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渤海动力对黄河入海泥沙输移的影响
引用本文:吴永胜,王兆印.渤海动力对黄河入海泥沙输移的影响[J].海洋科学进展,2002,20(2):22-30.
作者姓名:吴永胜  王兆印
作者单位:清华大学,水利系河流海洋研究所,北京,100084
基金项目:国家自然科学基金资助项目 (5 9890 2 0 0 )
摘    要:海洋动力过程对黄河入海泥沙的淤积和扩散具有决定性作用 ,利用三维斜压动力 -泥沙模型分析了黄河口外海域潮流动力变化与黄河入海泥沙淤积、扩散特性之间的响应关系。季节环流以及涨落潮的分布和变化很好地解释了黄河口南北浮泥的形成和消长变化以及黄河入海泥沙向海扩散的机理。结果表明 ,入海泥沙在洪季、枯季和表底层都具有不同的输移特性

关 键 词:黄河  三维斜压动力-泥沙模型  悬沙扩散  海洋动力过程
文章编号:1000-7199(2002)02-0022-09
修稿时间:2002年1月28日

Effect of the Bohai Sea Dynamics on Sediment Transport Discharged From the Yellow River
WU Yong sheng ,WANG Zhao yin.Effect of the Bohai Sea Dynamics on Sediment Transport Discharged From the Yellow River[J].Advances in Marine Science,2002,20(2):22-30.
Authors:WU Yong sheng  WANG Zhao yin
Institution:WU Yong sheng 1,WANG Zhao yin 1
Abstract:Marine dynamic process plays a decisive role in deposition and dispersion of sediment discharged from the Yellow River. In this paper, a 3 D dynamic and sediment model is used to analyse the relationship between the tidal current variations in the Yellow River mouth area and the sediment deposition discharged from the Yellow River. The mechanisms for the fluid mud formation and variation in the Yellow River mouth area and the seaward dispersion of sediment discharged from the Yellow river are well explained by the seasonal circulation and the tidal current distribution and variation. It is shown from the analysis results that there are different transport characteristics for the discharged sediments in flood and dry seasons and surface and bottom layers.
Keywords:Yellow River  3  D dynamic and sediment model  suspended sediment dispersion  marine dynamic process
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