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Registro Completo |
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Biblioteca(s): |
Embrapa Meio-Norte. |
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Data corrente: |
09/04/2008 |
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Data da última atualização: |
03/01/2024 |
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Tipo da produção científica: |
Resumo em Anais de Congresso |
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Autoria: |
CARVALHO, H. W. L. de; CARDOSO, M. J.; CUENCA, M. A. G.; LIRA, M. A.; BRITO, A. R. M. B.; AMIN, S. M. F.; PACHECO, C. A. P.; RODRIGUES, A. R. S. |
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Afiliação: |
HELIO WILSON LEMOS DE CARVALHO, CPATC; MILTON JOSE CARDOSO, CPAMN; MANUEL ALBERTO GUTIERREZ CUENCA, CPATC; MARCELO ABDON LIRA, EMPARN; ANA RITA MORAES BRANDAO BRITO; SANDRA MARIA FERREIRA AMIN, PESQUISADORA EBDA; CLESO ANTONIO PATTO PACHECO, CNPMS; AGNA RITA SANTOS RODRIGUES, BOLSISTA, DTI-G/CNPq/EMBRAPA TABULEIROS COSTEIROS. |
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Título: |
Adaptabilidade e estabilidade de cultivares de milho no Nordeste Brasileiro no ano agrícola de 2005. |
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Ano de publicação: |
2006 |
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Fonte/Imprenta: |
In: CONGRESSO NACIONAL DE MILHO E SORGO, 26.; SIMPÓSIO BRASILEIRO SOBRE A LAGARTA-DO-CARTUCHO, SPODOPTERA FRUGIPERDA, 2.; SIMPÓSIO SOBRE COLLETOTRICHUM GRAMINICOLA, 1., 2006, Belo Horizonte, Inovação para sistemas integrados de produção: resumos. Sete Lagoas: ABMS: Embrapa Milho e Sorgo, 2006. |
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Páginas: |
p. 443. |
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Idioma: |
Português |
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Notas: |
Meta 2007. |
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Palavras-Chave: |
Parâmetro. |
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Thesagro: |
Aclimatação; Interação Genética. |
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Categoria do assunto: |
G Melhoramento Genético |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/69760/1/AdaptabilidadeEstabilidade21819.pdf
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Marc: |
LEADER 00991nam a2200241 a 4500
001 1069760
005 2024-01-03
008 2006 bl uuuu u00u1 u #d
100 1 $aCARVALHO, H. W. L. de
245 $aAdaptabilidade e estabilidade de cultivares de milho no Nordeste Brasileiro no ano agrícola de 2005.$h[electronic resource]
260 $aIn: CONGRESSO NACIONAL DE MILHO E SORGO, 26.; SIMPÓSIO BRASILEIRO SOBRE A LAGARTA-DO-CARTUCHO, SPODOPTERA FRUGIPERDA, 2.; SIMPÓSIO SOBRE COLLETOTRICHUM GRAMINICOLA, 1., 2006, Belo Horizonte, Inovação para sistemas integrados de produção: resumos. Sete Lagoas: ABMS: Embrapa Milho e Sorgo$c2006
300 $ap. 443.
500 $aMeta 2007.
650 $aAclimatação
650 $aInteração Genética
653 $aParâmetro
700 1 $aCARDOSO, M. J.
700 1 $aCUENCA, M. A. G.
700 1 $aLIRA, M. A.
700 1 $aBRITO, A. R. M. B.
700 1 $aAMIN, S. M. F.
700 1 $aPACHECO, C. A. P.
700 1 $aRODRIGUES, A. R. S.
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Embrapa Meio-Norte (CPAMN) |
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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: |
19/02/2021 |
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Data da última atualização: |
03/11/2021 |
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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: |
CÂMARA, E. R. G.; SANTOS, J. C. B. dos; ARAUJO FILHO, J. C. de; SCHULZE, S. M. B. B.; CORRÊA, M. M.; FERREIRA, T. O.; SOUSA, J. E. S. de; SOUZA JÚNIOR, V. S. de. |
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Afiliação: |
ELIS REGINA GUIMARÃES CÂMARA, UFRPE; JEAN CHEYSON BARROS DOS SANTOS, UFRPE; JOSE COELHO DE ARAUJO FILHO, CNPS; SHEILA MARIA BRETAS BITTAR SCHULZE, UFRPE; MARCELO METRI CORRÊA, UFAPE; TIAGO OSÓRIO FERREIRA, ESALQ; JULIET EMÍLIA SANTOS DE SOUSA, UFRPE; VALDOMIRO SEVERINO DE SOUZA JÚNIOR, UFRPE. |
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Título: |
Parent rock-pedogenesis relationship: how the weathering of metamorphic rocks influences the genesis of Planosols and Luvisols under a semiarid climate in NE Brazil. |
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Ano de publicação: |
2021 |
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Fonte/Imprenta: |
Geoderma, v. 385, 114878, Mar. 2021. |
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DOI: |
https://doi.org/10.1016/j.geoderma.2020.114878 |
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Idioma: |
Inglês |
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Conteúdo: |
The expansion of the agricultural frontier in search of new productive regions around the world has raised the attention of the scientific community to the genesis and agricultural potential of soils in regions of the planet where the dry climate limits agricultural activities. In this context, our goal was to describe if there is a direct relationship between the weathering of different metamorphic rocks and the genesis of Luvisols and Planosols in a semiarid region of Brazil, describing the implications of the genesis of these soils for their agricultural potential. For this, two Planosols profiles and three Luvisols profiles were classified, described morphologically and sampled for the development of physical, chemical, mineralogical and micromorphological analyzes. Samples of the respective parent rocks were collected for petrographic analysis and physical and chemical attributes were used in multivariate statistical analysis. The results indicate that: a) weathering of gneiss and amphibolite results in genesis of Planosols and Luvisols respectively, b) hematite was more associated with Luvisols and goethite was more associated with Planossols, and this variation in the content of iron oxides influenced some morphological attributes of these soils, c) clay formation in situ called argillation was the main process responsible for the genesis of Bt horizons in both soils, d) alterations of plagioclases, biotite and amphibole influenced the release of plant nutrients such as Ca+2, Mg+2 and K+ and e) the set of attributes analyzed led us to affirm that Luvisols have a more relevant agricultural potential than Planosols in the semiarid region studied. Our conclusions can be extrapolated to other regions of the world under similar geoclimatic conditions. MenosThe expansion of the agricultural frontier in search of new productive regions around the world has raised the attention of the scientific community to the genesis and agricultural potential of soils in regions of the planet where the dry climate limits agricultural activities. In this context, our goal was to describe if there is a direct relationship between the weathering of different metamorphic rocks and the genesis of Luvisols and Planosols in a semiarid region of Brazil, describing the implications of the genesis of these soils for their agricultural potential. For this, two Planosols profiles and three Luvisols profiles were classified, described morphologically and sampled for the development of physical, chemical, mineralogical and micromorphological analyzes. Samples of the respective parent rocks were collected for petrographic analysis and physical and chemical attributes were used in multivariate statistical analysis. The results indicate that: a) weathering of gneiss and amphibolite results in genesis of Planosols and Luvisols respectively, b) hematite was more associated with Luvisols and goethite was more associated with Planossols, and this variation in the content of iron oxides influenced some morphological attributes of these soils, c) clay formation in situ called argillation was the main process responsible for the genesis of Bt horizons in both soils, d) alterations of plagioclases, biotite and amphibole influenced the release of plant nutrients such ... Mostrar Tudo |
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Palavras-Chave: |
Intemperismo de anfibolito; Intemperismo do gnaisse; Luvissolo; Processo de argumentação; Processo de bissialitização; Processo de rubificação. |
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Thesagro: |
Gênese do Solo; Planossolo. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02853naa a2200313 a 4500
001 2130147
005 2021-11-03
008 2021 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.geoderma.2020.114878$2DOI
100 1 $aCÂMARA, E. R. G.
245 $aParent rock-pedogenesis relationship$bhow the weathering of metamorphic rocks influences the genesis of Planosols and Luvisols under a semiarid climate in NE Brazil.$h[electronic resource]
260 $c2021
520 $aThe expansion of the agricultural frontier in search of new productive regions around the world has raised the attention of the scientific community to the genesis and agricultural potential of soils in regions of the planet where the dry climate limits agricultural activities. In this context, our goal was to describe if there is a direct relationship between the weathering of different metamorphic rocks and the genesis of Luvisols and Planosols in a semiarid region of Brazil, describing the implications of the genesis of these soils for their agricultural potential. For this, two Planosols profiles and three Luvisols profiles were classified, described morphologically and sampled for the development of physical, chemical, mineralogical and micromorphological analyzes. Samples of the respective parent rocks were collected for petrographic analysis and physical and chemical attributes were used in multivariate statistical analysis. The results indicate that: a) weathering of gneiss and amphibolite results in genesis of Planosols and Luvisols respectively, b) hematite was more associated with Luvisols and goethite was more associated with Planossols, and this variation in the content of iron oxides influenced some morphological attributes of these soils, c) clay formation in situ called argillation was the main process responsible for the genesis of Bt horizons in both soils, d) alterations of plagioclases, biotite and amphibole influenced the release of plant nutrients such as Ca+2, Mg+2 and K+ and e) the set of attributes analyzed led us to affirm that Luvisols have a more relevant agricultural potential than Planosols in the semiarid region studied. Our conclusions can be extrapolated to other regions of the world under similar geoclimatic conditions.
650 $aGênese do Solo
650 $aPlanossolo
653 $aIntemperismo de anfibolito
653 $aIntemperismo do gnaisse
653 $aLuvissolo
653 $aProcesso de argumentação
653 $aProcesso de bissialitização
653 $aProcesso de rubificação
700 1 $aSANTOS, J. C. B. dos
700 1 $aARAUJO FILHO, J. C. de
700 1 $aSCHULZE, S. M. B. B.
700 1 $aCORRÊA, M. M.
700 1 $aFERREIRA, T. O.
700 1 $aSOUSA, J. E. S. de
700 1 $aSOUZA JÚNIOR, V. S. de
773 $tGeoderma$gv. 385, 114878, Mar. 2021.
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