Electron transfer reactivity of the aqueous iron(IV)–oxo complex. Outer-sphere vs proton-coupled electron transfer
Here, the kinetics of oxidation of organic and inorganic reductants by aqueous iron(IV) ions, Fe IV (H 2 O) 5 O 2+ (hereafter Fe IV aq O 2+ ), are reported. The substrates examined include several water-soluble ferrocenes, hexachloroiridate(III), polypyridyl complexes M(NN) 3 2+ (M = Os, Fe and Ru; NN = phenanthroline, bipyridine and derivatives), HABTS–/ABTS 2– , phenothiazines, Co II (dmgBF 2 ) 2 , macrocyclic nickel(II) complexes, and aqueous cerium(III). Most of the reductants were oxidized cleanly to the corresponding one-electron oxidation products, with the exception of phenothiazines which produced the corresponding oxides in a single-step reaction, and polypyridyl complexes of Fe(II) and Ru(II) that generated ligand-modified products. Fe IV aq O 2+ oxidizes even Ce(III) (E 0 in 1 M HClO 4 = 1.7 V) with a rate constant greater than 10 4 M –1 s –1 . In 0.10 M aqueous HClO 4 at 25 °C, the reactions of Os(phen) 3 2+ (k = 2.5 × 10 5 M –1 s –1 ), IrCl 6 3– (1.6 × 10 6 ), ABTS 2– (4.7 × 10 7 ), and Fe(cp)(C 5 H 4 CH 2 OH) (6.4 × 10 7 ) appear to take place by outer sphere electron transfer (OSET). The rate constants for the oxidation of Os(phen) 3 2+ and of ferrocenes remained unchanged in the acidity range 0.05 < [H+] < 0.10 M, ruling out prior protonation of Fe IV aq O 2+ and further supporting the OSET assignment. A fit to Marcus cross-relation yielded a composite parameter (log k 22 + E 0 Fe /0.059) = 17.2 ± 0.8, where k 22 and E 0 Fe are the self-exchange rate constant and reduction potential, respectively, for the Fe IV aq O 2+ /Fe III aq O + couple. Comparison with literature work suggests k 22 < 10 –5 M –1 s –1 and thus E 0 (Fe IV aq O 2+ /Fe III aq O + ) > 1.3 V. For proton-coupled electron transfer, the reduction potential is estimated at E 0 (Fe IV aq O 2+ , H + /Fe III aq OH 2+ ) ≥ 1.95 V.