The chlorination of synthetic pseudobrookite was studied by thermogravimetr
y in the temperature range 700-950 degrees C; both isothermal and non-isoth
ermal measurements were made. The effect of reaction temperature on the chl
orination rate was correlated with the morphological evolution and elementa
l composition of the reacting solids by means of scanning-electron microsco
py, energy-dispersive X-ray spectroscopy and X-ray diffraction analysis. It
was found that chlorination took place as a topochemical process in which
the-ir;on was chlorinated selectively, forming FeCl3(g) and leaving TiO2 as
a solid residue. During the chlorination, however, some TiCl4(g) was forme
d and this was subsequently converted to TiO2 by its reaction with iron oxi
de.