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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: | , , , , , |
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フォーマット: | Artigo |
言語: | Inglês |
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Copernicus Publications
2017-01-01
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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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