A new modification of Fe(III) oxide - protohematite - was produced by therm
al decomposition of crystalline hydroxides and salts and by plasma chemical
method. Protohematite is a metastable phase which transforms into alpha-Fe
2O3 at 1100 degrees C, under pressure or mechanic chemical activation. IR a
nd Raman spectroscopy, X-ray powder diffraction, and transmission electron
microscopy were used to study the structure of protohematite. It was conclu
ded that protohematite has unique structural characteristics. The hypothesi
s concerning the structure of protohematite was suggested. Specific chemica
l activity of the protohematite was assumed to originate from the presence
of some ferric cations in quasi tetrahedral (distorted octahedral) coordina
tion. (C) 2000 Elsevier Science B.V. All rights reserved.