Reactions of H2O3 in the Pulse-Irradiated Fe(II)–O2 System

Abstract
G[Fe(III)] is measured in pulse‐irradiated O2‐saturated solutions of 20 to 160 μMFe(II), at the pH's 0.46, 1.51, and 2.74 H2SO4 and HClO4 and with dose rates between 1 and 8 krad/1 μsec pulse. Based on homogeneous kinetics, the results are interpreted by a system of 18 reactions. The formation of the hydrogen sesquioxide H2O3 as an intermediate in the reaction OH + HO2→H2O3→H2O + O2 is confirmed. In the absence of Fe(II), G(H2O3) varies from 2.04 at pH 0.46 to 1.57 at pH 2.74. The rate constant k[H2O3+Fe(II)] = 6.0 × 1 4M−1·sec−1 at the pH's studied. The direct reaction, OH + HO2 = H2O + O2, does not take place. In H1SO4, at pH 0.46, 151, and 2.74 and in HClO4 at pH 0.46 and 1.51, the complexes of Fe(III) produced by the radiation reach equilibrium before they react with HO2. However, equilibrium is not reached in HClO4 at pH 2.74, where the effective rate constant k(HO2+Fe(III)] is 6.2 times its value when Fe(III) is in its equilibrium form. This ratio is constant over the dose rate range studied. With dose rates up to 64 krad/1.4 μsec pulse G[Fe(III)] and G(H2) were measured in the air saturated 1‐mM FeSO4 dosimeter and G[Fe(III)] in the O2 saturated 10‐mM FeSO4 dosimeter, each in 0.4MH2SO4 . G[Fe(III)] decreases in both dosimeters less rapidly with increasing dose rate than was found by earlier workers. The principal reason for the decrease is the failure of O2 to scavenge the H atoms at high dose rates. Excellent agreement is obtained between experiment and theory except at high dose rates, where the calculated G[Fe(III)]'s are slightly too high in both dosimeters.