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![](/consulta/web/img/deny.png) | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
Registro Completo |
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
16/09/2021 |
Data da última atualização: |
16/09/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
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. |
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. |
Título: |
Umbric Ferralsols along a climosequence from the Atlantic coast to the highlands of northeastern Brazil: characterization and carbon mineralization. |
Ano de publicação: |
2017 |
Fonte/Imprenta: |
Geoderma, v. 293, p. 34-43, May 2017. |
DOI: |
https://doi.org/10.1016/j.geoderma.2017.01.022 |
Idioma: |
Inglês |
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 |
Palavras-Chave: |
Deep carbon; Microbial respiration; Semiárido; Soil nitrogen. |
Thesagro: |
Carbono; Nitrogênio. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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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![](/consulta/web/img/deny.png) | Acesso ao texto completo restrito à biblioteca da Embrapa Arroz e Feijão. Para informações adicionais entre em contato com cnpaf.biblioteca@embrapa.br. |
Registro Completo
Biblioteca(s): |
Embrapa Arroz e Feijão. |
Data corrente: |
29/03/2006 |
Data da última atualização: |
09/10/2008 |
Tipo da produção científica: |
Artigo em Anais de Congresso / Nota Técnica |
Circulação/Nível: |
-- - -- |
Autoria: |
GODOY, S. G. de; LANNA, A. C.; FERRAZ, D. M. M.; ROSA, J. R.; RABELO, V. C.; MOURÃO, V. C.; PALMA, F. R.; GUARDIOLA, M. F.; RAMOS, M. L. G.; HEINEMANN, A. B. MOREIRA, J. A. A.; DIDONET, A. D. |
Título: |
Quantidade e atividade da biomassa microbiana no solo sob cultivo orgânico do feijoeiro comum (Phaseolus vulgaris L.). |
Ano de publicação: |
2005 |
Fonte/Imprenta: |
In: CONGRESSO NACIONAL DE PESQUISA DE FEIJÃO, 8., 2005, Goiânia. Anais... Santo Antônio de Goiás: Embrapa Arroz e Feijão, 2005. |
Volume: |
v. 2. |
Páginas: |
p. 1070-1073. |
Série: |
(Embrapa Arroz e Feijão. Documentos, 182). |
Idioma: |
Português |
Conteúdo: |
Este trabalho teve como objetivo verificar alterações no estoque de carbono da biomassa microbiana e na atividade biológica, medida por meio da respiração basal/quociente metabólico e da atividade enzimática total, do solo sob cultivo do feijoeiro comum em sistema plantio direto e convencional, após um ano de implantação do sistema orgânico. |
Palavras-Chave: |
CONAFE; Orgânico; Sisterma. |
Thesagro: |
Biomassa; Carbono; Feijão; Phaseolus Vulgaris; Solo. |
Categoria do assunto: |
-- |
Marc: |
LEADER 01466naa a2200361 a 4500 001 1207409 005 2008-10-09 008 2005 bl uuuu u00u1 u #d 100 1 $aGODOY, S. G. de 245 $aQuantidade e atividade da biomassa microbiana no solo sob cultivo orgânico do feijoeiro comum (Phaseolus vulgaris L.). 260 $c2005 300 $ap. 1070-1073. v. 2. 490 $a(Embrapa Arroz e Feijão. Documentos, 182).$vv. 2. 520 $aEste trabalho teve como objetivo verificar alterações no estoque de carbono da biomassa microbiana e na atividade biológica, medida por meio da respiração basal/quociente metabólico e da atividade enzimática total, do solo sob cultivo do feijoeiro comum em sistema plantio direto e convencional, após um ano de implantação do sistema orgânico. 650 $aBiomassa 650 $aCarbono 650 $aFeijão 650 $aPhaseolus Vulgaris 650 $aSolo 653 $aCONAFE 653 $aOrgânico 653 $aSisterma 700 1 $aLANNA, A. C. 700 1 $aFERRAZ, D. M. M. 700 1 $aROSA, J. R. 700 1 $aRABELO, V. C. 700 1 $aMOURÃO, V. C. 700 1 $aPALMA, F. R. 700 1 $aGUARDIOLA, M. F. 700 1 $aRAMOS, M. L. G. 700 1 $aHEINEMANN, A. B. MOREIRA, J. A. A. 700 1 $aDIDONET, A. D. 773 $tIn: CONGRESSO NACIONAL DE PESQUISA DE FEIJÃO, 8., 2005, Goiânia. Anais... Santo Antônio de Goiás: Embrapa Arroz e Feijão, 2005.
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