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Registro Completo |
Biblioteca(s): |
Embrapa Cerrados. |
Data corrente: |
17/03/2005 |
Data da última atualização: |
17/03/2005 |
Autoria: |
LILIENFEIN, J.; WILCKE, W.; AYARZA, M. A.; VILELA, L.; LIMA, S. do C.; ZECH, W. |
Título: |
Chemical fractionation of phosphorus, sulphur, and molybdenum in Brazilian savannah oxisols under different land use. |
Ano de publicação: |
2000 |
Fonte/Imprenta: |
Geoderma, Amsterdam, v. 96, p. 31-46, 2000. |
Idioma: |
Inglês |
Conteúdo: |
In soils, P. S, and Mo occur organically bound or as oxyanions. In oxisols, oxyanions may be strongly sorbed due to the high positive surface charge. The objective of this work was to compare chemical fractions of P. S. and Mo in differently used Oxisols with similar properties in an on-farm experiment. Soil samples (0-0.15m) were taken from three replicate plots of each of conventional tillage (CT) and no-till (NT) maize-soybean and conventional tillage sugarcane (SC) cropping systems, degraded (DP) and productive pastures (PP), Eucalyptus (EU) and Pinus reforestations (PI), and native savannah (CE). The samples were sequentially extracted with (1) 0.5 M NaHCO3, (2) 0.1 M NaOH, (3) 1 M HCI, (4) hot concentrated HCl, and (5) concentrated HClO4/HNO3. In the extracts, inorganic (Pi) and total P, S, and Mo were determined. Organic P (Po) was calculated as total P-Pi. Total concentrations were 333-567 mg P kg (elevado a -1), 231-284 mg S kg (elevado a -1), and 3.2-3.9 mg Mo kg (elevado a -1). The most important fractions in all studied systems were the NaOH fraction for P (38-49% of total P), the HClO4/HNO3 fraction for S (27-35% of total S) and the concentrated HCl fraction for Mo (86-90% of total Mo). The proportion of the more easily extracted NaHCO3+NaOH fractions decreased along the line S>P>Mo. Fertilisation increased plant-availble P and S fractions in CT and NT whereas recalcitrant fraction (concentrated HCl and HClO4/HNO3) remained unchanged. The Pi/Po ratios in NT and CT were higher than CE because fertiliser P mainly accumulated in inorganic P fractions. The pasture soil had lower P concentrations indicating export by grazing. Thus, 12-20 years of land use had marked effects on P. smaller ones on S. and almost none on Mo concentrations and chemical fractions. MenosIn soils, P. S, and Mo occur organically bound or as oxyanions. In oxisols, oxyanions may be strongly sorbed due to the high positive surface charge. The objective of this work was to compare chemical fractions of P. S. and Mo in differently used Oxisols with similar properties in an on-farm experiment. Soil samples (0-0.15m) were taken from three replicate plots of each of conventional tillage (CT) and no-till (NT) maize-soybean and conventional tillage sugarcane (SC) cropping systems, degraded (DP) and productive pastures (PP), Eucalyptus (EU) and Pinus reforestations (PI), and native savannah (CE). The samples were sequentially extracted with (1) 0.5 M NaHCO3, (2) 0.1 M NaOH, (3) 1 M HCI, (4) hot concentrated HCl, and (5) concentrated HClO4/HNO3. In the extracts, inorganic (Pi) and total P, S, and Mo were determined. Organic P (Po) was calculated as total P-Pi. Total concentrations were 333-567 mg P kg (elevado a -1), 231-284 mg S kg (elevado a -1), and 3.2-3.9 mg Mo kg (elevado a -1). The most important fractions in all studied systems were the NaOH fraction for P (38-49% of total P), the HClO4/HNO3 fraction for S (27-35% of total S) and the concentrated HCl fraction for Mo (86-90% of total Mo). The proportion of the more easily extracted NaHCO3+NaOH fractions decreased along the line S>P>Mo. Fertilisation increased plant-availble P and S fractions in CT and NT whereas recalcitrant fraction (concentrated HCl and HClO4/HNO3) remained unchanged. The Pi/Po ratios in NT and ... Mostrar Tudo |
Thesagro: |
Cerrado; Eucalipto; Reflorestamento. |
Thesaurus Nal: |
Pinus. |
Categoria do assunto: |
-- |
Marc: |
LEADER 02429naa a2200229 a 4500 001 1568612 005 2005-03-17 008 2000 bl uuuu u00u1 u #d 100 1 $aLILIENFEIN, J. 245 $aChemical fractionation of phosphorus, sulphur, and molybdenum in Brazilian savannah oxisols under different land use. 260 $c2000 520 $aIn soils, P. S, and Mo occur organically bound or as oxyanions. In oxisols, oxyanions may be strongly sorbed due to the high positive surface charge. The objective of this work was to compare chemical fractions of P. S. and Mo in differently used Oxisols with similar properties in an on-farm experiment. Soil samples (0-0.15m) were taken from three replicate plots of each of conventional tillage (CT) and no-till (NT) maize-soybean and conventional tillage sugarcane (SC) cropping systems, degraded (DP) and productive pastures (PP), Eucalyptus (EU) and Pinus reforestations (PI), and native savannah (CE). The samples were sequentially extracted with (1) 0.5 M NaHCO3, (2) 0.1 M NaOH, (3) 1 M HCI, (4) hot concentrated HCl, and (5) concentrated HClO4/HNO3. In the extracts, inorganic (Pi) and total P, S, and Mo were determined. Organic P (Po) was calculated as total P-Pi. Total concentrations were 333-567 mg P kg (elevado a -1), 231-284 mg S kg (elevado a -1), and 3.2-3.9 mg Mo kg (elevado a -1). The most important fractions in all studied systems were the NaOH fraction for P (38-49% of total P), the HClO4/HNO3 fraction for S (27-35% of total S) and the concentrated HCl fraction for Mo (86-90% of total Mo). The proportion of the more easily extracted NaHCO3+NaOH fractions decreased along the line S>P>Mo. Fertilisation increased plant-availble P and S fractions in CT and NT whereas recalcitrant fraction (concentrated HCl and HClO4/HNO3) remained unchanged. The Pi/Po ratios in NT and CT were higher than CE because fertiliser P mainly accumulated in inorganic P fractions. The pasture soil had lower P concentrations indicating export by grazing. Thus, 12-20 years of land use had marked effects on P. smaller ones on S. and almost none on Mo concentrations and chemical fractions. 650 $aPinus 650 $aCerrado 650 $aEucalipto 650 $aReflorestamento 700 1 $aWILCKE, W. 700 1 $aAYARZA, M. A. 700 1 $aVILELA, L. 700 1 $aLIMA, S. do C. 700 1 $aZECH, W. 773 $tGeoderma, Amsterdam$gv. 96, p. 31-46, 2000.
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122. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | IKEDA, F. S.; MITJA, D.; VILELA, L.; SOUZA-SILVA, J. C. Banco de sementes em cerrado sensu stricto sob queimada e sistemas de cultivo. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 43, n. 6, p. 667-673, jun. 2008 Título em inglês: Seedbanks in cerrado sensu stricto under burning and cultivation system.Biblioteca(s): Embrapa Unidades Centrais. |
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130. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | VILELA, L.; SOUSA, D. M. G. de; MARTHA JÚNIOR, G. B. Calagem. In: MARTHA JÚNIOR, G. B.; VILELA, L.; SOUSA, D. M. G. de (Ed.). Cerrado: uso eficiente de corretivos e fertilizantes em pastagens. Planaltina, DF: Embrapa Cerrados, 2007. Cap. 4, p. 93-106.Tipo: Capítulo em Livro Técnico-Científico | Circulação/Nível: -- - -- |
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131. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | LILIENFEIN, J.; WILCKE, W.; AYARZA, M. A.; VILELA, L.; LIMA, S. do C.; ZECH, W. Chemical fractionation of phosphorus, sulphur, and molybdenum in Brazilian savannah oxisols under different land use. Geoderma, Amsterdam, v. 96, p. 31-46, 2000.Biblioteca(s): Embrapa Cerrados. |
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132. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | OLIVEIRA, J. R. A.; MENDES, I. de C.; VILELA, L.; VARGAS, M. A. T. Biomassa e atividade microbiana num LE de cerrado sob pastagens, culturas anuais e sistemas integrados de culturas anuais/pastagens. In: CONGRESSO BRASILEIRO DE CIENCIA DO SOLO, 27., 1999, Brasilia, DF. [Ciencia do solo e qualidade de vida: anais]. [Planaltina: Embrapa Cerrados, 1999]. Sessao de posteres 8. Resumo.Biblioteca(s): Embrapa Cerrados. |
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137. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | MARCHÃO, R. L.; BECQUER, T.; BRUNET, D.; BALBINO, L. C.; VILELA, L.; BROSSARD, M. Carbon and nitrogen stocks in a Brazilian clayey Oxisol: 13-year effects of integrated crop-livestock management systems. Soil and Tillage Research, Amsterdam, v. 103, p. 442-450, 2009.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
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