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| Registros recuperados : 45.890 | |
| 203. |  | OLIVEIRA, K. B.; NASCIMENTO, G. M.; BRIZOLA, D. C.; OLIVEIRA, T. B. M.; ALMEIDA, A. M. R.; OLIVEIRA, M. C. N. Análise de atividade microbiana do solo em diferentes sistemas de manejo e profundidades pelo método de hidrólise de diacetato de fluoresceína. In: JORNADA ACADÊMICA DA EMBRAPA SOJA, 9., 2014, Londrina. Resumos expandidos... Londrina: Embrapa Soja, 2014. p. 151-157.| Biblioteca(s): Embrapa Soja. |
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| 206. | | MACEDO, R. S.; TEIXEIRA, W. G.; LIMA, H. N.; GUIMARÃES, S. T.; GÓES FILHO, L. C. de; SILVA, F. W. R.; SOUZA, A. C. G. de; ENCINAS, O. C. Classificação de perfis com horizonte A antrópico (terra preta de índio) em áreas de várzea do Rio Solimões, AM. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 32., 2009, Fortaleza. O solo e a produção de bioenergia: perspectivas e desafios : resumos. [Viçosa, MG]: SBCS; Fortaleza: UFC, 2009. p. 495. PT2377.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 211. | | RODRIGUES, D. da C.; ALVES, M. E. dos S.; PALHARINI, W. G.; SANTOS, S. A. dos; MARSCHALL, I. R.; MARQUES, R. F.; CONCENCO, G.; SALTON, J. C.; TOMAZI, M. Composição de plantas daninhas em áreas agrícolas consolidadas em função do preparo do solo. In: JORNADA DE INICIAÇÃO À PESQUISA DA EMBRAPA, 2014, Dourados. Resumos... Brasília, DF: Embrapa, 2014. 1 CD-ROM; JIPE 2014.| Biblioteca(s): Embrapa Agropecuária Oeste. |
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| 213. | | DUPONT, P. B.; LIMA, C. L. R. de; PILLON, C. N.; ABREU, M. D. D.; PINTO M. B.; KUNDE, R. Carbono, nitrogênio e fracionamento granulométrico da matéria orgânica de um argissolo vermelho amarelo sob diferentes manejos da encosta do sudoeste, Turuçu, RS. In: REUNIÃO SUL-BRASILEIRA DE CIÊNCIA DO SOLO, 8., 2010, Santa Maria. A ciência do solo frente à diversidade da agricultura: do saraquá à agricultura de precisão. Santa Maria: Sociedade Brasileira de Ciência do Solo, UFSM, 2010. 1 CD-ROM| Biblioteca(s): Embrapa Clima Temperado. |
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| 218. | | AMARAL, F. C. S. do; CARVALHO JUNIOR, W. de; BHERING, S. B.; CHAGAS, C. da S.; AGLIO, M. L. D. Mapa de Ccasses de terras para irrigação localizada cultura da acerola localizada Projeto Jequitaí - MG. In: AMARAL, F. C. S. do; CARVALHO JUNIOR, W. de; BHERING, S. B.; CHAGAS, C. da S.; ÁGLIO, M. L. D. Classificação das Terras para Irrigação - SiBCTI. Rio de janeiro: Embrapa Solos; Brasília: CODEVASF, 2009. 68 p. 1 p. 1 Mapa color. escala 1: 50.000.| Biblioteca(s): Embrapa Solos. |
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| 219. | | AMARAL, F. C. S. do; CARVALHO JUNIOR, W. de; BHERING, S. B.; CHAGAS, C. da S.; AGLIO, M. L. D. Mapa de Classes de Terras para Irrigação Cultura da Acerola por Aspersão Projeto Jequitaí - MG. In: AMARAL, F. C. S. do; CARVALHO JUNIOR, W. de; BHERING, S. B.; CHAGAS, C. da S.; ÁGLIO, M. L. D. Classificação das Terras para Irrigação - SiBCTI. Rio de janeiro: Embrapa Solos; Brasília: CODEVASF, 2009. 68 p. 1 p. 1 mapa color. escala 1:50.000| Biblioteca(s): Embrapa Solos. |
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| 220. | | AMARAL, F. C. S. do; CARVALHO JUNIOR, W. de; BHERING, S. B.; CHAGAS, C. da S.; AGLIO, M. L. D. Mapa de Classes de Terras para Irrigação Cultura da Acerola por Superfície Projeto Jequitaí - MG In: AMARAL, F. C. S. do; CARVALHO JUNIOR, W. de; BHERING, S. B.; CHAGAS, C. da S.; ÁGLIO, M. L. D. Classificação das Terras para Irrigação - SiBCTI. Rio de janeiro: Embrapa Solos; Brasília: CODEVASF, 2009. 68 p. 1 p. 1 mapa color. escala: 10:950.000.| Biblioteca(s): Embrapa Solos. |
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| Registros recuperados : 45.890 | |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Soja. Para informações adicionais entre em contato com valeria.cardoso@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Soja. |
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Data corrente: |
14/12/2005 |
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Data da última atualização: |
31/08/2017 |
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Autoria: |
BLANCHART, E.; ALBRECHT, A.; BROWN, G.; DECAENS, T.; DUBOISSET, A.; LAVELLE, P.; MARIANI, L.; ROOSE, E. |
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Título: |
Effects of tropical endogeic earthworms on soil erosion. |
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Ano de publicação: |
2004 |
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Fonte/Imprenta: |
Agriculture, Ecosystems & Environment, v. 104, n. 2, p. 303-315, Oct. 2004. |
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Idioma: |
Inglês |
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Notas: |
Nome correto do terceiro autor: BROWN, G. G. |
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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 |
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Thesagro: |
Solo. |
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Categoria do assunto: |
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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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