Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 10, issue 10
Biogeosciences, 10, 6141–6160, 2013
https://doi.org/10.5194/bg-10-6141-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 10, 6141–6160, 2013
https://doi.org/10.5194/bg-10-6141-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 01 Oct 2013

Research article | 01 Oct 2013

Changes in soil carbon stocks in Brazil due to land use: paired site comparisons and a regional pasture soil survey

E. D. Assad1, H. S. Pinto2, S. C. Martins1, J. D. Groppo1, P. R. Salgado3, B. Evangelista4, E. Vasconcellos1, E. E. Sano4, E. Pavão1, R. Luna1, P. B. Camargo5, and L. A. Martinelli5 E. D. Assad et al.
  • 1Brazilian Agricultural Research Corporation, EMBRAPA Agricultural Informatics, Campinas, São Paulo State, Brazil
  • 2University of Campinas – UNICAMP, Campinas, São Paulo State, Brazil
  • 3Brazilian Agricultural Research Corporation, EMBRAPA Coffe, Brasilia, DF, Brazil
  • 4Brazilian Agricultural Research Corporation, EMBRAPA Agropecuária do Cerrado, Brasilia, DF, Brazil
  • 5University of São Paulo – USP, Centro de Energia Nuclear na Agricultura, Piracicaba, São Paulo State, Brazil

Abstract. In this paper we calculated soil carbon stocks in Brazil studying 17 paired sites where soil stocks were determined in native vegetation, pastures and crop-livestock systems (CPS), and in other regional samplings encompassing more than 100 pasture soils, from 6.58 to 31.53° S, involving three major Brazilian biomes: Cerrado, Atlantic Forest, and the Pampa. The average native vegetation soil carbon stocks at 10, 30 and 60 cm soil depth were equal to approximately 29, 64, and 92 Mg ha−1, respectively. In the paired sites, carbon losses of 7.5 Mg ha−1 and 11.6 Mg ha−1 in CPS systems were observed at 10 cm and 30 cm soil depths, respectively. In pasture soils, carbon losses were similar and equal to 7.5 Mg ha−1 and 11.0 Mg ha−1 at 10 cm and 30 cm soil depths, respectively. Differences at 60 cm soil depth were not significantly different between land uses. The average soil δ13C under native vegetation at 10 and 30 cm depth were equal to −25.4‰ and −24.0‰, increasing to −19.6‰ and −17.7‰ in CPS, and to −18.9‰, and −18.3‰ in pasture soils, respectively; indicating an increasing contribution of C4 carbon in these agrosystems. In the regional survey of pasture soils, the soil carbon stock at 30 cm was equal to approximately 51 Mg ha−1, with an average δ13C value of −19.67‰. Key controllers of soil carbon stock in pasture sites were sand content and mean annual temperature. Collectively, both could explain approximately half of the variance of soil carbon stocks. When pasture soil carbon stocks were compared with the average soil carbon stocks of native vegetation estimated for Brazilian biomes and soil types by Bernoux et al. (2002) there was a carbon gain of 6.7 Mg ha−1, which is equivalent to a carbon gain of 15% compared to the carbon soil stock of the native vegetation. The findings of this study are consistent with differences found between regional comparisons like our pasture sites and plot-level paired study sites in estimating soil carbon stocks changes due to land use changes.

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