Articles | Volume 9, issue 18
Atmos. Chem. Phys., 9, 7161–7182, 2009

Special issue: MILAGRO/INTEX-B 2006

Atmos. Chem. Phys., 9, 7161–7182, 2009

  28 Sep 2009

28 Sep 2009

Chemically-resolved aerosol volatility measurements from two megacity field studies

J. A. Huffman2,*,1, K. S. Docherty1, A. C. Aiken2,1, M. J. Cubison1, I. M. Ulbrich2,1, P. F. DeCarlo1, D. Sueper3,1, J. T. Jayne3, D. R. Worsnop3, P. J. Ziemann4, and J. L. Jimenez2,1 J. A. Huffman et al.
  • 1Cooperative Institute for Research in Environmental Sciences (CIRES), Boulder, Colorado, USA
  • 2Department of Chemistry and Biochemistry, University of Colorado, Boulder, Colorado, PSI, USA
  • 3Aerodyne Research, Inc., Billerica, Massachusetts, USA
  • 4Air Pollution Research Center, University of California-Riverside, USA
  • *now at: Max Planck Institute for Chemistry, Mainz, Germany
  • **now at: Paul Scherrer Institute (PSI), Villigen, Switzerland

Abstract. The volatilities of different chemical species in ambient aerosols are important but remain poorly characterized. The coupling of a recently developed rapid temperature-stepping thermodenuder (TD, operated in the range 54–230°C) with a High-Resolution Time-of-Flight Aerosol Mass Spectrometer (HR-ToF-AMS) during field studies in two polluted megacities has enabled the first direct characterization of chemically-resolved urban particle volatility. Measurements in Riverside, CA and Mexico City are generally consistent and show ambient nitrate as having the highest volatility of any AMS standard aerosol species while sulfate showed the lowest volatility. Total organic aerosol (OA) showed volatility intermediate between nitrate and sulfate, with an evaporation rate of 0.6%·K−1 near ambient temperature, although OA dominates the residual species at the highest temperatures. Different types of OA were characterized with marker ions, diurnal cycles, and positive matrix factorization (PMF) and show significant differences in volatility. Reduced hydrocarbon-like OA (HOA, a surrogate for primary OA, POA), oxygenated OA (OOA, a surrogate for secondary OA, SOA), and biomass-burning OA (BBOA) separated with PMF were all determined to be semi-volatile. The most aged OOA-1 and its dominant ion, CO2+, consistently exhibited the lowest volatility, with HOA, BBOA, and associated ions for each among the highest. The similar or higher volatility of HOA/POA compared to OOA/SOA contradicts the current representations of OA volatility in most atmospheric models and has important implications for aerosol growth and lifetime. A new technique using the AMS background signal was demonstrated to quantify the fraction of species up to four orders-of-magnitude less volatile than those detectable in the MS mode, which for OA represent ~5% of the non-refractory (NR) OA signal. Our results strongly imply that all OA types should be considered semivolatile in models. The study in Riverside identified organosulfur species (e.g. CH3HSO3+ ion, likely from methanesulfonic acid), while both studies identified ions indicative of amines (e.g. C5H12N+) with very different volatility behaviors than inorganic-dominated ions. The oxygen-to-carbon ratio of OA in each ambient study was shown to increase both with TD temperature and from morning to afternoon, while the hydrogen-to-carbon ratio showed the opposite trend.

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