Carbon stocks of an Oxisol after thirty-eight years under different tillage systems

Detalhes bibliográficos
Autor(a) principal: Magalhaes,Sulamirtes S. de A.
Data de Publicação: 2016
Outros Autores: Ramos,Fabricio T., Weber,Oscarlina L. dos S.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Revista Brasileira de Engenharia Agrícola e Ambiental (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1415-43662016000100085
Resumo: ABSTRACT Soil carbon (C) stock determination can subsidize discussions on the continuity of an agricultural management. This study aimed to evaluate the stocks of total organic C (STOC) and labile C (SLC), and the indices of C lability (CLI), C compartment (CCI) and C management (CMI), and correlate them with chemical and physical attributes of a Red Yellow Latosol (Oxisol) managed for 38 years with different tillage systems in a Cerrado region of Mato Grosso, Brazil. Disturbed and undisturbed soil samples were collected in three layers (0-0.05, 0.05-0.10 and 0.10-0.20 m). The CMI (CLI x CCI) showed higher STOC possibly as the tillage depth decreased, because none of the tillage systems conserved STOC and SLC in the layers of 0-0.05 and 0.05-0.10 m, compared with the Native Cerrado, i.e., soil C conservation only occurred in the layer of 0.10-0.20 m. Although the percentage of SLC in STOC was lower, only SLC was correlated with soil chemical and physical attributes and, based on the multiple linear regression analysis, SLC was explained in 54% (R2) by the cation exchange capacity and soil micropores. Therefore, for monitoring purposes, the SLCestimated can be useful to evaluate soil C storage.
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spelling Carbon stocks of an Oxisol after thirty-eight years under different tillage systemssoil conservationcrop rotationsoil organic matterABSTRACT Soil carbon (C) stock determination can subsidize discussions on the continuity of an agricultural management. This study aimed to evaluate the stocks of total organic C (STOC) and labile C (SLC), and the indices of C lability (CLI), C compartment (CCI) and C management (CMI), and correlate them with chemical and physical attributes of a Red Yellow Latosol (Oxisol) managed for 38 years with different tillage systems in a Cerrado region of Mato Grosso, Brazil. Disturbed and undisturbed soil samples were collected in three layers (0-0.05, 0.05-0.10 and 0.10-0.20 m). The CMI (CLI x CCI) showed higher STOC possibly as the tillage depth decreased, because none of the tillage systems conserved STOC and SLC in the layers of 0-0.05 and 0.05-0.10 m, compared with the Native Cerrado, i.e., soil C conservation only occurred in the layer of 0.10-0.20 m. Although the percentage of SLC in STOC was lower, only SLC was correlated with soil chemical and physical attributes and, based on the multiple linear regression analysis, SLC was explained in 54% (R2) by the cation exchange capacity and soil micropores. Therefore, for monitoring purposes, the SLCestimated can be useful to evaluate soil C storage.Departamento de Engenharia Agrícola - UFCG2016-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S1415-43662016000100085Revista Brasileira de Engenharia Agrícola e Ambiental v.20 n.1 2016reponame:Revista Brasileira de Engenharia Agrícola e Ambiental (Online)instname:Universidade Federal de Campina Grande (UFCG)instacron:UFCG10.1590/1807-1929/agriambi.v20n1p85-91info:eu-repo/semantics/openAccessMagalhaes,Sulamirtes S. de A.Ramos,Fabricio T.Weber,Oscarlina L. dos S.eng2016-01-11T00:00:00Zoai:scielo:S1415-43662016000100085Revistahttp://www.scielo.br/rbeaaPUBhttps://old.scielo.br/oai/scielo-oai.php||agriambi@agriambi.com.br1807-19291415-4366opendoar:2016-01-11T00:00Revista Brasileira de Engenharia Agrícola e Ambiental (Online) - Universidade Federal de Campina Grande (UFCG)false
dc.title.none.fl_str_mv Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
title Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
spellingShingle Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
Magalhaes,Sulamirtes S. de A.
soil conservation
crop rotation
soil organic matter
title_short Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
title_full Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
title_fullStr Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
title_full_unstemmed Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
title_sort Carbon stocks of an Oxisol after thirty-eight years under different tillage systems
author Magalhaes,Sulamirtes S. de A.
author_facet Magalhaes,Sulamirtes S. de A.
Ramos,Fabricio T.
Weber,Oscarlina L. dos S.
author_role author
author2 Ramos,Fabricio T.
Weber,Oscarlina L. dos S.
author2_role author
author
dc.contributor.author.fl_str_mv Magalhaes,Sulamirtes S. de A.
Ramos,Fabricio T.
Weber,Oscarlina L. dos S.
dc.subject.por.fl_str_mv soil conservation
crop rotation
soil organic matter
topic soil conservation
crop rotation
soil organic matter
description ABSTRACT Soil carbon (C) stock determination can subsidize discussions on the continuity of an agricultural management. This study aimed to evaluate the stocks of total organic C (STOC) and labile C (SLC), and the indices of C lability (CLI), C compartment (CCI) and C management (CMI), and correlate them with chemical and physical attributes of a Red Yellow Latosol (Oxisol) managed for 38 years with different tillage systems in a Cerrado region of Mato Grosso, Brazil. Disturbed and undisturbed soil samples were collected in three layers (0-0.05, 0.05-0.10 and 0.10-0.20 m). The CMI (CLI x CCI) showed higher STOC possibly as the tillage depth decreased, because none of the tillage systems conserved STOC and SLC in the layers of 0-0.05 and 0.05-0.10 m, compared with the Native Cerrado, i.e., soil C conservation only occurred in the layer of 0.10-0.20 m. Although the percentage of SLC in STOC was lower, only SLC was correlated with soil chemical and physical attributes and, based on the multiple linear regression analysis, SLC was explained in 54% (R2) by the cation exchange capacity and soil micropores. Therefore, for monitoring purposes, the SLCestimated can be useful to evaluate soil C storage.
publishDate 2016
dc.date.none.fl_str_mv 2016-01-01
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dc.language.iso.fl_str_mv eng
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dc.relation.none.fl_str_mv 10.1590/1807-1929/agriambi.v20n1p85-91
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dc.publisher.none.fl_str_mv Departamento de Engenharia Agrícola - UFCG
publisher.none.fl_str_mv Departamento de Engenharia Agrícola - UFCG
dc.source.none.fl_str_mv Revista Brasileira de Engenharia Agrícola e Ambiental v.20 n.1 2016
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