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cje ›› 2012, Vol. 31 ›› Issue (01): 152-157.

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Partial pressure of water body dissolved carbon dioxide in mainstream and Xiangxi bay of Three Gorges Reservoir area in autumn. 

YAO Chen-chen1, ZHANG Jing1, WU Yi-ying1, WANG Yu-chun2, JIANG Yan-xing1, GAO Yang1, WANG Fu-shun1**   

  1. 1 School of Environmental and Chemical Engineering, Shanghai University, Shanghai 200444, China; 2 Department of Water Environment, China Institute of Water Resources and Hydroelectric Power Research, Beijing 100038, China
  • Online:2012-01-08 Published:2012-01-08

Abstract: In September 2009, a cruise investigation was conducted to study the partial pressure of water body dissolved carbon dioxide (pCO2) in the mainstream and Xiangxi River of the Three Gorges Reservoir Area in autumn. The pCO2 in the surface water of the mainstream and Xiangxi River was 920-1140 and 150-240 μatm, respectively. At the joint area of mainstream and distributaries, the pCO2 had a minimum of 368 μatm in surface water, and increased markedly with increasing water depth, being the maximum (1300 μatm) at 10 m depth and keeping stable downward. The CO2 flux of the mainstream and Xiangxi River was 83.7±14.1 and -4.74±1.15 mmol·m-2·d-1, respectively, indicating that the mainstream was a sink, while Xiangxi River was a source of CO2. Therefore, when evaluating the influence of reservoir construction on the CO2 flux in reservoir’s surrounding regions, it would be necessary not only considering the local basins, but also investigating the entire study area comprehensively.

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