Abstract

Abstract. Little is known about the effects of subzero temperatures on the formation of secondary organic aerosol (SOA) from α-pinene. In the current work, ozone-initiated oxidation of α-pinene at initial concentrations of 10 and 50 ppb, respectively, is performed at temperatures of 20, 0, and −15 ∘C in the Aarhus University Research on Aerosol (AURA) smog chamber during the Aarhus Chamber Campaign on Highly Oxygenated Organic Molecules and Aerosols (ACCHA). Herein, we show how temperature influences the formation and chemical composition of α-pinene-derived SOA with a specific focus on the formation of organic acids and dimer esters. With respect to particle formation, the results show significant increase in particle-formation rates, particle number concentrations, and particle mass concentrations at low temperatures. In particular, the number concentrations of sub-10 nm particles were significantly increased at the lower 0 and −15 ∘C temperatures. Temperature also affects the chemical composition of formed SOA. Here, detailed offline chemical analyses show that organic acids contribute from 15 % to 30 % by mass, with highest contributions observed at the lowest temperatures, indicative of enhanced condensation of these semivolatile species. In comparison, a total of 30 identified dimer esters were seen to contribute between 4 % and 11 % to the total SOA mass. No significant differences in the chemical composition (i.e. organic acids and dimer esters) of the α-pinene-derived SOA particles are observed between experiments performed at 10 and 50 ppb initial α-pinene concentrations, thus suggesting a higher influence of reaction temperature compared to that of α-pinene loading on the SOA chemical composition. Interestingly, the effect of temperature on the formation of dimer esters differs between the individual species. The formation of less oxidized dimer esters – with oxygen-to-carbon ratio (O:C)<0.4 – is shown to increase at low temperatures, while the formation of the more oxidized species (O:C>0.4) is suppressed, consequently resulting in temperature-modulated composition of the α-pinene-derived SOA. Temperature ramping experiments exposing α-pinene-derived SOA to changing temperatures (heating and cooling) reveal that the chemical composition of the SOA with respect to dimer esters is governed almost solely by the temperature at which oxidization started and is insusceptible to subsequent changes in temperature. Similarly, the resulting SOA mass concentrations were found to be more influenced by the initial α-pinene oxidation temperatures, thus suggesting that the formation conditions to a large extent govern the type of SOA formed, rather than the conditions to which the SOA is later exposed. For the first time, we discuss the relation between the identified dimer ester and the highly oxygenated organic molecules (HOMs) measured by chemical ionization–atmospheric pressure interface–time-of-flight mass spectrometer (CI-APi-ToF) during the ACCHA experiments. We propose that, although very different in chemical structures and O:C ratios, many dimer esters and HOMs may be linked through similar RO2 reaction pathways and that dimer esters and HOMs merely represent two different fates of the RO2 radicals.

Highlights

  • The oxidation of volatile organic compounds (VOCs) constitutes an important source of secondary organic aerosol (SOA) in the atmosphere

  • This is supported by higher concentration of semivolatile organic acids, such as pinic acid and pinonic acid, in SOA particles formed at 0 ◦C and −15 ◦C compared to particles formed at 20 ◦C

  • These results indicate that temperature affects the formation of SOA mass in the atmosphere and alters the chemical composition through condensation and evaporation of semivolatile species, changes in the formation of highly oxygenated organic molecules (HOMs), and changes in the reaction pathways leading to the formation of dimer esters having high and low O : C ratios

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Summary

Introduction

The oxidation of volatile organic compounds (VOCs) constitutes an important source of secondary organic aerosol (SOA) in the atmosphere. (Sindelarova et al, 2014), the atmospheric oxidation of the biogenic VOC α-pinene has been widely studied. Lee et al (2020) and Zhang et al (2018) show that monoterpeneoriginated SOA are the largest sources of particulate matter in the southeastern US. For this reason, the oxidation of αpinene and subsequent formation of SOA is expected to occur at conditions with a wide range of VOC concentrations and atmospheric temperatures. The effect of subzero temperatures, on gas-phase oxidation products, nucleation, particle growth and particle chemical composition, remains a largely unexplored area (Huang et al, 2018; Stolzenburg et al, 2018)

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