STRUCTURAL AND MAGNETIC CHARACTERIZATION OF MAGHEMITES PREPARED FROM Al-SUBSTITUTED MAGNETITES

Synthetic aluminum-substituted maghemites were characterized by total chemical analysis, powder X-ray diffraction (XRD), Mossbauer spectroscopy (ME), and vibrating sample magnetometry (VSM). The aim was to determine the structural, magnetic, and hyperfine properties of gamma-Fe2-xAlxO3 as the Al concentration is varied. The XRD results of the synthetic products were indexed exclusively as maghemite. Increasing Al for Fe substitution decreased the mean crystalline dimension and shifted all diffraction peaks to higher degrees 2 theta angles. The a(0) dimension of the cubic unit cell decreased with increasing Al according to the equation a(o) = 0.8385 - 3.63 x 10(-5) Al (R-2 = 0.94). Most Mossbauer spectra were composed of one sextet, but at the highest substitution rate of 142.5 mmol mol(-1) Al, both a doublet and sextet were obtained at approximate to 300 K. All hyperfine parameters from the sub-spectra were consistent with high-spin Fe3+ (0.2 a 0.7 mms(-1)) and suggested a strong superparamagnetic component associated with the doublet. The magnetic hyperfine field of the sextets decreased with the amount of Al-substitution [B-hf (T) = 49.751 - 0.1202Al; R-2 = 0.94] while the linewidth increased linearly. The saturation magnetization also decreased with increasing isomorphous substitution.