10 Oct 2022
10 Oct 2022

Volatility of aerosol particles from NO3 oxidation of various biogenic organic precursors

Emelie L. Graham1,, Cheng Wu1,a,, David M. Bell2, Amelie Bertrand2, Sophie L. Haslett1, Urs Baltensperger2, Imad El Haddad2, Radovan Krejci1, Ilona Riipinen1, and Claudia Mohr1 Emelie L. Graham et al.
  • 1Department of Environmental Science (ACES) and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
  • 2Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, 5232 Villigen, Switzerland
  • anow at: Department of Chemistry and Molecular Biology, University of Gothenburg, Gothenburg, Sweden
  • These authors contributed equally to this work.

Abstract. Secondary organic aerosol (SOA) is formed through the oxidation of volatile organic compounds (VOC), which can be of both natural and anthropogenic origin. While the hydroxyl radical (OH) and ozone (O3) are the main atmospheric oxidants during the day, the nitrate radical (NO3) becomes more important during the night time. Yet, atmospheric nitrate chemistry has received less attention compared to OH and O3.

The Nitrate Aerosol and Volatility Experiment (NArVE) aimed to study the NO3-induced SOA formation and evolution from three biogenic VOCs (BVOC), namely isoprene, α-pinene and β-caryophyllene. The volatility of aerosol particles was studied using isothermal evaporation chambers, temperature-dependent evaporation in a volatility tandem differential mobility analyzer (VTDMA), and thermal desorption in a filter inlet for gases and aerosols coupled to a chemical ionization mass spectrometer (FIGAERO-CIMS). Data from these three setups present a cohesive picture of the volatility of the SOA formed in the dark from the three biogenic precursors. Under our experimental conditions, the SOA formed from NO3 + α-pinene was generally more volatile than SOA from α-pinene ozonolysis, while the NO3 oxidation of isoprene produced similar, although slightly less volatile SOA than α-pinene under our experimental conditions. β-caryophyllene reactions with NO3 resulted in the least volatile species.

Three different parametrizations for estimating the saturation vapor pressure of the oxidation products were tested for reproducing the observed evaporation in a kinetic modelling framework. Our results show that the SOA from nitrate oxidation of α-pinene or isoprene is dominated by low volatility organic compounds (LVOC) and semivolatile organic compounds (SVOC), while the corresponding SOA from β-caryophyllene consists primarily of extremely low volatility organic compounds (ELVOC) and LVOC. The parameterizations yielded variable results in terms of reproducing the observed evaporation, and generally the comparisons pointed to a need for re-evaluating the treatment of the nitrate group in such parameterizations. Strategies for improving the predictive power of the volatility parameterizations, particularly in relation to the contribution from the nitrate group, are discussed.

Emelie L. Graham et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-1043', Gabriel Isaacman-VanWertz, 31 Oct 2022
  • RC2: 'Comment on egusphere-2022-1043', Anonymous Referee #2, 07 Nov 2022

Emelie L. Graham et al.

Emelie L. Graham et al.


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Short summary
The volatility of an aerosol particle is an important parameter for describing its atmospheric lifetime. We studied the volatility of secondary organic aerosols from nitrate initiated oxidation of three biogenic precursors with experimental methods and model simulations. We saw higher volatility than for the corresponding ozone system and our simulations produced variable results with different parameterizations which warrant for a re-evaluation of the treatment of the nitrate functional group.