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| Registros recuperados : 91 | |
| 7. |  | PALMIERI, F. (coord.). Levantamento semidetalhado dos solos e avaliação da aptidão agrícola das terras da microbacia do Córrego da Cachoeira, Município de Paty do Alferes, RJ. Rio de Janeiro: Embrapa Solos, 2000. 32 p. il. color. (Embrapa Solos. Boletim de pesquisa, 12). Equipe técnica: Francesco Palmieri (Coord.), Braz Calderano Filho, Jorge Olmos Iturri Larach, José Francisco Lumbreras, Sebastião Barreiros Calderano, Osório Oscar Marques da Fonseca, José Ronaldo de Macedo, Ênio Fraga da Silva, Cláudio...| Biblioteca(s): Embrapa Solos. |
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| 8. | | PALMIERI, F.; SANTOS, H. G. dos. Levantamento semidetalhado e aptidão agrícola dos solos do Município do Rio de Janeiro, RJ. Rio de Janeiro: EMBRAPA-SNLCS, 1980. 389 p. (EMBRAPA-SNLCS. Boletim técnico, 66). Acompanha 2 mapas, p&b. Escala 1:50.000. Autores: Francesco Palmieri, Humberto Gonçalves dos Santos, Loiva Lizia Antonello, Franklin dos Santos Antunes, Washington de Oliveira Barreto, Maria Amélia de M. Duriez, Ruth A. Leal Johas, João...| Biblioteca(s): Embrapa Meio Ambiente; Embrapa Semiárido; Embrapa Solos; Embrapa Solos / UEP-Recife. |
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| 12. | | CALDERANO, S. B.; PALMIERI, F.; LEMOS, A. L. Geologia dos Latossolos Amarelos em Paty do Alferes, Região Serrana do estado do Rio de Janeiro. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 27., 1999, Brasília, DF. Resumos [...]. Planaltina, DF: Embrapa Cerrados, 1999. 1 CD-ROM.| Biblioteca(s): Embrapa Solos. |
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| 15. | | NÚÑEZ, J. E. V.; AMARAL SOBRINHO, N. M. B.; PALMIERI, F.; MESQUITA, A. A. Consequências de diferentes sistemas de preparo do solo sobre a contaminação do solo, sedimentos e água por metais pesados. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 23, n. 4, p. 981-990, out./dez. 1999.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| 16. | | MARTORANO, L. G.; TOSTO, S. G.; PALMIERI, F.; MARQUES, J.; PINHEIRO, F.; ALMEIDA JUNIOR, P. Condicoes climaticas e suas influencias na safra de tomate (96/97)( no municipio de Paty dos Alferes, RJ. In: CONGRESSO BRASILEIRO DE AGROMETEOROLOGIA, 12.; REUNIAO LATINO AMERICANA DE AGROMETEOROLOGIA, 3., Fortaleza. Anais... Fortaleza: SBA / FUNCEME, 2001. v.2. p.813-814.| Biblioteca(s): Embrapa Hortaliças. |
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| 17. | | 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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| 18. | | SANTOS, H. G. dos; PALMIERI, F.; RODRIGUES, T. E.; CAMARGO, M. N.; SANTANA, D. P. Estudo expedito de solos da região Sul de Minas Gerais, partes do Alto São Francisco e Campos das Vertentes, para fins de classificação, correlação e legenda preliminar. Rio de Janeiro: EMBRAPA-SNLCS, 1980. 158 p. (EMBRAPA-SNLCS. Boletim técnico, 72).| Biblioteca(s): Embrapa Meio Ambiente; Embrapa Semiárido; Embrapa Solos; Embrapa Solos / UEP-Recife. |
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| 19. | | OLMOS ITURRI LARACH, J.; CALDERANO, B.; LUMBRERAS, J. F.; PALMIERI, F.; CUNHA, T. J. F. Interpretacao da aptidao agricola das terras da microbacia do Corrego da Cachoeira em Paty do Alferes, RJ. In: WORKSHOP NACIONAL DE AGRICULTURA SUSTENTAVEL EM REGIOES DE RELEVO ACIDENTADO, 3., 1997. Paty do Alferes, RJ. Anais... Rio de Janeiro: EMBRAPA-CNPS, 1998. CD-ROM Nao paginado.| Biblioteca(s): Embrapa Solos. |
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| Registros recuperados : 91 | |
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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: |
11/05/2022 |
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Autoria: |
PALMIERI, F. |
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Afiliação: |
FRANCESCO PALMIERI, CNPS. |
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Título: |
A study of a climosequence of soils derived from volcanic rock parent material in Santa Catarina and Rio Grande do Sul States, Brazil. |
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Ano de publicação: |
1986 |
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Fonte/Imprenta: |
1986. |
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Páginas: |
259 f. |
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Idioma: |
Inglês |
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Notas: |
Tese (Doutorado) - Purdue University, West Lafayette. |
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Conteúdo: |
Ten soils formed from basic volcanic rocks were studied on a 450 km climosequence transect in Santa Catarina and Rio Grande do Sul States, Brazil, to learn how soil properties vary with climate and to provide a data base for the developing Brazilian soil classification system. From east to west the altitude drops from 1250 m to 270 m, the annual temperature increases from 14.1(DEGREES)C to 19.3(DEGREES)C, and the annual precipitation decreases from 2460 mm to 1850 mm. The soils were in the Cambisol, Terra Bruna Estruturada (a new class), Brown Latosol, Terra Roxa Estruturada, and Dusky Red Latosol soil classes of the Brazilian soil classification and in the Dystrochrept, Haplumbrept, Paleudult, Haplohumox and Haplorthox great groups of the U.S. Soil Taxonomy. As soil sites get warmer and drier, kaolinite and hematite contents increase, halloysite and goethite contents decrease, the crystal size of kaolin minerals (kaolinite and 0.7 nm halloysite) increases, soil color changes from brown to dusky red, soil structure changes from well developed blocky to ultra fine granular (massive-like), and surface area and soil swelling decrease. The soil materials mainly had isotic plasmic fabric (isotropic) and had few or no argillans visible in thin section. Gibbsite and halloysite form immediately adjacent to each other in the weathered basaltic rocks. Maghemite occurred in 2.5YR and redder soils. Upward in the solum organic carbon and goethite contents increase, hematite decreases, the soil color becomes yellower and crystal size of kaolin minerals increases. These Fe-rich soils sorbed large amounts of phosphate. Acccording to prevailing ideas, tropical and subtropical soils composed mainly of kaolin and iron-oxide minerals have low surface activity and low shrink-swell potential. These soils shrink enough to open subsoil cracks 10 mm wide in the summer and have a moderately high swelling index (COLE = 0.042). Typically kaolin minerals are described as having 6 to 43 m('2) g('-1) surface area but in these soils it is about 300 m('2) g('-1). Surface area was inversely related to the mean crystallite dimension of kaolin minerals and directly related to COLE values and to phosphate sorption. Soil shear strength measured by the Swedish fall-cone increased as the soil structure changed from ultra fine granular (massive-like) to blocky structure and with increasing halloysite and goethite contents. MenosTen soils formed from basic volcanic rocks were studied on a 450 km climosequence transect in Santa Catarina and Rio Grande do Sul States, Brazil, to learn how soil properties vary with climate and to provide a data base for the developing Brazilian soil classification system. From east to west the altitude drops from 1250 m to 270 m, the annual temperature increases from 14.1(DEGREES)C to 19.3(DEGREES)C, and the annual precipitation decreases from 2460 mm to 1850 mm. The soils were in the Cambisol, Terra Bruna Estruturada (a new class), Brown Latosol, Terra Roxa Estruturada, and Dusky Red Latosol soil classes of the Brazilian soil classification and in the Dystrochrept, Haplumbrept, Paleudult, Haplohumox and Haplorthox great groups of the U.S. Soil Taxonomy. As soil sites get warmer and drier, kaolinite and hematite contents increase, halloysite and goethite contents decrease, the crystal size of kaolin minerals (kaolinite and 0.7 nm halloysite) increases, soil color changes from brown to dusky red, soil structure changes from well developed blocky to ultra fine granular (massive-like), and surface area and soil swelling decrease. The soil materials mainly had isotic plasmic fabric (isotropic) and had few or no argillans visible in thin section. Gibbsite and halloysite form immediately adjacent to each other in the weathered basaltic rocks. Maghemite occurred in 2.5YR and redder soils. Upward in the solum organic carbon and goethite contents increase, hematite decreases, th... Mostrar Tudo |
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Palavras-Chave: |
Classificação; Propriedade; Rio Grande do Sul; Santa Catarina; Solos; Vulcão. |
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Thesagro: |
Classificação do Solo; Mineralogia; Rocha; Solo. |
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Thesaurus NAL: |
Soil. |
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Categoria do assunto: |
--
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 03168nam a2200265 a 4500
001 1330863
005 2022-05-11
008 1986 bl uuuu m 00u1 u #d
100 1 $aPALMIERI, F.
245 $aA study of a climosequence of soils derived from volcanic rock parent material in Santa Catarina and Rio Grande do Sul States, Brazil.
260 $a1986.$c1986
300 $a259 f.
500 $aTese (Doutorado) - Purdue University, West Lafayette.
520 $aTen soils formed from basic volcanic rocks were studied on a 450 km climosequence transect in Santa Catarina and Rio Grande do Sul States, Brazil, to learn how soil properties vary with climate and to provide a data base for the developing Brazilian soil classification system. From east to west the altitude drops from 1250 m to 270 m, the annual temperature increases from 14.1(DEGREES)C to 19.3(DEGREES)C, and the annual precipitation decreases from 2460 mm to 1850 mm. The soils were in the Cambisol, Terra Bruna Estruturada (a new class), Brown Latosol, Terra Roxa Estruturada, and Dusky Red Latosol soil classes of the Brazilian soil classification and in the Dystrochrept, Haplumbrept, Paleudult, Haplohumox and Haplorthox great groups of the U.S. Soil Taxonomy. As soil sites get warmer and drier, kaolinite and hematite contents increase, halloysite and goethite contents decrease, the crystal size of kaolin minerals (kaolinite and 0.7 nm halloysite) increases, soil color changes from brown to dusky red, soil structure changes from well developed blocky to ultra fine granular (massive-like), and surface area and soil swelling decrease. The soil materials mainly had isotic plasmic fabric (isotropic) and had few or no argillans visible in thin section. Gibbsite and halloysite form immediately adjacent to each other in the weathered basaltic rocks. Maghemite occurred in 2.5YR and redder soils. Upward in the solum organic carbon and goethite contents increase, hematite decreases, the soil color becomes yellower and crystal size of kaolin minerals increases. These Fe-rich soils sorbed large amounts of phosphate. Acccording to prevailing ideas, tropical and subtropical soils composed mainly of kaolin and iron-oxide minerals have low surface activity and low shrink-swell potential. These soils shrink enough to open subsoil cracks 10 mm wide in the summer and have a moderately high swelling index (COLE = 0.042). Typically kaolin minerals are described as having 6 to 43 m('2) g('-1) surface area but in these soils it is about 300 m('2) g('-1). Surface area was inversely related to the mean crystallite dimension of kaolin minerals and directly related to COLE values and to phosphate sorption. Soil shear strength measured by the Swedish fall-cone increased as the soil structure changed from ultra fine granular (massive-like) to blocky structure and with increasing halloysite and goethite contents.
650 $aSoil
650 $aClassificação do Solo
650 $aMineralogia
650 $aRocha
650 $aSolo
653 $aClassificação
653 $aPropriedade
653 $aRio Grande do Sul
653 $aSanta Catarina
653 $aSolos
653 $aVulcão
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