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![](/consulta/web/img/deny.png) | Acesso ao texto completo restrito à biblioteca da Embrapa Arroz e Feijão. Para informações adicionais entre em contato com cnpaf.biblioteca@embrapa.br. |
Registro Completo |
Biblioteca(s): |
Embrapa Arroz e Feijão. |
Data corrente: |
09/08/2011 |
Data da última atualização: |
09/08/2011 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
FAGERIA, N. K.; CARVALHO, G. D.; SANTOS, A. B.; FERREIRA, E. P. de B.; KNUPP, A. M. |
Afiliação: |
NAND KUMAR FAGERIA, CNPAF; GLAUCILENE DUARTE CARVALHO; ALBERTO BAETA DOS SANTOS, CNPAF; ENDERSON PETRONIO DE BRITO FERREIRA, CNPAF; ADRIANO MOREIRA KNUPP, CNPAF. |
Título: |
Chemistry of lowland rice soils and nutrient availability. |
Ano de publicação: |
2011 |
Fonte/Imprenta: |
Communications in Soil Science and Plant Analysis, New York, v. 42, n. 16, p. 1913-1933, 2011. |
Idioma: |
Inglês |
Conteúdo: |
Rice is the staple food crop for about 50% of the world?s population. It is grown mainly under two ecosystems, known as upland and lowland. Lowland rice contributes about 76% of the global rice production. The anaerobic soil environment created by flood irrigation of lowland rice brings several chemical changes in the rice rhizosphere that may influence growth and development and consequently yield. The main changes that occur in flooded or waterlogged rice soils are decreases in oxidation?reduction or redox potential and increases in iron (Fe2+) and manganese (Mn2+) concentrations because of the reductions of Fe3+ to Fe2+ and Mn4+ to Mn2+. The pH of acidic soils increased and alkaline soils decreased because of flooding. Other results are the reduction of nitrate (NO3 −) and nitrogen dioxide (NO2 −) to dinitrogen (N2) and nitrous oxide (N2O); reduction of sulfate (SO4 2−) to sulfide (S2−); reduction of carbon dioxide (CO2) to methane (CH4); improvement in the concentration and availability of phosphorus (P), calcium (Ca), magnesium (Mg), Fe, Mn, molybdenum (Mo), and silicon (Si); and decrease in concentration and availability of zinc (Zn), copper (Cu), and sulfur (S). Uptake of nitrogen (N) may increase if properly managed or applied in the reduced soil layer. The chemical changes occur because of physical reactions between the soil and water and also because of biological activities of anaerobic microorganisms. The magnitude of these chemical changes is determined by soil type, soil organic-matter content, soil fertility, cultivars, and microbial activities. The exclusion of oxygen (O2) from the flooded soils is accompanied by an increase of other gases (CO2, CH4, and H2), produced largely through processes of microbial respiration. The knowledge of the chemistry of lowland rice soils is important for fertility management and maximizing rice yield. This review discusses physical, biological, and chemical changes in flooded or lowland rice soils. MenosRice is the staple food crop for about 50% of the world?s population. It is grown mainly under two ecosystems, known as upland and lowland. Lowland rice contributes about 76% of the global rice production. The anaerobic soil environment created by flood irrigation of lowland rice brings several chemical changes in the rice rhizosphere that may influence growth and development and consequently yield. The main changes that occur in flooded or waterlogged rice soils are decreases in oxidation?reduction or redox potential and increases in iron (Fe2+) and manganese (Mn2+) concentrations because of the reductions of Fe3+ to Fe2+ and Mn4+ to Mn2+. The pH of acidic soils increased and alkaline soils decreased because of flooding. Other results are the reduction of nitrate (NO3 −) and nitrogen dioxide (NO2 −) to dinitrogen (N2) and nitrous oxide (N2O); reduction of sulfate (SO4 2−) to sulfide (S2−); reduction of carbon dioxide (CO2) to methane (CH4); improvement in the concentration and availability of phosphorus (P), calcium (Ca), magnesium (Mg), Fe, Mn, molybdenum (Mo), and silicon (Si); and decrease in concentration and availability of zinc (Zn), copper (Cu), and sulfur (S). Uptake of nitrogen (N) may increase if properly managed or applied in the reduced soil layer. The chemical changes occur because of physical reactions between the soil and water and also because of biological activities of anaerobic microorganisms. The magnitude of these chemical change... Mostrar Tudo |
Palavras-Chave: |
Submerged soil. |
Thesagro: |
Arroz; Desnitrificação; Oryza sativa. |
Thesaurus Nal: |
Denitrification; Redox potential. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02691naa a2200241 a 4500 001 1897588 005 2011-08-09 008 2011 bl uuuu u00u1 u #d 100 1 $aFAGERIA, N. K. 245 $aChemistry of lowland rice soils and nutrient availability. 260 $c2011 520 $aRice is the staple food crop for about 50% of the world?s population. It is grown mainly under two ecosystems, known as upland and lowland. Lowland rice contributes about 76% of the global rice production. The anaerobic soil environment created by flood irrigation of lowland rice brings several chemical changes in the rice rhizosphere that may influence growth and development and consequently yield. The main changes that occur in flooded or waterlogged rice soils are decreases in oxidation?reduction or redox potential and increases in iron (Fe2+) and manganese (Mn2+) concentrations because of the reductions of Fe3+ to Fe2+ and Mn4+ to Mn2+. The pH of acidic soils increased and alkaline soils decreased because of flooding. Other results are the reduction of nitrate (NO3 −) and nitrogen dioxide (NO2 −) to dinitrogen (N2) and nitrous oxide (N2O); reduction of sulfate (SO4 2−) to sulfide (S2−); reduction of carbon dioxide (CO2) to methane (CH4); improvement in the concentration and availability of phosphorus (P), calcium (Ca), magnesium (Mg), Fe, Mn, molybdenum (Mo), and silicon (Si); and decrease in concentration and availability of zinc (Zn), copper (Cu), and sulfur (S). Uptake of nitrogen (N) may increase if properly managed or applied in the reduced soil layer. The chemical changes occur because of physical reactions between the soil and water and also because of biological activities of anaerobic microorganisms. The magnitude of these chemical changes is determined by soil type, soil organic-matter content, soil fertility, cultivars, and microbial activities. The exclusion of oxygen (O2) from the flooded soils is accompanied by an increase of other gases (CO2, CH4, and H2), produced largely through processes of microbial respiration. The knowledge of the chemistry of lowland rice soils is important for fertility management and maximizing rice yield. This review discusses physical, biological, and chemical changes in flooded or lowland rice soils. 650 $aDenitrification 650 $aRedox potential 650 $aArroz 650 $aDesnitrificação 650 $aOryza sativa 653 $aSubmerged soil 700 1 $aCARVALHO, G. D. 700 1 $aSANTOS, A. B. 700 1 $aFERREIRA, E. P. de B. 700 1 $aKNUPP, A. M. 773 $tCommunications in Soil Science and Plant Analysis, New York$gv. 42, n. 16, p. 1913-1933, 2011.
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129. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | GODOY, S. G. de; STONE, L. F.; FERREIRA, E. P. de B.; COBUCCI, T.; LACERDA, M. C. Atributos físicos, químicos e biológicos do solo impactado por cultivos sucessivos de arroz. Revista Brasileira de Engenharia Agrícola e Ambiental, Campina Grande, v. 17, n. 12, p. 1278-1285, dez. 2013.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 2 |
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130. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | CUNHA, E. de Q.; STONE, L. F.; FERREIRA, E. P. de B.; DIDONET, A. D.; MOREIRA, J. A. A. Atributos físicos, químicos e biológicos de solo sob produção orgânica impactados por sistemas de cultivo. Revista Brasileira de Engenharia Agrícola e Ambiental, Campina Grande, v. 16, n. 1, p. 56-63, 2012.Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 1 |
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132. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | RIVERO HERRADA, M.; PLAZA ZAMBRANO, P. M.; GAIBOR FERNANDEZ, R. R.; LEANDRO, W. M.; FERREIRA, E. P. de B. Abonos verdes y su influencia en el crecimiento y rendimiento del frijol (Phaseolus vulgaris L), en condiciones agroecologicas. Biotecnia, v. 18, n. 1, p. 59-64, 2016.Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 5 |
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134. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | GODOY, S. G. de; STONE, L. F.; FERREIRA, E. P. de B.; COBUCCI, T.; LACERDA, M. C. Atributos do solo e a produtividade do arroz no sistema semeadura direta. In: SEMINÁRIO JOVENS TALENTOS, 7., 2013, Santo Antônio de Goiás. Coletânea dos resumos apresentados. Santo Antônio de Goiás: Embrapa Arroz e Feijão, 2013. p. 80. (Embrapa Arroz e Feijão. Documentos, 292). Pôster - pós-graduação.Tipo: Resumo em Anais de Congresso |
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136. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | FERREIRA, E. P. de B.; DUSI, A. N.; COSTA, J. R.; XAVIER, G. R.; RUMJANEK, N. G. Assessing insecticide and fungicide effects on the culturable soil bacterial community by analyses of variance of their DGGE fingerprinting data. European Journal of Soil Biology, New Jersey, v. 45, n. 5/6, p. 466-472, 2009.Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 1 |
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