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| Registros recuperados : 65 | |
| 41. |  | 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.| Biblioteca(s): Embrapa Solos. |
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| 42. | | 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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| 43. | | 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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| 44. | | 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).| Biblioteca(s): Embrapa Solos. |
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| 45. | | 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.| Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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| 46. | | 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.| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 47. | | 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.| Biblioteca(s): Embrapa Agrossilvipastoril. |
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| 48. | | 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.| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 49. | | 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.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 50. | | 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.| Biblioteca(s): Embrapa Solos. |
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| 51. | | 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| Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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| 52. | | POSSAS, J. M. C.; CORREA, M. M.; MOURA, G. B. DE A.; LOPES, P. M. O.; CALDAS, A. M.; FONTES JÚNIOR, R. V. DE P. Zoneamento agroclimático para a cultura do pinhão-manso no Estado de Pernambuco. Revista Brasileira de Engenharia Agrícola e Ambiental, v. 16, n. 9, p. 993-998, 2012.| Biblioteca(s): Embrapa Algodão. |
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| 53. | | TAVARES, V. do N.; SILVA, I. J. S. da; ROLIM NETO, F. C.; PARAHYBA, R. da B. V.; MENEZES, R. S. C.; CORREA, M. M.; ARAÚJO, M. do S. B. de. Influência da vinhaça e colheita mecanizada nos aspectos físicos e químicos do solo no Município de Paudalho - PE. Sociedade & Natureza, v. 36, n. 1, e69886, 2024. Também publicado em Inglês: Influence of vinasse application and mechanized harvesting on the physical and chemical characteristics of an Argisol cultivated with sugarcane in NE Brazil.| Biblioteca(s): Embrapa Solos. |
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| 54. | | 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.| Biblioteca(s): Embrapa Agrossilvipastoril; Embrapa Solos. |
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| 55. | | 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.| Biblioteca(s): Embrapa Solos. |
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| 56. | | 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.| Biblioteca(s): Embrapa Solos. |
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| 57. | | SOUZA, R. M. M. de; ROLIN NETO, F. C.; CALDAS, A. M.; MONTEIRO, L. S.; CRUZ, F. M. da; PARAHYBA, R. da B. V.; CORRÊA, M. M.; FIGUEIREDO, A. de C.; SILVA, R. R. da. Mapeamento da declividade da microbacia do prata, em Recife-PE, por SIG. JORNADA DE ENSINO, PESQUISA E EXTENSÃO DA UNIVERSIDADE FEDERAL DE PERNAMBUCO, 7., 2007, Recife. Resumo| Biblioteca(s): Embrapa Solos. |
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| 58. | | COSTA, E. U. C. da; ARAUJO, J. K. S.; NEVES, L. V. de M. W.; ARAUJO FILHO, J. C. de; SOUZA, J. E. S. de; CORRÊA, M. M.; RIBEIRO FILHO, M. R.; SOUZA JÚNIOR, V. S. de. Genesis and classification of Nitisols from volcano-sedimentary lithology in northeastern Brazil. Revista Brasileira de Ciência do Solo, v. 43, article e0180101, 2019.| Biblioteca(s): Embrapa Solos. |
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| 59. | | 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.| Biblioteca(s): Embrapa Solos. |
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| 60. | | FIGUEIREDO, R.; CORREA, M. M.; SALVADOR, L.; CARVALHO, L. M. J.; NUTTI, M. R.; CARVALHO, J. L. V.; DEL PELOSO, M. J.; WATANABE, E.; FREITAS, 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. Beijing: Chinese Institute of Food Science and Technology, 2008. p. 682. TS28-2.| Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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| Registros recuperados : 65 | |
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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: |
02/05/2023 |
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Data da última atualização: |
04/12/2023 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 3 |
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Autoria: |
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. |
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Afiliação: |
JULIET EMILIA SANTOS DE SOUSA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; GABRIEL RAMATIS PUGLIESE ANDRADE, UNIVERSIDADE ESTADUAL DO NORTE FLUMINENSE; JOSE COELHO DE ARAUJO FILHO, CNPS; JEAN CHEYSON BARROS DOS SANTOS, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; MARCELO METRI CORRÊA, UNIVERSIDADE FEDERAL DO AGRESTE DE PERNAMBUCO; TIAGO OSÓRIO FERREIRA, UNIVERSIDADE DE SÃO PAULO; PLÍNIO BARBOSA DE CAMARGO, UNIVERSIDADE DE SÃO PAULO; JANE KELLY SILVA ARAÚJO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; ARTUR HENRIQUE NASCIMENTO DA SILVA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; MARILYA GABRYELLA SOUSA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; VALDOMIRO SEVERINO DE SOUZA JÚNIOR, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO. |
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Título: |
Weathering and mineral alteration of metamorphic rocks and genesis of Planosols along a rainfall gradient in Borborema Province, Northeast Brazil. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
Geoderma Regional, v. 33, e00642, Jun. 2023. |
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DOI: |
https://doi.org/10.1016/j.geodrs.2023.e00642 |
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Idioma: |
Inglês |
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Conteúdo: |
Soils in Northeast Brazil have a correlation with soils in the Northwest Africa, as Planosols are predominant in these regions. However, the weathering and genesis of these soils are little understood, compromising their use and conservation. The present study aimed to investigate weathering and mineralogical changes as well as genesis of Planosols along a pluviometric gradient, considering their formation from gneiss rocks, and analyze climate influence on soil formation. We collected three profiles in different climatic regions of the Brazilian northeastern region and described and classified the samples morphologically. We also performed the physical, chemical, mineralogical, and micromorphological analyses. The results indicated that external material added to soil surface contributed to the formation of surface horizons rich in coarser fractions. Subsurface horizons however were rich in clay (e.g.: P1-2Bn: 433 g kg-1; P2-2B: 427 g kg-1; P3-2Bn1: 429 g kg-1) and were formed from changes of the parent material and the clay formation in situ. Biotite, plagioclases, K-feldspars, and hornblende are the main primary minerals sources for the formation of clay minerals (mainly smectite and kaolinite) from transformation processes and neoformation. Pedoplasmation, monosiallitization, bisiallitization, redoximorphism, and alkalization contributed to the formation of the Planosols studied. Despite incipient soil evolution, the Planosols displayed variation according to the climatic condition. Nevertheless, the incipient mineral alteration favored important soil attributes that could influence agricultural productivity, even in the region with higher precipitation rates. MenosSoils in Northeast Brazil have a correlation with soils in the Northwest Africa, as Planosols are predominant in these regions. However, the weathering and genesis of these soils are little understood, compromising their use and conservation. The present study aimed to investigate weathering and mineralogical changes as well as genesis of Planosols along a pluviometric gradient, considering their formation from gneiss rocks, and analyze climate influence on soil formation. We collected three profiles in different climatic regions of the Brazilian northeastern region and described and classified the samples morphologically. We also performed the physical, chemical, mineralogical, and micromorphological analyses. The results indicated that external material added to soil surface contributed to the formation of surface horizons rich in coarser fractions. Subsurface horizons however were rich in clay (e.g.: P1-2Bn: 433 g kg-1; P2-2B: 427 g kg-1; P3-2Bn1: 429 g kg-1) and were formed from changes of the parent material and the clay formation in situ. Biotite, plagioclases, K-feldspars, and hornblende are the main primary minerals sources for the formation of clay minerals (mainly smectite and kaolinite) from transformation processes and neoformation. Pedoplasmation, monosiallitization, bisiallitization, redoximorphism, and alkalization contributed to the formation of the Planosols studied. Despite incipient soil evolution, the Planosols displayed variation according to the climati... Mostrar Tudo |
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Palavras-Chave: |
Colluviation; Interstratifications. |
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Thesaurus NAL: |
Clay minerals; Sodic soils. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
|
Marc: |
LEADER 02669naa a2200301 a 4500
001 2153467
005 2023-12-04
008 2023 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.geodrs.2023.e00642$2DOI
100 1 $aSOUSA, J. E. S. de
245 $aWeathering and mineral alteration of metamorphic rocks and genesis of Planosols along a rainfall gradient in Borborema Province, Northeast Brazil.$h[electronic resource]
260 $c2023
520 $aSoils in Northeast Brazil have a correlation with soils in the Northwest Africa, as Planosols are predominant in these regions. However, the weathering and genesis of these soils are little understood, compromising their use and conservation. The present study aimed to investigate weathering and mineralogical changes as well as genesis of Planosols along a pluviometric gradient, considering their formation from gneiss rocks, and analyze climate influence on soil formation. We collected three profiles in different climatic regions of the Brazilian northeastern region and described and classified the samples morphologically. We also performed the physical, chemical, mineralogical, and micromorphological analyses. The results indicated that external material added to soil surface contributed to the formation of surface horizons rich in coarser fractions. Subsurface horizons however were rich in clay (e.g.: P1-2Bn: 433 g kg-1; P2-2B: 427 g kg-1; P3-2Bn1: 429 g kg-1) and were formed from changes of the parent material and the clay formation in situ. Biotite, plagioclases, K-feldspars, and hornblende are the main primary minerals sources for the formation of clay minerals (mainly smectite and kaolinite) from transformation processes and neoformation. Pedoplasmation, monosiallitization, bisiallitization, redoximorphism, and alkalization contributed to the formation of the Planosols studied. Despite incipient soil evolution, the Planosols displayed variation according to the climatic condition. Nevertheless, the incipient mineral alteration favored important soil attributes that could influence agricultural productivity, even in the region with higher precipitation rates.
650 $aClay minerals
650 $aSodic soils
653 $aColluviation
653 $aInterstratifications
700 1 $aANDRADE, G. R. P.
700 1 $aARAUJO FILHO, J. C. de
700 1 $aSANTOS, J. C. B. dos
700 1 $aCORRÊA, M. M.
700 1 $aFERREIRA, T. O.
700 1 $aCAMARGO, P. B. de
700 1 $aARAÚJO, J. K. S.
700 1 $aSILVA, A. H. N. da
700 1 $aSOUSA, M. G.
700 1 $aSOUZA JÚNIOR, V. S. de
773 $tGeoderma Regional$gv. 33, e00642, Jun. 2023.
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