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ESTUDO COMPARATIVO DE PROPRIEDADES DE LATOSSOLOS
DO BRASIL.
1/Gabriel Antonio de Souza —
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ESTUDO COMPARATIVO DE PROPRIEDADES DE LATOSSOLOS
DO BRASIL
Autor: Gabriel Antonio de SouzaOrientador: Prof. Egon Klamt
SINOPSE
Caracterizações morfológicas, físicas, químicas e minera lógicas foram efetuadas em Latossolo Roxo, Vermelho Escuro, Vermelho Amarelo e Amarelo, do Brasil, visando obter informa-ções sobre a génese e testar parâmetros que possibilitem a separação destes solos a nível de Grande Grupo ou Sub-Grupo.
Quartzo, caulinita, gibbsita, materiais amorfos, hemati-ta e goethita são os principais constituintes mineralógicos destes solos. Os latossolos do Brasil Central apresentam teo-res elevados de gibbsita, que não ocorrem nos do Rio Grande do Sul e Amazônia. A maior estabilidade das superfícies geo-mórficas do Brasil Central e portanto o maior tempo de atua-ção dos processos pedogenéticos deve ser a causa desta diferença. Os teores de óxidos de ferro são mais elevados nos Latossolo Roxo seguido dos Latossolo Vermelho Escuro, Vermelho Amarelo e Amarelo, estando a cor mais relacionada ao tipo de óxido de ferro presente do que ao teor. As diferenças na composição mineralógica dos compostos de ferro indicam que a cor deve continuar sendo utilizada para fins de classificação. Apesar de apresentarem diferenças marcantes em textura,concentração em óxidos de ferro e mineralogia, estes solos apresentam capacidade de adsorção de fósforo similar, devendo a adsorção estar relacionada ao tipo de óxido ou argilo-mineral presente.
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COMPARISON OF PROPERTIES OF LATOSOLS OF BRAZIL
Author: Gabriel Antonio de Souza Adviser: Prof. Egon Klamt
SUMMARY
Morphological, phisical, chemical and mineralogical cha-racteristics of Dusky Red, Dark Red, Yellow Red and Yellow Latosols of Brazil were determined in the present study to obtain information related to the genesis of these soils and to test parameters for taxonomic classification at Great Group or Sub-Group level.
Quartz, kaolinite, gibbsite, amorphous material, hematite and goethite are the most important minerals of these soils. The soils of Central Brazil contain high concentrations of gibbsite, which is absent in the Rio Grande do Sul and Amazonia soils. The stability of geomorphic surface of Central Brazil and time of action of the pedogenetic processes appear to be the cause of these differences. In general the content of iron oxides decreases from the Dusk Red to Dark Red, Yellow Red and Yellow Latosols. The color of these soils is more associate to the form than to the content of iron oxides present. The differences in the mineralogical composition of the iron compounds indicate that color can be used as parameter for taxonomic classification.
These soils present similar phosphate adsorption capaci-ty in spite of large differences in particle size distribu-tion, contend of iron oxides and mineralogical composition.
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