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| Registros recuperados : 48 | |
| 5. |  | SCHLINWEIN, J. A.; GIANELLO, C. Calibração de métodos de determinação de fósforo em solos cultivados sob sistema plantio direto. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, n. 5, p. 2037-2049, set./out., 2008. Separata de Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, n. 5, set./out., 2008.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| 10. | | NICOLODI, M.; ANGHINONI, I.; GIANELLO, C. Indicadores da acidez do solo para recomendação de calagem no sistema plantio direto. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, n. 1, p. 237-247, jan./fev. 2008. Separata de Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, n. 1, jan./fev. 2008.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| 11. | | NICOLODI, M.; GIANELLO, C.; BORTOLON, L.; ANGHINONI, I. Adubação dos sistema de cultivo e adubação por cultura, na linha de semeadura, no trigo cultivado em solo com alta fertilidade sob sistema plantio direto. Revista Plantio Direto, Passo Fundo, v. 27, n. 157, p. 6-19, maio/jun. 2017.| Biblioteca(s): Embrapa Pesca e Aquicultura. |
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| 13. | | CAMARGO, F. A. de O.; GIANELLO, C.; VIDOR, C. Distribuição do nitrogênio de fácil e dificil mineralização, da fração labil e recalcitrante, do fluxo inicial e meia vida da mineralização e fração ativa do nitrogênio em solos do Rio Grande do Sul. IN: CONGRESSO BRASILEIRO DE CIÊNÇIA DO SOLO, 25., 1995, Viçosa, MG. Resumos expandidos. Viçosa: UFV, 1995. v.2, p. 710-712.| Biblioteca(s): Embrapa Tabuleiros Costeiros. |
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| 16. | | NICOLODI, M.; GIANELLO, C.; ANGHINONI, I.; MARRÉ, J.; MIELNICZUK, J. Insuficiência do conceito mineralista para expressar a fertilidade do solo percebida pelas plantas cultivadas no sistema plantio direto. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, número especial, p. 2735-2744, nov./dez., 2008. Separata de Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, número especial, nov./dez., 2008.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| Registros recuperados : 48 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Pesca e Aquicultura. |
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Data corrente: |
17/11/2016 |
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Data da última atualização: |
17/11/2016 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 2 |
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Autoria: |
ROGERI, D. A.; GIANELLO, C.; BORTOLON, L.; AMORIM, M. B. |
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Afiliação: |
DOUGLAS ANTONIO ROGERI, INSTITUTO FEDERAL DE SANTA CATARINA; CLESIO GIANELLO, UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL; LEANDRO BORTOLON, CNPASA; MAGNO BATISTA AMORIM, UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL. |
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Título: |
Substitution of clay content for P-Remaining as an index of the phosphorus buffering capacity for soils of Rio Grande do Sul. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 40, 2016 |
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Idioma: |
Inglês |
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Conteúdo: |
Mehlich-1 soil extract is currently used in Rio Grande do Sul (RS) and Santa Catarina (SC) States, in Brazil, to evaluate soil phosphorus available to plants and Mehlich-1 is sensitive to soil buffering capacity. This limitation is overcome partly by soil separation into buffering classes based on soil clay content. However, soil clay content has some technical and operational limitations, such as the underestimation of soil clay levels in soils under no-till. The aim of this study was to evaluate the remaining phosphorus (P-rem) compared to soil clay content as an index of the buffering capacity in soils of RS. The relationship between P-rem and soil clay content was assessed using 200 soil samples from a wide range of locations across the state. In 20 representative soil types, P-rem, soil clay content, P maximum adsorption capacity, total and pedogenic Fe contents, amount of P2O5 needed to increase soil P in 1 mg kg-1 extracted by Mehlich-1 and -3 methods and P capacity factor were determined. Furthermore, a pot experiment was carried out with plants to determine soil P content extracted by Mehlich-1 and -3 at the maximum technical efficiency (MET) and the maximum absorption efficiency (MEA). Correlation analyses were performed between P-rem and soil clay content and, with the attributes of soils involving the P buffering capacity. The relationship between P-rem and soil clay content was described as a decreasing exponential function; however, the adjustment was not adequate to propose critical levels for P-rem. The P-rem index was superior to soil clay index in practically all relationships with the attributes related to the soil buffering capacity of the soils. In some cases, the indexes were similar; however, P-rem was not lower than the soil clay content in any case. The P-rem is a more reliable index to represent soil buffering capacity than the soil clay content in soils from RS, and P-rem might be used to implement soil classes for Mehlich-1 and Mehlich-3 determinations of soil P. MenosMehlich-1 soil extract is currently used in Rio Grande do Sul (RS) and Santa Catarina (SC) States, in Brazil, to evaluate soil phosphorus available to plants and Mehlich-1 is sensitive to soil buffering capacity. This limitation is overcome partly by soil separation into buffering classes based on soil clay content. However, soil clay content has some technical and operational limitations, such as the underestimation of soil clay levels in soils under no-till. The aim of this study was to evaluate the remaining phosphorus (P-rem) compared to soil clay content as an index of the buffering capacity in soils of RS. The relationship between P-rem and soil clay content was assessed using 200 soil samples from a wide range of locations across the state. In 20 representative soil types, P-rem, soil clay content, P maximum adsorption capacity, total and pedogenic Fe contents, amount of P2O5 needed to increase soil P in 1 mg kg-1 extracted by Mehlich-1 and -3 methods and P capacity factor were determined. Furthermore, a pot experiment was carried out with plants to determine soil P content extracted by Mehlich-1 and -3 at the maximum technical efficiency (MET) and the maximum absorption efficiency (MEA). Correlation analyses were performed between P-rem and soil clay content and, with the attributes of soils involving the P buffering capacity. The relationship between P-rem and soil clay content was described as a decreasing exponential function; however, the adjustment was not adequ... Mostrar Tudo |
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Palavras-Chave: |
Rio Grande do Sul. |
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Thesagro: |
Fertilizante fosfatado; Solo. |
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Thesaurus NAL: |
Adsorption; Phosphorus. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/150179/1/CNPASA-2016-rbcs.pdf
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Marc: |
LEADER 02697naa a2200217 a 4500
001 2056565
005 2016-11-17
008 2016 bl uuuu u00u1 u #d
100 1 $aROGERI, D. A.
245 $aSubstitution of clay content for P-Remaining as an index of the phosphorus buffering capacity for soils of Rio Grande do Sul.$h[electronic resource]
260 $c2016
520 $aMehlich-1 soil extract is currently used in Rio Grande do Sul (RS) and Santa Catarina (SC) States, in Brazil, to evaluate soil phosphorus available to plants and Mehlich-1 is sensitive to soil buffering capacity. This limitation is overcome partly by soil separation into buffering classes based on soil clay content. However, soil clay content has some technical and operational limitations, such as the underestimation of soil clay levels in soils under no-till. The aim of this study was to evaluate the remaining phosphorus (P-rem) compared to soil clay content as an index of the buffering capacity in soils of RS. The relationship between P-rem and soil clay content was assessed using 200 soil samples from a wide range of locations across the state. In 20 representative soil types, P-rem, soil clay content, P maximum adsorption capacity, total and pedogenic Fe contents, amount of P2O5 needed to increase soil P in 1 mg kg-1 extracted by Mehlich-1 and -3 methods and P capacity factor were determined. Furthermore, a pot experiment was carried out with plants to determine soil P content extracted by Mehlich-1 and -3 at the maximum technical efficiency (MET) and the maximum absorption efficiency (MEA). Correlation analyses were performed between P-rem and soil clay content and, with the attributes of soils involving the P buffering capacity. The relationship between P-rem and soil clay content was described as a decreasing exponential function; however, the adjustment was not adequate to propose critical levels for P-rem. The P-rem index was superior to soil clay index in practically all relationships with the attributes related to the soil buffering capacity of the soils. In some cases, the indexes were similar; however, P-rem was not lower than the soil clay content in any case. The P-rem is a more reliable index to represent soil buffering capacity than the soil clay content in soils from RS, and P-rem might be used to implement soil classes for Mehlich-1 and Mehlich-3 determinations of soil P.
650 $aAdsorption
650 $aPhosphorus
650 $aFertilizante fosfatado
650 $aSolo
653 $aRio Grande do Sul
700 1 $aGIANELLO, C.
700 1 $aBORTOLON, L.
700 1 $aAMORIM, M. B.
773 $tRevista Brasileira de Ciência do Solo, Viçosa, MG$gv. 40, 2016
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Embrapa Pesca e Aquicultura (CNPASA) |
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