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Registro Completo |
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Biblioteca(s): |
Embrapa Agroenergia. |
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Data corrente: |
23/01/2018 |
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Data da última atualização: |
23/01/2018 |
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Tipo da produção científica: |
Artigo em Anais de Congresso |
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Autoria: |
GUIRRA, L. S.; RODRIGUES, A. de A.; CAMPANHA, R. B.; PACHECO, T. F.; SCHULTZ, E. L.; VAZ JUNIOR, S.; DAMASO, M. C. T.; RODRIGUES, C. M. |
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Afiliação: |
LAYANNE S. GUIRRA; ARIANE DE A. RODRIGUES; RAQUEL BOMBARDA CAMPANHA, CNPAE; THALYTA FRAGA PACHECO, CNPAE; EMERSON LEO SCHULTZ, CNPAE; SILVIO VAZ JUNIOR, CNPAE; MONICA CARAMEZ TRICHES DAMASO, CNPAE; CLENILSON MARTINS RODRIGUES, CNPAE. |
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Título: |
Aplicação da extração em fase sólida na eliminação de furano-aldeídos e derivados de ácidos fenólicos do licor do bagaço de cana-de-açúcar. |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
In: ENCONTRO DE PESQUISA E INOVAÇÃO DA EMBRAPA AGROENERGIA, 1., 2014, Brasília, DF. Anais... Brasília, DF : Embrapa Agroenergia, 2014. |
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Páginas: |
p. 84-85. |
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Idioma: |
Português |
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Palavras-Chave: |
Eliminação de derivados de ácidos fenólicos; Eliminação de furano-aldeídos; Licor de bagaço de cana-de-açúcar; Potencial da SPE. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/171546/1/I-ENPI-v2014-Silvio-Vaz-Juniorl.pdf
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Marc: |
LEADER 00950nam a2200241 a 4500
001 2086113
005 2018-01-23
008 2014 bl uuuu u00u1 u #d
100 1 $aGUIRRA, L. S.
245 $aAplicação da extração em fase sólida na eliminação de furano-aldeídos e derivados de ácidos fenólicos do licor do bagaço de cana-de-açúcar.$h[electronic resource]
260 $aIn: ENCONTRO DE PESQUISA E INOVAÇÃO DA EMBRAPA AGROENERGIA, 1., 2014, Brasília, DF. Anais... Brasília, DF : Embrapa Agroenergia$c2014
300 $ap. 84-85.
653 $aEliminação de derivados de ácidos fenólicos
653 $aEliminação de furano-aldeídos
653 $aLicor de bagaço de cana-de-açúcar
653 $aPotencial da SPE
700 1 $aRODRIGUES, A. de A.
700 1 $aCAMPANHA, R. B.
700 1 $aPACHECO, T. F.
700 1 $aSCHULTZ, E. L.
700 1 $aVAZ JUNIOR, S.
700 1 $aDAMASO, M. C. T.
700 1 $aRODRIGUES, C. M.
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Registro original: |
Embrapa Agroenergia (CNPAE) |
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Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
27/11/2017 |
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Data da última atualização: |
10/09/2021 |
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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: |
FONTANA, A.; CHAGAS, C. da S.; DONAGEMMA, G. K.; MENEZES, A. R. de; CALDERANO FILHO, B. |
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Afiliação: |
ADEMIR FONTANA, CNPS; CESAR DA SILVA CHAGAS, CNPS; GUILHERME KANGUSSU DONAGEMMA, CNPS; AMDRESSA ROSAS DE MENEZES, UFRRJ; BRAZ CALDERANO FILHO, CNPS. |
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Título: |
Soils developed on geomorphic surfaces in the mountain region of the State of Rio de Janeiro. |
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Ano de publicação: |
2017 |
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Fonte/Imprenta: |
Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 41, p. 1-17, 2017. |
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DOI: |
10.1590/18069657rbcs20160574 |
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Idioma: |
Inglês |
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Conteúdo: |
The evaluation of soils in representative landscapes constitutes an opportunity to evaluate spatial distribution, discuss formation processes, and apply this knowledge to land use and management. In this sense, from the perspective of an environmentally diversified region, the aim of the present study is to evaluate the occurrence and understand the formation of soils in different geomorphic surfaces of a landscape from a mountain region in the state of Rio de Janeiro. The study was developed in the Pito Aceso microbasin in the municipality of Bom Jardim, composed of narrow valleys and a rugged mountain domain, with elevation between 640 and 1,270 m. In a representative landscape, the geomorphic surfaces were obtained from the slope segments and flow lines. On the geomorphic surfaces, soil profiles were described by their morphological properties, collected, and analyzed to describe the chemical and physical properties of each horizon. Geomorphological aspects and possible variations of the parent material directly affected pedogenesis and led to distinct soil classes in the landscape. Variation in the geomorphic surfaces directs the processes for soil formation under current conditions, as well as the preservation of polygenetic soils. Soils of lower development and with greater participation of the exchangeable cations were identified at the summit (talus deposit) (Neossolo Litólico and Cambissolo Húmico) and toeslope (colluvial-alluvial) (Neossolo Flúvico), whereas more developed soils with lower nutrient content occur in the concave (Argissolos Vermelho and Amarelo) and convex (Latossolo Amarelo) backslope, except for the Argissolo Vermelho-Amarelo in the shoulder, which had high exchangeable cations contents. MenosThe evaluation of soils in representative landscapes constitutes an opportunity to evaluate spatial distribution, discuss formation processes, and apply this knowledge to land use and management. In this sense, from the perspective of an environmentally diversified region, the aim of the present study is to evaluate the occurrence and understand the formation of soils in different geomorphic surfaces of a landscape from a mountain region in the state of Rio de Janeiro. The study was developed in the Pito Aceso microbasin in the municipality of Bom Jardim, composed of narrow valleys and a rugged mountain domain, with elevation between 640 and 1,270 m. In a representative landscape, the geomorphic surfaces were obtained from the slope segments and flow lines. On the geomorphic surfaces, soil profiles were described by their morphological properties, collected, and analyzed to describe the chemical and physical properties of each horizon. Geomorphological aspects and possible variations of the parent material directly affected pedogenesis and led to distinct soil classes in the landscape. Variation in the geomorphic surfaces directs the processes for soil formation under current conditions, as well as the preservation of polygenetic soils. Soils of lower development and with greater participation of the exchangeable cations were identified at the summit (talus deposit) (Neossolo Litólico and Cambissolo Húmico) and toeslope (colluvial-alluvial) (Neossolo Flúvico), whereas more d... Mostrar Tudo |
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Palavras-Chave: |
Classes de solos; Desenvolvimento pedogenético; Relação solo-paisagem. |
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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/167548/1/2017-055.pdf
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Marc: |
LEADER 02463naa a2200217 a 4500
001 2080804
005 2021-09-10
008 2017 bl uuuu u00u1 u #d
024 7 $a10.1590/18069657rbcs20160574$2DOI
100 1 $aFONTANA, A.
245 $aSoils developed on geomorphic surfaces in the mountain region of the State of Rio de Janeiro.$h[electronic resource]
260 $c2017
520 $aThe evaluation of soils in representative landscapes constitutes an opportunity to evaluate spatial distribution, discuss formation processes, and apply this knowledge to land use and management. In this sense, from the perspective of an environmentally diversified region, the aim of the present study is to evaluate the occurrence and understand the formation of soils in different geomorphic surfaces of a landscape from a mountain region in the state of Rio de Janeiro. The study was developed in the Pito Aceso microbasin in the municipality of Bom Jardim, composed of narrow valleys and a rugged mountain domain, with elevation between 640 and 1,270 m. In a representative landscape, the geomorphic surfaces were obtained from the slope segments and flow lines. On the geomorphic surfaces, soil profiles were described by their morphological properties, collected, and analyzed to describe the chemical and physical properties of each horizon. Geomorphological aspects and possible variations of the parent material directly affected pedogenesis and led to distinct soil classes in the landscape. Variation in the geomorphic surfaces directs the processes for soil formation under current conditions, as well as the preservation of polygenetic soils. Soils of lower development and with greater participation of the exchangeable cations were identified at the summit (talus deposit) (Neossolo Litólico and Cambissolo Húmico) and toeslope (colluvial-alluvial) (Neossolo Flúvico), whereas more developed soils with lower nutrient content occur in the concave (Argissolos Vermelho and Amarelo) and convex (Latossolo Amarelo) backslope, except for the Argissolo Vermelho-Amarelo in the shoulder, which had high exchangeable cations contents.
653 $aClasses de solos
653 $aDesenvolvimento pedogenético
653 $aRelação solo-paisagem
700 1 $aCHAGAS, C. da S.
700 1 $aDONAGEMMA, G. K.
700 1 $aMENEZES, A. R. de
700 1 $aCALDERANO FILHO, B.
773 $tRevista Brasileira de Ciência do Solo, Viçosa, MG$gv. 41, p. 1-17, 2017.
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Embrapa Solos (CNPS) |
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