A Novel Pathway of Atmospheric Sulfate Formation Through Carbonate Radical
Yangyang LiuYue DengJiarong LiuXiaozhong FangTao WangKejian LiKedong GongAziz-Ur-Rahim BachaIqra NabiXiuhui ZhangC. GeorgeLiwu Zhang
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Abstract. Carbon dioxide is considered an inert gas that rarely participates in atmospheric chemical reactions. However, we show here that CO2 is involved in some important photo-oxidation reactions in the atmosphere through the formation of carbonate radicals (CO3∙-). This potentially active intermediate CO3∙- is routinely overlooked in atmospheric chemistry regarding its effect on sulfate formation. Present work demonstrates that SO2 uptake coefficient is enhanced by 17 times on mineral dust particles driven by CO3∙-. It can be produced through two routes over mineral dust surfaces: i) hydroxyl radical + CO32-; ii) holes (h+) + CO32-. Employing a suite of laboratory investigations of sulfate formation in the presence of carbonate radical on the model and authentic dust particles, field measurements of sulfate and (bi)carbonate ions within ambient PM, together with density functional theory (DFT) calculations for single electron transfer processes in terms of CO3∙--initiated S(IV) oxidation, a new role of carbonate radical in atmospheric chemistry is elucidated.Keywords:
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Hydroxyl value
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The hydroxyl radical plays a critical role in the chemistry of the lower atmosphere. Understanding its production, interconversion, and sinks is central to modeling and predicting the chemistry of the troposphere. The OH measurements made during the 1993 Tropospheric OH Photochemistry Experiment provide a detailed look at these mechanisms since NO x , j (O 3 ), RO 2 , HO 2 , nonmethane hydrocarbons (NMHC), and many other relevant species were measured simultaneously. The relationship of OH to NO x and to primary production is extensively examined. Close agreement with theory is shown in the NO x /OH relation with OH concentrations increasing with increasing NO to a maximum at 1–2 ppbv due to conversion of HO 2 to OH, and then OH decreasing with further increasing NO x due to conversion of NO 2 to HNO 3 . Close correlations of OH concentrations with primary production (water, ozone, j (O 3 )) are also shown both on average and on rapid timescales.
Hydroxyl radical
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