Abstract

Ice plays a crucial role in contaminant transformation in seasonally ice-covered waters. In this study, the characteristics and mechanisms of an emerging contaminant oxcarbazepine (OXC) degradation by a disinfection by-product bromate (BrO3–) in ice were explored via combined experiments and theoretical calculations. Results showed that 74.0 % and 86.4 % of OXC was degraded by BrO3– in ice after 140 min in dark and 120 min under solar irradiation, respectively, while the reaction was negligible in water. The oxidation-reduction potential of BrO3– solution at 1000 μmol L−1 was 56.9 % higher than that at 50 μmol L−1. The oxidation-reduction potential of BrO3– solution at pH 2 was 14.8 %–109.5 % higher than those at other pH values. Enhanced OXC degradation by BrO3– in ice could be attributed to increased BrO3– oxidation capacity resulting from locally elevated BrO3– and H+ concentrations. Hypobromous acid (HOBr), •OH, and Br• generated by direct photolysis under solar irradiation further promoted the OXC degradation in ice. Br• formed by the direct photolysis of accumulated HOBr under solar irradiation caused the generation of bromine-containing degradation products. Bromine-containing degradation products possessed higher potential toxicities, which could contribute to increase the secondary pollution of water environment.

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