Microbial reduction of iron and porewater biogeochemistry in acidic peatlands
Temporal drying of upper soil layers of acidic methanogenic peatlands might divert the flow of reductants from CH<sub>4</sub> formation to other electron-accepting processes due to a renewal of alternative electron acceptors. In this study, we evaluated the in situ releva...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2008-11-01
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Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/5/1537/2008/bg-5-1537-2008.pdf |