|
Registro Completo |
|
Biblioteca(s): |
Embrapa Solos. |
|
Data corrente: |
07/06/2011 |
|
Data da última atualização: |
03/11/2021 |
|
Tipo da produção científica: |
Artigo em Periódico Indexado |
|
Autoria: |
TEIXEIRA, S. C. G.; ZIOLLI, R. L.; MARQUES, M. R. da C.; PEREZ, D. V. |
|
Afiliação: |
Sílvio Cesár Godinho Teixeira, UERJ; Roberta Lourenço Ziolli, PUC-RJ; Monica Regina da Costa Marques, UERJ; DANIEL VIDAL PEREZ, CNPS. |
|
Título: |
Study of pyrene adsorption on two brazilian soils. |
|
Ano de publicação: |
2011 |
|
Fonte/Imprenta: |
Water, Air & Soil Pollution, v. 219, p. 297-301, 2011. |
|
DOI: |
https://doi.org/10.1007/s11270-010-0707-3 |
|
Idioma: |
Inglês |
|
Conteúdo: |
This study investigated pyrene adsorption on two contrasting Brazilian soils: a Kandiudult and a Vertisol. It was found that the time taken to reach thermodynamic equilibrium depended on the soil type. The curves for different pyrene-to-soil mass ratios for Vertisol soil showed significant differences. This is probably related to the presence of 2:1 clays that may increase the adsorption of pyrene due to the resulting interlamellar space. The adsorption of pyrene on the Kandiudult showed, in general, good agreement with the Langmuir isotherm. In the case of the Vertisol, there was good agreement with the linear isotherm. The kinetic model that best explains the adsorption in Kandiudult was the pseudo second-order model. For the Vertisol, the Morris Weber model best explains the behavior of pyrene. |
|
Palavras-Chave: |
Kinetic. |
|
Thesaurus Nal: |
adsorption; hydrocarbons. |
|
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
|
Marc: |
LEADER 01403naa a2200205 a 4500
001 1890871
005 2021-11-03
008 2011 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1007/s11270-010-0707-3$2DOI
100 1 $aTEIXEIRA, S. C. G.
245 $aStudy of pyrene adsorption on two brazilian soils.$h[electronic resource]
260 $c2011
520 $aThis study investigated pyrene adsorption on two contrasting Brazilian soils: a Kandiudult and a Vertisol. It was found that the time taken to reach thermodynamic equilibrium depended on the soil type. The curves for different pyrene-to-soil mass ratios for Vertisol soil showed significant differences. This is probably related to the presence of 2:1 clays that may increase the adsorption of pyrene due to the resulting interlamellar space. The adsorption of pyrene on the Kandiudult showed, in general, good agreement with the Langmuir isotherm. In the case of the Vertisol, there was good agreement with the linear isotherm. The kinetic model that best explains the adsorption in Kandiudult was the pseudo second-order model. For the Vertisol, the Morris Weber model best explains the behavior of pyrene.
650 $aadsorption
650 $ahydrocarbons
653 $aKinetic
700 1 $aZIOLLI, R. L.
700 1 $aMARQUES, M. R. da C.
700 1 $aPEREZ, D. V.
773 $tWater, Air & Soil Pollution$gv. 219, p. 297-301, 2011.
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Solos (CNPS) |
|
