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Registro Completo |
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
30/01/2023 |
Data da última atualização: |
13/03/2023 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
NEVES, L. V. de M. W.; SOUSA, J. E. S. de; SANTOS, J. C. B. dos; ARAUJO FILHO, J. C. de; CORRÊA, M. M.; SOUSA, M. G.; FRACETTO, F. J. C.; FRACETTO, G. G. M.; ARAUJO, J. K. S.; FREIRE, G. A. P.; FERREIRA, T. O.; SOUZA JÚNIOR, V. S. de. |
Afiliação: |
LAÉRCIO VIEIRA DE MELO WANDERLEY NEVES, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JULIET EMILIA SANTOS DE SOUSA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JEAN CHEYSON BARROS DOS SANTOS, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JOSE COELHO DE ARAUJO FILHO, CNPS; MARCELO METRI CORRÊA, UNIVERSIDADE FEDERAL DO AGRESTE DE PERNAMBUCO; MARILYA GABRYELLA SOUSA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; FELIPE JOSÉ CURY FRACETTO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; GISELLE GOMES MONTEIRO FRACETTO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JANE KELLY SILVA ARAUJO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; GABRIEL ARAÚJO PAES FREIRE, FUNDAÇÃO UNIVERSITÁRIA FEDERAL DE RONDÔNIA; TIAGO OSÓRIO FERREIRA, UNIVERSIDADE DE SÃO PAULO; VALDOMIRO SEVERINO DE SOUZA JÚNIOR, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO. |
Título: |
Weathering of gneiss saprolites and formation of Planosols under semiarid climate (NE Brazil). |
Ano de publicação: |
2023 |
Fonte/Imprenta: |
Journal of South American Earth Sciences, v. 123, 104206, Mar. 2023. |
DOI: |
https://doi.org/10.1016/j.jsames.2023.104206 |
Idioma: |
Inglês |
Conteúdo: |
The Brazilian semiarid is one of the most populous regions in the world. The main income for populations in this region is agricultural production, which in turn is limited by climatic and soil conditions. This region has environmental and economic correlations with underdeveloped regions in northwestern Africa, displaying soil surface with monotonous landscapes of smooth undulating relief with large extensions of Planosols. Climatic conditions that lead to the formation of poorly developed soils and to losses of surface layers make these soils susceptible to degradation. In the Brazilian semiarid, lithology shows that felsic rocks are the main factor in pedogenesis of Planosols, conferring the main physical, chemical, and mineralogical attributes to the soil. In this study, we evaluated the pedogenesis by weathering of gneisses (felsic rocks) in two profiles of Planosols in the Cabrobó Desertification Nucleus, Pernambuco State, northeast Brazil, highlighting the role of the parent material in the soil intrinsic characteristics in the pedogenetic processes. The primary assemblage and pedological features were determined by optical microscopy in thin sections of the A, B, and C horizons from the two soil profiles. The secondary assemblage was identified by X-ray diffractometry using the technique: SEM-scanning electron microscopy. Clay formation in situ, colluvial contribution, and elutriation process contributed to the formation of the gradient textural in both Planosols, with no evidence of argilluviation. For total regolith profile, acidic metamorphic rocks present high structural variability directly influencing the evolution of saprolites, the alteration of primary minerals, and the formation routes of secondary minerals. The secondary assemblage was rather similar and comprised illite, smectite, and kaolinite in both regoliths. The saprolite inclination in P1 favors water movement in relation to P2. The regolith in P1 shows greater mineral alteration with increased pedogenic development. MenosThe Brazilian semiarid is one of the most populous regions in the world. The main income for populations in this region is agricultural production, which in turn is limited by climatic and soil conditions. This region has environmental and economic correlations with underdeveloped regions in northwestern Africa, displaying soil surface with monotonous landscapes of smooth undulating relief with large extensions of Planosols. Climatic conditions that lead to the formation of poorly developed soils and to losses of surface layers make these soils susceptible to degradation. In the Brazilian semiarid, lithology shows that felsic rocks are the main factor in pedogenesis of Planosols, conferring the main physical, chemical, and mineralogical attributes to the soil. In this study, we evaluated the pedogenesis by weathering of gneisses (felsic rocks) in two profiles of Planosols in the Cabrobó Desertification Nucleus, Pernambuco State, northeast Brazil, highlighting the role of the parent material in the soil intrinsic characteristics in the pedogenetic processes. The primary assemblage and pedological features were determined by optical microscopy in thin sections of the A, B, and C horizons from the two soil profiles. The secondary assemblage was identified by X-ray diffractometry using the technique: SEM-scanning electron microscopy. Clay formation in situ, colluvial contribution, and elutriation process contributed to the formation of the gradient textural in both Planosols, wi... Mostrar Tudo |
Palavras-Chave: |
Ilita; K-feldspars; K-feldspato; Perfis de regolito; Plagioclásio; Regolith profile. |
Thesaurus Nal: |
Illite; Plagioclase. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 03117naa a2200361 a 4500 001 2151336 005 2023-03-13 008 2023 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1016/j.jsames.2023.104206$2DOI 100 1 $aNEVES, L. V. de M. W. 245 $aWeathering of gneiss saprolites and formation of Planosols under semiarid climate (NE Brazil).$h[electronic resource] 260 $c2023 520 $aThe Brazilian semiarid is one of the most populous regions in the world. The main income for populations in this region is agricultural production, which in turn is limited by climatic and soil conditions. This region has environmental and economic correlations with underdeveloped regions in northwestern Africa, displaying soil surface with monotonous landscapes of smooth undulating relief with large extensions of Planosols. Climatic conditions that lead to the formation of poorly developed soils and to losses of surface layers make these soils susceptible to degradation. In the Brazilian semiarid, lithology shows that felsic rocks are the main factor in pedogenesis of Planosols, conferring the main physical, chemical, and mineralogical attributes to the soil. In this study, we evaluated the pedogenesis by weathering of gneisses (felsic rocks) in two profiles of Planosols in the Cabrobó Desertification Nucleus, Pernambuco State, northeast Brazil, highlighting the role of the parent material in the soil intrinsic characteristics in the pedogenetic processes. The primary assemblage and pedological features were determined by optical microscopy in thin sections of the A, B, and C horizons from the two soil profiles. The secondary assemblage was identified by X-ray diffractometry using the technique: SEM-scanning electron microscopy. Clay formation in situ, colluvial contribution, and elutriation process contributed to the formation of the gradient textural in both Planosols, with no evidence of argilluviation. For total regolith profile, acidic metamorphic rocks present high structural variability directly influencing the evolution of saprolites, the alteration of primary minerals, and the formation routes of secondary minerals. The secondary assemblage was rather similar and comprised illite, smectite, and kaolinite in both regoliths. The saprolite inclination in P1 favors water movement in relation to P2. The regolith in P1 shows greater mineral alteration with increased pedogenic development. 650 $aIllite 650 $aPlagioclase 653 $aIlita 653 $aK-feldspars 653 $aK-feldspato 653 $aPerfis de regolito 653 $aPlagioclásio 653 $aRegolith profile 700 1 $aSOUSA, J. E. S. de 700 1 $aSANTOS, J. C. B. dos 700 1 $aARAUJO FILHO, J. C. de 700 1 $aCORRÊA, M. M. 700 1 $aSOUSA, M. G. 700 1 $aFRACETTO, F. J. C. 700 1 $aFRACETTO, G. G. M. 700 1 $aARAUJO, J. K. S. 700 1 $aFREIRE, G. A. P. 700 1 $aFERREIRA, T. O. 700 1 $aSOUZA JÚNIOR, V. S. de 773 $tJournal of South American Earth Sciences$gv. 123, 104206, Mar. 2023.
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Registros recuperados : 15 | |
1. | | 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.Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 1 |
Biblioteca(s): Embrapa Solos. |
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3. | | 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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4. | | ARAÚJO, F. H. V.; SANTOS, J. C. B. dos; SANTOS, J. B. dos; SILVA, A. F. da; RAMOS, R. S.; SILVA, R. S. da; SHABANI, F. Spread of Striga asiatica through suitable climatic conditions: risk assessment in new areas producing Zea mays in South America. Journal of Arid Environments, v. 210, 104924, 2023.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 2 |
Biblioteca(s): Embrapa Milho e Sorgo. |
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5. | | SOUSA, M. G.; ARAUJO, J. K. S.; FERREIRA, T. O.; ANDRADE, G. R. P.; ARAUJO FILHO, J. C. de; FRACETTO, G. G. M.; SANTOS, J. C. B.; FRACETTO, F. J. C.; LIMA, G. K.; SOUZA JUNIOR, V. Long-term effects of irrigated agriculture on Luvisol pedogenesis in semi-arid region, northeastern Brazil. Catena, v. 206, 105529, Nov. 2021.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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6. | | SILVA, D. L. de A.; CAMÊLO, D. de L.; ARAUJO FILHO, J. C. de; SANTOS, J. C. B. dos; SOUZA JUNIOR, A. J. de; SOUZA JUNIOR, V.; CORRÊA, M. M. Genesis of clay skins in tropical eutric soils: a case study from NE-Brazil. Catena, v. 202, 105236, Jul. 2021.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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7. | | 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. Parent rock-pedogenesis relationship: how the weathering of metamorphic rocks influences the genesis of Planosols and Luvisols under a semiarid climate in NE Brazil. Geoderma, v. 385, 114878, Mar. 2021.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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8. | | COSTA, E. U. C. da; SANTOS, J. C. B. dos; AZEVEDO, A. C. de; ARAUJO FILHO, J. C. de; CORRÊA, M. M.; NEVES, L. V. de M. W.; VIDAL-TORRADO, P.; SOUZA-JÚNIOR, V. S. de. Mineral alteration and genesis of Al-rich soils derived from conglomerate deposits in Cabo Basin, NE Brazil. Catena, v. 167, p. 198-211, Aug. 2018.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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9. | | SOUSA, J. E. S. de; SANTOS, J. C. B. dos; CORRÊA, M. M.; NASCIMENTO, A. F. do; SCHULZE, S. M. B. B.; FERREIRA, T. O.; ARAUJO FILHO, J. C. de; SOUZA JÚNIOR, V. S. de. Mineralogy and genesis of Planosols under a semi-arid climate, Borborema Plateau, NE Brazil. Catena, v. 184, 104260, Jan. 2020.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Agrossilvipastoril; Embrapa Solos. |
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10. | | NEVES, L. V. de M. W.; FRACETTO, F. J. C.; FRACETTO, G. G. M.; ARAUJO FILHO, J. C. de; ARAUJO, J. K. S.; SANTOS, J. C. B. dos; MENDES JÚNIOR, J. P.; SOUZA JÚNIOR, V. D. de. Microbial abundance and C and N stocks in tropical degraded Planosols from semiarid northeastern Brazil. Catena, v. 196, 104931, Jan. 2021.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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11. | | SOUZA JUNIOR, V. S. de; NEVES, L. V. de M. W.; SANTOS, J. C. B. dos; ARAUJO FILHO, J. C. de; CORREA, M. M.; SILVA, L. F. I. da. Weathering of metamorphic rocks and formation of planosols in semi-arid environment, Brazil. 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. 50-51. WCSS 2018.Tipo: Resumo em Anais de Congresso |
Biblioteca(s): Embrapa Solos. |
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12. | | SOUSA, M. G.; ARAUJO, J. K. S.; FRACETTO, G. G. M.; FERREIRA, T. O.; FRACETTO, F. J. C.; ARAUJO FILHO, J. C. de; OTERO, X. L.; SANTOS, J. C. B. dos; SILVA, A. H. N. da; SOUZA JUNIOR, V. S. de. Changes in organic carbon and microbiology community structure due to long-term irrigated agriculture on Luvisols in the Brazilian semi-arid region. Catena, v. 212, 106058, May 2022.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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13. | | SOUSA, J. E. S. de; ARAUJO, J. K. S.; SILVA, A. H. N. da; SANTOS, J. C. B. dos; FERREIRA, T. O.; ARAUJO FILHO, J. C. de; SOUSA, M. G.; OTERO, X. L.; CORREA, M. M.; CAMARGO, P. B. de; SOUZA JÚNIOR, V. S. de. Carbon stocks in Planosols along a rainfall gradient in Northeast Brazil. Catena, v. 245, 108295, Oct. 2024.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Solos. |
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14. | | NEVES, L. V. de M. W.; SOUSA, J. E. S. de; SANTOS, J. C. B. dos; ARAUJO FILHO, J. C. de; CORRÊA, M. M.; SOUSA, M. G.; FRACETTO, F. J. C.; FRACETTO, G. G. M.; ARAUJO, J. K. S.; FREIRE, G. A. P.; FERREIRA, T. O.; SOUZA JÚNIOR, V. S. de. Weathering of gneiss saprolites and formation of Planosols under semiarid climate (NE Brazil). Journal of South American Earth Sciences, v. 123, 104206, Mar. 2023.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 2 |
Biblioteca(s): Embrapa Solos. |
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15. | | SOUSA, J. E. S. de; ANDRADE, G. R. P.; ARAUJO FILHO, J. C. de; SANTOS, J. C. B. dos; CORRÊA, M. M.; FERREIRA, T. O.; CAMARGO, P. B. de; ARAÚJO, J. K. S.; SILVA, A. H. N. da; SOUSA, M. G.; SOUZA JÚNIOR, V. S. de. Weathering and mineral alteration of metamorphic rocks and genesis of Planosols along a rainfall gradient in Borborema Province, Northeast Brazil. Geoderma Regional, v. 33, e00642, Jun. 2023.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 3 |
Biblioteca(s): Embrapa Solos. |
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Registros recuperados : 15 | |
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