Oxidation of CoII by HSO5– to CoIII in weakly acidic solution, in the presence of molybdate, resulted in the formation of (primarily) the soluble dicobalt species [H4Co2Mo10O38]6–. The kinetics of formation of this species was examined at 15–35 °C over the range pH 4.0–5.5 and found to exhibit three separate kinetically observable steps, oxidation of CoII to CoIII, followed by a ligand-breakdown reaction and a slow ligand-replacement step which produces the observed product(s). The first stage followed the expanded rate expression +d[CoIII]/dt=kox[Co2+][HSO5–]/[H+][HMoO4–]3. A value for kox of 7.05(4)× 10–14 mol3 dm–9 s–1 at 25 °C was calculated using reported formation constants describing the speciation of [MoO4]2–, [Mo7O24]6–, and their protonated forms in solution. This rate expression may be accounted for by a mechanism arising from a series of pre-equilibria involving the loss of three [HMoO4]– units and a H+ from a cobalt(II) heteropolymolybdate, most likely [H6CoMo6O24]4–, which then allows the one-electron oxidation of Co2+ to Co3+ by HSO5– to occur following co-ordination of the latter. In keeping with this proposal, [NH4]4[H6CoMo6O24]· 4H2O was crystallized from an acidic (pH 4.5) solution containing Co2+(aq) and molybdate, and its structure determined by X-ray diffraction methods. The heteropolymetalate anion exhibits a standard Anderson structure with six octahedral molybdate edge-sharing units surrounding the central cobalt, and all metal atoms effectively in a common plane. The second observable kinetic step shows no dependences on [Co3+], [oxidant], pH or [molybdate], and is interpreted as a ligand-breakdown reaction, involving loss of an OH˙ radical from the co-ordinated ‘HSO52–’(radical) present following the actual one-electron oxidation step. Dimerization is then assumed to occur, followed by slow [H4Co2Mo10O38]6– formation stemming from further reaction of the immediate product of the dimerization step, involving loss of co-ordinated SO42–.
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Nolan et al. (1996) studied this question.
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