This research demonstrates carbonate's photoactivation to generate radicals in the atmosphere, implying potential for atmospheric oxidizing capacity.
Carbonate is a common component of soil and coarse atmospheric particulate matter, while few studies have focused on its photochemical reactivity. We present a novel photoactivation mechanism of carbonate and O2 in the absence of additional potent oxidants. Under light conditions, carbonate ions (CO32-), O2, and H3O+/OH- could spontaneously form a complex and generate CO3- and HO2/O2- radicals through an electron transfer process. Under these conditions, the H2O2 production in 1 mM Na2CO3 solution was 0.37 ± 0.10 μg·L-1 and the cumulative concentration of OH radicals in 4 h was 34.6 nM. The proposed mechanism could be a potential source of atmospheric oxidizing capacity, and the reactive species produced by the CO32--O2 photoactivation process could promote secondary sulfate production. Our findings underscore the importance of carbonate atmospheric reactivity, especially at special reaction surfaces such as air-water interfaces and microdroplets.
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Cao et al. (2025) studied this question.
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