Methane flux dynamics in an Irish lowland blanket bog


Pristine peatlands are a significant source of atmospheric methane (CH4). Large spatio–temporal variation has been observed in flux rates within and between peatlands. Variation is commonly associated with water level, vegetation structure, soil chemistry and climatic variability. We measured spatial and temporal variation in CH4 fluxes in a blanket bog… (More)
DOI: 10.1007/s11104-007-9374-6


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