Abiotic drivers and their interactive effect on the flux and carbon isotope (14C and d13C) composition of peat-respired CO2

Hardie, S.M.L.; Garnett, M.H.; Fallick, A.E.; Rowland, A.P.; Ostle, N.J.; Flowers, T.H.. 2011 Abiotic drivers and their interactive effect on the flux and carbon isotope (14C and d13C) composition of peat-respired CO2. Soil Biology and Biochemistry, 43 (12). 2432-2440. 10.1016/j.soilbio.2011.08.010

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Official URL: http://www.sciencedirect.com/science/article/pii/S...

Abstract/Summary

Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO2 emissions, thus exacerbating climate change. The contribution that soil respiration makes to these terrestrial emissions, particularly from carbon-rich soils such as peatlands, is of significant importance and its response to changing climatic conditions is of considerable debate.We collected intact soil cores from an upland blanket bog situated within the northern Pennines, England, UK and investigated the individual and interactive effects of three primary controls on soil organic matter decomposition: (i) temperature (5, 10 and 15 C); (ii) moisture (50 and 100% field capacity e FC); and (iii) substrate quality, using increasing depth from the surface (0e10, 10e20 and 20e30 cm) as an analogue for increased recalcitrance of soil organic material. Statistical analysis of the results showed that temperature, moisture and substrate quality all significantly affected rates of peat decomposition. Q10 values indicated that the temperature sensitivity of older/more recalcitrant soil organic matter significantly increased (relative to more labile peat) under reduced soil moisture (50% FC) conditions, but not under 100% FC, suggesting that soil microorganisms decomposing the more recalcitrant soil material preferred more aerated conditions. Radiocarbon analyses revealed that soil decomposers were able to respire older, more recalcitrant soil organic matter and that the source of the material (deduced from the d13C analyses) subject to decomposition, changed depending on depth in the peat profile.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/j.soilbio.2011.08.010
Programmes:	CEH Topics & Objectives 2009 - 2012 > Biogeochemistry
UKCEH and CEH Sections/Science Areas:	Shore
ISSN:	0038-0717
Additional Keywords:	CO2, 14C, δ13C, respiration, climate change, Q10, temperature, substrate quality, moisture, carbon cycling
NORA Subject Terms:	Agriculture and Soil Science Ecology and Environment
Date made live:	19 Oct 2011 15:26 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/15212

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/j.soilbio.2011.08.010

Programmes:

CEH Topics & Objectives 2009 - 2012 > Biogeochemistry

UKCEH and CEH Sections/Science Areas:

Shore

ISSN:

0038-0717

Additional Keywords:

CO2, 14C, δ13C, respiration, climate change, Q10, temperature, substrate quality, moisture, carbon cycling