695-6 Mineralogy and Mass Specific Magnetic Susceptibility of Synthetic Aluminum Substituted Maghemites (γ-Fe2-xAlxO3).

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)

Tuesday, 7 October 2008
George R. Brown Convention Center, Exhibit Hall E

Marcelo Batista, The School of Environment and Natural Resources, The Ohio State University, Columbus, OH, Antonio Costa, Departamento de Agronomia, Universidade Estadual de Maringa, Maringá - Paraná, Brazil, Jerry Bigham, Ohio State Univ., Columbus, Columbus, OH and Ivan G. Souza Junior, Departamento de Agronomia, Universidade Estadual de Maringa, Maringá - Paraná, Brazil
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)