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Registro Completo |
Biblioteca(s): |
Embrapa Agropecuária Oeste. |
Data corrente: |
02/12/2008 |
Data da última atualização: |
13/09/2012 |
Tipo da produção científica: |
Artigo em Anais de Congresso / Nota Técnica |
Autoria: |
RAMOS, M. B. M.; SILVA M. A. da; SANTOS, J. S.; QUITAISKI, E.; ZAMPIVA, W.; TAVARES, G. F.; BORGES, E. L.; SALVIATO, R. A.; SANTOS, E. de J.; NASCIMENTO, L. S.; MARCATO, M. I.; MATTIAZZO, C. B. PADOVAN, M. P. |
Afiliação: |
Marisa Bento Martins Ramos, UFGD; Maria Augusta da Silva, Escola Família Agrícola de Itaquiraí; José Silva Santos, Escola Família Agrícola de Itaquiraí; QUITAISKI, Elias Quitaiski, Escola Família Agrícola de Itaquiraí; , Wagner Zampiva Escola Família Agrí. |
Título: |
A Agroecologia na Escola Família Agrícola de Itaquiraí, em Mato Grosso do Sul. |
Ano de publicação: |
2008 |
Fonte/Imprenta: |
In: SEMINÁRIO DE AGROECOLOGIA DE MATO GROSSO DO SUL, 2., 2008, Dourados. A construção participativa da agroecologia em Mato Grosso do Sul: anais. Dourados: Embrapa Agropecuária Oeste, 2008. |
Descrição Física: |
1 CD-ROM. |
ISBN: |
978-85-7540-019-7 |
Idioma: |
Português |
Notas: |
Organizado por: Alberto Feiden, Milton Parron Padovan, Adalgiza Inês Campolim, Aurélio Vinícius Borsato, Ivo de Sá Motta, João Batista Catto, Tércio Jacques Fehlauer. |
Palavras-Chave: |
Agroecologia. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/66246/1/31208.pdf
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Marc: |
LEADER 01097nam a2200277 a 4500 001 1238778 005 2012-09-13 008 2008 bl uuuu u00u1 u #d 020 $a978-85-7540-019-7 100 1 $aRAMOS, M. B. M. 245 $aA Agroecologia na Escola Família Agrícola de Itaquiraí, em Mato Grosso do Sul. 260 $aIn: SEMINÁRIO DE AGROECOLOGIA DE MATO GROSSO DO SUL, 2., 2008, Dourados. A construção participativa da agroecologia em Mato Grosso do Sul: anais. Dourados: Embrapa Agropecuária Oeste$c2008 300 $c1 CD-ROM. 500 $aOrganizado por: Alberto Feiden, Milton Parron Padovan, Adalgiza Inês Campolim, Aurélio Vinícius Borsato, Ivo de Sá Motta, João Batista Catto, Tércio Jacques Fehlauer. 653 $aAgroecologia 700 1 $aSILVA M. A. da 700 1 $aSANTOS, J. S. 700 1 $aQUITAISKI, E. 700 1 $aZAMPIVA, W. 700 1 $aTAVARES, G. F. 700 1 $aBORGES, E. L. 700 1 $aSALVIATO, R. A. 700 1 $aSANTOS, E. de J. 700 1 $aNASCIMENTO, L. S. 700 1 $aMARCATO, M. I. 700 1 $aMATTIAZZO, C. B. PADOVAN, M. P.
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Registro original: |
Embrapa Agropecuária Oeste (CPAO) |
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Registro Completo
Biblioteca(s): |
Embrapa Gado de Corte. |
Data corrente: |
02/03/2017 |
Data da última atualização: |
02/03/2017 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
B - 1 |
Autoria: |
ALOVISI, A. M. T.; FURTINI NETO, A. E.; SERRA, A. P.; ALOVISI, A. A.; TOKURA, L. K.; LOURENTE, E. R. P.; SILVA, R. S. da; SILVA, C. F. B. da; FERNANDES, J. S. |
Afiliação: |
ALESSANDRA MAYUMI TOKURA ALOVISI, UFGD; ANTONIO EDUARDO FURTINI NETO, UFLA; ADEMAR PEREIRA SERRA, CNPGC; ALVES ALEXANDRE ALOVISI, UFGD; LUCIENE KAZUE TOKURA, Universidade Estadual do Oeste do Paraná; ELAINE REIS PINHEIRO LORUENTE, UFGD; ROBERVALDO SOARES DA SILVA, UFGD; CAMILA FARAH BORGES DA SILVA, UFGD; JUCINEI SOUZA FERNANDES, UFGD. |
Título: |
Phosphorus and silicon fertilizaer rates effects on dynamics of soil phosphorus fractions in oxisol under common bean cultivation. |
Ano de publicação: |
2016 |
Fonte/Imprenta: |
African Journal of Agricultural Research, v. 11, n. 30, p. 2697-2707, July, 2016. |
Idioma: |
Inglês |
Conteúdo: |
The purpose of this research was to evaluate the effects of P and Si fertilizer rates in dynamic of P fractions in clay soil under greenhouse. The research was carried out in a Dystroferric Red Latosol of a very loamy texture from Lavras city, Minas Gerais State, Brazil. The experimental design was entirely randomized, arranged in 4 × 3 factorial design, with four repetitions. The treatments included four inorganic fertilizer P rates (0, 110, 330 and 560 mg dm-3) and three Si rates (0, 110, 330 and 560 mg dm-3). The preview application of Si fertilizer did not contribute to decrease P desorption. Possibly, the silicate has lower affinity with the bound sites of adsorption than phosphates. The effects of inorganic fertilizer P were higher in increasing the moderately labile and labile P inorganic fractions. Among the organic P fractions, the NaHCO3-Po fraction was the only one that contributes to plant nutrition. The Hedley sequential phosphorus fractionation promoted information about different pools where P was accumulated in the soil after common bean cultivation. The highest amount of P was obtained in stable P fraction, followed by moderately labile and labile P fraction. The moderately labile P fraction decreased after common bean cultivation possibly due to the time of P contact in the soil and redistribution to stable P fraction. The labile form was the lowest P pool in soil; nevertheless the increase in fertilizer P rates increases the amount of P content in labile fraction. MenosThe purpose of this research was to evaluate the effects of P and Si fertilizer rates in dynamic of P fractions in clay soil under greenhouse. The research was carried out in a Dystroferric Red Latosol of a very loamy texture from Lavras city, Minas Gerais State, Brazil. The experimental design was entirely randomized, arranged in 4 × 3 factorial design, with four repetitions. The treatments included four inorganic fertilizer P rates (0, 110, 330 and 560 mg dm-3) and three Si rates (0, 110, 330 and 560 mg dm-3). The preview application of Si fertilizer did not contribute to decrease P desorption. Possibly, the silicate has lower affinity with the bound sites of adsorption than phosphates. The effects of inorganic fertilizer P were higher in increasing the moderately labile and labile P inorganic fractions. Among the organic P fractions, the NaHCO3-Po fraction was the only one that contributes to plant nutrition. The Hedley sequential phosphorus fractionation promoted information about different pools where P was accumulated in the soil after common bean cultivation. The highest amount of P was obtained in stable P fraction, followed by moderately labile and labile P fraction. The moderately labile P fraction decreased after common bean cultivation possibly due to the time of P contact in the soil and redistribution to stable P fraction. The labile form was the lowest P pool in soil; nevertheless the increase in fertilizer P rates increases the amount of P content in labile f... Mostrar Tudo |
Palavras-Chave: |
Nutrients interaction. |
Thesagro: |
Phaseolus Vulgaris. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/156823/1/Phosphorus-and-silicon.pdf
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Marc: |
LEADER 02281naa a2200241 a 4500 001 2065716 005 2017-03-02 008 2016 bl uuuu u00u1 u #d 100 1 $aALOVISI, A. M. T. 245 $aPhosphorus and silicon fertilizaer rates effects on dynamics of soil phosphorus fractions in oxisol under common bean cultivation. 260 $c2016 520 $aThe purpose of this research was to evaluate the effects of P and Si fertilizer rates in dynamic of P fractions in clay soil under greenhouse. The research was carried out in a Dystroferric Red Latosol of a very loamy texture from Lavras city, Minas Gerais State, Brazil. The experimental design was entirely randomized, arranged in 4 × 3 factorial design, with four repetitions. The treatments included four inorganic fertilizer P rates (0, 110, 330 and 560 mg dm-3) and three Si rates (0, 110, 330 and 560 mg dm-3). The preview application of Si fertilizer did not contribute to decrease P desorption. Possibly, the silicate has lower affinity with the bound sites of adsorption than phosphates. The effects of inorganic fertilizer P were higher in increasing the moderately labile and labile P inorganic fractions. Among the organic P fractions, the NaHCO3-Po fraction was the only one that contributes to plant nutrition. The Hedley sequential phosphorus fractionation promoted information about different pools where P was accumulated in the soil after common bean cultivation. The highest amount of P was obtained in stable P fraction, followed by moderately labile and labile P fraction. The moderately labile P fraction decreased after common bean cultivation possibly due to the time of P contact in the soil and redistribution to stable P fraction. The labile form was the lowest P pool in soil; nevertheless the increase in fertilizer P rates increases the amount of P content in labile fraction. 650 $aPhaseolus Vulgaris 653 $aNutrients interaction 700 1 $aFURTINI NETO, A. E. 700 1 $aSERRA, A. P. 700 1 $aALOVISI, A. A. 700 1 $aTOKURA, L. K. 700 1 $aLOURENTE, E. R. P. 700 1 $aSILVA, R. S. da 700 1 $aSILVA, C. F. B. da 700 1 $aFERNANDES, J. S. 773 $tAfrican Journal of Agricultural Research$gv. 11, n. 30, p. 2697-2707, July, 2016.
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