Published in

European Geosciences Union, Biogeosciences, 8(9), p. 2847-2857, 2012

DOI: 10.5194/bg-9-2847-2012

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Fire-derived organic carbon in soil turns over on a centennial scale

Journal article published in 2012 by Samuel Abiven ORCID, Nimisha Singh, Margaret S. Torn, Michael W. I. Schmidt
This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Postprint: archiving allowed
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Abstract

Abstract. Pyrogenic carbon (PyC), the residue of an incomplete combustion of biomass, is considered as a carbon (C) sink due to its assumed stability in soil. PyC turnover time estimated using two modelling approaches, based on data from 16 published studies (n = 54) on PyC degradation, ranged from a decadal to centennial time scale, varying with initial biomass type, pyrolysis temperature, and incubation or field study. The average turnover time using a one-pool approach was 88 y, and the best estimate using a two-pool approach was 3 y for a fast-cycling pool and 870 y for a slow-cycling pool. Based on this meta-analysis, PyC cannot be assumed to persist in soils for thousands of years, and its use as a strategy for offsetting carbon emissions requires prudence and further research.