Registro completo |
Provedor de dados: |
Rev. Bras. Ciênc. Solo
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País: |
Brazil
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Título: |
Carbon Stocks and Pools in Relation to the Texture of Kaolinitic Soils from the Brazilian East Coast
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Autores: |
Gomes,João Bosco Vasconcellos
Silva,Carlos Alberto
Ferreira,Tamara Letícia de Azevedo
Ferreira,Mozart Martins
Inda,Alberto Vasconcellos
Curi,Nilton
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Data: |
2018-01-01
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Ano: |
2018
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Palavras-chave: |
Dissolved organic C
Aggregate size distribution
Coastal Tablelands
Organic matter-mineral complexes
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Resumo: |
ABSTRACT: Extremely kaolinitic soils of Tertiary age elevations on the Brazilian east coast present a wide range of texture, which is recognized as one of the main factors controlling the soil organic matter contents. This study aimed to investigate the organic C storage of different compartments of kaolinitic soils. The studied soils had a wide particle size gradient, were under native forest vegetation, and located on Brazil's eastern coast (Coruripe - CF, Umbaúba - UF, Nova Viçosa - VF, Sooretama - SF, and Itaboraí - IF). The forest cover of all sites allows to record soil properties reference values for a land use condition closer to that of the original sites. We determined soil organic C (SOC) content and SOC stock up to a depth of 1 m, C of topsoil (0.00-0.08 m), aggregate size classes, and dissolved organic carbon (DOC) of the soil surface horizon (A horizon). Soil C stocks at the 0.00-1.00 m depth ranged from 105 to 137 Mg ha−1 and were not regulated by soil texture. The SF soils stored more C up to a depth of 1 m, while lower mean C stocks were found for UF and CF soils. Soil texture was not a reliable index to predict the C contents of the aggregate size classes of the 0.00-0.08 m layer (within each class and in total, using equivalent soil mass of the classes). The most clayey soils had a high percentage of 2-4 mm aggregates and, as a consequence, high aggregate stability indices, which are positively correlated to silt plus clay contents of the soil surface horizon. The proportion of DOC in relation to the total organic C of the surface soil horizon was high for IF and UF areas, which are the less preserved forest fragments among all studied fragments.
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Tipo: |
Info:eu-repo/semantics/article
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Idioma: |
Inglês
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Identificador: |
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832018000100422
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Editor: |
Sociedade Brasileira de Ciência do Solo
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Relação: |
10.1590/18069657rbcs20170260
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Formato: |
text/html
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Fonte: |
Revista Brasileira de Ciência do Solo v.42 2018
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Direitos: |
info:eu-repo/semantics/openAccess
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