Molecular Understanding of the Enhancement in Organic Aerosol Mass at High Relative Humidity. 2023

Mihnea Surdu, and Houssni Lamkaddam, and Dongyu S Wang, and David M Bell, and Mao Xiao, and Chuan Ping Lee, and Dandan Li, and Lucía Caudillo, and Guillaume Marie, and Wiebke Scholz, and Mingyi Wang, and Brandon Lopez, and Ana A Piedehierro, and Farnoush Ataei, and Rima Baalbaki, and Barbara Bertozzi, and Pia Bogert, and Zoé Brasseur, and Lubna Dada, and Jonathan Duplissy, and Henning Finkenzeller, and Xu-Cheng He, and Kristina Höhler, and Kimmo Korhonen, and Jordan E Krechmer, and Katrianne Lehtipalo, and Naser G A Mahfouz, and Hanna E Manninen, and Ruby Marten, and Dario Massabò, and Roy Mauldin, and Tuukka Petäjä, and Joschka Pfeifer, and Maxim Philippov, and Birte Rörup, and Mario Simon, and Jiali Shen, and Nsikanabasi Silas Umo, and Franziska Vogel, and Stefan K Weber, and Marcel Zauner-Wieczorek, and Rainer Volkamer, and Harald Saathoff, and Ottmar Möhler, and Jasper Kirkby, and Douglas R Worsnop, and Markku Kulmala, and Frank Stratmann, and Armin Hansel, and Joachim Curtius, and André Welti, and Matthieu Riva, and Neil M Donahue, and Urs Baltensperger, and Imad El Haddad
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland.

The mechanistic pathway by which high relative humidity (RH) affects gas-particle partitioning remains poorly understood, although many studies report increased secondary organic aerosol (SOA) yields at high RH. Here, we use real-time, molecular measurements of both the gas and particle phase to provide a mechanistic understanding of the effect of RH on the partitioning of biogenic oxidized organic molecules (from α-pinene and isoprene) at low temperatures (243 and 263 K) at the CLOUD chamber at CERN. We observe increases in SOA mass of 45 and 85% with increasing RH from 10-20 to 60-80% at 243 and 263 K, respectively, and attribute it to the increased partitioning of semi-volatile compounds. At 263 K, we measure an increase of a factor 2-4 in the concentration of C10H16O2-3, while the particle-phase concentrations of low-volatility species, such as C10H16O6-8, remain almost constant. This results in a substantial shift in the chemical composition and volatility distribution toward less oxygenated and more volatile species at higher RH (e.g., at 263 K, O/C ratio = 0.55 and 0.40, at RH = 10 and 80%, respectively). By modeling particle growth using an aerosol growth model, which accounts for kinetic limitations, we can explain the enhancement in the semi-volatile fraction through the complementary effect of decreased compound activity and increased bulk-phase diffusivity. Our results highlight the importance of particle water content as a diluting agent and a plasticizer for organic aerosol growth.

UI MeSH Term Description Entries
D006813 Humidity A measure of the amount of WATER VAPOR in the air. Humidities
D000336 Aerosols Colloids with a gaseous dispersing phase and either liquid (fog) or solid (smoke) dispersed phase; used in fumigation or in inhalation therapy; may contain propellant agents. Aerosol
D000393 Air Pollutants Any substance in the air which could, if present in high enough concentration, harm humans, animals, vegetation or materials. Substances include GASES; PARTICULATE MATTER; and volatile ORGANIC CHEMICALS. Air Pollutant,Air Pollutants, Environmental,Environmental Air Pollutants,Environmental Pollutants, Air,Air Environmental Pollutants,Pollutant, Air,Pollutants, Air,Pollutants, Air Environmental,Pollutants, Environmental Air
D039821 Monoterpenes Compounds with a core of 10 carbons generally formed via the mevalonate pathway from the combination of 3,3-dimethylallyl pyrophosphate and isopentenyl pyrophosphate. They are cyclized and oxidized in a variety of ways. Due to the low molecular weight many of them exist in the form of essential oils (OILS, VOLATILE). Monoterpene,Monoterpenoid,Monoterpenoids

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