Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil
Autor(a) principal: | |
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Data de Publicação: | 2017 |
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/27560 |
Resumo: | The crop-livestock integration (CLI) and crop-livestock-forest integration (CLFI) management systems, have been shown to be viable approaches for increasing carbon sequestration in soils, resulting in the improvement of physical and chemical soil attributes. The objective of this study was to evaluate the chemical attributes and organic matter in soils under Natural Forest (NF) converted to different uses and managed differently: rotational pasture area (PAST), crop-livestock integration (CLI), and crop-livestock-forest integration (CLIF). The research was conducted at the São Paulo farm, in Iracema, located in the south-central region of the state of Roraima, Brazil. The studied soil type was classified as Ultisol. Soil samples were taken by opening ditches and examining layers at 0.1-m depth intervals from surface to 0.60-m depth. Total organic carbon (TOC), chemical and granulometric fractionation of soil organic matter (SOM), oxidizable fractions, and light organic matter in water were analyzed. Our results showed low levels of the analyzed chemical elements, a characteristic of a soil with low natural fertility. This matches conditions inherent in source material, weathered by high rainfall, a warm and humid climate, and flat topographic relief. In the 0-0.1 m layer, the PAST and CLI systems had the highest TOC contents relative to the other systems studied. At other depths, there were no statistical differences among TOC levels. The highest concentration of C in the particulate fraction (POC) was noted in the surface layer in all management systems. The pasture system had the highest concentration POC in the top 0.10 m. Our results also showed that the upper 0.10 m of soil in NF contained the lowest content of organic carbon associated with mineral (MOC) relative to the managed agrosystems. In addition, humin provided the largest contribution to SOM in all evaluated management systems. The crop-livestock integration (CLI) and crop-livestock integration forest (CLIF) systems, emerged as a strong alternative to carbon incorporation and subsequently the improvement of physical and chemical soil attributes. The objective of this work to evaluate the chemical attributes and organic matter in soils under Natural forest (NF) converted into different use and management systems: pasture (PAST), crop-livestock Integration (CLI) and crop-livestock Integration forest (CLIF). The research was conducted at São Paulo farm in Iracema, located in the Center-South region of the State of Roraima, Brazil. The soil studied was classified as Argissolo Amarelo Distrófico. The samples were taken by the opening of trenches in layers of 0-0.10, 0.10- 0.20, 0.20- 0.40, and 0.40-0.60 m depth. Total organic carbon (TOC), chemical and granulometric fractionation of soil organic matter (SOM), oxidizable fractions and organic matter in water were analyzed. The results showed low levels of the analyzed chemical elements which characterizes soils with low natural fertility, which matches the conditions of the source material, high rainfall and regional temperature, as well as the flat local relief. In the 0-0.1 m layer, the PAST and CLI systems had the highest TOC contents when compared to the other systems studied, in the other depths there were no statistical differences between the TOC levels. The highest amount of C in the particulate fraction (COp) was verified in the surface layer in all evaluated management systems. The pasture area was the system with the greatest contribution of COp to the depth of 0-0.0 m. In relation to the carbon content associated with minerals (COam), the results showed that the depth of 0-0.05 m NF area presented the lowest levels when compared to the other systems. Regarding the humic substances, there was a larger contribution of humin in all evaluated systems. |
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Chemical and physical fractions of soil organic matter under various management regimes in Roraima, BrazilFrações químicas e físicas da matéria orgânica do solo sob diferentes sistemas de uso em RoraimaSoil FertilityOrganic Carbon FractionationCharacterization of Soil Organic Matter.Fertilidade do soloSistemas de manejoFracionamento do Carbono OrgânicoCaracterização da Matéria Orgânica do Solo.The crop-livestock integration (CLI) and crop-livestock-forest integration (CLFI) management systems, have been shown to be viable approaches for increasing carbon sequestration in soils, resulting in the improvement of physical and chemical soil attributes. The objective of this study was to evaluate the chemical attributes and organic matter in soils under Natural Forest (NF) converted to different uses and managed differently: rotational pasture area (PAST), crop-livestock integration (CLI), and crop-livestock-forest integration (CLIF). The research was conducted at the São Paulo farm, in Iracema, located in the south-central region of the state of Roraima, Brazil. The studied soil type was classified as Ultisol. Soil samples were taken by opening ditches and examining layers at 0.1-m depth intervals from surface to 0.60-m depth. Total organic carbon (TOC), chemical and granulometric fractionation of soil organic matter (SOM), oxidizable fractions, and light organic matter in water were analyzed. Our results showed low levels of the analyzed chemical elements, a characteristic of a soil with low natural fertility. This matches conditions inherent in source material, weathered by high rainfall, a warm and humid climate, and flat topographic relief. In the 0-0.1 m layer, the PAST and CLI systems had the highest TOC contents relative to the other systems studied. At other depths, there were no statistical differences among TOC levels. The highest concentration of C in the particulate fraction (POC) was noted in the surface layer in all management systems. The pasture system had the highest concentration POC in the top 0.10 m. Our results also showed that the upper 0.10 m of soil in NF contained the lowest content of organic carbon associated with mineral (MOC) relative to the managed agrosystems. In addition, humin provided the largest contribution to SOM in all evaluated management systems. The crop-livestock integration (CLI) and crop-livestock integration forest (CLIF) systems, emerged as a strong alternative to carbon incorporation and subsequently the improvement of physical and chemical soil attributes. The objective of this work to evaluate the chemical attributes and organic matter in soils under Natural forest (NF) converted into different use and management systems: pasture (PAST), crop-livestock Integration (CLI) and crop-livestock Integration forest (CLIF). The research was conducted at São Paulo farm in Iracema, located in the Center-South region of the State of Roraima, Brazil. The soil studied was classified as Argissolo Amarelo Distrófico. The samples were taken by the opening of trenches in layers of 0-0.10, 0.10- 0.20, 0.20- 0.40, and 0.40-0.60 m depth. Total organic carbon (TOC), chemical and granulometric fractionation of soil organic matter (SOM), oxidizable fractions and organic matter in water were analyzed. The results showed low levels of the analyzed chemical elements which characterizes soils with low natural fertility, which matches the conditions of the source material, high rainfall and regional temperature, as well as the flat local relief. In the 0-0.1 m layer, the PAST and CLI systems had the highest TOC contents when compared to the other systems studied, in the other depths there were no statistical differences between the TOC levels. The highest amount of C in the particulate fraction (COp) was verified in the surface layer in all evaluated management systems. The pasture area was the system with the greatest contribution of COp to the depth of 0-0.0 m. In relation to the carbon content associated with minerals (COam), the results showed that the depth of 0-0.05 m NF area presented the lowest levels when compared to the other systems. Regarding the humic substances, there was a larger contribution of humin in all evaluated systems.Os sistemas de integração lavoura-pecuária (ILP) e lavoura-pecuária floresta (ILPF) surgiram como forte alternativa para incorporação de carbono e consequentemente melhoria nos atributos físicos e químicas do solo. Objetivou-se com o presente trabalho avaliar os atributos químicos e matéria orgânica em solos sob Floresta Natural (FN) convertidos em diferentes sistemas de uso e manejo: pastagem (PAST), Integração lavoura-pecuária (ILP) e Integração lavoura-pecuária floresta (ILPF). O estudo foi realizado na fazenda São Paulo, em Iracema, localizada na região centro-sul do estado de Roraima. O solo estudado foi classificado em Argissolo Amarelo Distrófico. As amostras foram retiradas mediante a abertura de trincheiras nas camadas de 0-0,10, 0,10-0,20, 0,20-0,40 e 0,40-0,60 m de profundidade. Foram analisados o carbono orgânico total (COT), fracionamento químico e granulométrico da MOS, as frações oxidáveis e a matéria orgânica leve em água. Os resultados mostraram baixos teores dos elementos químicos analisados, o que caracteriza solos com baixa fertilidade natural, que condiz com as condições do material de origem, elevadas precipitações e temperatura regional, bem como ao relevo local plano. Na camada de 0-0,1 m os sistemas PAST e ILP apresentaram os maiores teores de COT quando comparados aos outros sistemas estudados, nas demais profundidades não se verificou diferenças estatísticas entre os teores de COT. A maior quantidade de C na fração particulada (COp) foi verificada na camada superficial em todos os sistemas de manejo avaliados. A área de pastagem foi o sistema com a maior contribuição do COp na profundidade de 0-0,10 m. Com relação aos teores do carbono associado aos minerais (COam), os resultados demostraram que na profundidade de 0-0,10 m área de FN apresentou os menores teores quando comparados aos outros sistemas. Em relação às substâncias húmicas houve uma maior contribuição da Humina em todos os sistemas avaliados.UEL2017-08-25info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionPesquisa Empírica de Campoapplication/pdfhttps://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/2756010.5433/1679-0359.2017v38n4Supl1p2419Semina: Ciências Agrárias; Vol. 38 No. 4Supl1 (2017); 2419-2432Semina: Ciências Agrárias; v. 38 n. 4Supl1 (2017); 2419-24321679-03591676-546Xreponame:Semina. Ciências Agrárias (Online)instname:Universidade Estadual de Londrina (UEL)instacron:UELenghttps://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/27560/21494Copyright (c) 2017 Semina: Ciências Agráriashttp://creativecommons.org/licenses/by-nc/4.0info:eu-repo/semantics/openAccessGuardiola, Marden Daniel EspinozaVale Júnior, José FrutuosoSilva, Edmilson Evangelista daRossi, Celeste QueirozPereira, Marcos Gervasio2022-10-21T15:08:02Zoai:ojs.pkp.sfu.ca:article/27560Revistahttp://www.uel.br/revistas/uel/index.php/semagrariasPUBhttps://ojs.uel.br/revistas/uel/index.php/semagrarias/oaisemina.agrarias@uel.br1679-03591676-546Xopendoar:2022-10-21T15:08:02Semina. Ciências Agrárias (Online) - Universidade Estadual de Londrina (UEL)false |
dc.title.none.fl_str_mv |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil Frações químicas e físicas da matéria orgânica do solo sob diferentes sistemas de uso em Roraima |
title |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil |
spellingShingle |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil Guardiola, Marden Daniel Espinoza Soil Fertility Organic Carbon Fractionation Characterization of Soil Organic Matter. Fertilidade do solo Sistemas de manejo Fracionamento do Carbono Orgânico Caracterização da Matéria Orgânica do Solo. |
title_short |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil |
title_full |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil |
title_fullStr |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil |
title_full_unstemmed |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil |
title_sort |
Chemical and physical fractions of soil organic matter under various management regimes in Roraima, Brazil |
author |
Guardiola, Marden Daniel Espinoza |
author_facet |
Guardiola, Marden Daniel Espinoza Vale Júnior, José Frutuoso Silva, Edmilson Evangelista da Rossi, Celeste Queiroz Pereira, Marcos Gervasio |
author_role |
author |
author2 |
Vale Júnior, José Frutuoso Silva, Edmilson Evangelista da Rossi, Celeste Queiroz Pereira, Marcos Gervasio |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Guardiola, Marden Daniel Espinoza Vale Júnior, José Frutuoso Silva, Edmilson Evangelista da Rossi, Celeste Queiroz Pereira, Marcos Gervasio |
dc.subject.por.fl_str_mv |
Soil Fertility Organic Carbon Fractionation Characterization of Soil Organic Matter. Fertilidade do solo Sistemas de manejo Fracionamento do Carbono Orgânico Caracterização da Matéria Orgânica do Solo. |
topic |
Soil Fertility Organic Carbon Fractionation Characterization of Soil Organic Matter. Fertilidade do solo Sistemas de manejo Fracionamento do Carbono Orgânico Caracterização da Matéria Orgânica do Solo. |
description |
The crop-livestock integration (CLI) and crop-livestock-forest integration (CLFI) management systems, have been shown to be viable approaches for increasing carbon sequestration in soils, resulting in the improvement of physical and chemical soil attributes. The objective of this study was to evaluate the chemical attributes and organic matter in soils under Natural Forest (NF) converted to different uses and managed differently: rotational pasture area (PAST), crop-livestock integration (CLI), and crop-livestock-forest integration (CLIF). The research was conducted at the São Paulo farm, in Iracema, located in the south-central region of the state of Roraima, Brazil. The studied soil type was classified as Ultisol. Soil samples were taken by opening ditches and examining layers at 0.1-m depth intervals from surface to 0.60-m depth. Total organic carbon (TOC), chemical and granulometric fractionation of soil organic matter (SOM), oxidizable fractions, and light organic matter in water were analyzed. Our results showed low levels of the analyzed chemical elements, a characteristic of a soil with low natural fertility. This matches conditions inherent in source material, weathered by high rainfall, a warm and humid climate, and flat topographic relief. In the 0-0.1 m layer, the PAST and CLI systems had the highest TOC contents relative to the other systems studied. At other depths, there were no statistical differences among TOC levels. The highest concentration of C in the particulate fraction (POC) was noted in the surface layer in all management systems. The pasture system had the highest concentration POC in the top 0.10 m. Our results also showed that the upper 0.10 m of soil in NF contained the lowest content of organic carbon associated with mineral (MOC) relative to the managed agrosystems. In addition, humin provided the largest contribution to SOM in all evaluated management systems. The crop-livestock integration (CLI) and crop-livestock integration forest (CLIF) systems, emerged as a strong alternative to carbon incorporation and subsequently the improvement of physical and chemical soil attributes. The objective of this work to evaluate the chemical attributes and organic matter in soils under Natural forest (NF) converted into different use and management systems: pasture (PAST), crop-livestock Integration (CLI) and crop-livestock Integration forest (CLIF). The research was conducted at São Paulo farm in Iracema, located in the Center-South region of the State of Roraima, Brazil. The soil studied was classified as Argissolo Amarelo Distrófico. The samples were taken by the opening of trenches in layers of 0-0.10, 0.10- 0.20, 0.20- 0.40, and 0.40-0.60 m depth. Total organic carbon (TOC), chemical and granulometric fractionation of soil organic matter (SOM), oxidizable fractions and organic matter in water were analyzed. The results showed low levels of the analyzed chemical elements which characterizes soils with low natural fertility, which matches the conditions of the source material, high rainfall and regional temperature, as well as the flat local relief. In the 0-0.1 m layer, the PAST and CLI systems had the highest TOC contents when compared to the other systems studied, in the other depths there were no statistical differences between the TOC levels. The highest amount of C in the particulate fraction (COp) was verified in the surface layer in all evaluated management systems. The pasture area was the system with the greatest contribution of COp to the depth of 0-0.0 m. In relation to the carbon content associated with minerals (COam), the results showed that the depth of 0-0.05 m NF area presented the lowest levels when compared to the other systems. Regarding the humic substances, there was a larger contribution of humin in all evaluated systems. |
publishDate |
2017 |
dc.date.none.fl_str_mv |
2017-08-25 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Pesquisa Empírica de Campo |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/27560 10.5433/1679-0359.2017v38n4Supl1p2419 |
url |
https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/27560 |
identifier_str_mv |
10.5433/1679-0359.2017v38n4Supl1p2419 |
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/27560/21494 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2017 Semina: Ciências Agrárias http://creativecommons.org/licenses/by-nc/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2017 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. 38 No. 4Supl1 (2017); 2419-2432 Semina: Ciências Agrárias; v. 38 n. 4Supl1 (2017); 2419-2432 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 |
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1799306077116825600 |