Fine particles of ferrimagnetic MgFe2O4 were synthesized through a sol
-gel supercritical drying procedure, then cold-pressed and heated at 5
00 and 800-degrees-C. These materials were characterized by Mossbauer
spectrometry in the temperature range 25-298 K, and in the presence of
a small applied magnetic field. The Mossbauer measurements show that
heat treatment results in the formation of a small percentage of alpha
-Fe2O3, an increase in the mean particle size and hyperfine magnetic f
ield, and a decrease in the inversion parameter of the magnesioferrite
. An average anisotropy constant equivalent to the bulk magnetocrystal
line anisotropy is estimated for particles with diameter D = 14 nm.