| 长江口沙波统计特征及输移规律 |
| |
| 引用本文： | 郭兴杰,程和琴,莫若瑜,杨忠勇.长江口沙波统计特征及输移规律[J].海洋学报,2015,37(5):148-158. |
| |
| 作者姓名： | 郭兴杰 程和琴 莫若瑜 杨忠勇 |
| |
| 作者单位： | 1.华东师范大学 河口海岸学国家重点实验室, 上海 200062;上海市地质调查研究院, 上海 200072 |
| |
| 基金项目： | 国家自然科学基金资助项目(41476075);国家自然科学基金资助项目(41340044);国家自然科学基金中荷合作专项(51061130544)。 |
| |
| 摘 要： | 利用多波束测深系统对长江口南港、北槽、横沙通道和北港水下地貌进行测量,对沙波波高、波长、迎流倾角、背流倾角、水深和沉积物特征进行统计,并根据流速、沉积物粒径及水深估算其潮周期内净位移。结果表明:长江口沙波基本都为大型沙波,且沙波大小与其所在区域沉积物粒径呈正比关系;长江口各个区域沙波的对称性不同,涨、落潮优势流越明显,则沙波对称性越差,净位移越大;沙波对称性能反映此区域水动力强弱及潮周期内沙波净位移大小。
|
| 关 键 词： | 沙波 长江口 涨潮 落潮 位移 |
| 收稿时间： | 2014/5/18 0:00:00 |
| 修稿时间： | 2014/10/18 0:00:00 |
Statistical characteristics and transport law of sand waves in the Yangtze Estuary |
| |
| Guo Xingjie,Cheng Heqin,Mo Ruoyu and Yang Zhongyong.Statistical characteristics and transport law of sand waves in the Yangtze Estuary[J].Acta Oceanologica Sinica (in Chinese),2015,37(5):148-158. |
| |
| Authors: | Guo Xingjie Cheng Heqin Mo Ruoyu and Yang Zhongyong |
| |
| Institution: | 1.State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China;Shanghai Institute of Geological Survey, Shanghai 200072, China2.State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China3.The Third Haber Engineering Investigation and Design of the Ministry of Communications, Shanghai 200032, China4.College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China |
| |
| Abstract: | The underwater topography at the South Channel,North Passage,Channel of Hengsha and North Channel of the Yangtze Estuary were surveyed by using multibeam echo-sounding system,wave height,wavelength,inflow angle,the dorsal stream angle and sediment characteristics of sand waves in these areas were calculated statistically,and the net displacement of sand waves in one tidal period was estimated on the basis of data for flow rate,grain sizes of sediments and water depths. The results showed that the sand waves in the Yangtze Estuary were basically large,and there took on a proportional relationship between wavelengths with sediment particle sizes. The symmetry of sand waves is different among all surveyed area in the Yangtze Estuary. The more obvious the ebb flow is,the worse the symmetry of sand wave and the more net displacement is. The symmetry of sand waves can reflect the power of water and net displacement of sand waves. |
| |
| Keywords: | sand waves Yangtze Estuary flood ebb displacement |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《海洋学报》浏览原始摘要信息 |
| 点击此处可从《海洋学报》下载免费的PDF全文 |
|
