| 磨刀门河口环流与咸淡水混合层化机制 |
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| 引用本文： | 吕紫君,冯佳佳,郜新宇,汪玉平,张梦茹,孔俊.磨刀门河口环流与咸淡水混合层化机制[J].水科学进展,2017,28(6):908-921. |
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| 作者姓名： | 吕紫君 冯佳佳 郜新宇 汪玉平 张梦茹 孔俊 |
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| 作者单位： | 1.河海大学江苏省海岸海洋资源开发与环境安全重点试验室, 江苏 南京 210098; |
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| 基金项目： | 水利部公益性行业科研专项经费资助项目（201501010）；江苏省第十三批六大人才高峰项目（HYGC-004） |
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| 摘 要： | 为研究磨刀门盐水混合层化特征，基于SCHISM模型，建立了三维盐度数值模型，根据实测资料对其进行验证。结合水体势能异常理论，对枯季磨刀门河口混合层化的时空变化特征及深槽与浅滩的层化机制差异进行分析。结果表明:磨刀门河口小潮时水体层化最强，中潮时水体层化最弱，且拦门沙至挂定角段水体层化始终较强。磨刀门深槽水体层化主要受纵向平流、纵向水深平均应变和垂向混合影响，而浅滩水体层化则受横向平流、横向水深平均应变和垂向混合影响；磨刀门河口表、底层水体湍动能耗散率较高，而中间水层存在低耗散区，且涨潮时湍动能耗散率比落潮时大。
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| 关 键 词： | 混合与层化 势能异常 河口环流 湍动能耗散率 磨刀门河口 |
| 收稿时间： | 2017-04-18 |
Estuarine circulation and mechanism of mixing and stratification in the Modaomen Estuary |
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| LYU Zijun,FENG Jiajia,GAO Xinyu,WANG Yuping,ZHANG Mengru,KONG Jun.Estuarine circulation and mechanism of mixing and stratification in the Modaomen Estuary[J].Advances in Water Science,2017,28(6):908-921. |
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| Authors: | LYU Zijun FENG Jiajia GAO Xinyu WANG Yuping ZHANG Mengru KONG Jun |
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| Affiliation: | 1.Jiangsu Key Laboratory of Coast Ocean Resources Development and Environment Security, Hohai University, Nanjing 210098, China;2.Nanjing Water Planning and Designing Institute Corp, Ltd, Nanjing 210006, China;3.Nanjing University of Information Science & Technology, Nanjing 210044, China |
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| Abstract: | To study the characteristics of mixing and stratification in the Modaomen Estuary, a three-dimensional numerical salinity model was established based on SCHISM and then calibrated against measured data. Combined with the theory of the water potential difference, the temporal and spatial variation characteristics of mixing and stratification in the dry season and stratification mechanism of a deep channel and shoal were studied. The results show that water stratification is the strongest during the neap tide and is the weakest during the medium tide. Saltwater from the sandbar to Guadingjiao is always highly stratified. Along-channel advection, along-channel depth-mean straining and vertical mixing are the main factors that influence the water stratification of the deep channel. While cross-channel advection, cross-channel depth-mean straining and vertical mixing are the main factors that influence the water stratification of the shoal. In addition, there is a relatively high dissipation of turbulent kinetic energy (TKE) at the surface and bottom of the water column and low TKE dissipation at the middle of it. There is an asymmetric flood/ebb tidal distribution, with the flood higher than the ebb. |
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| Keywords: | mixing and stratification potential energy anomaly estuarine circulation dissipation of turbulent kinetic energy Modaomen Estuary |
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