Au. Gehring et Am. Hofmeister, THE TRANSFORMATION OF LEPIDOCROCITE DURING HEATING - A MAGNETIC AND SPECTROSCOPIC STUDY, Clays and clay minerals, 42(4), 1994, pp. 409-415
Infrared (IR) spectroscopy, in combination with magnetic methods, was
used to study the thermally induced transformation of synthetic lepido
crocite (gamma-FeOOH) to maghemite (gamma-Fe2O3). Magnetic analyses sh
owed that the thermal conversion began at about 175 degrees C with the
formation of superparamagnetic maghemite clusters. The overall struct
ural transformation to ferrimagnetic gamma-Fe2O3 occurred at 200 degre
es C and was complete around 300 degrees C. At higher temperatures, th
e maghemite converted into hematite (alpha-Fe2O3). Observation of the
transformation from gamma-FeOOH to gamma-Fe2O3 using variable-temperat
ure IR spectroscopy indicated that dehydroxilation on a molecular leve
l was initiated between 145 degrees C and 155 degrees C. The lag time
between the onset of the breaking of OH bonds and the release of H2O f
rom lepidocrocite around 175 degrees C can be explained by diffusive p
rocesses. Overall dehydroxilation and the subsequent breakdown of the
lepidocrocite structure was complete below 219 degrees C. The comparis
on of the magnetic and IR data provides evidence that the dehydroxilat
ion may precede the structural conversion to maghemite.