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| Registros recuperados : 88 | |
| 10. |  | FREITAS, F. G. de; GOMES, I. A. Levantamento de reconhecimento dos solos do Distrito Federal. Rio de Janeiro: EMBRAPA-SNLCS, 1978. 455 p. (EMBRAPA-SNLCS. Boletim Tecnico, 53). Acompanha 02 mapas color. escala 1:100.000. Autores: Flavio Garcia de Freitas, Idare Azevedo Gomes, Roberto Chaves Ferreira, Loiva Lizia Antonello, Ney Pinto Tavares, Washington de Oliveira Barreto, Jose Lopes de Paula, Maria Amelia de...| Biblioteca(s): Embrapa Meio Ambiente. |
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| 15. | | PALMIERI, F.; SANTOS, H. G. dos; GOMES, I. A.; LUMBRERAS, J. F.; AGLIO, M. L. D. The Brazilian Soil Classification System. In: ESWARAN, H.; RICE, T.; AHRENS, R.; STEWART, B. A. (Ed.). Soil classification: a global desk reference. Boca Raton: CRC Press, 2003. cap. 11, p. 127-146.| Biblioteca(s): Embrapa Solos. |
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| 17. | | RIBEIRO, C. C. D.; REGO, A. S.; GOMES, I. A. S.; OLIVEIRA, M. E. C. Comparação de métodos de cálculo do teor de lipídeos em frutos de tucumã (Astrocaryum vulgare). In: SEMINÁRIO DE INICIAÇÃO CIENTÍFICA DA EMBRAPA AMAZÔNIA ORIENTAL, 15., 2011, Belém, PA. A ciência de fazer ciência: anais. Belém, PA: Embrapa Amazônia Oriental, 2011. 1 CD-ROM. PIBIC-2011.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 19. | | GOMES, I. A.; MARKOVÁ, E.; SILVA, J. P. L. da; VENÂNCIO, A.; FREITAS-SILVA, O. Global trends for patulin adsorption: A review. Research, Society and Development, v. 10, n. 6, e58310616162, 2021.| Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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| Registros recuperados : 88 | |
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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: |
22/11/2002 |
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Data da última atualização: |
22/11/2002 |
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Autoria: |
GOMES, I. A. |
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Título: |
Oxisols and inceptisols from gneiss in a subtropical area of Espirito Santo State, Brazil. |
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Ano de publicação: |
1976 |
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Fonte/Imprenta: |
s.l.: Purdue University, 1976. |
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Páginas: |
115p. |
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Idioma: |
Inglês |
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Notas: |
Tese Mestrado. |
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Conteúdo: |
A study was conducted to gain information on the genesis, classification and management of certain soils from a subtropical area of Brazil. The objective was accomplished by studying the physical, chemical and mineralogical properties, substantiated by the morphological description of the six soil profiles. The soils occupy steep slopes in the Crystalline Plateau of the state of Espirito Santo, which receives a relatively high rainfall. The climate is subtropical due to the altitude, which varies between 500 and 1300 meters. One part of the area is always humid and another part showe a short dry season. The mean annual precipitation ranges from 1200 to 2000 mm and the mean annual temperature ranges from 18 to 20oC. The parent material of the soils is a deeply weathered material, generally transported in its landscape, derived from acid gneiss. Quartz, kaolinite and/or gibbsite, and goethite are the main minerals present in all profiles. Also, muscovite and slightly altered biotite (micaceous material with paler colors and broadening of 10oA peak of biotite to biotita to around 11oA) occur in noticeable amounts in two profiles. The sand fraction of most profiles shows high amounts of quartz. The content of quartz sharply decreases in the silt fraction and reaches the breakdown point in the clay fraction. The fine silt fraction (20 to 2u) is dominated by kaolinite and gibbsite in all profiles. Kaolinite, gibbsite and goethite are the main minerals in the clay fraction of all profiles. Kaolinite has been.............. MenosA study was conducted to gain information on the genesis, classification and management of certain soils from a subtropical area of Brazil. The objective was accomplished by studying the physical, chemical and mineralogical properties, substantiated by the morphological description of the six soil profiles. The soils occupy steep slopes in the Crystalline Plateau of the state of Espirito Santo, which receives a relatively high rainfall. The climate is subtropical due to the altitude, which varies between 500 and 1300 meters. One part of the area is always humid and another part showe a short dry season. The mean annual precipitation ranges from 1200 to 2000 mm and the mean annual temperature ranges from 18 to 20oC. The parent material of the soils is a deeply weathered material, generally transported in its landscape, derived from acid gneiss. Quartz, kaolinite and/or gibbsite, and goethite are the main minerals present in all profiles. Also, muscovite and slightly altered biotite (micaceous material with paler colors and broadening of 10oA peak of biotite to biotita to around 11oA) occur in noticeable amounts in two profiles. The sand fraction of most profiles shows high amounts of quartz. The content of quartz sharply decreases in the silt fraction and reaches the breakdown point in the clay fraction. The fine silt fraction (20 to 2u) is dominated by kaolinite and gibbsite in all profiles. Kaolinite, gibbsite and goethite are the main minerals in the clay fraction of all p... Mostrar Tudo |
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Palavras-Chave: |
Brasil; Classificacao; Espirito Santo; Origem; Solos. |
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Thesagro: |
Manejo. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02066nam a2200205 a 4500
001 1331326
005 2002-11-22
008 1976 bl uuuu m 00u1 u #d
100 1 $aGOMES, I. A.
245 $aOxisols and inceptisols from gneiss in a subtropical area of Espirito Santo State, Brazil.
260 $as.l.: Purdue University$c1976
300 $a115p.
500 $aTese Mestrado.
520 $aA study was conducted to gain information on the genesis, classification and management of certain soils from a subtropical area of Brazil. The objective was accomplished by studying the physical, chemical and mineralogical properties, substantiated by the morphological description of the six soil profiles. The soils occupy steep slopes in the Crystalline Plateau of the state of Espirito Santo, which receives a relatively high rainfall. The climate is subtropical due to the altitude, which varies between 500 and 1300 meters. One part of the area is always humid and another part showe a short dry season. The mean annual precipitation ranges from 1200 to 2000 mm and the mean annual temperature ranges from 18 to 20oC. The parent material of the soils is a deeply weathered material, generally transported in its landscape, derived from acid gneiss. Quartz, kaolinite and/or gibbsite, and goethite are the main minerals present in all profiles. Also, muscovite and slightly altered biotite (micaceous material with paler colors and broadening of 10oA peak of biotite to biotita to around 11oA) occur in noticeable amounts in two profiles. The sand fraction of most profiles shows high amounts of quartz. The content of quartz sharply decreases in the silt fraction and reaches the breakdown point in the clay fraction. The fine silt fraction (20 to 2u) is dominated by kaolinite and gibbsite in all profiles. Kaolinite, gibbsite and goethite are the main minerals in the clay fraction of all profiles. Kaolinite has been..............
650 $aManejo
653 $aBrasil
653 $aClassificacao
653 $aEspirito Santo
653 $aOrigem
653 $aSolos
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