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Acta Prataculturae Sinica ›› 2011, Vol. 20 ›› Issue (3): 51-61.

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A preliminary study on carbon dioxide, methane and nitrous oxide fluxes from intertidal flat wetlands of the Yellow River estuary

WANG Ling-ling1,2, SUN Zhi-gao1, MOU Xiao-jie1,2, SUN Wan-long1,2, SONG Hong-li1,2, JIANG Huan-huan1,2   

  1. 1.Lab of Coastal Wetland Ecology, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, China;
    2.Graduate School of Chinese Academy Sciences, Beijing 100039, China
  • Received:2010-04-16 Online:2011-03-25 Published:2011-06-20

Abstract: The diurnal variation characteristics of carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) fluxes from intertidal flat wetland of the Yellow River estuary were observed in situ with a static-chamber and GC in August 2009. CO2, CH4 and N2O fluxes from the low tidal flat sediment showed an obvious diurnal variation. The flux ranges were from -18.754 6 to 43.730 8, -0.069 8 to 0.224 2 and -0.001 6 to 0.008 3 mg/(m2·h), and the daily average fluxes were 11.629 7, 0.078 7 and 0.004 6 mg/(m2·h), respectively, which showed that the low tidal flat sediment was the source of atmospheric CO2, CH4 and N2O. The flux ranges of CO2, CH4 and N2O in the middle tidal flat sediment were from -30.779 9 to 25.734 2, -0.111 3 to 0.1001 and -0.004 4 to 0.006 3 mg/(m2·h), and the daily average fluxes were 4.569 9, 0.011 3 and 0.002 3 mg/(m2·h), respectively, which showed that the middle tidal flat sediment was also the source of atmospheric CO2, CH4 and N2O. The flux ranges of CO2, CH4 and N2O in the high tidal flat were from 46.253 3 to 102.637 4, -0.210 9 to 0.047 5 and -0.008 3 to 0.007 8 mg/(m2·h), and the daily average fluxes were 76.656 1, -0.037 9 and -0.002 0 mg/(m2·h), respectively, which showed that the high tidal flat was not only the source of atmospheric CO2 but also a sink for atmospheric CH4 and N2O. Further analysis showed that CO2 flux from the middle tidal flat sediment was significantly positively correlated with atmospheric temperatures (P<0.05), as was the CH4 flux from the low tidal flat sediment (0 and 5 cm ground temperatures (P<0.01)), but the N2O flux from the middle tidal flat sediment was significantly negatively correlated with atmospheric temperatures and different depths of ground temperatures (5, 10 and 20 cm) (P<0.05 or 0.01). In addition, sediment solvent and the Suaeda salsa community were the main factors affecting the flux characteristics of CO2, CH4 and N2O, while soil water content and salinity also affected them.

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