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Soil methane oxidation in both dry and wet temperate eucalypt forests shows a near-identical relationship with soil air-filled porosity

Well-drained, aerated soils are important sinks for atmospheric methane (CH<sub>4</sub>) via the process of CH<sub>4</sub> oxidation by methane-oxidising bacteria (MOB). This terrestrial CH<sub>4</sub> sink may contribute towards climate change mitigation, but the...

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主要な著者: B. J. Fest, N. Hinko-Najera, T. Wardlaw, D. W. T. Griffith, S. J. Livesley, S. K. Arndt
フォーマット: Artigo
言語:Inglês
出版事項: Copernicus Publications 2017-01-01
シリーズ:Biogeosciences
オンライン・アクセス:http://www.biogeosciences.net/14/467/2017/bg-14-467-2017.pdf
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