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Multiple field studies have led to suggestions that nitrate radical (NO3) participates in oxidizing gaseous Hg(0) in the atmosphere. These suppositions are hard to reconcile with the two-step mechanism of Hg(0) conversion to Hg(II) via Hg(I), due to the instability of the NO3-Hg(I). We use a high level of computational chemistry to determine its bond energy as 6.5 kcal mol-1. We use statistical mechanics to compute the equilibrium constant, Kc(T) for NO3 + Hg(0) = NO3Hg(I), and a box model to investigate a field study and laboratory kinetic investigation of this chemistry. Under the conditions of the one field study showing a correlation between [NO3] and [Hg(II) (g)] , NO3 could not have contributed significantly to the formation of Hg(II). In addition, we find that the one experimental kinetic study of this reaction does not constrain the rate constant.
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Edirappulige et al. (2024) studied this question.
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