| |
|
|
 | Acesso ao texto completo restrito à biblioteca da Embrapa Rondônia. Para informações adicionais entre em contato com cpafro.biblioteca@embrapa.br. |
|
Registro Completo |
|
Biblioteca(s): |
Embrapa Rondônia. |
|
Data corrente: |
12/03/2018 |
|
Data da última atualização: |
07/03/2022 |
|
Tipo da produção científica: |
Artigo em Periódico Indexado |
|
Autoria: |
DELARMELINDA, E. A.; SOUZA JÚNIOR, V. S. de; WADT, P. G. S.; DENG, Y.; CAMPOS, M. C. C.; CÂMARA, E. R. G. |
|
Afiliação: |
Elaine Almeida Delarmelinda, Universidade Federal Rural de Pernambuco; Valdomiro Severino de Souza Júnior, Universidade Federal Rural de Pernambuco; PAULO GUILHERME SALVADOR WADT, CPAF-Rondonia; Youjun Deng, Texas A&M University; Milton César Costa Campos, Universidade Federal do Amazonas; Elis Regina Guimarães Câmara, Universidade Federal Rural de Pernambuco. |
|
Título: |
Soil-landscape relationship in a chronosequence of the middle Madeira River in southwestern Amazon, Brazil. |
|
Ano de publicação: |
2017 |
|
Fonte/Imprenta: |
Catena, v. 149, part. 1, p. 199-208, 2017. |
|
Idioma: |
Inglês |
|
Conteúdo: |
High temperatures and rainfall prevail in the Brazilian Amazon, but some areas have soils with high clay mineral contents of 2:1, and there is limited information concerning their properties. Therefore, it is important to study the soil formation and understand the environmental conditions in which they were formed. This study aimed to investigate the physical, chemical and mineralogical properties of the soil in relation to the environmental factors acting on a chronosequence in the Late Pleistocene sediments of the Middle Madeira River. Soil profiles were selected on three alluvial terraces. Morphological, physical, chemical, mineralogical, X-ray fluorescence, TEM and SEM characterizations were performed. The soils that exhibited a clayey texture, acidic reaction, low values of exchangeable bases and high values of aluminum had profiles containing a considerable presence of 2:1 clay minerals, especially illite, vermiculite, mica-vermiculite, hydroxyl-interlayered vermiculite and pyrophyllite. Soil mineralogy indicated that these soils were recently weathered, where the low values of sum of bases correspond to the low presence of these cations in the parent material. Meanwhile, high values of exchangeable aluminum were derived from the pyrophyllite alteration, different parent material and 2:1 clay minerals recent alteration. Therefore, the parent material, presence of amorphous silica, different climate conditions in the past and current drainage restriction contribute to the slow alteration rate of 2:1 clay minerals of the soils of the humid tropical Amazon environment MenosHigh temperatures and rainfall prevail in the Brazilian Amazon, but some areas have soils with high clay mineral contents of 2:1, and there is limited information concerning their properties. Therefore, it is important to study the soil formation and understand the environmental conditions in which they were formed. This study aimed to investigate the physical, chemical and mineralogical properties of the soil in relation to the environmental factors acting on a chronosequence in the Late Pleistocene sediments of the Middle Madeira River. Soil profiles were selected on three alluvial terraces. Morphological, physical, chemical, mineralogical, X-ray fluorescence, TEM and SEM characterizations were performed. The soils that exhibited a clayey texture, acidic reaction, low values of exchangeable bases and high values of aluminum had profiles containing a considerable presence of 2:1 clay minerals, especially illite, vermiculite, mica-vermiculite, hydroxyl-interlayered vermiculite and pyrophyllite. Soil mineralogy indicated that these soils were recently weathered, where the low values of sum of bases correspond to the low presence of these cations in the parent material. Meanwhile, high values of exchangeable aluminum were derived from the pyrophyllite alteration, different parent material and 2:1 clay minerals recent alteration. Therefore, the parent material, presence of amorphous silica, different climate conditions in the past and current drainage restriction contribute to ... Mostrar Tudo |
|
Palavras-Chave: |
Alluvial terrace; Minerais de argila; Pedogênese; Pedogenesis; Savana; Savannah; Terraço aluvial; Tropical forest. |
|
Thesagro: |
Cerrado; Floresta Tropical; Solo. |
|
Thesaurus Nal: |
clay minerals. |
|
Categoria do assunto: |
-- |
|
Marc: |
LEADER 02509naa a2200325 a 4500
001 2088950
005 2022-03-07
008 2017 bl uuuu u00u1 u #d
100 1 $aDELARMELINDA, E. A.
245 $aSoil-landscape relationship in a chronosequence of the middle Madeira River in southwestern Amazon, Brazil.$h[electronic resource]
260 $c2017
520 $aHigh temperatures and rainfall prevail in the Brazilian Amazon, but some areas have soils with high clay mineral contents of 2:1, and there is limited information concerning their properties. Therefore, it is important to study the soil formation and understand the environmental conditions in which they were formed. This study aimed to investigate the physical, chemical and mineralogical properties of the soil in relation to the environmental factors acting on a chronosequence in the Late Pleistocene sediments of the Middle Madeira River. Soil profiles were selected on three alluvial terraces. Morphological, physical, chemical, mineralogical, X-ray fluorescence, TEM and SEM characterizations were performed. The soils that exhibited a clayey texture, acidic reaction, low values of exchangeable bases and high values of aluminum had profiles containing a considerable presence of 2:1 clay minerals, especially illite, vermiculite, mica-vermiculite, hydroxyl-interlayered vermiculite and pyrophyllite. Soil mineralogy indicated that these soils were recently weathered, where the low values of sum of bases correspond to the low presence of these cations in the parent material. Meanwhile, high values of exchangeable aluminum were derived from the pyrophyllite alteration, different parent material and 2:1 clay minerals recent alteration. Therefore, the parent material, presence of amorphous silica, different climate conditions in the past and current drainage restriction contribute to the slow alteration rate of 2:1 clay minerals of the soils of the humid tropical Amazon environment
650 $aclay minerals
650 $aCerrado
650 $aFloresta Tropical
650 $aSolo
653 $aAlluvial terrace
653 $aMinerais de argila
653 $aPedogênese
653 $aPedogenesis
653 $aSavana
653 $aSavannah
653 $aTerraço aluvial
653 $aTropical forest
700 1 $aSOUZA JÚNIOR, V. S. de
700 1 $aWADT, P. G. S.
700 1 $aDENG, Y.
700 1 $aCAMPOS, M. C. C.
700 1 $aCÂMARA, E. R. G.
773 $tCatena$gv. 149, part. 1, p. 199-208, 2017.
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Rondônia (CPAF-RO) |
|
|
Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
URL |
Voltar
|
|
|
| Registros recuperados : 6 | |
| 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. |
|    |
| 2. | | 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.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Solos. |
| |
| 3. | | 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. |
|  |
| 4. | | 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| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
| Biblioteca(s): Embrapa Rondônia. |
| |
| 5. | | 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.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
| Biblioteca(s): Embrapa Rondônia. |
| |
| 6. | | 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. |
| |
| Registros recuperados : 6 | |
|
| Nenhum registro encontrado para a expressão de busca informada. |
|
|
