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...

Full description

Bibliographic Details
Main Authors: K. Küsel, M. Blöthe, D. Schulz, M. Reiche, H. L. Drake
Format: Article
Language:English
Published: Copernicus Publications 2008-11-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/5/1537/2008/bg-5-1537-2008.pdf