Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in the Anthropocene

Haijie Tong; Pascale S. J. Lakey; Andrea M. Arangio; Joanna Socorro; Christopher J. Kampf; Thomas Berkemeier; William H. Brune; Ulrich Pöschl; Manabu Shiraiwa

doi:10.1039/C7FD00023E

Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in the Anthropocene†

Haijie Tong,

*^a Pascale S. J. Lakey,^a Andrea M. Arangio,^a Joanna Socorro,^a Christopher J. Kampf,

^ab Thomas Berkemeier,^c William H. Brune,^d Ulrich Pöschl^a and Manabu Shiraiwa*^ae

Author affiliations

* Corresponding authors

^a Multiphase Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
E-mail: h.tong@mpic.de

^b Institute for Organic Chemistry, Johannes Gutenberg University, Mainz, Germany

^c School of Chemical & Biomolecular Engineering, Georgia Institute of Technology, Atlanta, USA

^d Department of Meteorology, Pennsylvania State University, University Park, PA, USA

^e Department of Chemistry, University of California, Irvine, CA, USA
E-mail: m.shiraiwa@uci.edu

Abstract

Mineral dust and secondary organic aerosols (SOA) account for a major fraction of atmospheric particulate matter, affecting climate, air quality and public health. How mineral dust interacts with SOA to influence cloud chemistry and public health, however, is not well understood. Here, we investigated the formation of reactive oxygen species (ROS), which are key species of atmospheric and physiological chemistry, in aqueous mixtures of SOA and mineral dust by applying electron paramagnetic resonance (EPR) spectrometry in combination with a spin-trapping technique, liquid chromatography-tandem mass spectrometry (LC-MS/MS), and a kinetic model. We found that substantial amounts of ROS including OH, superoxide as well as carbon- and oxygen-centred organic radicals can be formed in aqueous mixtures of isoprene, α-pinene, naphthalene SOA and various kinds of mineral dust (ripidolite, montmorillonite, kaolinite, palygorskite, and Saharan dust). The molar yields of total radicals were ∼0.02–0.5% at 295 K, which showed higher values at 310 K, upon 254 nm UV exposure, and under low pH (<3) conditions. ROS formation can be explained by the decomposition of organic hydroperoxides, which are a prominent fraction of SOA, through interactions with water and Fenton-like reactions with dissolved transition metal ions. Our findings imply that the chemical reactivity and aging of SOA particles can be enhanced upon interaction with mineral dust in deliquesced particles or cloud/fog droplets. SOA decomposition could be comparably important to the classical Fenton reaction of H₂O₂ with Fe²⁺ and that SOA can be the main source of OH radicals in aqueous droplets at low concentrations of H₂O₂ and Fe²⁺. In the human respiratory tract, the inhalation and deposition of SOA and mineral dust can also lead to the release of ROS, which may contribute to oxidative stress and play an important role in the adverse health effects of atmospheric aerosols in the Anthropocene.

This article is part of the themed collection: Atmospheric chemistry in the Anthropocene

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Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in the Anthropocene†

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Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in the Anthropocene

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