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      Particulate nitrate photolysis in the atmosphere

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          Abstract

          Particulate nitrate photolysis can lead to the formation of secondary inorganic and organic aerosols that affect climate, air quality, and human health.

          Abstract

          Multiphase and heterogeneous photochemistry is an emerging component of atmospheric and air pollution research. It is primarily driven by reactions of photochemically produced free radicals in the particle phase with dissolved gaseous species. It has significant implications to promote the oxidation of aerosol particles, one of the most important atmospheric processes for secondary inorganic and organic aerosol formation. Nitrate is an increasingly important component in atmospheric aerosol particles with the trend of dominating over sulfate. Nitrate photolysis has long been known to produce highly reactive oxidants such as hydroxyl radicals in both gas and bulk or cloud phases. Recent studies have found that nitrate photolysis in the particle phase ( i.e., particulate nitrate photolysis) proceeds faster than bulk solutions or cloud droplets by many orders of magnitude. Factors and mechanisms affecting particulate nitrate photolysis include the formation of solvent cages, pH, and co-existing species, but they remain controversial. Hence, the impact of nitrate photolysis in atmospheric chemistry is still uncertain. This paper reviews the current status of knowledge about the effects of particulate nitrate photolysis, instead of relatively well-known gas- and bulk-phase nitrate photolysis, in the atmosphere. Recommendations for future research directions on the mechanistic understanding of particulate nitrate photolysis and its parameterizations in air quality models are also made.

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          Organic aerosol (OA) particles affect climate forcing and human health, but their sources and evolution remain poorly characterized. We present a unifying model framework describing the atmospheric evolution of OA that is constrained by high-time-resolution measurements of its composition, volatility, and oxidation state. OA and OA precursor gases evolve by becoming increasingly oxidized, less volatile, and more hygroscopic, leading to the formation of oxygenated organic aerosol (OOA), with concentrations comparable to those of sulfate aerosol throughout the Northern Hemisphere. Our model framework captures the dynamic aging behavior observed in both the atmosphere and laboratory: It can serve as a basis for improving parameterizations in regional and global models.
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              Compilation of Henry's law constants (version 4.0) for water as solvent

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                Author and article information

                Contributors
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                Journal
                ESANC9
                Environmental Science: Atmospheres
                Environ. Sci.: Atmos.
                Royal Society of Chemistry (RSC)
                2634-3606
                March 17 2022
                2022
                : 2
                : 2
                : 111-127
                Affiliations
                [1 ]Faculty of Frontier Engineering, Institute of Science and Engineering, Kanazawa University, Kanazawa, 920-1192, Japan
                [2 ]School of Energy and Environment, City University of Hong Kong, Hong Kong, China
                [3 ]City University of Hong Kong Shenzhen Research Institute, Shenzhen, China
                [4 ]Guy Carpenter Asia-Pacific Climate Impact Center, City University of Hong Kong, Hong Kong, China
                Article
                10.1039/D1EA00087J
                b3be322f-087f-4b03-9f0a-55566d9ec5eb
                © 2022

                http://creativecommons.org/licenses/by/3.0/

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