Methane Oxidation in the Water Column of Xiangxi Bay, Three Gorges Reservoir

2019 ◽  
Vol 47 (9) ◽  
pp. 1800516 ◽  
Author(s):  
Dan Lei ◽  
Jia Liu ◽  
Junwei Zhang ◽  
Andreas Lorke ◽  
Shangbin Xiao ◽  
...  
2017 ◽  
Vol 51 (7) ◽  
pp. 3794-3801 ◽  
Author(s):  
Kai Zhang ◽  
Xiong Xiong ◽  
Hongjuan Hu ◽  
Chenxi Wu ◽  
Yonghong Bi ◽  
...  

2016 ◽  
Vol 35 (3) ◽  
pp. 826-833 ◽  
Author(s):  
Lin Ye ◽  
Qinghua Cai ◽  
Min Zhang ◽  
Lu Tan ◽  
Henglun Shen

2012 ◽  
Vol 46 (7) ◽  
pp. 2121-2130 ◽  
Author(s):  
Liu Liu ◽  
Defu Liu ◽  
David M. Johnson ◽  
Zhongqiang Yi ◽  
Yuling Huang

2008 ◽  
Vol 28 (5) ◽  
pp. 2073-2079 ◽  
Author(s):  
Li Fengqing ◽  
Ye Lin ◽  
Liu Ruiqiu ◽  
Cao Ming ◽  
Cai Qinghua

2013 ◽  
Vol 3 (1) ◽  
Author(s):  
Shangbin Xiao ◽  
Defu Liu ◽  
Yuchun Wang ◽  
Zhengjian Yang ◽  
Wenzhong Chen

2016 ◽  
Vol 75 (8) ◽  
Author(s):  
Yuling Huang ◽  
Dongxing Fan ◽  
Defu Liu ◽  
Linxu Song ◽  
Daobin Ji ◽  
...  

2011 ◽  
Vol 29 (5) ◽  
pp. 1057-1064 ◽  
Author(s):  
Min Yang ◽  
Yonghong Bi ◽  
Jianlin Hu ◽  
Kongxian Zhu ◽  
Guangjie Zhou ◽  
...  

2021 ◽  
Author(s):  
RANOJIT KUMAR DUTTA ◽  
BAISHAKHI DAS

Abstract A two-dimensional (2D), laterally averaged, hydrodynamic and water quality model, CE-QUAL-W2, was used to simulate the hydrodynamics and water temperatures of Xiangxi Bay (XXB) of the Three Gorges Reservoir (TGR). Algal blooms occurred seasonally in XXB which is influenced by density currents. The CE-QUAL-W2 model was calibrated using data collected in XXB from January to December 2010. The model was then used to examine the environmental factors that affect the density currents. The model predicted density currents such as overflows, interflows and underflows of the XXB. The results suggest that more than 25%, 58.33% and 16.67% of the density currents that occurred in the XXB were overflow, interflow and underflow, respectively. Field observations were conducted including travel distance and thickness of intrusion layer for 24 days in 2010. The average travel distance of overflow, interflow and underflow in XXB was 15.50 km, 8.78 km, and 9 km based on observations and 16 km, 9.40 km, 9.60 km based on the model results. Therefore, numerical simulations of density currents can be predicted to better understand the hydrodynamics and aquatic ecosystems in XXB of TGR.


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