Sj. Angusdunne et al., REACTION-KINETICS AND MECHANISM OF FORMATION OF [MNMO9O32]6- BY HYPOCHLOROUS ACID OXIDATION OF MN2+ (AQ) IN THE PRESENCE OF MOLYBDATE, Journal of the Chemical Society. Dalton transactions, (18), 1993, pp. 2717-2726
Oxidation of Mn2+ (aq) by HOCl in weakly acidic solution, in the prese
nce of molybdate, results in the formation of the soluble heteropolymo
lybdate [MnMo9O32]6-. The speciation of Mn2+ in solution prior to oxid
ation has been examined using ESR spectroscopy and it has been establi
shed that the principal species is [Mn(OH2)6]2+, there being evidence
for weak interactions only with molybdate and isopolymolybdate anions.
In keeping with this conclusion, the secondary manganese(II) polymoly
bdate species Na4[MnMo8O27].2OH2O Was crystallized from an acidic (pH
4.5) solution containing Mn2+ (aq) and isopolymolybdate ions by slow v
apour diffusion of ethanol into the aqueous phase. The compound crysta
llizes in the triclinic space group P1BAR, a = 9.568(2), b = 9.868(2),
c = 11.703(3) angstrom, alpha = 103.60(1), beta = 100.86(1) and gamma
= 96.05(1)-degrees, and the structure was determined by X-ray diffrac
tion methods to an R of 0.026 (R' = 0.040) for 3182 independent observ
ed reflections. It consists of polymerized octamolybdate units linked
through the sharing of common oxygen atoms and hydrated Mn2+ groups re
sulting in a sheet structure, with hydrated Na+ ions also attached to
the octamolybdate units. Uncomplexed water is also present. The kineti
cs of oxidation of Mn(II) by HOCl was studied at 5-20-degrees-C over t
he range pH 4.0-5.4 and found to exhibit solution autocatalytic behavi
our. The oxidation kinetics followed the expanded rate expression +d[M
nMo9O326-]/dt = k(AC)[Mn2+][MnMo9O326-][HOCL]-[MoO42-][HMoO4-] based o
n an examination of [HOCl], pH and total [MoO42-] dependences, and arg
uments based on molybdate speciation under the reaction conditions. An
approximate value of k(AC) at 25-degrees-C, 1.36(10) x 10(8) dm12 mol
-4 s-1, was estimated from an extrapolated value of the second-order a
utocatalytic rate constant using an Arrhenius plot and the reported fo
rmation constants describing the speciation of molybdate, isopolymolyb
date and their protonated analogues in solution. A mechanism involving
sequential one-electron oxidation steps of Mn2+ through to Mn4+ via M
n3+, together with the equilibrium Mn2+ + Mn4+ half arrow right over h
alf arrow left 2Mn3+, which favours Mn2+ and Mn4+, is able to account
for the observed autocatalysis.