A turbidimetric method was used to study the dissolution kinetics of d
ifferent chromium (hydr)oxides in aqueous HClO4. There was a very good
agreement between the results obtained with this method and those obt
ained with a standard one (quantifying the amount of chromium released
to solution at different reaction times, after the separation of the
solid and liquid phases by centrifugation or filtration), revealing th
at turbidimetry can be used to monitor the dissolution behavior of the
studied materials. Theoretical support for the use of turbidimetry in
dissolution studies can be obtained from light scattering theory. Chr
omium (hydr)oxide particles were composed of a mixture of monomeric an
d low oligomeric Cr(III) species that dissolves almost instantaneously
in HClO4 (rapidly dissolving material) and a more polymerized materia
l that undergoes dissolution at a lower and measurable rate (slowly di
ssolving material). The dissolution product was also a mixture of mono
mers and more polymerized Cr(III) species. Apparent activation energie
s (40-70 kJ/mol) for the dissolution of the slowly dissolving material
were high enough to discard diffusion in aqueous solution as the rate
-determining step and considerably lower than those corresponding to l
igand exchange in Cr(III) species. This suggests that diffusion into t
he solid could be controlling the dissolution rate, although more dire
ct evidence is needed.