Poster Number 612
See more from this Division: S09 Soil Mineralogy
See more from this Session: Soil Mineralogy: Reactions and Transformations: II (includes Graduate Student Competition) (Posters)
Abstract:
Mineralogy and Mass Specific Magnetic Susceptibility of Synthetic Aluminum Substituted Maghemites (γ-Fe2-xAlxO3)
M.A. Batista, A.C.S. Costa, I.G. Souza Junior & J.M. Bigham
Maghemite (γ-Fe2O3) is a ferrimagnetic iron oxide commonly found in the red, basalt-derived soils of Brazil. Variable degrees of ionic substitution of Fe3+ by different cations (mainly Al3+) in the maghemite structure under natural conditions can influence many of the crystallochemical properties of this mineral. To study these effects, in a systematic manner, synthetic Al-substituted maghemites were prepared by co-precipitation of FeSO4.7H2O with increasing amounts of Al2(SO4)3.18H2O in aqueous media. The resulting magnetites were heated to 250ºC for 4 hours to form a series of brown maghemites that were subsequently characterized by chemical analysis, X-ray diffraction specific surface area, and mass specific magnetic susceptibility. Although Al - for - Fe substitution rates from 0.000 to 0.3000 mol mol-1 were expected, the observed levels of solid solution ranged from 0.000 to 0.064 mol mol-1, thereby forming a series of maghemites with compositions ranging from Fe2.000Al0.000O3 to Fe1.874Al0.126O3. An increase in Al - for - Fe substitution, [Al mol mol-1] decreased the a0 dimension of the cubic unit cells according to the regression equation: a0 = 0.8357 - 0.0855Al (R2 = 0.75). A corresponding decrease was observed for the mean crystallite dimensions calculated using the Scherrer equation. Mass specific magnetic susceptibility for the samples (χLF) initially increased with increasing Al-for-Fe substitution. The maximum value of χLF (52,503 108 m3 kg-1) was observed with 0.0246 mol mol-1 of Al-substitution. After this point, the values of χLF decreased to 35,487 108 m3 kg-1. Frequency dependence values of the mass specific magnetic susceptibility (χFD) varied from 0.2 to 4.9%. Maghemites with 0.021 to 0.064 mol mol-1 Al (χFD ≥ 2) appear to be admixtures of superparamagnetic and coarser, single-domain and multi-domain grains.
See more from this Division: S09 Soil Mineralogy
See more from this Session: Soil Mineralogy: Reactions and Transformations: II (includes Graduate Student Competition) (Posters)