Organic matter and soil aggregation in agricultural systems with different adoption times
Autor(a) principal: | |
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Data de Publicação: | 2019 |
Outros Autores: | , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Semina. Ciências Agrárias (Online) |
Texto Completo: | https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/35380 |
Resumo: | In conservation management systems, such as no-till (NT), it is important to analyze the pattern of changes in soil quality as a function of the time since adoption of the system. This study evaluated the physical fractions of organic matter and soil aggregation in management systems in areas cultivated with different times since implementation of NT: 6, 14, and 22 successive years of soybean and maize/wheat crops (NT6, NT14, and NT22, respectively); 12 years of no-till with successive years of soybean and maize/wheat crops, and the last 4 years with integration of maize and ruzi grass (Brachiaria ruziziensis) - (NT+B); pasture; and forest. Physical fractionation of organic matter determined the total carbon (TC), particulate organic matter (POM), and mineral organic matter (MOM) by calculating the carbon management index (CMI) and variables related to soil structural stability. Forest and pasture areas showed the highest contents of TC, POM, and MOM, as well as higher stocks of POM and MOM. Among the cultivated areas, higher TC and particulate fractions of organic matter and the best CMI values were observed in the area of NT22. There were changes in aggregation indices, depending on the time since implementation of NT. Areas of NT22, pasture, and forest showed the greatest evolution in C-CO2, indicating increased biological activity, with positive effects on soil structural stability. |
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Semina. Ciências Agrárias (Online) |
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Organic matter and soil aggregation in agricultural systems with different adoption timesMatéria orgânica e agregação de solo em sistemas agrícolas com diferentes tempos de adoçãoLabile carbonCarbon stocksConservation management.Carbono lábilEstoques de carbonoManejo conservacionista.In conservation management systems, such as no-till (NT), it is important to analyze the pattern of changes in soil quality as a function of the time since adoption of the system. This study evaluated the physical fractions of organic matter and soil aggregation in management systems in areas cultivated with different times since implementation of NT: 6, 14, and 22 successive years of soybean and maize/wheat crops (NT6, NT14, and NT22, respectively); 12 years of no-till with successive years of soybean and maize/wheat crops, and the last 4 years with integration of maize and ruzi grass (Brachiaria ruziziensis) - (NT+B); pasture; and forest. Physical fractionation of organic matter determined the total carbon (TC), particulate organic matter (POM), and mineral organic matter (MOM) by calculating the carbon management index (CMI) and variables related to soil structural stability. Forest and pasture areas showed the highest contents of TC, POM, and MOM, as well as higher stocks of POM and MOM. Among the cultivated areas, higher TC and particulate fractions of organic matter and the best CMI values were observed in the area of NT22. There were changes in aggregation indices, depending on the time since implementation of NT. Areas of NT22, pasture, and forest showed the greatest evolution in C-CO2, indicating increased biological activity, with positive effects on soil structural stability.Em sistemas de manejo conservacionistas, como o plantio direto (PD), é importante analisar o padrão de mudanças na qualidade do solo em função do tempo desde a adoção do sistema. Este estudo avaliou as frações físicas de matéria orgânica e agregação do solo em sistemas de manejo em áreas cultivadas com diferentes épocas desde a implantação do PD: 6, 14 e 22 anos sucessivos de soja e milho/trigo (PD6, PD14 e PD22, respectivamente); 12 anos de plantio direto com anos sucessivos de lavouras de soja e milho/trigo, e os últimos 4 anos com integração de milho e braquiária ruziziensis (Brachiaria ruziziensis) - (PD+B); pastagem e floresta nativa. O fracionamento físico da matéria orgânica determinou o carbono total (CT), matéria orgânica particulada (MOP) e matéria orgânica mineral (MOM), calculando o índice de manejo do carbono (IMC) e variáveis relacionadas à estabilidade estrutural do solo. As áreas de floresta e pastagem apresentaram os maiores teores de TC, MOP e MOM, assim como maiores estoques de MOP e MOM. Entre as áreas cultivadas, maiores teores de CT, frações particuladas de matéria orgânica e os maiores valores de IMC foram observados na área de PD22. Houve alterações nos índices de agregação, dependendo do tempo desde a implementação do PD. Áreas de PD22, pastagem e floresta apresentaram a maior evolução em C-CO2 , indicando maior atividade biológica, com efeitos positivos na estabilidade estrutural do solo.UEL2019-10-16info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/3538010.5433/1679-0359.2019v40n6Supl3p3443Semina: Ciências Agrárias; Vol. 40 No. 6Supl3 (2019); 3443-3460Semina: Ciências Agrárias; v. 40 n. 6Supl3 (2019); 3443-34601679-03591676-546Xreponame:Semina. Ciências Agrárias (Online)instname:Universidade Estadual de Londrina (UEL)instacron:UELenghttps://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/35380/26230Copyright (c) 2019 Semina: Ciências Agráriashttp://creativecommons.org/licenses/by-nc/4.0info:eu-repo/semantics/openAccessRosset, Jean SérgioLana, Maria do CarmoPereira, Marcos GervasioSchiavo, Jolimar AntonioRampim, LeandroSarto, Marcos Vinicius Mansano2022-10-10T15:15:41Zoai:ojs.pkp.sfu.ca:article/35380Revistahttp://www.uel.br/revistas/uel/index.php/semagrariasPUBhttps://ojs.uel.br/revistas/uel/index.php/semagrarias/oaisemina.agrarias@uel.br1679-03591676-546Xopendoar:2022-10-10T15:15:41Semina. Ciências Agrárias (Online) - Universidade Estadual de Londrina (UEL)false |
dc.title.none.fl_str_mv |
Organic matter and soil aggregation in agricultural systems with different adoption times Matéria orgânica e agregação de solo em sistemas agrícolas com diferentes tempos de adoção |
title |
Organic matter and soil aggregation in agricultural systems with different adoption times |
spellingShingle |
Organic matter and soil aggregation in agricultural systems with different adoption times Rosset, Jean Sérgio Labile carbon Carbon stocks Conservation management. Carbono lábil Estoques de carbono Manejo conservacionista. |
title_short |
Organic matter and soil aggregation in agricultural systems with different adoption times |
title_full |
Organic matter and soil aggregation in agricultural systems with different adoption times |
title_fullStr |
Organic matter and soil aggregation in agricultural systems with different adoption times |
title_full_unstemmed |
Organic matter and soil aggregation in agricultural systems with different adoption times |
title_sort |
Organic matter and soil aggregation in agricultural systems with different adoption times |
author |
Rosset, Jean Sérgio |
author_facet |
Rosset, Jean Sérgio Lana, Maria do Carmo Pereira, Marcos Gervasio Schiavo, Jolimar Antonio Rampim, Leandro Sarto, Marcos Vinicius Mansano |
author_role |
author |
author2 |
Lana, Maria do Carmo Pereira, Marcos Gervasio Schiavo, Jolimar Antonio Rampim, Leandro Sarto, Marcos Vinicius Mansano |
author2_role |
author author author author author |
dc.contributor.author.fl_str_mv |
Rosset, Jean Sérgio Lana, Maria do Carmo Pereira, Marcos Gervasio Schiavo, Jolimar Antonio Rampim, Leandro Sarto, Marcos Vinicius Mansano |
dc.subject.por.fl_str_mv |
Labile carbon Carbon stocks Conservation management. Carbono lábil Estoques de carbono Manejo conservacionista. |
topic |
Labile carbon Carbon stocks Conservation management. Carbono lábil Estoques de carbono Manejo conservacionista. |
description |
In conservation management systems, such as no-till (NT), it is important to analyze the pattern of changes in soil quality as a function of the time since adoption of the system. This study evaluated the physical fractions of organic matter and soil aggregation in management systems in areas cultivated with different times since implementation of NT: 6, 14, and 22 successive years of soybean and maize/wheat crops (NT6, NT14, and NT22, respectively); 12 years of no-till with successive years of soybean and maize/wheat crops, and the last 4 years with integration of maize and ruzi grass (Brachiaria ruziziensis) - (NT+B); pasture; and forest. Physical fractionation of organic matter determined the total carbon (TC), particulate organic matter (POM), and mineral organic matter (MOM) by calculating the carbon management index (CMI) and variables related to soil structural stability. Forest and pasture areas showed the highest contents of TC, POM, and MOM, as well as higher stocks of POM and MOM. Among the cultivated areas, higher TC and particulate fractions of organic matter and the best CMI values were observed in the area of NT22. There were changes in aggregation indices, depending on the time since implementation of NT. Areas of NT22, pasture, and forest showed the greatest evolution in C-CO2, indicating increased biological activity, with positive effects on soil structural stability. |
publishDate |
2019 |
dc.date.none.fl_str_mv |
2019-10-16 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/35380 10.5433/1679-0359.2019v40n6Supl3p3443 |
url |
https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/35380 |
identifier_str_mv |
10.5433/1679-0359.2019v40n6Supl3p3443 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/35380/26230 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2019 Semina: Ciências Agrárias http://creativecommons.org/licenses/by-nc/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2019 Semina: Ciências Agrárias http://creativecommons.org/licenses/by-nc/4.0 |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
UEL |
publisher.none.fl_str_mv |
UEL |
dc.source.none.fl_str_mv |
Semina: Ciências Agrárias; Vol. 40 No. 6Supl3 (2019); 3443-3460 Semina: Ciências Agrárias; v. 40 n. 6Supl3 (2019); 3443-3460 1679-0359 1676-546X reponame:Semina. Ciências Agrárias (Online) instname:Universidade Estadual de Londrina (UEL) instacron:UEL |
instname_str |
Universidade Estadual de Londrina (UEL) |
instacron_str |
UEL |
institution |
UEL |
reponame_str |
Semina. Ciências Agrárias (Online) |
collection |
Semina. Ciências Agrárias (Online) |
repository.name.fl_str_mv |
Semina. Ciências Agrárias (Online) - Universidade Estadual de Londrina (UEL) |
repository.mail.fl_str_mv |
semina.agrarias@uel.br |
_version_ |
1799306081045839872 |