Methane Fluxes and Controlling Factors in the Intertidal Zone of the Yellow River Estuary in Autumn
秋季黄河口滨岸潮滩湿地系统CH4通量特征及影响因素研究

The characteristics of methane (CH4) fluxes from tidal wetlands of the Yellow River estuary were observed in situ with static-chamber and GC methods in September and October 2009, and the key factors affecting CH4 fluxes were discussed. From the aspect of space, the CH4 flux ranges in high tidal wetland, middle tidal wetland, low tidal wetland, bare flat are -0.206-1.264, -0.197-0.431, -0.125-0.659 and -0.742-1.767 mg·(m2·h)-1, the day average fluxes are 0.089, 0.038, 0.197 and 0.169 mg·(m2·h)-1, respectively, indicating that the tidal wetlands are the sources of CH4 and the source function of CH4 differed among the four study sites, in the order of low tidal wetland>bare flat>high tidal wetland>middle tidal wetland. From the aspect of time, the ranges of CH4 fluxes from the tidal wetland ecosystems are -0.444-1.767 and -0.742-1.264 mg·(m2·h)-1, and the day average fluxes are 0.218 and 0.028 mg·(m2·h)-1 in September and October, respectively. The CH4 fluxes in each tidal wetland in September are higher than those in October except that the high tidal wetland acts as weak sink in September. Further studies indicate that the changes of environmental factors in the Yellow River estuary are complicated, and the CH4 fluxes are affected by multiple factors. The differences of CH4 fluxes characteristics among different tidal wetlands in autumn are probably related to temperature (especially atmospheric temperature) and vegetation growth status, while the effects of water or salinity condition and tide status on the CH4 flux characteristics might not be ignored.