Mineralogical Evolution of Magnetic Rhodic Oxisols under Different Lithological Influences in Brazil
25/Sep/2019
ABSTRACT Ferrimagnetic Fe-oxides are important soil components, which are present in most of the agricultural soils of Brazil. Distinction, origin, and assessment of the influence of these minerals on magnetism and geochemistry is a challenge for mineralogists. This study aimed to characterize mineralogically Fe-rich Rhodic Oxisols ( Latossolos Vermelhos ) originating from several mafic rocks in Brazil, and assess the implications on their magnetic and geochemical properties. We present results on magnetic measurements, chemical dissolutions, X-ray diffractometry, Rietveld refinement, Raman, […]
Effectiveness of Arsenic Co-Precipitation with Fe-Al Hydroxides for Treatment of Contaminated Water
23/Mar/2018
ABSTRACT Wastewater treatment is a challenging problem faced by the mining industry, especially when mine effluents include acid mine drainage with elevated arsenic levels. Iron (hydr)oxides are known to be effective in removal of As from wastewater, and although the resulting compounds are relatively unstable, the presence of structural Al enhances their stability, particularly under reducing conditions. The purpose of this study was to assess the effectiveness of Al-Fe (hydr)oxide co-precipitates for the removal of As from wastewater and to […]
Genesis of latosols and cambisols developed from pelitic rocks of the Bambui group, Minas Gerais state – Brazil
01/Aug/2010
The widespread occurrence of Cambisols (shallow, dense and silty) and of clayey and very clayey Latosols is typical of pelitic rocks of the pre-Cambrian Bambui Group landscape, but few studies are focused on the genesis and agricultural potential of these soils. Two areas were selected in Curvelo, state of Minas Gerais, for a detailed study of physical, chemical and mineralogical properties of these soils, to deepen the understanding of the pedogenesis of this area. Soils classified as Haplic Cambisols (Inceptisols), […]
Magnetic susceptibility of B horizon of soils in the State of Paraná
01/Apr/2010
The ferrimagnetic minerals maghemite (γFe2O3) are closely related with metal availability and P adsorption capacity. Magnetization is spontaneous in a significant percentage of Brazilian soils. In the State of Paraná (Brazil) this area represents up to 50 %. The determination of the mass-specific magnetic susceptibility (ΧBF) is the simplest method of identification and quantification of ferrimagnetic minerals in soils. The ΧLF is a quick, cheap, non-destructive technique, with satisfactory reproducibility, and can be used as a criterion in pedogenetic studies […]