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 | Acesso ao texto completo restrito à biblioteca da Embrapa Agrossilvipastoril. Para informações adicionais entre em contato com cpamt.biblioteca@embrapa.br. |
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Registro Completo |
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Biblioteca(s): |
Embrapa Agrossilvipastoril. |
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Data corrente: |
02/12/2021 |
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Data da última atualização: |
02/12/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
FIRMINO, F. H. T.; CAMÊLO, D. de L.; NASCIMENTO, A. F. do; LIMA, J. R. de S.; SOUZA JUNIOR, V.; ALMEIDA, B. G. de; CORRÊA, M. M. |
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Afiliação: |
FRANCIS HENRIQUE TENÓRIO FIRMINO, UFRPE, Recife-PE; DANILO DE LIMA CAMÊLO, UFES, Alegre-ES; ALEXANDRE FERREIRA DO NASCIMENTO, CPAMT; JOSÉ ROMUALDO DE SOUZA LIMA, UFAPE, Garanhuns-PE; VALDOMIRO SOUZA JUNIOR, UFRPE, Recife-PE; BRIVALDO GOMES DE ALMEIDA, UFRPE, Recife-PE; MARCELO METRI CORRÊA, UFAPE, Garanhuns-PE. |
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Título: |
Genesis of lamellae in sandy soils: A case study in a semi-arid region in NE-Brazil. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
Geoderma, v. 406, 115447, 2022. |
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ISSN: |
0016-7061 |
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DOI: |
https://doi.org/10.1016/j.geoderma.2021.115447 |
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Idioma: |
Inglês |
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Conteúdo: |
The occurrence of lamellae in soils and sediments has direct implications for agricultural production, and for stratigraphic and geomorphological studies. Although lamellae have been studied for more than a century, their origin remains controversial. The aim of this study was to identify the origin and formation mechanisms of lamellae in autochthonous soils developed from metamorphic rocks in a semi-arid area of Northeast Brazil. As such, the spatial organization of soil profiles was evaluated in a topolithosequence, through structural analysis of the pedological coverage for subsequent soil sampling. Morphological, chemical, physical, sedimentological, mineralogical, and micromorphological analyses were carried out on the studied slope and in greater detail in four soil profiles. The results indicated that clay particles predominantly smaller than 0.2 µm are eluviated in a sandy soil matrix, infilling voids and coating quartz grains, which are organized in layers of densely packed fine sand, impeding clay translocation and helping form lamellae. Although the micromorphological properties of the lamellae demonstrate their pedogenic origin, the contribution of strips of polycrystalline quartz constitutes a petrogenic component of the illuviation process. Therefore, the genesis of the lamellae is better described based on a petro-pedogenic origin. We suggest a restructuring of the concept of petro-pedogenic origins, including the structural influence of metamorphic rocks, as illuviated clay deposition occurs in accordance with a physical barrier provoked by the increase and organization of fine sand particles, distributed horizontally and in parallel, arising from the disintegration of polycrystalline quartz grains, which indicates geological control in the genesis of lamellae, corresponding to petrogenic evidence. Furthermore, the morphological distinction of the lamellae seems to be more associated with the fine sand content (<0.25 mm), and its packing with larger grains of quartz in the soils. MenosThe occurrence of lamellae in soils and sediments has direct implications for agricultural production, and for stratigraphic and geomorphological studies. Although lamellae have been studied for more than a century, their origin remains controversial. The aim of this study was to identify the origin and formation mechanisms of lamellae in autochthonous soils developed from metamorphic rocks in a semi-arid area of Northeast Brazil. As such, the spatial organization of soil profiles was evaluated in a topolithosequence, through structural analysis of the pedological coverage for subsequent soil sampling. Morphological, chemical, physical, sedimentological, mineralogical, and micromorphological analyses were carried out on the studied slope and in greater detail in four soil profiles. The results indicated that clay particles predominantly smaller than 0.2 µm are eluviated in a sandy soil matrix, infilling voids and coating quartz grains, which are organized in layers of densely packed fine sand, impeding clay translocation and helping form lamellae. Although the micromorphological properties of the lamellae demonstrate their pedogenic origin, the contribution of strips of polycrystalline quartz constitutes a petrogenic component of the illuviation process. Therefore, the genesis of the lamellae is better described based on a petro-pedogenic origin. We suggest a restructuring of the concept of petro-pedogenic origins, including the structural influence of metamorphic rocks, as ... Mostrar Tudo |
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Thesagro: |
Solo Arenoso. |
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Thesaurus Nal: |
Clay; Geomorphology; Infiltration (hydrology); Metamorphic rocks; Quartz; Regosols; Sandy soils; Sediments; Semiarid soils; Semiarid zones; Stratigraphy. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 03044naa a2200361 a 4500
001 2136974
005 2021-12-02
008 2022 bl uuuu u00u1 u #d
022 $a0016-7061
024 7 $ahttps://doi.org/10.1016/j.geoderma.2021.115447$2DOI
100 1 $aFIRMINO, F. H. T.
245 $aGenesis of lamellae in sandy soils$bA case study in a semi-arid region in NE-Brazil.$h[electronic resource]
260 $c2022
520 $aThe occurrence of lamellae in soils and sediments has direct implications for agricultural production, and for stratigraphic and geomorphological studies. Although lamellae have been studied for more than a century, their origin remains controversial. The aim of this study was to identify the origin and formation mechanisms of lamellae in autochthonous soils developed from metamorphic rocks in a semi-arid area of Northeast Brazil. As such, the spatial organization of soil profiles was evaluated in a topolithosequence, through structural analysis of the pedological coverage for subsequent soil sampling. Morphological, chemical, physical, sedimentological, mineralogical, and micromorphological analyses were carried out on the studied slope and in greater detail in four soil profiles. The results indicated that clay particles predominantly smaller than 0.2 µm are eluviated in a sandy soil matrix, infilling voids and coating quartz grains, which are organized in layers of densely packed fine sand, impeding clay translocation and helping form lamellae. Although the micromorphological properties of the lamellae demonstrate their pedogenic origin, the contribution of strips of polycrystalline quartz constitutes a petrogenic component of the illuviation process. Therefore, the genesis of the lamellae is better described based on a petro-pedogenic origin. We suggest a restructuring of the concept of petro-pedogenic origins, including the structural influence of metamorphic rocks, as illuviated clay deposition occurs in accordance with a physical barrier provoked by the increase and organization of fine sand particles, distributed horizontally and in parallel, arising from the disintegration of polycrystalline quartz grains, which indicates geological control in the genesis of lamellae, corresponding to petrogenic evidence. Furthermore, the morphological distinction of the lamellae seems to be more associated with the fine sand content (<0.25 mm), and its packing with larger grains of quartz in the soils.
650 $aClay
650 $aGeomorphology
650 $aInfiltration (hydrology)
650 $aMetamorphic rocks
650 $aQuartz
650 $aRegosols
650 $aSandy soils
650 $aSediments
650 $aSemiarid soils
650 $aSemiarid zones
650 $aStratigraphy
650 $aSolo Arenoso
700 1 $aCAMÊLO, D. de L.
700 1 $aNASCIMENTO, A. F. do
700 1 $aLIMA, J. R. de S.
700 1 $aSOUZA JUNIOR, V.
700 1 $aALMEIDA, B. G. de
700 1 $aCORRÊA, M. M.
773 $tGeoderma$gv. 406, 115447, 2022.
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Registro original: |
Embrapa Agrossilvipastoril (CPAMT) |
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| Registros recuperados : 53 | |
| 21. |  | FIGUEIREDO, R.; CARVALHO, L. M. J.; CORREA, M. M.; SALVADOR, L.; DEL PELOSO, M. J.; CARVALHO, J. L. V. de. Retenção de ferro e zinco em cultivares de feijão comum (Phaseolus vulgaris, L,) após cozimento. In: CONGRESSO BRASILEIRO DE CIÊNCIA E TECNOLOGIA DE ALIMENTOS, 21.; SEMINÁRIO LATINO AMERICANO E DO CARIBE DE CIÊNCIA E TECNOLOGIA DE ALIMENTOS, 15., 2008, Belo Horizonte. Ciência e inovação para o desenvolvimento sustentável. Campinas: SBCTA, 2008.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 22. | | CALDAS, A. M.; ROLIM NETO, F. C.; PARAHYBA, R. da B. V.; CORRÊA, M. M.; RODRIGUES, A. de C. F. Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. Engenharia Agrícola, v. 43, n. 4, e20230147, 2023.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 1 |
| Biblioteca(s): Embrapa Solos. |
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| 24. | | 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.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Agrossilvipastoril. |
|  |
| 25. | | 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.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 2 |
| Biblioteca(s): Embrapa Solos. |
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| 26. | | FIGUEIREDO, R.; CORREA, M. M.; SALVADOR, L.; JAEGER, L. M.; NUTTI, M. R.; CARVALHO, J. L. V.; DEL PELOSO, M. J.; WATANABE, E.; FREITAS, S. C. Assessment of iron and zinc retention in varieties of common beans (Phaseolus vulgaris, L. ) after cooking process. In: WORLD CONGRESS OF FOOD SCIENCE & TECHNOLOGY, 14., 2008, Shanghai, China. Abstracts. Shangai: Chinese Institute of Food Science and Technology, 2008. p. 682.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 28. | | CORREA, M. M.; CARVALHO, L. M. J.; NUTTI, M. R.; CARVALHO, J. L. V.; DEL PELOSO, M. J.; RANGEL, C. N. Hard-shell of common beans (Phaseolus Vulgaris, L.) from seven cultivars before and after home cooking. In: WORLD CONGRESS OF FOOD SCIENCE & TECHNOLOGY, 14., 2008, Shanghai, China. Abstracts. Beijing: Chinese Institute of Food Science and Technology, 2008. p. 693. TS29-2.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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| 29. | | CORREA, M. M.; CARVALHO, L. M. J.; NUTTI, M. R.; CARVALHO, J. L. V.; DEL PELOSO, M. J.; RANGEL, C. N. Hard-shell of common beans (Phaseolus Vulgaris, L.) from seven cultivars before and after home cooking. In: WORLD CONGRESS OF FOOD SCIENCE & TECHNOLOGY, 14., 2008, Shanghai, China. Abstracts. Shangai: Chinese Institute of Food Science and Technology, 2008. p. 693.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 30. | | 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.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Solos. |
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| 31. | | FIRMINO, F. H. T.; CAMÊLO, D. de L.; NASCIMENTO, A. F. do; LIMA, J. R. de S.; SOUZA JUNIOR, V.; ALMEIDA, B. G. de; CORRÊA, M. M. Genesis of lamellae in sandy soils: A case study in a semi-arid region in NE-Brazil. Geoderma, v. 406, 115447, 2022.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
| Biblioteca(s): Embrapa Agrossilvipastoril. |
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| 32. | | MONTEIRO, L. S.; CALDAS, A. M.; ROLIM NETO, F. C.; CORREA, M. M.; PARAHYBA, R. V.; CRUZ, F. M. da; GUERRA, S. M. S. Mineralogia e morfometria da microbacia do Prata no Parque Estadual de Dois Irmãos em Recife-PE. In: JORNADA DE ENSINO, PESQUISA E EXTENSÃO DA UFRPE - JEPEX, 8., 24-31 out. 2008. Recife. Anais... Recife: UFRPE, 2008. 4 p.| Tipo: Artigo em Anais de Congresso / Nota Técnica |
| Biblioteca(s): Embrapa Solos. |
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| 33. | | SANTOS, S. N. dos; ROLIM NETO, F. C.; OLIVEIRA, M. A.; CORRÊA, M. M.; PARAHYBA, R. da B. V.; CALDAS, A. M.; ARRUDA, V. C. M. de. Neglected area of meiobenthos: bibliometric analysis in the status of research on hyporheic meiofauna. Journal of Environmental Analysis and Progress, v. 8, n. 4, p. 252-262, 2023.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 4 |
| Biblioteca(s): Embrapa Solos. |
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| 34. | | CORRÊA, M. M.; BEIRIGO, R. M.; NASCIMENTO, A. F. do; OLIVEIRA JUNIOR, J. C. de; COUTO, E. G.; VIDAL-TORRADO, P. Micromorfologia de Plintossolos do Pantanal-MT. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 34., 2013, Florianópolis. Ciência do solo: para quê e para quem: anais. Viçosa, MG: Sociedade Brasileira de Ciência do Solo, 2013.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Solos. |
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| 35. | | ROLIM NETO, F. C.; SCHAEFER, C. E. G. R.; CAMÊLO, D. de L.; CORRÊA, M. M.; PARAHYBA, R. da B. V.; CALDAS, A. M.; IBRAIMO, A. S. M. Micromorphology and genesis of soils from topolitosequences in the brazilian central plateau. Revista Brasileira de Ciência do Solo, v. 43, e0180219, 2019.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 2 |
| Biblioteca(s): Embrapa Solos. |
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| 36. | | 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.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 1 |
| Biblioteca(s): Embrapa Solos. |
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| 37. | | CORRÊA, M. M.; CARVALHO, L. M. J. de; NUTTI, M. R.; CARVALHO, J. L. V. de; HOHN NETO, A. R.; RIBEIRO, E. M. G. Water absorption, hard shell and cooking time of Common Beans (Phaseolus vulgaris L.). African Journal of Food Science and Technology, v. 1, n. 1, p. 013-020, jul. 2010| Tipo: Artigo em Periódico Indexado | Circulação/Nível: C - 0 |
| Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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| 38. | | ARAUJO FILHO, J. C. de; CORREA, M. M.; PAIVA, A. Q.; COSTA, O. V.; VALLADARES, G. S.; RIBEIRO, M. R.; SCHAEFER, C. E. G. R. Semi-arid soils of the caatinga biome of Northeastern Brazil. In: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 6, p. 175-193. (World soils book series).| Tipo: Capítulo em Livro Técnico-Científico |
| Biblioteca(s): Embrapa Solos. |
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| 39. | | 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. Umbric Ferralsols along a climosequence from the Atlantic coast to the highlands of northeastern Brazil: characterization and carbon mineralization. Geoderma, v. 293, p. 34-43, May 2017.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
| Biblioteca(s): Embrapa Solos. |
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| 40. | | BASTOS, T. X.; SÁ, T. D. de A.; PACHECO, N. A.; CORREA, M. M.; VEIGA, J. A. P.; RIBEIRO, W. M. N. Variabilidade hídrica espacial e temporal na Amazônia e implicações para a cultura do dendê. In: CONGRESSO BRASILEIRO DE AGROMETEOROLOGIA, 10., 1997, Piracicaba. Agrometeorologia, monitoramento ambiental e agricultura sustentável: anais. Piracicaba: SBA: USP: ESALQ, 1997. p. 454-456.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Amazônia Oriental. |
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| Registros recuperados : 53 | |
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| Nenhum registro encontrado para a expressão de busca informada. |
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