Photolysis of ferric ions in the presence of sulfate or chloride ions: implications for the photo-Fenton process

The photo-Fenton process (Fe 2+ /Fe 3+ , H 2 O 2 , UV light) is one of the most efficient and advanced oxidation processes for the mineralization of the organic pollutants of industrial effluents and wastewater. The overall rate of the photo-Fenton process is controlled by the rate of the photolytic step that converts Fe 3+ back to Fe 2+ . In this paper, the effect of sulfate or chloride ions on the net yield of Fe 2+ during the photolysis of Fe 3+ has been investigated in aqueous solution at pH 3.0 and 1.0 in the absence of hydrogen peroxide. A kinetic model based on the principal reactions that occur in the system fits the data for formation of Fe 2+ satisfactorily. Both experimental data and model prediction show that the availability of Fe 2+ produced by photolysis of Fe 3+ is inhibited much more in the presence of sulfate ion than in the presence of chloride ion as a function of the irradiation time at pH 3.0.