Lag. Rodenas et al., SURFACE COMPLEXATION DESCRIPTION OF THE DISSOLUTION OF CHROMIUM(III) HYDROUS OXIDES BY OXALIC-ACID, Inorganic chemistry, 36(27), 1997, pp. 6423-6430
Aqueous oxalic acid forms surface Cr-III-oxalato complexes with suspen
ded chromium(III) oxide particles; the FTIR spectra demonstrate that b
oth carboxylate groups of the ligand are bound to surface Cr-III. Surf
ace complexation is followed by changes in the surface redox potential
toward more negative values and by the dissolution of the oxide. The
dissolving steady state potential is in the range -60 to -210 mV again
st SHE. During surface conditioning, traces of oxidants at the interfa
ce are reduced, and some reduced metal ions accumulate. Minor amounts
of dissolved Cr-II are generated and can be collected at a vicinal rin
g electrode set at -60 mV. In agreement, dissolution kinetics suggest
that generation of Cr-II by ligand-to-metal charge transfer within the
surface complexes produces a large increase in the rate of phase tran
sfer, as expected from the properties of Cr-III and Cr-II. Added chrom
ous salts also catalyze the dissolution through intervalence charge tr
ansfer within an oxalato-bridged Cr-III-L-Cr-II surface dimeric comple
x. The rate of dissolution at 65 degrees C follows a Langmuir-Hinshelw
ood dependence on oxalic acid concentration, a power law (order 0.31)
dependence on proton concentration, and an a + b[Cr-II](0.64) dependen
ce on [Cr(II)]. The Langmuir-Hinshelwood parameters are interpreted in
terms of the stability constant of the surface Cr-III-oxalato complex
.