Effects of liquid–liquid phase separation and relative humidity on the heterogeneous OH oxidation of inorganic–organic aerosols: insights from methylglutaric acid and ammonium sulfate particles
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Published:2021-02-11
Issue:3
Volume:21
Page:2053-2066
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Lam Hoi Ki, Xu Rongshuang, Choczynski Jack, Davies James F., Ham Dongwan, Song Mijung, Zuend AndreasORCID, Li Wentao, Tse Ying-Lung Steve, Chan Man Nin
Abstract
Abstract. Organic compounds residing near the surface of atmospheric aerosol particles
are exposed to chemical reactions initiated by gas-phase oxidants, such as
hydroxyl (OH) radicals. Aqueous droplets composed of inorganic salts and
organic compounds can undergo phase separation into two liquid phases,
depending on aerosol composition and relative humidity (RH). Such phase
behavior can govern the surface characteristics and morphology of the
aerosols, which in turn affect the heterogeneous reactivity of organic
compounds toward gas-phase oxidants. In this work, we used an aerosol flow
tube reactor coupled with an atmospheric pressure ionization source (direct
analysis in real time) and a high-resolution mass spectrometer to
investigate how phase separation in model aqueous droplets containing an
inorganic salt (ammonium sulfate, AS) and an organic acid (3-methylglutaric
acid, 3-MGA) with an organic-to-inorganic dry mass ratio (OIR) of 1 alters
the heterogeneous OH reactivity. At high RH, 3-MGA/AS aerosols were aqueous
droplets with a single liquid phase. When the RH decreased, aqueous 3-MGA/AS
droplets underwent phase separation at ∼75 % RH. Once the
droplets were phase-separated, they exhibited either a core–shell,
partially engulfed or a transition from core–shell to partially engulfed
structure, with an organic-rich outer phase and an inorganic-rich inner
phase. The kinetics, quantified by an effective heterogenous OH rate
constant, was found to increase gradually from 1.01±0.02×10-12 to 1.73±0.02×10-12 cm3 molec.−1 s−1 when the RH decreased from 88 % to 55 %. The heterogeneous reactivity of phase-separated droplets is slightly
higher than that of aqueous droplets with a single liquid phase. This could
be explained by the finding that when the RH decreases, higher
concentrations of organic molecules (i.e., 3-MGA) are present at or near the
droplet surface, which are more readily exposed to OH oxidation, as
demonstrated by phase separation measurements and model simulations. This
could increase the reactive collision probability between 3-MGA molecules
and OH radicals dissolved near the droplet surface and secondary chain
reactions. Even for phase-separated droplets with a fully established
core–shell structure, the diffusion rate of organic molecules across the
organic-rich outer shell is predicted to be fast in this system. Thus, the
overall rate of reactions is likely governed by the surface concentration of
3-MGA rather than a diffusion limitation. Overall, understanding the aerosol
phase state (single liquid phase versus two separate liquid phases) is
essential to better probe the heterogenous reactivity under different
aerosol chemical composition and environmental conditions (e.g., RH).
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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