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

被引:183
作者
Singh, N. [2 ]
Abiven, S. [2 ]
Torn, M. S. [1 ]
Schmidt, M. W. I. [2 ]
机构
[1] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Berkeley, CA 94720 USA
[2] Univ Zurich, Dept Geog, CH-8057 Zurich, Switzerland
基金
瑞士国家科学基金会;
关键词
BLACK CARBON; PYROGENIC CARBON; WOOD-CHARCOAL; CENTRAL AMAZONIA; GRASSLAND SOILS; MATTER; OXIDATION; NMR; MINERALIZATION; DECOMPOSITION;
D O I
10.5194/bg-9-2847-2012
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
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.
引用
收藏
页码:2847 / 2857
页数:11
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