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Formation of brown carbon via reactions of ammonia with secondary organic aerosols from biogenic and anthropogenic precursors
Abstract Filter samples of secondary organic aerosols (SOA) generated from the ozone (O3)- and hydroxyl radical (OH)-initiated oxidation of various biogenic (isoprene, α-pinene, limonene, α-cedrene, α-humulene, farnesene, pine leaf essential oils, cedar leaf essential oils) and anthropogenic (tetradecane, 1,3,5-trimethylbenzene, naphthalene) precursors were exposed to humid air containing approximately 100 ppb of gaseous ammonia (NH3). Reactions of SOA compounds with NH3 resulted in production of light-absorbing “brown carbon” compounds, with the extent of browning ranging from no observable change (isoprene SOA) to visible change in color (limonene SOA). The aqueous phase reactions with dissolved ammonium (NH4 +) salts, such as ammonium sulfate, were equally efficient in producing brown carbon. Wavelength-dependent mass absorption coefficients (MAC) of the aged SOA were quantified by extracting known amounts of SOA material in methanol and recording its UV/Vis absorption spectra. For a given precursor, the OH-generated SOA had systematically lower MAC compared to the O3-generated SOA. The highest MAC values, for brown carbon from SOA resulting from O3 oxidation of limonene and sesquiterpenes, were comparable to MAC values for biomass burning particles but considerably smaller than MAC values for black carbon aerosols. The NH3/NH4 + + SOA brown carbon aerosol may contribute to aerosol optical density in regions with elevated concentrations of NH3 or ammonium sulfate and high photochemical activity.
Graphical abstract Display Omitted Highlights ► Secondary organic aerosols change color from white to brown in presence of ammonia. ► Browning reaction occurs for a wide range of biogenic and anthropogenic aerosols. ► Aqueous reaction with ammonium ion is equally efficient in producing brown carbon. ► The mass absorption coefficient is comparable to that of biomass burning aerosols. ► Secondary brown carbon may contribute to absorption of solar radiation by aerosols.
Formation of brown carbon via reactions of ammonia with secondary organic aerosols from biogenic and anthropogenic precursors
Abstract Filter samples of secondary organic aerosols (SOA) generated from the ozone (O3)- and hydroxyl radical (OH)-initiated oxidation of various biogenic (isoprene, α-pinene, limonene, α-cedrene, α-humulene, farnesene, pine leaf essential oils, cedar leaf essential oils) and anthropogenic (tetradecane, 1,3,5-trimethylbenzene, naphthalene) precursors were exposed to humid air containing approximately 100 ppb of gaseous ammonia (NH3). Reactions of SOA compounds with NH3 resulted in production of light-absorbing “brown carbon” compounds, with the extent of browning ranging from no observable change (isoprene SOA) to visible change in color (limonene SOA). The aqueous phase reactions with dissolved ammonium (NH4 +) salts, such as ammonium sulfate, were equally efficient in producing brown carbon. Wavelength-dependent mass absorption coefficients (MAC) of the aged SOA were quantified by extracting known amounts of SOA material in methanol and recording its UV/Vis absorption spectra. For a given precursor, the OH-generated SOA had systematically lower MAC compared to the O3-generated SOA. The highest MAC values, for brown carbon from SOA resulting from O3 oxidation of limonene and sesquiterpenes, were comparable to MAC values for biomass burning particles but considerably smaller than MAC values for black carbon aerosols. The NH3/NH4 + + SOA brown carbon aerosol may contribute to aerosol optical density in regions with elevated concentrations of NH3 or ammonium sulfate and high photochemical activity.
Graphical abstract Display Omitted Highlights ► Secondary organic aerosols change color from white to brown in presence of ammonia. ► Browning reaction occurs for a wide range of biogenic and anthropogenic aerosols. ► Aqueous reaction with ammonium ion is equally efficient in producing brown carbon. ► The mass absorption coefficient is comparable to that of biomass burning aerosols. ► Secondary brown carbon may contribute to absorption of solar radiation by aerosols.
Formation of brown carbon via reactions of ammonia with secondary organic aerosols from biogenic and anthropogenic precursors
Updyke, Katelyn M. (author) / Nguyen, Tran B. (author) / Nizkorodov, Sergey A. (author)
Atmospheric Environment ; 63 ; 22-31
2012-09-09
10 pages
Article (Journal)
Electronic Resource
English