Biogenic, urban, and wildfire influences on the molecular composition of dissolved organic compounds in cloud water
Ryan D. Cook1,*,Ying-Hsuan Lin1,2,a,*,Zhuoyu Peng1,b,Eric Boone1,c,Rosalie K. Chu3,James E. Dukett4,Matthew J. Gunsch1,Wuliang Zhang1,d,Nikola Tolic3,Alexander Laskin3,e,and Kerri A. Pratt1,5Ryan D. Cook et al.Ryan D. Cook1,*,Ying-Hsuan Lin1,2,a,*,Zhuoyu Peng1,b,Eric Boone1,c,Rosalie K. Chu3,James E. Dukett4,Matthew J. Gunsch1,Wuliang Zhang1,d,Nikola Tolic3,Alexander Laskin3,e,and Kerri A. Pratt1,5
Received: 04 Jul 2017 – Discussion started: 22 Aug 2017 – Revised: 28 Oct 2017 – Accepted: 02 Nov 2017 – Published: 21 Dec 2017
Abstract. Organic aerosol formation and transformation occurs within aqueous aerosol and cloud droplets, yet little is known about the composition of high molecular weight organic compounds in cloud water. Cloud water samples collected at Whiteface Mountain, New York, during August–September 2014 were analyzed by ultra-high-resolution mass spectrometry to investigate the molecular composition of dissolved organic carbon, with a focus on sulfur- and nitrogen-containing compounds. Organic molecular composition was evaluated in the context of cloud water inorganic ion concentrations, pH, and total organic carbon concentrations to gain insights into the sources and aqueous-phase processes of the observed high molecular weight organic compounds. Cloud water acidity was positively correlated with the average oxygen : carbon ratio of the organic constituents, suggesting the possibility for aqueous acid-catalyzed (prior to cloud droplet activation or during/after cloud droplet evaporation) and/or radical (within cloud droplets) oxidation processes. Many tracer compounds recently identified in laboratory studies of bulk aqueous-phase reactions were identified in the cloud water. Organosulfate compounds, with both biogenic and anthropogenic volatile organic compound precursors, were detected for cloud water samples influenced by air masses that had traveled over forested and populated areas. Oxidation products of long-chain (C10−12) alkane precursors were detected during urban influence. Influence of Canadian wildfires resulted in increased numbers of identified sulfur-containing compounds and oligomeric species, including those formed through aqueous-phase reactions involving methylglyoxal. Light-absorbing aqueous-phase products of syringol and guaiacol oxidation were observed in the wildfire-influenced samples, and dinitroaromatic compounds were observed in all cloud water samples (wildfire, biogenic, and urban-influenced). Overall, the cloud water molecular composition depended on air mass source influence and reflected aqueous-phase reactions involving biogenic, urban, and biomass burning precursors.
Reactions occur within water in both atmospheric particles and cloud droplets, yet little is known about the organic compounds in cloud water. In this work, cloud water samples were collected at Whiteface Mountain, New York, and analyzed using ultra-high-resolution mass spectrometry to investigate the molecular composition of the dissolved organic compounds. The results focus on changes in cloud water composition with air mass origin – influences of forest, urban, and wildfire emissions.
Reactions occur within water in both atmospheric particles and cloud droplets, yet little is...