Methane consumption in temperate and subarctic forest soils: Rates, vertical zonation, and responses to water and nitrogen
Rates of methane consumption were measured in subarctic coniferous and temperate mixed-hardwood forest soils, using static chambers and intact soil cores. Rates at both sites were generally between 1 and 3 mg of CH4 m-2 day-1 and decreased with increasing soil water contents above 20%. Addition of a...
| Published in: | Applied and Environmental Microbiology |
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| Main Authors: | , |
| Format: | Text |
| Language: | unknown |
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LSU Digital Commons
1993
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| Subjects: | |
| Online Access: | https://digitalcommons.lsu.edu/biosci_pubs/2036 https://doi.org/10.1128/aem.59.2.485-490.1993 https://digitalcommons.lsu.edu/context/biosci_pubs/article/3035/viewcontent/2036.pdf |
| Summary: | Rates of methane consumption were measured in subarctic coniferous and temperate mixed-hardwood forest soils, using static chambers and intact soil cores. Rates at both sites were generally between 1 and 3 mg of CH4 m-2 day-1 and decreased with increasing soil water contents above 20%. Addition of ammonium (1 μmol g of soil-1) strongly inhibited methane oxidation in the subarctic soils; a lesser inhibition was observed for temperate forest samples. The response to nitrogen additions occurred within a few hours and was probably due to physiological changes in the active methane-consuming populations. Methane consumption in soils from both sites was stratified vertically, with a pronounced subsurface maximum. This maximum was coincident with low levels of both nitrate and ammonium in the mixed-hardwood forest soil. |
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