Carbon budgets of an upland blanket bog managed by prescribed fire
Article first published online: 18 DEC 2010
DOI: 10.1029/2010JG001331
Copyright 2010 by the American Geophysical Union.
Issue
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Journal of Geophysical Research: Biogeosciences (2005–2012)
Volume 115, Issue G4, December 2010
Additional Information
How to Cite
, , and (2010), Carbon budgets of an upland blanket bog managed by prescribed fire, J. Geophys. Res., 115, G04037, doi:10.1029/2010JG001331.
Publication History
- Issue published online: 18 DEC 2010
- Article first published online: 18 DEC 2010
- Manuscript Accepted: 25 AUG 2010
- Manuscript Revised: 11 AUG 2010
- Manuscript Received: 16 FEB 2010
Keywords:
- DOC;
- primary productivity;
- net ecosystem respiration;
- biomass combustion;
- carbon stocks
[1] This study presents the carbon budget of a blanket bog, North Pennines, UK, subject to grazing and prescribed burning for vegetation management. The budget considers both fluvial and gaseous carbon fluxes and the following uptake and release pathways: dissolved organic carbon, particulate organic carbon, excess dissolved CO2, release of methane (CH4), net ecosystem respiration of CO2, and uptake of CO2 through primary productivity. Measurements of CH4 were not directly measured as part of this study but were estimated from hydroclimatic variables measured within the study. The results show that, if management combinations were extrapolated across the catchment, then over a 3 year period, the catchment would be a net source of carbon of between 62 and 206 gC m−2 yr−1. The action of both burning and grazing was to significantly decrease the magnitude of the carbon source relative to unburnt controls. Over the study period burnt sites were a mean source of approximately 117.8 gC m−2 yr−1 compared to unburnt sites with a mean source of 156.7 gC m−2 yr−1. Even when including the loss of carbon during the vegetation combustion, there are conditions under which the long-term loss of carbon is less than if no burning had occurred. If total combustion of vegetation occurs, provided burning occurs at cycles longer than 32 years, then less carbon is predicted to be lost than in a no-burn scenario.

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