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The spatial variability of methane emission from subtaiga and forest–steppe grass–moss fens of Western Siberia

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Abstract

Methane emission from the grass–moss fens of the Western Siberia subtaiga was studied using a static chamber method. It was established that CH4 flux median ± half of the interquartile range in the studied wetland ecosystems constituted 4.9 ± 2.9 mg of CH4/(m2 h). It was shown that such a high spatial variability of emission is caused mainly by the difference in the water table level. It was found that, in these observations, a higher water table level correlates with lower emission values. The causes of this phenomenon are discussed, and recommendations for conducting field studies for estimating the regional flux are given.

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Correspondence to A. F. Sabrekov.

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Original Russian Text © A.F. Sabrekov, I.V. Filippov, I.E. Terentieva, M.V. Glagolev, D.V. Il’yasov, B.A. Smolentsev, S.S. Maksyutov, 2016, published in Izvestiya Akademii Nauk, Seriya Biologicheskaya, 2016, No. 2, pp. 199–206.

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Sabrekov, A.F., Filippov, I.V., Terentieva, I.E. et al. The spatial variability of methane emission from subtaiga and forest–steppe grass–moss fens of Western Siberia. Biol Bull Russ Acad Sci 43, 162–168 (2016). https://doi.org/10.1134/S1062359016020060

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  • DOI: https://doi.org/10.1134/S1062359016020060

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