Notas sobre a formação de gibsita em solos de Viçosa

Autores

  • Onofre C B Pinto UFV

Palavras-chave:

origem gibsita, intemperismo solos, caolinita plagioclásios, drenagem lixiviação, difração raios

Resumo

Four soil profiles from Viçosa, Minas Gerais, Brazil, were studied. A strongly weathered biotite-feldspar gneiss (plasioclase) formed the parent material on which these soils developed. The minerals present in each of the profiles were identified by x-ray technique. Kaolinite and quartz were found to be present in large amounts; gibbsite and iron oxides, in smaller amounts.

Referências

ALEXANDER, L.T., HENDRICKS, S.B & FAUST, G.T. Occurence of gibbsite in some soil-forming material. Soil Sei.Soc.Amer Proc., Madison, 6:52-57. 1942.

BATES, T.F. Halloysite and gibbsite formation in Hawaii. Clays and Clay Minerals. New York, 11: 315-328. 1962.

GARDNER, L.R. A chemical model for the origin of gibbsite from kaolinite. Amer. Min., Lancaster, 55:1380-1939.1970.

JACKSON, M.L. Soil chemical analysis, advanced course. Ma- dison. Dept. of Soil Science, University of Wisconsin, 1956. 894 p.

JACKSON, M.L. Chemical composition of soils. In: BEAR, F.E, ed., Chemistry of the soil. New York, Reinolds Publishing Corporation, 1964, pp. 71-141.

KELLER, W.D. Principles of chemical weathering. Columbia, Missouri, Lucas Brothers Publishers, 1lp. 1968.

PINTO, 0.C.B., YAHNER, J.E., & ROTH, C.B. Natureza e formação de caolinita em forma de pseudomica, em solos de Viçosa, Minas Gerais. Experientiae, Viçosa, 13: 383-421. 1972.

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Publicado

2025-02-21

Como Citar

C B Pinto , O. (2025). Notas sobre a formação de gibsita em solos de Viçosa . Revista Ceres, 19(104), 299–305. Recuperado de https://ojs.ceres.ufv.br/ceres/article/view/6658

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