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Registro Completo |
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Biblioteca(s): |
Embrapa Recursos Genéticos e Biotecnologia. |
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Data corrente: |
23/03/2011 |
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Data da última atualização: |
23/03/2011 |
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Tipo da produção científica: |
Resumo em Anais de Congresso |
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Autoria: |
SANTOS, V. B.; COSTA, T. S.; MUNDIM, R. C.; SALOMAO, A. N. |
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Afiliação: |
ROSANGELA CALDAS MUNDIM, CENARGEN; ANTONIETA NASSIF SALOMAO, CENARGEN. |
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Título: |
Comportamento de sementes de espécies nativas durante a conservação A ?20ºC. |
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Ano de publicação: |
2010 |
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Fonte/Imprenta: |
In: ENCONTRO DO TALENTO ESTUDANTIL DA EMBRAPA RECURSOS GENÉTICOS E BIOTECNOLOGIA, 15., 2010, Brasília, DF. Anais: resumos dos trabalhos. Brasília, DF: Embrapa Recursos Genéticos e Biotecnologia, 2010. Resumo 102. |
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Páginas: |
p. 149 |
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Idioma: |
Português |
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Palavras-Chave: |
Germinabilidade; Jacaranda caroba; Lafoensia pacari; Magonia pubescens; Peltogyne confertiflora; Plathymenia reticulata; Triplaris gardneriana. |
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Thesagro: |
Apuleia Leiocarpa; Conservação; Cybistax Antisyphilitica; Enterolobium Contortisiliquum; Germoplasma; Myracrodruon Urundeuva. |
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Thesaurus Nal: |
Sterculia striata. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 01102nam a2200313 a 4500
001 1882311
005 2011-03-23
008 2010 bl uuuu u01u1 u #d
100 1 $aSANTOS, V. B.
245 $aComportamento de sementes de espécies nativas durante a conservação A ?20ºC.
260 $aIn: ENCONTRO DO TALENTO ESTUDANTIL DA EMBRAPA RECURSOS GENÉTICOS E BIOTECNOLOGIA, 15., 2010, Brasília, DF. Anais: resumos dos trabalhos. Brasília, DF: Embrapa Recursos Genéticos e Biotecnologia, 2010. Resumo 102.$c2010
300 $ap. 149
650 $aSterculia striata
650 $aApuleia Leiocarpa
650 $aConservação
650 $aCybistax Antisyphilitica
650 $aEnterolobium Contortisiliquum
650 $aGermoplasma
650 $aMyracrodruon Urundeuva
653 $aGerminabilidade
653 $aJacaranda caroba
653 $aLafoensia pacari
653 $aMagonia pubescens
653 $aPeltogyne confertiflora
653 $aPlathymenia reticulata
653 $aTriplaris gardneriana
700 1 $aCOSTA, T. S.
700 1 $aMUNDIM, R. C.
700 1 $aSALOMAO, A. N.
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Registro original: |
Embrapa Recursos Genéticos e Biotecnologia (CENARGEN) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
16/09/2021 |
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Data da última atualização: |
16/09/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
ARAUJO, J. K. S.; SOUZA JÚNIOR, V. S. de; MARQUES, F. A.; VORONEY, P.; SOUZA, R. A. da S.; CORRÊA, M. M.; CÂMARA, E. R. G. |
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Afiliação: |
JANE KELLY SILVA ARAUJO, UFRPE; VALDOMIRO SEVERINO DE SOUZA JÚNIOR, UFRPE; FLAVIO ADRIANO MARQUES, CNPS; PAUL VORONEY, UNIVERSITY OF GUELPH; REGILENE ANGELICA DA SILVA SOUZA, UFRAM; MARCELO METRI CORRÊA, UFRPE; ELIS REGINA GUIMARÃES CÂMARA, UFRPE. |
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Título: |
Umbric Ferralsols along a climosequence from the Atlantic coast to the highlands of northeastern Brazil: characterization and carbon mineralization. |
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Ano de publicação: |
2017 |
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Fonte/Imprenta: |
Geoderma, v. 293, p. 34-43, May 2017. |
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DOI: |
https://doi.org/10.1016/j.geoderma.2017.01.022 |
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Idioma: |
Inglês |
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Conteúdo: |
A thick umbric horizon (~ 1 m) is an important component in the balance of the carbon (C) cycle. However, little is known about the characteristics and C stability in the umbric horizon of Ferralsols, the tropical environments surrounded by semi-arid regions in northeastern (NE) Brazil. This study aimed to evaluate (i) morphological, physical, chemical, biological and mineralogical attributes and (ii) C accumulation in the surface and subsurface within five Umbric Ferralsols along a 475-km climosequence from 143 to 963 m a.s.l. located in coastal and upland areas in NE Brazil. Soil samples were collected in all of the horizons. Umbric Ferralsols present characteristics that are primarily influenced by their sedimentary parent material, which are mostly kaolinitic. The texture ranges from sandy clay loam to very clayey with an absence of macroscopic coal in depth. There is greater C storage of the umbric horizon in the coastal areas with hot and humid climates. This indicates that the current climate is not the predominant factor in the formation of the umbric epipedon. C mineralization in the surface horizons was related to potentially mineralizable nitrogen (N) and labile and organic C, suggesting that the quality of the organic substrate and mainly the N dynamic can drive the accumulation of C. In contrast, C mineralization in subsurface horizons was primarily influenced by forms of aluminum and oxalate-extractable iron and was independent of soil organic matter fractions. However, in the umbric horizon, crystalline forms of iron were mainly associated with protection against C mineralization. MenosA thick umbric horizon (~ 1 m) is an important component in the balance of the carbon (C) cycle. However, little is known about the characteristics and C stability in the umbric horizon of Ferralsols, the tropical environments surrounded by semi-arid regions in northeastern (NE) Brazil. This study aimed to evaluate (i) morphological, physical, chemical, biological and mineralogical attributes and (ii) C accumulation in the surface and subsurface within five Umbric Ferralsols along a 475-km climosequence from 143 to 963 m a.s.l. located in coastal and upland areas in NE Brazil. Soil samples were collected in all of the horizons. Umbric Ferralsols present characteristics that are primarily influenced by their sedimentary parent material, which are mostly kaolinitic. The texture ranges from sandy clay loam to very clayey with an absence of macroscopic coal in depth. There is greater C storage of the umbric horizon in the coastal areas with hot and humid climates. This indicates that the current climate is not the predominant factor in the formation of the umbric epipedon. C mineralization in the surface horizons was related to potentially mineralizable nitrogen (N) and labile and organic C, suggesting that the quality of the organic substrate and mainly the N dynamic can drive the accumulation of C. In contrast, C mineralization in subsurface horizons was primarily influenced by forms of aluminum and oxalate-extractable iron and was independent of soil organic matter fractions.... Mostrar Tudo |
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Palavras-Chave: |
Deep carbon; Microbial respiration; Semiárido; Soil nitrogen. |
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Thesagro: |
Carbono; Nitrogênio. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02499naa a2200277 a 4500
001 2134501
005 2021-09-16
008 2017 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.geoderma.2017.01.022$2DOI
100 1 $aARAUJO, J. K. S.
245 $aUmbric Ferralsols along a climosequence from the Atlantic coast to the highlands of northeastern Brazil$bcharacterization and carbon mineralization.$h[electronic resource]
260 $c2017
520 $aA thick umbric horizon (~ 1 m) is an important component in the balance of the carbon (C) cycle. However, little is known about the characteristics and C stability in the umbric horizon of Ferralsols, the tropical environments surrounded by semi-arid regions in northeastern (NE) Brazil. This study aimed to evaluate (i) morphological, physical, chemical, biological and mineralogical attributes and (ii) C accumulation in the surface and subsurface within five Umbric Ferralsols along a 475-km climosequence from 143 to 963 m a.s.l. located in coastal and upland areas in NE Brazil. Soil samples were collected in all of the horizons. Umbric Ferralsols present characteristics that are primarily influenced by their sedimentary parent material, which are mostly kaolinitic. The texture ranges from sandy clay loam to very clayey with an absence of macroscopic coal in depth. There is greater C storage of the umbric horizon in the coastal areas with hot and humid climates. This indicates that the current climate is not the predominant factor in the formation of the umbric epipedon. C mineralization in the surface horizons was related to potentially mineralizable nitrogen (N) and labile and organic C, suggesting that the quality of the organic substrate and mainly the N dynamic can drive the accumulation of C. In contrast, C mineralization in subsurface horizons was primarily influenced by forms of aluminum and oxalate-extractable iron and was independent of soil organic matter fractions. However, in the umbric horizon, crystalline forms of iron were mainly associated with protection against C mineralization.
650 $aCarbono
650 $aNitrogênio
653 $aDeep carbon
653 $aMicrobial respiration
653 $aSemiárido
653 $aSoil nitrogen
700 1 $aSOUZA JÚNIOR, V. S. de
700 1 $aMARQUES, F. A.
700 1 $aVORONEY, P.
700 1 $aSOUZA, R. A. da S.
700 1 $aCORRÊA, M. M.
700 1 $aCÂMARA, E. R. G.
773 $tGeoderma$gv. 293, p. 34-43, May 2017.
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