Modeling density currents in a typical tributary of the Three Gorges Reservoir, China

被引:63
|
作者
Ma, Jun [1 ,2 ]
Liu, Defu [3 ,4 ]
Wells, Scott A. [5 ]
Tang, Hongwu [1 ,2 ]
Ji, Daobin [6 ]
Yang, Zhengjian [3 ]
机构
[1] Hohai Univ, Coll Water Conservancy & Hydropower Engn, Nanjing 210098, Jiangsu, Peoples R China
[2] State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210098, Jiangsu, Peoples R China
[3] Hubei Univ Technol, Coll Resources & Environm Engn, Wuhan 430068, Peoples R China
[4] China Three Gorges Univ, Engn Res Ctr Ecoenvironm Gorges Reservoir Reg 3, Yichang 443002, Peoples R China
[5] Portland State Univ, Dept Civil & Environm Engn, Portland, OR 97207 USA
[6] China Three Gorges Univ, Coll Hydraul & Environm Engn, Yichang 443002, Peoples R China
基金
中国国家自然科学基金;
关键词
Three Gorges Reservoir (TGR); Xiangxi Bay (XXB); Density currents; Water temperature stratification; CE-QUAL-W2; PHYTOPLANKTON GROWTH; WATER-QUALITY; THERMAL STRUCTURE; TAGUCHI METHOD; XIANGXI BAY; EUTROPHICATION; OPTIMIZATION; SIMULATIONS; NUTRIENTS; BLOOMS;
D O I
10.1016/j.ecolmodel.2014.10.030
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The initial filling of the Three Gorges Reservoir (TGR), China, has caused serious phytoplankton blooms in its tributary bays. A two-dimensional, laterally averaged, hydrodynamic and water quality CE-QUAL-W2 model was used to simulate the hydrodynamics and water temperature of a typical tributary (Xiangxi Bay XXB) of the TGR to study the relationship between phytoplankton and density currents. The CE-QUAL-W2 model was calibrated to data collected in XXB (depth profiles of velocity and water temperature at three locations) from January 2008 through December 2008. The model performed well in simulating (1) flow velocity profiles, (2) unusual water temperature profiles, (3) the plunge point location of the intrusion layer, (4) propagation speed, and (5) the travel distance of the density currents. The model was then used to examine potential factors that affect the density currents, such as water level fluctuations in the mainstem of the TGR, water temperature differences between the mainstem and XXB, and inflow rates to XXB. Therefore, a better understanding of the hydrodynamics of tributaries in the TGR can be used to understand the aquatic ecosystem dynamics of these tributaries. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:113 / 125
页数:13
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