iron and aluminum forms and their relationship with texture, mineralogy and organic carbon in the cerrado oxisol
formas de ferro e alumínio e suas relações com textura, mineralogia e carbono orgânico em latossolos do cerrado

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ID: 150461
2011
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Abstract
The Oxisols of the Cerrado region have a simple mineralogy, and are composed mainly of kaolinite and iron and aluminium oxides. The aim of this work was to perform a sequential extraction of iron and aluminium and to relate them to texture, mineralogy and organic carbon in Oxisols of the Cerrado region. The soil samples, 35 in total, were taken from the 0–20 cm layer in Oxisols under pasture located in the Brazilian Cerrado Region. The levels of iron and aluminum extracted by full attack, dithionite-citrate-bicarbonate, ammonium oxalate and sodium pyrophosphate were analyzed according to the textural classes using the Kruskal-Wallis nonparametric test. Then these data were related to the mineralogy and organic carbon through a principal component analysis. Whatever the textures, iron oxides of high degree of crystallinity were the main form of iron and are positively correlated with the iron total content. The aluminum oxides have a high affinity to organic carbon than iron oxides. The levels of iron and aluminum extracted by sodium pyrophosphate were closely related to soil pH.

Os Latossolos da região do Cerrado apresentam mineralogia da fração argila relativamente simples, sendo constituídos principalmente por caulinita e óxidos de ferro e de alumínio. O objetivo deste trabalho foi realizar extrações sequênciais de ferro e de alumínio e relacioná-los à mineralogia, textura e teores de carbono orgânico em Latossolos da região do Cerrado. Coletaram-se 35 amostras na camada de 0-20 cm de Latossolos sob pastagem da Região do Cerrado. Os teores de ferro e de alumínio extraídos pelo ataque total, ditionito-citrato-bicarbonato de sódio, oxalato ácido de amônia e pirofosfato de sódio foram analisados de acordo com a classe textural através do teste não paramétrico de Kruskal-Wallis. Em seguida estes dados foram relacionados com a mineralogia e o carbono orgânico por meio de uma análise de componentes principais. Independentemente da classe textural, os óxidos de ferro de alto grau de cristalinidade representaram a principal forma de ferro e se correlacionam positivamente com os teores totais de ferro. Os óxidos de alumínio apresentaram maior afinidade ao carbono orgânico do que os óxidos de ferro. Os teores de ferro e alumínio extraídos pelo pirofosfato foram estreitamente relacionados ao pH dos solos.

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marcho2011semina:iron Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;Robélio Lenadro Marchão;Osmar Rodrigues Brito;Diogo Néia Eberhardt;Pedro Rodolfo Siqueira Vendrame;Cécile Quantin;Thierry Becquer
Journal frontiers in neuroendocrinology
Year 2011
DOI
10.5433/1679-0359.2011v32n4Sup1p1657
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