Magnetic properties of magnetite powder prepared by ball-milling of stoichi
ometric mixture of hematite and iron in an inert atmosphere are reported. H
ysteresis loops, isothermal remanence acquisition curves and temperature de
pendence of magnetic susceptibility measurements are used to characterise t
his material and to examine the effects of heating in air and in an argon a
tmosphere. Ball-milling of hematite with iron during periods ranging from 3
0 min up to almost 5 h yields magnetite which exhibits high magnetic hardne
ss, characterised by coercive force three times higher than that typical fo
r single-domain natural magnetites. However, the magnetite produced is unst
able upon heating in air, reoxidising almost completely to hematite. Heatin
g in an argon atmosphere causes enhancement of typical magnetic parameters,
but decreases the magnetic hardness. (C) 2000 Elsevier Science B.V. All ri
ghts reserved.