
%0 Journal Article
%A Matthews, RW 
%T The radiation chemistry of aqueous ferrous sulfate solutions at natural pH
%J Australian Journal of Chemistry
%D 1983/07/01
%V 36
%N 7
%P 1305-1317
%K 
%R https://doi.org/10.1071/CH9831305
%U https://www.publish.csiro.au/paper/CH9831305 
%X The yield of FeIII species has been determined in FeSO4 solutions irradiated at natural pH with 60Co &#947;-rays for a wide range of solute conditions. The stoichiometry of the hydrogen peroxide reaction was investigated and found to be abnormal if H2O2 is present in excess. If, however, FeS04 is present in excess, as it is in the irradiation of FeSO4 solutions, deviations from the normal stoichiometry are trivial. In nitrous oxide saturated solutions initial G(FeIII) values were found to be from 6.90 to 7.72 for FeSO4 concentrations in the range (0.5-2.0) &#215; 10-3 M. Non-linearity in the yield of ferric ion concentration against dose plots was attributed to competition between hydrogen atom reduction of ferric species with hydrogen atom oxidation of ferrous species. The reaction between hydrogen atom and the ferric species was estimated to be close to diffusion controlled. In aerated solutions, the FeIII yield was, within experimental error, a linear function of dose for FeSO4 concentrations in the range (0.5 - 2.0) &#215; 10.-3 M with G(FeIII) values of 12.27 &#177; 0.06, 12.62 &#177; 0.07 and 12.77 &#177; 0.10 for 0.5, 1.0 and 2.0 &#215; M respectively. At lower FeSO4 concentrations. deviation from linearity was noticeable. The deviation was attributed to competition between FeII and FeIII species for the O2- radical anion. k(O2-&#183; + FeII)/k(O2-&#183;+ FeIII) was determined to be about 4.0. In deaerated solu- tion, the FeIII yield against absorbed dose for 1 &#215; M FeSO4 solution was followed to extended doses. A limiting FeIII yield of about 0.75 times the aerated solution yield was observed in the closed system. The data were quite well described by values calculated from the reaction mechanism, published rate constants and the rate ratio of 0.016 for k(H&#183; + FeII)/k(H&#183; + FeIII) determined from the N2O experiments, and demonstrate the importance of reducing radical reactions with insoluble ferric species. 
