between north and south dykes is predicted.
出处
《水动力学研究与进展(A辑)》
CSCD
北大核心
1999年第1期90-100,共11页
Chinese Journal of Hydrodynamics
基金
国家自然科学基金
中国科学院力学研究所所长择优基金