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Registro Completo |
Biblioteca(s): |
Embrapa Soja. |
Data corrente: |
14/12/2005 |
Data da última atualização: |
31/08/2017 |
Autoria: |
BLANCHART, E.; ALBRECHT, A.; BROWN, G.; DECAENS, T.; DUBOISSET, A.; LAVELLE, P.; MARIANI, L.; ROOSE, E. |
Título: |
Effects of tropical endogeic earthworms on soil erosion. |
Ano de publicação: |
2004 |
Fonte/Imprenta: |
Agriculture, Ecosystems & Environment, v. 104, n. 2, p. 303-315, Oct. 2004. |
Idioma: |
Inglês |
Notas: |
Nome correto do terceiro autor: BROWN, G. G. |
Conteúdo: |
Soil biota play a crucial role in influencing soil structure and related soil physical properties. In particular, an abundant literature shows that earthworms, through their burrowing and feeding activities, influence particle size distribution, organic matter content, organic matter location, soil aggregation, aggregate stability and tensile strength, soil roughness, and water infiltration. All those properties greatly influence soil erodibility and soil erosion. Nevertheless, there are few quantitative studies of the influence of earthworms on soil erosion. In some cases, earthworms are said to increase soil losses while other studies emphasize their control on structural stability inducing a reduction in soil erosion. This paper analyses the effects of endogeic earthworms on soil erosion, using recently published data collected in the humid tropics. Endogeics comprise two separate functional groups regarding their effects on soil physical properties, i.e. "compacting" and "decompacting" species whose effects on soil erosion may differ substantially. The effects of these earthworms on soil erodibility and erosion in the tropics ultimately depend on soil types and on the organic matter content in soils. In kaolinitic soils, irrespective of clay content, endogeics greatly influence aggregation, aggregate stability, total porosity and pore size distribution; whereas in smectitic soils (such as vertisols), earthworms have a smaller effect on soil erodibility than soil organic matter and cations. Some options for managing earthworms and organic matter in order to limit soil erosion are also discussed in this paper. MenosSoil biota play a crucial role in influencing soil structure and related soil physical properties. In particular, an abundant literature shows that earthworms, through their burrowing and feeding activities, influence particle size distribution, organic matter content, organic matter location, soil aggregation, aggregate stability and tensile strength, soil roughness, and water infiltration. All those properties greatly influence soil erodibility and soil erosion. Nevertheless, there are few quantitative studies of the influence of earthworms on soil erosion. In some cases, earthworms are said to increase soil losses while other studies emphasize their control on structural stability inducing a reduction in soil erosion. This paper analyses the effects of endogeic earthworms on soil erosion, using recently published data collected in the humid tropics. Endogeics comprise two separate functional groups regarding their effects on soil physical properties, i.e. "compacting" and "decompacting" species whose effects on soil erosion may differ substantially. The effects of these earthworms on soil erodibility and erosion in the tropics ultimately depend on soil types and on the organic matter content in soils. In kaolinitic soils, irrespective of clay content, endogeics greatly influence aggregation, aggregate stability, total porosity and pore size distribution; whereas in smectitic soils (such as vertisols), earthworms have a smaller effect on soil erodibility than soil organic ... Mostrar Tudo |
Thesagro: |
Solo. |
Categoria do assunto: |
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Marc: |
LEADER 02271naa a2200229 a 4500 001 1468644 005 2017-08-31 008 2004 bl --- 0-- u #d 100 1 $aBLANCHART, E. 245 $aEffects of tropical endogeic earthworms on soil erosion. 260 $c2004 500 $aNome correto do terceiro autor: BROWN, G. G. 520 $aSoil biota play a crucial role in influencing soil structure and related soil physical properties. In particular, an abundant literature shows that earthworms, through their burrowing and feeding activities, influence particle size distribution, organic matter content, organic matter location, soil aggregation, aggregate stability and tensile strength, soil roughness, and water infiltration. All those properties greatly influence soil erodibility and soil erosion. Nevertheless, there are few quantitative studies of the influence of earthworms on soil erosion. In some cases, earthworms are said to increase soil losses while other studies emphasize their control on structural stability inducing a reduction in soil erosion. This paper analyses the effects of endogeic earthworms on soil erosion, using recently published data collected in the humid tropics. Endogeics comprise two separate functional groups regarding their effects on soil physical properties, i.e. "compacting" and "decompacting" species whose effects on soil erosion may differ substantially. The effects of these earthworms on soil erodibility and erosion in the tropics ultimately depend on soil types and on the organic matter content in soils. In kaolinitic soils, irrespective of clay content, endogeics greatly influence aggregation, aggregate stability, total porosity and pore size distribution; whereas in smectitic soils (such as vertisols), earthworms have a smaller effect on soil erodibility than soil organic matter and cations. Some options for managing earthworms and organic matter in order to limit soil erosion are also discussed in this paper. 650 $aSolo 700 1 $aALBRECHT, A. 700 1 $aBROWN, G. 700 1 $aDECAENS, T. 700 1 $aDUBOISSET, A. 700 1 $aLAVELLE, P. 700 1 $aMARIANI, L. 700 1 $aROOSE, E. 773 $tAgriculture, Ecosystems & Environment$gv. 104, n. 2, p. 303-315, Oct. 2004.
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Registro original: |
Embrapa Soja (CNPSO) |
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Registro Completo
Biblioteca(s): |
Embrapa Agropecuária Oeste; Embrapa Cerrados; Embrapa Soja. |
Data corrente: |
25/07/2012 |
Data da última atualização: |
14/08/2012 |
Tipo da produção científica: |
Artigo em Anais de Congresso |
Autoria: |
CARNEIRO, G. E. de S.; PIPOLO, A. E.; GOMIDE, F. B.; ARIAS, C. A. A.; KASTER, M.; DIAS, W. P.; SOARES, R. M.; ALMEIDA, A. M. R.; OLIVEIRA, M. F.; MOREIRA, J. U. V.; MIRANDA, L. C.; PETEK, M. R.; LIMA, D.; BROGIN, R. L.; ABDELNOOR, R. V.; MELO, C. L. P. de; TEIXEIRA, M. R. O.; MARANHO, E.; BERTAGNOLLI, P. F.; COSTAMILAN, L. M.; CARRÃO-PANIZZI, M. C.; FRONZA, V.; MELLO FILHO, O. L.; ZITO, R. K.; SILVA NETO, S. P.; MOREIRA, C. T.; PEREIRA, M. J. Z. |
Afiliação: |
GERALDO ESTEVAM DE SOUZA CARNEIRO, CNPSO; ANTONIO EDUARDO PIPOLO, CNPSO; Fundação Meridional; CARLOS ALBERTO ARRABAL ARIAS, CNPSO; MILTON KASTER, CNPSO; WALDIR PEREIRA DIAS, CNPSO; RAFAEL MOREIRA SOARES, CNPSO; ALVARO MANUEL RODRIGUES ALMEIDA, CNPSO; MARCELO FERNANDES DE OLIVEIRA, CNPSO; JOSE UBIRAJARA VIEIRA MOREIRA, CNPSO; LUIZ CARLOS MIRANDA, SNTEEN Londrina; MARCOS RAFAEL PETEK, SNTEEN Londrina; DIVANIA DE LIMA, CNPSO; RODRIGO LUIS BROGIN, CNPSO; RICARDO VILELA ABDELNOOR, CNPSO; CARLOS LASARO PEREIRA DE MELO, CPAO; MARIA DO ROSARIO DE O TEIXEIRA, CPAO; CPAO; PAULO FERNANDO BERTAGNOLLI, CNPT; LEILA MARIA COSTAMILAN, CNPT; MERCEDES CONCORDIA CARRAO PANIZZI, CNPT; VANOLI FRONZA, CNPSO; ODILON LEMOS DE MELLO FILHO, CNPSO; ROBERTO KAZUHIKO ZITO, CNPSO; SEBASTIAO PEDRO DA SILVA NETO, CPAC; CLAUDETE TEIXEIRA MOREIRA, CPAC; MONICA JULIANI ZAVAGLIA PEREIRA, CNPSO. |
Título: |
BRS 361: nova cultivar de soja convencional. |
Ano de publicação: |
2012 |
Fonte/Imprenta: |
In: CONGRESSO BRASILEIRO DE SOJA, 6., 2012, Cuiabá. Soja: integração nacional e desenvolvimento sustentável: anais. Brasília, DF: Embrapa, 2012. |
Descrição Física: |
1 CD-ROM. |
Idioma: |
Português |
Conteúdo: |
A soja é uma das principais culturas do Brasil. Entre os fatores que contribuem para a sustentabilidade do seu cultivo está o uso de cultivares com alta produtividade e estabilidade, além de ciclo e tipo de planta adequados aos diferentes sistemas de produção nas várias regiões produtoras. A cultivar de soja BRS 361, cujas características marcantes são o alto potencial produtivo, ciclo precoce e bom porte, foi desenvolvida pela Embrapa - Empresa Brasileira de Pesquisa Agropecuária, em parceria com a Fundação Meridional de Apoio à Pesquisa Agropecuária. |
Palavras-Chave: |
BRS 361; Cultivar; Soybean. |
Thesagro: |
Soja. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/62378/1/301-s99.pdf
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/62394/1/BRS-361.pdf
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/62428/1/CD403-9.pdf
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Marc: |
LEADER 01914nam a2200481 a 4500 001 1929269 005 2012-08-14 008 2012 bl uuuu u00u1 u #d 100 1 $aCARNEIRO, G. E. de S. 245 $aBRS 361$bnova cultivar de soja convencional. 260 $aIn: CONGRESSO BRASILEIRO DE SOJA, 6., 2012, Cuiabá. Soja: integração nacional e desenvolvimento sustentável: anais. Brasília, DF: Embrapa$c2012 300 $c1 CD-ROM. 520 $aA soja é uma das principais culturas do Brasil. Entre os fatores que contribuem para a sustentabilidade do seu cultivo está o uso de cultivares com alta produtividade e estabilidade, além de ciclo e tipo de planta adequados aos diferentes sistemas de produção nas várias regiões produtoras. A cultivar de soja BRS 361, cujas características marcantes são o alto potencial produtivo, ciclo precoce e bom porte, foi desenvolvida pela Embrapa - Empresa Brasileira de Pesquisa Agropecuária, em parceria com a Fundação Meridional de Apoio à Pesquisa Agropecuária. 650 $aSoja 653 $aBRS 361 653 $aCultivar 653 $aSoybean 700 1 $aPIPOLO, A. E. 700 1 $aGOMIDE, F. B. 700 1 $aARIAS, C. A. A. 700 1 $aKASTER, M. 700 1 $aDIAS, W. P. 700 1 $aSOARES, R. M. 700 1 $aALMEIDA, A. M. R. 700 1 $aOLIVEIRA, M. F. 700 1 $aMOREIRA, J. U. V. 700 1 $aMIRANDA, L. C. 700 1 $aPETEK, M. R. 700 1 $aLIMA, D. 700 1 $aBROGIN, R. L. 700 1 $aABDELNOOR, R. V. 700 1 $aMELO, C. L. P. de 700 1 $aTEIXEIRA, M. R. O. 700 1 $aMARANHO, E. 700 1 $aBERTAGNOLLI, P. F. 700 1 $aCOSTAMILAN, L. M. 700 1 $aCARRÃO-PANIZZI, M. C. 700 1 $aFRONZA, V. 700 1 $aMELLO FILHO, O. L. 700 1 $aZITO, R. K. 700 1 $aSILVA NETO, S. P. 700 1 $aMOREIRA, C. T. 700 1 $aPEREIRA, M. J. Z.
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