| |
|
|
| Registros recuperados : 65 | |
| 41. |  | 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.| Biblioteca(s): Embrapa Solos. |
|    |
| 42. | | 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.| Biblioteca(s): Embrapa Solos. |
| |
| 43. | | 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.| Biblioteca(s): Embrapa Solos. |
| |
| 44. | | 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. |
| |
| 46. | | 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. |
|  |
| 47. | | 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. |
| |
| 48. | | 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. |
| |
| 49. | | 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. |
| |
| 50. | | 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. |
| |
| 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. |
| |
| 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. |
| |
| 53. | | 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. |
| |
| 54. | | 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. |
| |
| 55. | | 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. |
| |
| 56. | | 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. |
| |
| 57. | | 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. |
| |
| 58. | | 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. |
| |
| 59. | | 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. |
| |
| 60. | | ROLIM NETO, F. C.; SCHAEFER, C. E. G. R.; FERNANDES FILHO, E. I.; CORRÊA, M. M.; COSTA, L. M. da; PARAHYBA, R. da B. V.; GUERRA, S. M. S.; HECK, R. Topolitossequências de solos do Alto Paranaíba: atributos físicos, químicos e mineralógicos. Revista Brasileira de Ciência do solo, v. 33, n. 6, p. 1795-1809, dez. 2009.| Biblioteca(s): Embrapa Solos. |
| |
| Registros recuperados : 65 | |
|
|
|
 | Acesso ao texto completo restrito à biblioteca da Embrapa Agrossilvipastoril. Para informações adicionais entre em contato com cpamt.biblioteca@embrapa.br. |
Registro Completo
|
Biblioteca(s): |
Embrapa Agrossilvipastoril; Embrapa Solos. |
|
Data corrente: |
17/01/2020 |
|
Data da última atualização: |
04/02/2020 |
|
Tipo da produção científica: |
Artigo em Periódico Indexado |
|
Circulação/Nível: |
A - 1 |
|
Autoria: |
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. |
|
Afiliação: |
JULIET EMÍLIA SANTOS DE SOUSA, UFRPE; JEAN CHEYSON BARROS DOS SANTOS, UFRPE; MARCELO METRI CORRÊA, UFRPE; ALEXANDRE FERREIRA DO NASCIMENTO, CPAMT; SHEILA MARIA BRETAS BITTAR SCHULZE, UFRPE; TIAGO OSÓRIO FERREIRA, USP; JOSE COELHO DE ARAUJO FILHO, CNPS; VALDOMIRO SEVERINO DE SOUZA JÚNIOR, UFRPE. |
|
Título: |
Mineralogy and genesis of Planosols under a semi-arid climate, Borborema Plateau, NE Brazil. |
|
Ano de publicação: |
2020 |
|
Fonte/Imprenta: |
Catena, v. 184, 104260, Jan. 2020. |
|
DOI: |
10.1016/j.catena.2019.104260 |
|
Idioma: |
Inglês |
|
Conteúdo: |
Planosols, such as those found on the Borborema Plateau, NE Brazil, form an important class of moderately weathered soils that support subsistence agriculture in underdeveloped regions of Africa, Asia, and South America. Despite its socioeconomic importance, the genesis of this soil class has not yet been fully elucidated. This study was conducted with the aim of improving knowledge about the genesis of Planosols under a semi-arid climate. Three Planosol profiles on the Borborema Plateau in NE Brazil were collected, classified, and described morphologically, and the main physical and chemical attributes, the pedogenetic forms of iron oxides, and the mineralogical compositions of the sand, silt, and clay fractions were determined. The results indicate that: (a) parent materials richer in feldspar and biotite favor the formation of Planosols with a higher clay content; (b) the dissolution of primary minerals and the formation of clay minerals (known as the argillation process) are fundamental for the genesis of Bt horizons; (c) depth-drainage deficiency leads to hydromorphism, an associated gray color, and the formation of mottles; and (d) monosialitization and bisialitization processes (kaolinite formation and the formation of 2:1 clay minerals, respectively) prevail in Planosols located within landscape positions that have good and poor drainage, respectively. In addition, the present study shows that Planosols under a semi-arid climate can have a clay fraction consisting predominantly of kaolinite, and mineralogical alteration pathways similar to those described in soils under an analogous climate and geology in Northwest Africa; this refutes classical theories that soils with 2:1 clay minerals prevail in warmer and drier regions. This study thus provides greater knowledge about the attributes of Planosols in dry and poor regions and can be used as a reference in studies on the sustainable use and management of such soils. MenosPlanosols, such as those found on the Borborema Plateau, NE Brazil, form an important class of moderately weathered soils that support subsistence agriculture in underdeveloped regions of Africa, Asia, and South America. Despite its socioeconomic importance, the genesis of this soil class has not yet been fully elucidated. This study was conducted with the aim of improving knowledge about the genesis of Planosols under a semi-arid climate. Three Planosol profiles on the Borborema Plateau in NE Brazil were collected, classified, and described morphologically, and the main physical and chemical attributes, the pedogenetic forms of iron oxides, and the mineralogical compositions of the sand, silt, and clay fractions were determined. The results indicate that: (a) parent materials richer in feldspar and biotite favor the formation of Planosols with a higher clay content; (b) the dissolution of primary minerals and the formation of clay minerals (known as the argillation process) are fundamental for the genesis of Bt horizons; (c) depth-drainage deficiency leads to hydromorphism, an associated gray color, and the formation of mottles; and (d) monosialitization and bisialitization processes (kaolinite formation and the formation of 2:1 clay minerals, respectively) prevail in Planosols located within landscape positions that have good and poor drainage, respectively. In addition, the present study shows that Planosols under a semi-arid climate can have a clay fraction consisting pr... Mostrar Tudo |
|
Palavras-Chave: |
Caulinita; Esmectita. |
|
Thesagro: |
Argila; Hidrolise; Mineralogia. |
|
Thesaurus NAL: |
Clay; Hydrolysis; Kaolinite; Mineralogy; Smectite. |
|
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
|
Marc: |
LEADER 02893naa a2200337 a 4500
001 2119821
005 2020-02-04
008 2020 bl uuuu u00u1 u #d
024 7 $a10.1016/j.catena.2019.104260$2DOI
100 1 $aSOUSA, J. E. S. de
245 $aMineralogy and genesis of Planosols under a semi-arid climate, Borborema Plateau, NE Brazil.$h[electronic resource]
260 $c2020
520 $aPlanosols, such as those found on the Borborema Plateau, NE Brazil, form an important class of moderately weathered soils that support subsistence agriculture in underdeveloped regions of Africa, Asia, and South America. Despite its socioeconomic importance, the genesis of this soil class has not yet been fully elucidated. This study was conducted with the aim of improving knowledge about the genesis of Planosols under a semi-arid climate. Three Planosol profiles on the Borborema Plateau in NE Brazil were collected, classified, and described morphologically, and the main physical and chemical attributes, the pedogenetic forms of iron oxides, and the mineralogical compositions of the sand, silt, and clay fractions were determined. The results indicate that: (a) parent materials richer in feldspar and biotite favor the formation of Planosols with a higher clay content; (b) the dissolution of primary minerals and the formation of clay minerals (known as the argillation process) are fundamental for the genesis of Bt horizons; (c) depth-drainage deficiency leads to hydromorphism, an associated gray color, and the formation of mottles; and (d) monosialitization and bisialitization processes (kaolinite formation and the formation of 2:1 clay minerals, respectively) prevail in Planosols located within landscape positions that have good and poor drainage, respectively. In addition, the present study shows that Planosols under a semi-arid climate can have a clay fraction consisting predominantly of kaolinite, and mineralogical alteration pathways similar to those described in soils under an analogous climate and geology in Northwest Africa; this refutes classical theories that soils with 2:1 clay minerals prevail in warmer and drier regions. This study thus provides greater knowledge about the attributes of Planosols in dry and poor regions and can be used as a reference in studies on the sustainable use and management of such soils.
650 $aClay
650 $aHydrolysis
650 $aKaolinite
650 $aMineralogy
650 $aSmectite
650 $aArgila
650 $aHidrolise
650 $aMineralogia
653 $aCaulinita
653 $aEsmectita
700 1 $aSANTOS, J. C. B. dos
700 1 $aCORRÊA, M. M.
700 1 $aNASCIMENTO, A. F. do
700 1 $aSCHULZE, S. M. B. B.
700 1 $aFERREIRA, T. O.
700 1 $aARAUJO FILHO, J. C. de
700 1 $aSOUZA JÚNIOR, V. S. de
773 $tCatena$gv. 184, 104260, Jan. 2020.
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Agrossilvipastoril (CPAMT) |
|
|
Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
Fechar
|
| Nenhum registro encontrado para a expressão de busca informada. |
|
|
