Please use this identifier to cite or link to this item:
http://www.alice.cnptia.embrapa.br/alice/handle/doc/1099369
Title: | Carbon stocks and pools in relation to the texture of kaolinitic soils from the Brazilian East Coast. |
Authors: | GOMES, J. B. V.![]() ![]() SILVA, C. A. ![]() ![]() FERREIRA, T. L. de A. ![]() ![]() FERREIRA, M. M. ![]() ![]() INDA, A. V. ![]() ![]() CURI, N. ![]() ![]() |
Affiliation: | JOAO BOSCO VASCONCELLOS GOMES, CNPF; Carlos Alberto Silva, UFLA; Tamara Letícia de Azevedo Ferreira, UFLA; Mozart Martins Ferreira, UFLA; Alberto Vasconcellos Inda, UFRGS; Nilton Curi, UFLA. |
Date Issued: | 2018 |
Citation: | Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 42, e0170260, set. 2018. 15 p. |
Description: | 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. |
Thesagro: | Solo |
NAL Thesaurus: | Soil |
Keywords: | Argilito caolítico Estoque de carbono Dissolved organic C Aggregate size distribution Coastal tablelands Organic matter-mineral complexes |
DOI: | 10.1590/18069657rbcs20170260 |
Type of Material: | Artigo de periódico |
Access: | openAccess |
Appears in Collections: | Artigo em periódico indexado (CNPF)![]() ![]() |
Files in This Item:
File | Description | Size | Format | |
---|---|---|---|---|
2018J.BoscoRBCSCarbon.pdf | 527.93 kB | Adobe PDF | ![]() View/Open |