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1. | | SOUZA JÚNIOR, V. S.; RIBEIRO, M. R.; OLIVEIRA, L. B. Propriedades químicas e manejo de solos tiomórficos da várzea do Rio Coruripe, estado de Alagoas. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 25, n. 4, p. 811-822, out./dez. 2001. Biblioteca(s): Embrapa Solos / UEP-Recife. |
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2. | | SOUZA JÚNIOR, V. S.; RIBEIRO, M. R.; OLIVEIRA, L. B. Caracterização e classificação de solos tiomórficos da várzea do Rio Coruripe, estado de Alagoas. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 25, n. 4, p. 977-986, out./dez. 2001. Biblioteca(s): Embrapa Solos / UEP-Recife. |
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3. | | BISPO, F. H. A.; SILVA, A. C.; TORRADO, P. V.; SOUZA JÚNIOR, V. S. de. Highlands of the upper Jequitinhonha Valey, Brazil. II - Mineralogy, micromorphology, and landscape evolution. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 35, n. 4, p. 1081-1091, jul./ago. 2011. Título em Português: Chapadas do Alto Vale do Jequitinhonha, MG. II - Mineralogia, micromorfologia e evolução da paisagem. Biblioteca(s): Embrapa Solos / UEP-Recife. |
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5. | | CARVALHO, V. S. de; RIBEIRO, M. R.; SOUZA JÚNIOR, V. S. de; BRILHANTE, S. A. Caracterização de espodossolos dos estados da Paraíba e do Pernambuco, Nordeste do Brasil. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 37, n. 6, p. 1454-1463, jul./ago. 2013. Biblioteca(s): Embrapa Solos / UEP-Recife. |
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6. | | FURQUIM, S. A. C.; ARAUJO FILHO, J. C. de; ALVES, G. B.; SOUZA JUNIOR, V. S. de; OLIVEIRA, F. S. Grau de intemperismo em Vertissolos do Nordeste brasileiro. In: CONGRESSO LATINO-AMERICANO DE CIÊNCIA DO SOLO, 23.; CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 38., 2023, Florianópolis. Anais [...]. Florianópolis: Epagri, 2023. p. 42. Ref. ID 1413. Biblioteca(s): Embrapa Solos. |
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10. | | ARAUJO, J. K. S.; SOUZA-JÚNIOR, V. S.; MARQUES, F. A.; SOUZA, R. A. S.; VORONEY, P. Relações entre o carbono e atributos químicos de latossolos húmicos, Nordeste-Brasil. In: CONGRESO LATINOAMERICANO DE LA CIENCIA DEL SUELO, 20.; CONGRESO PERUANO DE LA CIENCIA DEL SUELO, 16., 2014, Cusco. Educar para preservar el suelo y conservar la vida en la tierra: trabajos. Cusco: Sociedad Latinoamericana de la Ciencia del Suelo, 2014. Biblioteca(s): Embrapa Solos. |
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11. | | ARAUJO, J. K. S.; SOUZA-JÚNIOR, V. S.; MARQUES, F. A.; SOUZA, R. A. S.; VORONEY, P. Frações húmicas e caracterização termogravimétrica da humina de latossolos húmicos. In: CONGRESO LATINOAMERICANO DE LA CIENCIA DEL SUELO, 20.; CONGRESO PERUANO DE LA CIENCIA DEL SUELO, 16., 2014, Cusco. Educar para preservar el suelo y conservar la vida en la tierra: trabajos. Cusco: Sociedad Latinoamericana de la Ciencia del Suelo, 2014. Biblioteca(s): Embrapa Solos. |
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14. | | 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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15. | | SÁ, E. S. dos S. C. G. de; SOUZA JÚNIOR, V. S. de; SILVA, A. H. N. da; SOUSA, J. E. S. de; ARAUJO FILHO, J. C. de. Pedogenesis in a semi-arid wetland. 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. 48. WCSS 2018. Biblioteca(s): Embrapa Solos. |
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16. | | QUEIROZ, A. F. de; SALVIANO, A. M.; CUNHA, T. J. F.; OLSZEVSKI, N.; SOUZA JUNIOR, V. S.; OLIVEIRA NETO, M. B. de. Potentialities and limitations of agricultural use in soils of semi-arid region of the state of Bahia. Anais da Academia Brasileira de Ciências, v. 90, n. 4, p. 3373-3387, oct./dec. 2018. Biblioteca(s): Embrapa Semiárido; Embrapa Solos. |
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17. | | SANTANA, M. de B.; RIBEIRO FILHO, M. R.; SOUZA JÚNIOR, V. S.; SCHULZE, S. M. B. B.; CUNHA, T. J. F.; MARCQUES, F. A. Mineralogia e morfologia da fração areia grossa e fina de solos aluviais no Semiárido brasileiro. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 36., 2017, Belém, PA. Amazônia e seus solos: peculiaridades e potencialidades. Belém, PA: SBCS, 2017. Biblioteca(s): Embrapa Semiárido. |
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18. | | ARAUJO FILHO, J. C. de; MARQUES, F. A.; AMARAL, A. J. do; CUNHA, T. J. F.; SOUZA JÚNIOR, V. S. de; GALVÃO, P. V. M. Solos do Semiárido: características e estoque de carbono In: GIONGO, V.; ANGELOTTI, F. (ed.). Agricultura de baixa emissão de carbono em regiões semiáridas: experiência brasileira. Brasília, DF: Embrapa, 2022. cap. 6, p. 93-112. Biblioteca(s): Embrapa Semiárido; Embrapa Solos; Embrapa Trigo. |
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19. | | 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 Biblioteca(s): Embrapa Rondônia. |
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20. | | 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. Biblioteca(s): Embrapa Rondônia. |
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Registros recuperados : 42 | |
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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 |
Circulação/Nível: |
A - 1 |
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.
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