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| 潮流对黄河入海泥沙在渤海中输运的贡献 | |
| 引用本文： | 王海龙,韩树宗,郭佩芳,李国胜. 潮流对黄河入海泥沙在渤海中输运的贡献[J]. 泥沙研究, 2011, 0(1) |
| 作者姓名： | 王海龙 韩树宗 郭佩芳 李国胜 |
| 作者单位： | 1. 广东省电力设计研究院,广东,广州,510663 2. 中国海洋大学海洋系,山东,青岛,266003 3. 中国科学院,地理科学与资源研究所,北京,100101 |
| 基金项目： | 自然科学基金项目(40506024、40771030、41076003) |
| 摘 要： | 基于ECOMSED模型研究分析单纯潮流作用下黄河入海泥沙在渤海中的输运特征。研究表明,渤海海域陆架坡度远小于内波特征参量,因此除黄河入海口附近以及其他近岸极浅海域之外,单纯潮流作用下渤海大部分海域的表层悬沙含量较低,但与实际水动力条件的空间分布格局基本一致。悬沙含量垂向分布特征明显,底边界层内因为较大的垂向湍流粘性系数,因此悬沙含量可以维持较高的水平,而底边界层之外悬沙含量迅速降低2～3个数量级;同时悬沙含量呈现出比较明显的潮周期(M2)变化特征。潮流作用下,绝大部分黄河入海泥沙沉积在黄河三角洲附近,只有少量悬沙可以发生长距离输送。黄河入海泥沙输运通量在口门外呈现一对涡状结构,成为水下三角洲南北两侧泥质沉积区形成的主要机制。 |
| 关 键 词： | 黄河入海泥沙 渤海 潮流 数值模拟 |
Transportation of sediment from Yellow River in Bohai Sea due to tidal currents |
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| WANG Hai-long,HAN Shu-zong,GUO Pei-fang,LI Guo-sheng. Transportation of sediment from Yellow River in Bohai Sea due to tidal currents[J]. Journal of Sediment Research, 2011, 0(1) | |
| Authors: | WANG Hai-long HAN Shu-zong GUO Pei-fang LI Guo-sheng |
| Affiliation: | WANG Hai-long1,HAN Shu-zong2,GUO Pei-fang2,LI Guo-sheng3(1.Guangdong Electric Power Design Institute,Guangdong Guangzhou,510663,China,2.Department of Oceanography,Ocean University of China,Shandong Qingdao 266003,3.Institute of Geographical Science and Natural Resource Research,CAS,Beijing 100101,China) |
| Abstract: | On the basis of ECOMSED,a state-of-the-art model considering 3D baroclinic circulation and sediment transportation,the contribution due to the tidal currents to the transportation of the sediment from the Yellow River in the Bohai Sea is investigated.Calculations found that the continental slope of the Bohai Sea is far less than that of the internal wave characteristics.Although it was almost the same spatial distribution structure with those under the actual hydrodynamical environment,the surface sediment ... |
| Keywords: | suspended sediment Yellow River Bohai Sea tidal current numerical simulation |
| 本文献已被 CNKI 万方数据 等数据库收录！ | |