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Registro Completo |
Biblioteca(s): |
Embrapa Agrossilvipastoril. |
Data corrente: |
16/01/2019 |
Data da última atualização: |
16/01/2019 |
Tipo da produção científica: |
Resumo em Anais de Congresso |
Autoria: |
SOUZA, L. HL C. de; COUTO, E. G.; MATOS, E. da S.; MAGALHÃES, C. A. de S.; SILVEIRA, J. G.; CARVALHO, G. de; BEHLING, M.; SOUZA, A. L. de. |
Afiliação: |
LETICIA H. C. DE SOUZA, UFMT; EDUARDO G. COUTO, UFMT; EDUARDO DA SILVA MATOS, SIRE; CIRO AUGUSTO DE SOUZA MAGALHAES, CPAMT; JÚLIA G. SILVEIRA, UFV; GÉSSICA DE CARVALHO, UFV; MAUREL BEHLING, CPAMT; ANDRÉ L. DE SOUZA, UFMT. |
Título: |
Carbono total do solo em sistemas integrados de produção sob plantio direto. |
Ano de publicação: |
2018 |
Fonte/Imprenta: |
In: ENCONTRO NACIONAL DE PLANTIO DIRETO NA PALHA, 16., Sorriso, MT. Sistema de Plantiodireto: entenda os desafios atuais. Prepare-se para o futuro: resumos. Sorriso, MT: FEBRAPDP, 2018. |
Páginas: |
p. 31 |
Idioma: |
Português |
Conteúdo: |
Objetivamos quantificar o total de carbono do solo em sistemas de produção agrícola sob plantio direto. O experimento está localizado na Embrapa Agrossilvipastoril, Sinop-MT. Foram avaliados 6 sistemas produtivos: Eucalipto; Lavoura; Pastagem; Lavoura-Pecuária; Pecuária-Lavoura; e Integração Lavoura-Pecuária-Floresta. Amostras de solo foram coletadas até 30 cm de forma estratificada. A camada de 0-5 cm de solo é a que expressa maior diferença de Carbono Total entre os sistemas de produção. O menor teor de C nesta camada foi verificado para o sistema de plantio exclusivo de Floresta, e o renque de floresta de eucalipto na ILPF obteve teor de C superior a esta. Já os maiores teores de C no solo, para esta mesma camada, são atribuídos aos sistemas em que a gramínea (pastagem) é inserida por períodos mais longos (2 anos pelo menos), são eles os sistemas com pastagem exclusiva, pastagem-lavoura e lavoura-pastagem. Os sistemas cultivados com gramíneas apenas como segunda safra demonstraram menor teor de C, sendo, a lavoura exclusiva e a ILPF. Entre as distâncias dos renques de eucalipto na ILPF, para ambas faces, não observamos diferenças relevantes. O teor de C do solo foi inferior à área de referência para todos sistemas e camadas de solo. |
Palavras-Chave: |
Estoque de Carbono; Mitigação de Gases de Efeito Estufa; Sustentabilidade. |
Thesagro: |
Manejo do Solo; Matéria Orgânica. |
Categoria do assunto: |
A Sistemas de Cultivo |
Marc: |
LEADER 02233naa a2200277 a 4500 001 2104292 005 2019-01-16 008 2018 bl uuuu u00u1 u #d 100 1 $aSOUZA, L. HL C. de 245 $aCarbono total do solo em sistemas integrados de produção sob plantio direto.$h[electronic resource] 260 $c2018 300 $ap. 31 520 $aObjetivamos quantificar o total de carbono do solo em sistemas de produção agrícola sob plantio direto. O experimento está localizado na Embrapa Agrossilvipastoril, Sinop-MT. Foram avaliados 6 sistemas produtivos: Eucalipto; Lavoura; Pastagem; Lavoura-Pecuária; Pecuária-Lavoura; e Integração Lavoura-Pecuária-Floresta. Amostras de solo foram coletadas até 30 cm de forma estratificada. A camada de 0-5 cm de solo é a que expressa maior diferença de Carbono Total entre os sistemas de produção. O menor teor de C nesta camada foi verificado para o sistema de plantio exclusivo de Floresta, e o renque de floresta de eucalipto na ILPF obteve teor de C superior a esta. Já os maiores teores de C no solo, para esta mesma camada, são atribuídos aos sistemas em que a gramínea (pastagem) é inserida por períodos mais longos (2 anos pelo menos), são eles os sistemas com pastagem exclusiva, pastagem-lavoura e lavoura-pastagem. Os sistemas cultivados com gramíneas apenas como segunda safra demonstraram menor teor de C, sendo, a lavoura exclusiva e a ILPF. Entre as distâncias dos renques de eucalipto na ILPF, para ambas faces, não observamos diferenças relevantes. O teor de C do solo foi inferior à área de referência para todos sistemas e camadas de solo. 650 $aManejo do Solo 650 $aMatéria Orgânica 653 $aEstoque de Carbono 653 $aMitigação de Gases de Efeito Estufa 653 $aSustentabilidade 700 1 $aCOUTO, E. G. 700 1 $aMATOS, E. da S. 700 1 $aMAGALHÃES, C. A. de S. 700 1 $aSILVEIRA, J. G. 700 1 $aCARVALHO, G. de 700 1 $aBEHLING, M. 700 1 $aSOUZA, A. L. de 773 $tIn: ENCONTRO NACIONAL DE PLANTIO DIRETO NA PALHA, 16., Sorriso, MT. Sistema de Plantiodireto: entenda os desafios atuais. Prepare-se para o futuro: resumos. Sorriso, MT: FEBRAPDP, 2018.
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Embrapa Agrossilvipastoril (CPAMT) |
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Registro Completo
Biblioteca(s): |
Embrapa Amazônia Ocidental. |
Data corrente: |
20/05/1999 |
Data da última atualização: |
04/04/2022 |
Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
Autoria: |
SCHROTH, G.; SALAZAR, E.; SILVA JUNIOR, J. P. da; SEIXAS, R.; MACEDO, J. L. V. de. |
Afiliação: |
JOSE PEREIRA DA SILVA JUNIOR, CPAA; JEFERSON LUIS VASCONCELOS DE MACEDO, CPAA. |
Título: |
Spatial and temporal patterns of N availability and N mineralization under tree crops and a cover crop in a multi-strata agroforestry system of central Amazonia. |
Ano de publicação: |
1999 |
Fonte/Imprenta: |
In: SHIFT PROJECT ENV 23 (Manaus-AM). Recuperacao de areas degradadas e abandonadas, atraves de sistemas de policultivo. Manaus: Embrapa Amazônia Ocidental, 1999. |
Páginas: |
p. 58-89. |
Idioma: |
Inglês |
Notas: |
Relatório Anual 1998. |
Conteúdo: |
Under rainforest vegetation, the Oxisols and Ultisols which dominate Amazonian uplands are characterized by relatively high availability of N in relation to other nutrients. When the rainforest vegetation is converted into agricultural systems, the disruption of the nutrient recycling mechanisms of the forest under conditions of intensive rainfalls and permeable soils increases the potencial for N leaching. In a previous study, substantial amounts of mineral N were found in the subsoil of central Amazonia Oxisol under various tree crops and a legumenous cover crops, indicating that even under perennial cropping systems, much of the mineralized soil and fertilizer N may be lost unproductively. We hypothesized that the spatial and temporal patterns of N availability and N mineralization in the soil of a polycultural system would influence the efficiency with which N is taken up by the trees instead of being leached. The analysis of such pattens coul lead to strategies for improving this efficiency and reducing the dependence of the system on external nutrient inputs. The concentration of mineral N and the net N mineralization in the topsoil were measured at five occasions during 10 months in a multi-strata agroforestry system on an Oxisol in central Amazonia, Brazil. The system was composed of three tree crop species and a leguminous cover crop, and was studied at two fertilization levels. The net N mineralization was highest under the cover crop, intermediate under a tree crop where the soil was also covered by the cover crop. This resulted in higher mineral N concentrations in the soil under the cover crop than under the tree crops during part of the rainy season. The increased N mineralization under the cover crop was due to higher total N in the soil, higher soil moisture and presumably a larger pool of readily mineralizable N components in the soil compared to the tree crops. Other fertility parameters also differed significantly between sampling positions within the plots, but this had no major influence on net N mineralization. Also, the fertilization level had no significant influence on N mineralization. As most of the N was mineralized under the cover crop at some distance from the trees, the uptake of the mineralized N by the tree crops could presumably be increased, and N leaching reduced, by a higher tree density and an altered management of the cover crop to increase N mineralization in the soil close to the trees. In view of the high total N mineralization rates in the system (349 kg ha-1 yr-1) and unclear yield responses of the tree crops to N fertilization at this site, it is concluded that after an establishment phase, the fertilization with N of tree crops with well-developed root systems may not always be necessary on this soil type. MenosUnder rainforest vegetation, the Oxisols and Ultisols which dominate Amazonian uplands are characterized by relatively high availability of N in relation to other nutrients. When the rainforest vegetation is converted into agricultural systems, the disruption of the nutrient recycling mechanisms of the forest under conditions of intensive rainfalls and permeable soils increases the potencial for N leaching. In a previous study, substantial amounts of mineral N were found in the subsoil of central Amazonia Oxisol under various tree crops and a legumenous cover crops, indicating that even under perennial cropping systems, much of the mineralized soil and fertilizer N may be lost unproductively. We hypothesized that the spatial and temporal patterns of N availability and N mineralization in the soil of a polycultural system would influence the efficiency with which N is taken up by the trees instead of being leached. The analysis of such pattens coul lead to strategies for improving this efficiency and reducing the dependence of the system on external nutrient inputs. The concentration of mineral N and the net N mineralization in the topsoil were measured at five occasions during 10 months in a multi-strata agroforestry system on an Oxisol in central Amazonia, Brazil. The system was composed of three tree crop species and a leguminous cover crop, and was studied at two fertilization levels. The net N mineralization was highest under the cover crop, intermediate under a tree cro... Mostrar Tudo |
Palavras-Chave: |
Agrofloresta; Amazonas; Brasil; Manaus. |
Thesagro: |
Cultivo Multiplo; Fertilidade do Solo; Floresta Tropical Úmida; Nitrogênio; Solo. |
Thesaurus NAL: |
agroforestry; multiple cropping; nitrogen; nitrogen fertilizers; soil; soil fertility; tropical rain forests. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/181178/1/ID-4037-2-47-72.pdf
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Marc: |
LEADER 04017naa a2200385 a 4500 001 1668177 005 2022-04-04 008 1999 bl uuuu u00u1 u #d 100 1 $aSCHROTH, G. 245 $aSpatial and temporal patterns of N availability and N mineralization under tree crops and a cover crop in a multi-strata agroforestry system of central Amazonia. 260 $c1999 300 $ap. 58-89. 500 $aRelatório Anual 1998. 520 $aUnder rainforest vegetation, the Oxisols and Ultisols which dominate Amazonian uplands are characterized by relatively high availability of N in relation to other nutrients. When the rainforest vegetation is converted into agricultural systems, the disruption of the nutrient recycling mechanisms of the forest under conditions of intensive rainfalls and permeable soils increases the potencial for N leaching. In a previous study, substantial amounts of mineral N were found in the subsoil of central Amazonia Oxisol under various tree crops and a legumenous cover crops, indicating that even under perennial cropping systems, much of the mineralized soil and fertilizer N may be lost unproductively. We hypothesized that the spatial and temporal patterns of N availability and N mineralization in the soil of a polycultural system would influence the efficiency with which N is taken up by the trees instead of being leached. The analysis of such pattens coul lead to strategies for improving this efficiency and reducing the dependence of the system on external nutrient inputs. The concentration of mineral N and the net N mineralization in the topsoil were measured at five occasions during 10 months in a multi-strata agroforestry system on an Oxisol in central Amazonia, Brazil. The system was composed of three tree crop species and a leguminous cover crop, and was studied at two fertilization levels. The net N mineralization was highest under the cover crop, intermediate under a tree crop where the soil was also covered by the cover crop. This resulted in higher mineral N concentrations in the soil under the cover crop than under the tree crops during part of the rainy season. The increased N mineralization under the cover crop was due to higher total N in the soil, higher soil moisture and presumably a larger pool of readily mineralizable N components in the soil compared to the tree crops. Other fertility parameters also differed significantly between sampling positions within the plots, but this had no major influence on net N mineralization. Also, the fertilization level had no significant influence on N mineralization. As most of the N was mineralized under the cover crop at some distance from the trees, the uptake of the mineralized N by the tree crops could presumably be increased, and N leaching reduced, by a higher tree density and an altered management of the cover crop to increase N mineralization in the soil close to the trees. In view of the high total N mineralization rates in the system (349 kg ha-1 yr-1) and unclear yield responses of the tree crops to N fertilization at this site, it is concluded that after an establishment phase, the fertilization with N of tree crops with well-developed root systems may not always be necessary on this soil type. 650 $aagroforestry 650 $amultiple cropping 650 $anitrogen 650 $anitrogen fertilizers 650 $asoil 650 $asoil fertility 650 $atropical rain forests 650 $aCultivo Multiplo 650 $aFertilidade do Solo 650 $aFloresta Tropical Úmida 650 $aNitrogênio 650 $aSolo 653 $aAgrofloresta 653 $aAmazonas 653 $aBrasil 653 $aManaus 700 1 $aSALAZAR, E. 700 1 $aSILVA JUNIOR, J. P. da 700 1 $aSEIXAS, R. 700 1 $aMACEDO, J. L. V. de 773 $tIn: SHIFT PROJECT ENV 23 (Manaus-AM). Recuperacao de areas degradadas e abandonadas, atraves de sistemas de policultivo. Manaus: Embrapa Amazônia Ocidental, 1999.
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