Abstract
In agreement with earlier studies, neutron diffraction measurements show that off-stoichiometric Fe3-xO4 is the main product of wet-milling haematite, α-Fe2O3, in vacuum with defect magnetite, ∼ Fe2.8O4, being obtained after milling for 72 and 144 h. Reitveld refinements of the room-temperature neutron diffraction patterns show that ∼ Fe2.8O4 exhibits reduced lattice parameters (∼0.1%) and magnetic moment values (∼5%) compared with stoichiometric Fe3O4. Comparison of the Fe2O3 content as determined from the phase fractions of the 72-h milled sample (∼ 7%) and following heat treatment at ∼ 950 K (∼37%) reveals that a significant fraction of α-Fe2O3 is present in the milled product in an amorphous-like or disordered state.
| Original language | English |
|---|---|
| Pages (from-to) | S1233-S1235 |
| Journal | Applied Physics A: Materials Science and Processing |
| Volume | 74 |
| Issue number | SUPPL.II |
| DOIs | |
| Publication status | Published - Dec 2002 |
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