The oxidation of Cr-III to Cr-VI in aqueous suspensions of Na-buserite
(Na4Mn14O27. 9H(2)O) has been investigated as a function of the solut
ion pH and solids concentration. The rate of Cr-VI formation in soluti
on exhibits two apparent domains of rate control. At low solids concen
trations the rate of reaction appears to be controlled by the transfer
of an electron from Cr-III to the solid. At high solids concentration
s the rate of Cr-VI formation appears to be controlled by the octahedr
al to tetrahedral coordination change that must occur during the oxida
tion of Cr-III to Cr-VI. A weak dependence of the rate of oxidation on
the solution pH is observed, which is interpreted as evidence for an
outer-sphere electron transfer process between Cr-III and the solid. N
a-buserite pre-equilibrated at low pH (H-buserite) reacts considerably
more slowly with Cr-III. This observation is correlated with an appar
ent retardation of Mn-II release from the H-buserite solid and suggest
s some equilibration of the aqueous chromium species with the solid ph
ase. An energy level model of electron transfer is presented which all
ows some quantitative understanding of both the pH dependence of this
reaction and the reasons for the reduced reactivity of the H-buserite
phase.