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2. | | BISPO, F. H. A.; SILVA, A. C.; TORRADO, P. V.; SOUZA JÚNIOR, V. S. de. Highlands of the upper Jequitinhonha Valey, Brazil. II - Mineralogy, micromorphology, and landscape evolution. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 35, n. 4, p. 1081-1091, jul./ago. 2011. Título em Português: Chapadas do Alto Vale do Jequitinhonha, MG. II - Mineralogia, micromorfologia e evolução da paisagem. Biblioteca(s): Embrapa Solos / UEP-Recife. |
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3. | | CARVALHO, V. S. de; RIBEIRO, M. R.; SOUZA JÚNIOR, V. S. de; BRILHANTE, S. A. Caracterização de espodossolos dos estados da Paraíba e do Pernambuco, Nordeste do Brasil. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 37, n. 6, p. 1454-1463, jul./ago. 2013. Biblioteca(s): Embrapa Solos / UEP-Recife. |
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5. | | FURQUIM, S. A. C.; ARAUJO FILHO, J. C. de; ALVES, G. B.; SOUZA JUNIOR, V. S. de; OLIVEIRA, F. S. Grau de intemperismo em Vertissolos do Nordeste brasileiro. In: CONGRESSO LATINO-AMERICANO DE CIÊNCIA DO SOLO, 23.; CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 38., 2023, Florianópolis. Anais [...]. Florianópolis: Epagri, 2023. p. 42. Ref. ID 1413. Biblioteca(s): Embrapa Solos. |
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10. | | CÂMARA, E. R. G.; BRILHANTE, S. A.; SOUSA, M. G. F. de; ARAUJO FILHO, J. C. de; LIMA, J. F. W. F.; SOUZA JÚNIOR, V. S. de. Atributos morfológicos de Luvissolo no Núcleo de Desertificação de Cabrobó no Estado de Pernambuco. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 35., 2015, Natal. O solo e suas múltiplas funções: anais. Natal: Sociedade Brasileira de Ciência do Solo, 2015. Biblioteca(s): Embrapa Solos. |
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11. | | SOUSA, H. E. S. de; SOUSA, M. G. F. de; DELARMELINDA, E. A.; SOUZA JÚNIOR, V. S. de; NASCIMENTO, A. F. do; CORRÊA, M. M. Atributos morfológicos de Planossolo sobre a Província da Borborema, Agreste meridional, Pernambuco. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 35., 2015, Natal. O solo e suas múltiplas funções: anais. Natal: Sociedade Brasileira de Ciência do Solo, 2015. Biblioteca(s): Embrapa Agrossilvipastoril. |
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12. | | BARROS, G. M.; SANTOS, J. C. B. dos; SOUZA JÚNIOR, V. S. de; DELARMELINDA, E. A.; ARAUJO FILHO, J. C. de; CÂMARA, E. R. G. Association between parent materials and soil attributes along different geological environments in western Pará, Brazil. Acta Amazonica, v. 48, n. 3, p. 261-270, 2018. Biblioteca(s): Embrapa Solos. |
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14. | | LIMA NETO, J. de A.; RIBEIRO, M. R.; CORRÊA, M. M.; SOUZA-JÚNIOR, V. S. de; ARAUJO FILHO, J. C. de; LIMA, J. F. W. F. Atributos químicos, mineralógicos e micromorfológicos de horizontes coesos de Latossolos e Argissolos dos tabuleiros costeiros do estado de Alagoas. Revista Brasileira de Ciência do Solo, v. 34, n. 2, p. 473-486, abr. 2010. Biblioteca(s): Embrapa Solos. |
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15. | | SILVA, G. A. da; CAMÊLO, D. de L.; CORRÊA, M. M.; SOUZA JÚNIOR, V. S. de; RIBEIRO FILHO, M. R.; ARAUJO FILHO, J. C. de. Pedogenesis on coastal tablelands area with low range altimetry in Paraíba state. Revista Caatinga, v. 32, n. 2, p. 458-471, abr./jun. 2019. Biblioteca(s): Embrapa Solos. |
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16. | | SÁ, E. S. dos S. C. G. de; SOUZA JÚNIOR, V. S. de; SILVA, A. H. N. da; SOUSA, J. E. S. de; ARAUJO FILHO, J. C. de. Pedogenesis in a semi-arid wetland. In: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science: beyond food and fuel: proceedings... Viçosa, MG: SBCS, 2019. v. 2, p. 48. WCSS 2018. Biblioteca(s): Embrapa Solos. |
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17. | | SANTOS, J. C. B. dos; SARTOR, L. R.; AZEVEDO, A. C. de; SOUZA JUNIOR, V. S. de; CORRÊA, M. M.; ARAUJO FILHO, J. C. de. Relação Feldspatos e Quartzo em Neossolos provenientes de Gnaisses: Metodologia experimental por Difratometria de Raios X. In: CONGRESSO BRASILEIRO DE CIÊNCIAS DO SOLO, 34., 2013. Florianópolis. Anais... Viçosa, MG: Sociedade Brasileira de Ciência do Solo, 2013. 4 p. Biblioteca(s): Embrapa Solos. |
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18. | | DELARMELINDA, E. A.; SOUZA JÚNIOR, V. S. de; WADT, P. G. S.; DENG, Y.; CAMPOS, M. C. C.; CÂMARA, E. R. G. Soil-landscape relationship in a chronosequence of the middle madeira river in southwestern Amazon, Brasil Catena, v. 149, p.199-208, 2017 Biblioteca(s): Embrapa Rondônia. |
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19. | | DELARMELINDA, E. A.; SOUZA JÚNIOR, V. S. de; WADT, P. G. S.; DENG, Y.; CAMPOS, M. C. C.; CÂMARA, E. R. G. Soil-landscape relationship in a chronosequence of the middle Madeira River in southwestern Amazon, Brazil. Catena, v. 149, part. 1, p. 199-208, 2017. Biblioteca(s): Embrapa Rondônia. |
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20. | | ARAUJO FILHO, J. C. de; MARQUES, F. A.; AMARAL, A. J. do; CUNHA, T. J. F.; SOUZA JÚNIOR, V. S. de; GALVÃO, P. V. M. Solos do Semiárido: características e estoque de carbono In: GIONGO, V.; ANGELOTTI, F. (ed.). Agricultura de baixa emissão de carbono em regiões semiáridas: experiência brasileira. Brasília, DF: Embrapa, 2022. cap. 6, p. 93-112. Biblioteca(s): Embrapa Semiárido; Embrapa Solos; Embrapa Trigo. |
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Registros recuperados : 35 | |
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Registro Completo
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
19/02/2021 |
Data da última atualização: |
03/11/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
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. |
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. |
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. |
Ano de publicação: |
2021 |
Fonte/Imprenta: |
Geoderma, v. 385, 114878, Mar. 2021. |
DOI: |
https://doi.org/10.1016/j.geoderma.2020.114878 |
Idioma: |
Inglês |
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 |
Palavras-Chave: |
Intemperismo de anfibolito; Intemperismo do gnaisse; Luvissolo; Processo de argumentação; Processo de bissialitização; Processo de rubificação. |
Thesagro: |
Gênese do Solo; Planossolo. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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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