Articles | Volume 17, issue 2
Atmos. Chem. Phys., 17, 1453–1469, 2017
Atmos. Chem. Phys., 17, 1453–1469, 2017
Research article
31 Jan 2017
Research article | 31 Jan 2017

Real-time detection of highly oxidized organosulfates and BSOA marker compounds during the F-BEACh 2014 field study

Martin Brüggemann1,2,a, Laurent Poulain3, Andreas Held4, Torsten Stelzer1, Christoph Zuth1, Stefanie Richters3, Anke Mutzel3, Dominik van Pinxteren3, Yoshiteru Iinuma3, Sarmite Katkevica4, René Rabe3, Hartmut Herrmann3, and Thorsten Hoffmann1 Martin Brüggemann et al.
  • 1Institute of Inorganic and Analytical Chemistry, University of Mainz, Duesbergweg 10–14, 55128 Mainz, Germany
  • 2Max Planck Graduate Center, Staudinger Weg 9, 55128 Mainz, Germany
  • 3Leibniz-Institut für Troposphärenforschung (TROPOS), Permoserstr. 15, 04318 Leipzig, Germany
  • 4University of Bayreuth, Atmospheric Chemistry, Dr.-Hans-Frisch-Straße 1–3, 95448 Bayreuth, Germany
  • anow at: CNRS – UMR5256, IRCELYON, Institut de Recherches sur la Catalyse et l'Environnement de Lyon, 69626 Villeurbanne, France

Abstract. The chemical composition of ambient organic aerosols was analyzed using complementary mass spectrometric techniques during a field study in central Europe in July 2014 (Fichtelgebirge – Biogenic Emission and Aerosol Chemistry, F-BEACh 2014). Among several common biogenic secondary organic aerosol (BSOA) marker compounds, 93 acidic oxygenated hydrocarbons were detected with elevated abundances and were thus attributed to be characteristic for the organic aerosol mass at the site. Monoterpene measurements exhibited median mixing ratios of 1.6 and 0.8 ppbV for in and above canopy levels respectively. Nonetheless, concentrations for early-generation oxidation products were rather low, e.g., pinic acid (c  =  4.7 (±2.5) ng m−3). In contrast, high concentrations were found for later-generation photooxidation products such as 3-methyl-1,2,3-butanetricarboxylic acid (MBTCA, c  =  13.8 (±9.0) ng m−3) and 3-carboxyheptanedioic acid (c  =  10.2 (±6.6) ng m−3), suggesting that aged aerosol masses were present during the campaign period. In agreement, HYSPLIT trajectory calculations indicate that most of the arriving air masses traveled long distances (>  1500 km) over land with high solar radiation.

In addition, around 47 % of the detected compounds from filter sample analysis contained sulfur, confirming a rather high anthropogenic impact on biogenic emissions and their oxidation processes. Among the sulfur-containing compounds, several organosulfates, nitrooxy organosulfates, and highly oxidized organosulfates (HOOS) were tentatively identified by high-resolution mass spectrometry. Correlations among HOOS, sulfate, and highly oxidized multifunctional organic compounds (HOMs) support the hypothesis of previous studies that HOOS are formed by reactions of gas-phase HOMs with particulate sulfate. Moreover, periods with high relative humidity indicate that aqueous-phase chemistry might play a major role in HOOS production. However, for dryer periods, coinciding signals for HOOS and gas-phase peroxyradicals (RO2) were observed, suggesting RO2 to be involved in HOOS formation.

Short summary
Using complementary mass spectrometric techniques during a field study in central Europe, characteristic contributors to the organic aerosol mass were identified. Besides common marker compounds for biogenic secondary organic aerosol, highly oxidized sulfur species were detected in the particle phase. High-time-resolution measurements revealed correlations between these organosulfates and particulate sulfate as well as gas-phase peroxyradicals, giving hints to underlying formation mechanisms.
Final-revised paper