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Registro Completo |
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
27/09/2021 |
Data da última atualização: |
27/09/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
BERTOLINO, A. V. F. A.; FERNANDES, N. F.; MIRANDA, J. P. L.; SOUZA, A. P.; LOPES, M. R. S.; PALMIERI, F. |
Afiliação: |
ANA V. F. A. BERTOLINO, UERJ; NELSON F. FERNANDES, UFRJ; JOÃO P. L. MIRANDA, UFRJ; ANDRÉA P. SOUZA, UERJ; MARCEL R. S. LOPES, UFRJ; FRANCESCO PALMIERI, CNPS. |
Título: |
Effects of plough pan development on surface hydrology and on soil physical properties in Southeastern Brazilian plateau. |
Ano de publicação: |
2010 |
Fonte/Imprenta: |
Journal of Hydrology, v. 393, n. 1/2, p. 94-104, Oct. 2010. |
DOI: |
https://doi.org/10.1016/j.jhydrol.2010.07.038 |
Idioma: |
Inglês |
Conteúdo: |
Conventional tillage may impose changes in soil physical properties that lead to a decrease in soil physical quality. Although plough pan formation is considered to be an important consequence of conventional tillage practices in Southeastern Brazil, few studies have focused on its hydrological consequences. Detailed investigations in two experimental plots located in the hilly landscape of Serra do Mar close to Rio de Janeiro city were carried out to characterize the changes in soil physical properties and in soil hydrology due to plough pan formation. Conventional (CT) and minimum tillage (MT) practices were implemented in two plots for 3 years and soil matric potential (SMP) was monitored in each plot via nests of tensiometers and Watermark (R) sensors installed at different depths. Undisturbed soil blocks were collected for micromorphological analyses to quantify the total pore space in soils under CT and MT systems, and in soils under natural tropical forest. Results suggest that soils under the CT system developed a plough pan layer at about 20 cm depth that had 44% less total porosity as compared to surface conditions. It is shown that soils under the CT system tended to stay saturated for longer periods of time after each rainfall event. Besides, during intense rainy periods soils under the CT system may develop hydrologic conditions that favor lateral flows while soils under the MT system were still draining. Such hydrological responses may explain why average soil erosion rates measured for individual rainfall events under the CT system were about 2.5 times greater than the ones observed at MT. The results attested that conventional tillage in this area generated modifications in soil fabric, especially in pore-size distribution and connectivity, which induced important changes in soil hydrology and soil erosion. The agricultural practices used in this area, associated with the local steep hillslopes and intense rainfall events, are definitely not adequate and require the introduction of soil and water conservation practices in order to become sustainable. MenosConventional tillage may impose changes in soil physical properties that lead to a decrease in soil physical quality. Although plough pan formation is considered to be an important consequence of conventional tillage practices in Southeastern Brazil, few studies have focused on its hydrological consequences. Detailed investigations in two experimental plots located in the hilly landscape of Serra do Mar close to Rio de Janeiro city were carried out to characterize the changes in soil physical properties and in soil hydrology due to plough pan formation. Conventional (CT) and minimum tillage (MT) practices were implemented in two plots for 3 years and soil matric potential (SMP) was monitored in each plot via nests of tensiometers and Watermark (R) sensors installed at different depths. Undisturbed soil blocks were collected for micromorphological analyses to quantify the total pore space in soils under CT and MT systems, and in soils under natural tropical forest. Results suggest that soils under the CT system developed a plough pan layer at about 20 cm depth that had 44% less total porosity as compared to surface conditions. It is shown that soils under the CT system tended to stay saturated for longer periods of time after each rainfall event. Besides, during intense rainy periods soils under the CT system may develop hydrologic conditions that favor lateral flows while soils under the MT system were still draining. Such hydrological responses may explain why average soil ... Mostrar Tudo |
Palavras-Chave: |
Plough pan. |
Thesagro: |
Compactação do Solo; Erosão do Solo; Hidrologia. |
Thesaurus Nal: |
Soil compaction; Soil erosion; Soil micromorphology. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02984naa a2200277 a 4500 001 2134793 005 2021-09-27 008 2010 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1016/j.jhydrol.2010.07.038$2DOI 100 1 $aBERTOLINO, A. V. F. A. 245 $aEffects of plough pan development on surface hydrology and on soil physical properties in Southeastern Brazilian plateau.$h[electronic resource] 260 $c2010 520 $aConventional tillage may impose changes in soil physical properties that lead to a decrease in soil physical quality. Although plough pan formation is considered to be an important consequence of conventional tillage practices in Southeastern Brazil, few studies have focused on its hydrological consequences. Detailed investigations in two experimental plots located in the hilly landscape of Serra do Mar close to Rio de Janeiro city were carried out to characterize the changes in soil physical properties and in soil hydrology due to plough pan formation. Conventional (CT) and minimum tillage (MT) practices were implemented in two plots for 3 years and soil matric potential (SMP) was monitored in each plot via nests of tensiometers and Watermark (R) sensors installed at different depths. Undisturbed soil blocks were collected for micromorphological analyses to quantify the total pore space in soils under CT and MT systems, and in soils under natural tropical forest. Results suggest that soils under the CT system developed a plough pan layer at about 20 cm depth that had 44% less total porosity as compared to surface conditions. It is shown that soils under the CT system tended to stay saturated for longer periods of time after each rainfall event. Besides, during intense rainy periods soils under the CT system may develop hydrologic conditions that favor lateral flows while soils under the MT system were still draining. Such hydrological responses may explain why average soil erosion rates measured for individual rainfall events under the CT system were about 2.5 times greater than the ones observed at MT. The results attested that conventional tillage in this area generated modifications in soil fabric, especially in pore-size distribution and connectivity, which induced important changes in soil hydrology and soil erosion. The agricultural practices used in this area, associated with the local steep hillslopes and intense rainfall events, are definitely not adequate and require the introduction of soil and water conservation practices in order to become sustainable. 650 $aSoil compaction 650 $aSoil erosion 650 $aSoil micromorphology 650 $aCompactação do Solo 650 $aErosão do Solo 650 $aHidrologia 653 $aPlough pan 700 1 $aFERNANDES, N. F. 700 1 $aMIRANDA, J. P. L. 700 1 $aSOUZA, A. P. 700 1 $aLOPES, M. R. S. 700 1 $aPALMIERI, F. 773 $tJournal of Hydrology$gv. 393, n. 1/2, p. 94-104, Oct. 2010.
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Registros recuperados : 10 | |
1. | | BRANDAO, E. S.; LOPES, M. R. Cadeia do tomate industrial no Brasil. In: VIEIRA, R.C.M.; TEIXEIRA FILHO, A.R.; OLIVEIRA, A.J. de; LOPES, M.R. Cadeias produtivas no Brasil: analise da competitividade. Brasilia, Embrapa Comunicacao para Transferencia e Tecnologia, 2001. p. 377-393.Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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4. | | TALAMINI, D. J. D.; LOPES, M. R.; MARTINS, F. M.; OLIVEIRA, A. J.; FILHO, J. R. L.; BARCELOS, F. C. Efeito das políticas públicas na cadeia do frango - estudo de caso no Oeste Catarinense. In: CONGRESSO LATINOAMERICANO DE AVICULTURA, 20., 2007, Porto Alegre. Memorias. Porto Alegre: UBA : FIERGS, 2007. p. 261-263. Projeto n. 03.04.11.400-02Tipo: Artigo em Anais de Congresso / Nota Técnica | Circulação/Nível: -- - -- |
Biblioteca(s): Embrapa Suínos e Aves. |
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Biblioteca(s): Embrapa Agrobiologia. |
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6. | | ALVES, M. G. de O.; COSTA, M. F. O. e; EIFERT, E. da C.; BRUNES, L. C.; LOPES, M. R.; MAGNABOSCO, C. U. Interrelações entre características de precocidade sexual e de eficiência alimentar em fêmeas Nelore. In: SEMINÁRIO JOVENS TALENTOS, 13., 2019, Santo Antônio de Goiás. Resumos... Santo Antônio de Goiás: Embrapa Arroz e Feijão, 2019. p. 97.Tipo: Resumo em Anais de Congresso |
Biblioteca(s): Embrapa Arroz e Feijão. |
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7. | | BERTOLINO, A. V. F. A.; FERNANDES, N. F.; MIRANDA, J. P. L.; SOUZA, A. P.; LOPES, M. R. S.; PALMIERI, F. Effects of plough pan development on surface hydrology and on soil physical properties in Southeastern Brazilian plateau. Journal of Hydrology, v. 393, n. 1/2, p. 94-104, Oct. 2010.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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8. | | LIMA, N. A. P. de; COSTA, M. F. O. e; MAGNABOSCO, C. U.; BRUNES, L. C.; LOPES, M. R.; EIFERT, E. da C. Evolução genética para características de carcaça em bovinos Nelore sob seleção para maciez da carne. In: SEMINÁRIO JOVENS TALENTOS, 13., 2019, Santo Antônio de Goiás. Resumos... Santo Antônio de Goiás: Embrapa Arroz e Feijão, 2019. p. 49.Tipo: Resumo em Anais de Congresso |
Biblioteca(s): Embrapa Arroz e Feijão. |
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9. | | LIMA, R. L.; MIRANDA, J. P. L.; SILVA, L. M.; DONAGEMMA, G. K.; BERTOLINO, A. V. F. A.; LOPES, M. R. S.; FERNANDES, N. F. Relação entre a estabilidade de agregados e o escoamento superficial de um solo sob coberturas e manejos distintos na região serrana fluminense - Bom Jardim (RJ). In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 31., 2007, Gramado. Conquistas e desafios da ciência do solo brasileira. Porto Alegre: Universidade Federal do Rio Grande do Sul, 2007. 1 CD-ROM.Tipo: Artigo em Anais de Congresso |
Biblioteca(s): Embrapa Solos. |
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10. | | MIRANDA, J. P. L.; SILVA, L. M.; LIMA, R. L.; DONAGEMMA, G. K.; BERTOLINO, A. V. F. A.; LOPES, M. R. S.; FERNANDES, N. F. Relação do manejo e cultivos distintos com propriedades físicas de um cambissolo em ambiente agrícola serrano - Bom Jardim (RJ). CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 31., 2007, Gramado. ResumoTipo: Resumo em Anais de Congresso | Circulação/Nível: -- - -- |
Biblioteca(s): Embrapa Solos. |
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