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Registro Completo |
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Biblioteca(s): |
Embrapa Pecuária Sudeste. |
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Data corrente: |
09/11/1995 |
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Data da última atualização: |
04/05/2023 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
MANZANO, A.; POLLI, H. de; FREIRE, J. C.; SOBRAL, L. F.; SOUZA, M. de; VENTORIN, N.; MELLO, F. de A. F. |
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Afiliação: |
AIRTON MANZANO, CPPSE; HELVÉCIO DE POLLI, USP-ESALQ; JESIEL C. FREIRE, USP-ESALQ; LAFAYETTE F. SOBRAL, USP-ESALQ; MAURICIO DE SOUZA, USP-ESALQ; NELSON VENTORIN, USP-ESALQ; FRANCISCO DE A. F. DE MELLO, USP-ESALQ. |
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Título: |
Fixação de fósforo por um latossolo do estado de Minas Gerais. |
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Ano de publicação: |
1976 |
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Fonte/Imprenta: |
Anais da Escola Superior de Agricultura Luiz de Queiroz, Piracicaba, v. 33, p. 635-645, 1976. |
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Idioma: |
Português |
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Conteúdo: |
Foi estudada absorção do fósforo por amostras de três horizontes, A1, (0-22cm), A3(22-56cm) e B22(155-200cm), de um Latossolo do Estado de Minas Gerais por meio da isoterma de Langmuir. Os valores de adsorção máxima (b) e da constante de seletividade (K) calculados a partir da forma linear da equação de Langmuir foram correlacionados com algumas características físicas e químicas apresentadas pelos citados horizontes. Os resultados encontrados permitiram concluir que: As isotérmicas de adsorção mostram duas regiões distintas: aquela em que o fosfato é fortemente retido foi convenientemente descrita pela equação de Langmuir. Em virtude da diversidade das características físicas e químicas dos horizontes houve grande variação nos valores de adsorção máxima (b) e da constante seletividade (K). |
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Palavras-Chave: |
Fixação. |
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Thesagro: |
Fósforo; Nutrição; Solo. |
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Thesaurus Nal: |
nutrition; soil. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/111266/1/56.pdf
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Marc: |
LEADER 01559naa a2200265 a 4500
001 1042597
005 2023-05-04
008 1976 bl uuuu u00u1 u #d
100 1 $aMANZANO, A.
245 $aFixação de fósforo por um latossolo do estado de Minas Gerais.$h[electronic resource]
260 $c1976
520 $aFoi estudada absorção do fósforo por amostras de três horizontes, A1, (0-22cm), A3(22-56cm) e B22(155-200cm), de um Latossolo do Estado de Minas Gerais por meio da isoterma de Langmuir. Os valores de adsorção máxima (b) e da constante de seletividade (K) calculados a partir da forma linear da equação de Langmuir foram correlacionados com algumas características físicas e químicas apresentadas pelos citados horizontes. Os resultados encontrados permitiram concluir que: As isotérmicas de adsorção mostram duas regiões distintas: aquela em que o fosfato é fortemente retido foi convenientemente descrita pela equação de Langmuir. Em virtude da diversidade das características físicas e químicas dos horizontes houve grande variação nos valores de adsorção máxima (b) e da constante seletividade (K).
650 $anutrition
650 $asoil
650 $aFósforo
650 $aNutrição
650 $aSolo
653 $aFixação
700 1 $aPOLLI, H. de
700 1 $aFREIRE, J. C.
700 1 $aSOBRAL, L. F.
700 1 $aSOUZA, M. de
700 1 $aVENTORIN, N.
700 1 $aMELLO, F. de A. F.
773 $tAnais da Escola Superior de Agricultura Luiz de Queiroz, Piracicaba$gv. 33, p. 635-645, 1976.
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Registro original: |
Embrapa Pecuária Sudeste (CPPSE) |
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Origem |
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Registro Completo
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Biblioteca(s): |
Embrapa Florestas; Embrapa Solos. |
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Data corrente: |
16/05/2017 |
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Data da última atualização: |
30/05/2017 |
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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: |
GOMES, J. B. V.; ARAUJO FILHO, J. C. de; VIDAL-TORRADO, P.; COOPER, M.; SILVA, E. A. da; CURI, N. |
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Afiliação: |
JOAO BOSCO VASCONCELLOS GOMES, CNPF; JOSE COELHO DE ARAUJO FILHO, CNPS; PABLO VIDAL-TORRADO, UNIVERSIDADE DE SÃO PAULO, ESCOLA SUPERIOR DE AGRICULTURA LUIZ DE QUEIROZ; MIGUEL COOPER, UNIVERSIDADE DE SÃO PAULO, ESCOLA SUPERIOR DE AGRICULTURA LUIZ DE QUEIROZ; ELEN ALVARENGA DA SILVA, UNIVERSIDADE FEDERAL DE LAVRAS; NILTON CURI, UNIVERSIDADE FEDERAL DE LAVRAS. |
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Título: |
Cemented horizons and hardpans in the coastal tablelands of Northeastern Brazil. |
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Ano de publicação: |
2017 |
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Fonte/Imprenta: |
Revista Brasileira de Ciência do Solo, Viçosa, v. 41, fev. 2017. |
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DOI: |
10.1590/18069657rbcs20150453 |
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Idioma: |
Inglês |
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Conteúdo: |
Horizons with varying degrees of cementation are a common feature of the soils from the coastal tablelands of Northeastern Brazil. In most cases, these horizons are represented by the following subsurface horizons: fragipan, duripan, ortstein, and placic. The aims of this study were to analyze differences regarding the development and the degree of expression of cementation in soils from the coastal tablelands of Northeastern Brazil: Planossolo Háplico (p-SX), Espodossolo Humilúvico (p-EK), Espodossolo Ferrihumilúvico (p-ESK), and Argissolo Acinzentado (p-PAC) pedons. The pedons studied displayed features related to drainage impediments. The cemented horizons from p-SX and p-EK had the same designation (Btgm), displaying a duric character that coincided with gleization features and are under podzolized horizons. In the p-ESK, the podzolization process is of such magnitude that it leads to the cementation of its own spodic horizons, which were both of the ortstein type (Bhsx and Bsm). In the p-PAC cementation is observed in two placic horizons and in the Btx/Bt horizon, as well as in the upper parts of the Bt/Btx horizon. Analysis of the micrographies from the cemented horizons showed predominance of a low porosity matrix. Such porosity is relatively greater in the horizons of ?x? subscript than in the horizons with duric character. The Fe segregation lines were notable in the cemented horizons from p-EK and p-PAC, which corroborates the presence of placic horizons in such pedons. The preponderance of kaolinite in the clay fraction was widely verified in all the cemented horizons analyzed. Water immersion tests were the criteria adopted to define the duric character of the Btgm horizons from p-SX and p-EK, and in the Bsm horizon from the p-ESK. These tests were also used to confirm field morphology. In most cases, the maximum values of Fe, Al, and Si, determined by different extractions, occurred in positions overlaying the cemented horizons, whether they were spodic or not. The extracts of the aqueous solution displayed a noticeable accumulation of Si in the cemented horizons, except in the p-PAC. The presence of argillans in all cemented horizons allows them to be defined as illuvial, with the exception of the placic horizons, regardless of the presence of podzolization processes. The cemented horizons were preponderantly apedal, with a matrix of little porosity. The Fe, Al, and Si contents extracted by acid ammonium oxalate were effective at highlighting the influence of compounds with a low degree of crystallinity in the morphology of cemented horizons. MenosHorizons with varying degrees of cementation are a common feature of the soils from the coastal tablelands of Northeastern Brazil. In most cases, these horizons are represented by the following subsurface horizons: fragipan, duripan, ortstein, and placic. The aims of this study were to analyze differences regarding the development and the degree of expression of cementation in soils from the coastal tablelands of Northeastern Brazil: Planossolo Háplico (p-SX), Espodossolo Humilúvico (p-EK), Espodossolo Ferrihumilúvico (p-ESK), and Argissolo Acinzentado (p-PAC) pedons. The pedons studied displayed features related to drainage impediments. The cemented horizons from p-SX and p-EK had the same designation (Btgm), displaying a duric character that coincided with gleization features and are under podzolized horizons. In the p-ESK, the podzolization process is of such magnitude that it leads to the cementation of its own spodic horizons, which were both of the ortstein type (Bhsx and Bsm). In the p-PAC cementation is observed in two placic horizons and in the Btx/Bt horizon, as well as in the upper parts of the Bt/Btx horizon. Analysis of the micrographies from the cemented horizons showed predominance of a low porosity matrix. Such porosity is relatively greater in the horizons of ?x? subscript than in the horizons with duric character. The Fe segregation lines were notable in the cemented horizons from p-EK and p-PAC, which corroborates the presence of placic horizons in such pe... Mostrar Tudo |
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Palavras-Chave: |
Duric character; Fragipan; Podzolization. |
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Categoria do assunto: |
--
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/159929/1/A519.pdf
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Marc: |
LEADER 03294naa a2200229 a 4500
001 2069681
005 2017-05-30
008 2017 bl uuuu u00u1 u #d
024 7 $a10.1590/18069657rbcs20150453$2DOI
100 1 $aGOMES, J. B. V.
245 $aCemented horizons and hardpans in the coastal tablelands of Northeastern Brazil.$h[electronic resource]
260 $c2017
520 $aHorizons with varying degrees of cementation are a common feature of the soils from the coastal tablelands of Northeastern Brazil. In most cases, these horizons are represented by the following subsurface horizons: fragipan, duripan, ortstein, and placic. The aims of this study were to analyze differences regarding the development and the degree of expression of cementation in soils from the coastal tablelands of Northeastern Brazil: Planossolo Háplico (p-SX), Espodossolo Humilúvico (p-EK), Espodossolo Ferrihumilúvico (p-ESK), and Argissolo Acinzentado (p-PAC) pedons. The pedons studied displayed features related to drainage impediments. The cemented horizons from p-SX and p-EK had the same designation (Btgm), displaying a duric character that coincided with gleization features and are under podzolized horizons. In the p-ESK, the podzolization process is of such magnitude that it leads to the cementation of its own spodic horizons, which were both of the ortstein type (Bhsx and Bsm). In the p-PAC cementation is observed in two placic horizons and in the Btx/Bt horizon, as well as in the upper parts of the Bt/Btx horizon. Analysis of the micrographies from the cemented horizons showed predominance of a low porosity matrix. Such porosity is relatively greater in the horizons of ?x? subscript than in the horizons with duric character. The Fe segregation lines were notable in the cemented horizons from p-EK and p-PAC, which corroborates the presence of placic horizons in such pedons. The preponderance of kaolinite in the clay fraction was widely verified in all the cemented horizons analyzed. Water immersion tests were the criteria adopted to define the duric character of the Btgm horizons from p-SX and p-EK, and in the Bsm horizon from the p-ESK. These tests were also used to confirm field morphology. In most cases, the maximum values of Fe, Al, and Si, determined by different extractions, occurred in positions overlaying the cemented horizons, whether they were spodic or not. The extracts of the aqueous solution displayed a noticeable accumulation of Si in the cemented horizons, except in the p-PAC. The presence of argillans in all cemented horizons allows them to be defined as illuvial, with the exception of the placic horizons, regardless of the presence of podzolization processes. The cemented horizons were preponderantly apedal, with a matrix of little porosity. The Fe, Al, and Si contents extracted by acid ammonium oxalate were effective at highlighting the influence of compounds with a low degree of crystallinity in the morphology of cemented horizons.
653 $aDuric character
653 $aFragipan
653 $aPodzolization
700 1 $aARAUJO FILHO, J. C. de
700 1 $aVIDAL-TORRADO, P.
700 1 $aCOOPER, M.
700 1 $aSILVA, E. A. da
700 1 $aCURI, N.
773 $tRevista Brasileira de Ciência do Solo, Viçosa$gv. 41, fev. 2017.
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Registro original: |
Embrapa Florestas (CNPF) |
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