Abstract

Natural wetlands are an important methane (CH 4) source. However, emission inventories of them are rather uncertain. One reason for this is the existence of ubiquitous wetland patches. Using a static-chamber technique, we performed field measurements in the inner Mongolia marshes to compare the CH 4 fluxes between a sandy marsh and an organic marsh, and between a patch and the vicinity, and determine the seasonal variation of CH 4 fluxes. For each marsh, the CH 4 flux in the patch was significantly higher than that in the vicinity. Both marshes presented the similar patch pattern of CH 4 emissions. Another remarkable result was the very high CH 4 fluxes in the organic marsh, which averaged 1817.3 and 517.4 mg CH 4 m −2 d −1 in the patch and the vicinity, respectively, during July–September 2004. The very high fluxes mainly resulted from the dense plants. It could be proposed that CH 4 emission patches need to be accounted for in developing an accurate estimate of the global source strength of wetlands.

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