Journal of Shanghai University(Natural Science Edition) ›› 2015, Vol. 21 ›› Issue (03): 294-300.doi: 10.3969/j.issn.1007-2861.2015.01.013

• Metallurgical Materials • Previous Articles     Next Articles

Carbon and nitrogen coupled biogeochemical cycle in cascade reservoirs of the Wujiang River

WANG Bao-li1, LIU Cong-qiang1, WANG Fu-shun2,Liu Xiao-long3, PENG Xi1, ZHAO Yan-chuang1   

  1. 1. State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry,Chinese Academy of Sciences, Guiyang 550002, China;2. School of Environmental and Chemical Engineering, Shanghai University,Shanghai 200444, China;3. Tianjin Key Laboratory of Water Resources and Environment,Tianjin Normal University, Tianjin 300387, China
  • Received:2015-04-20 Online:2015-06-22 Published:2015-06-22

Abstract: Concentrations of dissolved CO2 and NO3 were investigated in cascade reservoirs and related river reaches along the Wujiang River to understand temporal and spatial variations. The average of dissolved CO2 were (113.6±105.7) μmol·L−1, ranging from 1.6 to 934.6 μmol·L−1. The average of NO3were (163.0±104.9) μmol·L−1, ranging from 0.4 to 632.0 μmol·L−1. Averages and amplitudes of dissolved CO2 and NO3 in the reservoirs are less than those in the rivers. Due to different resources and influencing factors, no significant correlation was found between dissolved CO2 and NO3 in rivers. After damming, the activity of phytoplankton was enhanced, and became an important factor controlling material cycle in reservoirs. Photosynthesis and respiration couple C and N biogeochemical cycle, and dissolved CO2 and NO3 in reservoirs were significantly correlated. The results indicate that C and N biogeochemical cycles in the original rivers are changed by cascade hydropower exploitation.

Key words: C-N coupling, hydropower exploitation, phytoplankton, respiration, the Wujiang River

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