4.0 Article

Effects of Acidity on Reactive Oxygen Species Formation from Secondary Organic Aerosols

期刊

ACS ENVIRONMENTAL AU
卷 2, 期 4, 页码 336-345

出版社

AMER CHEMICAL SOC
DOI: 10.1021/acsenvironau.2c00018

关键词

pH; secondary organic aerosols; reactive oxygen species; organic hydroperoxides; quinones; electron paramagnetic resonance

资金

  1. Health Effects Institute (HEI) (Walter A. Rosenblith New Investigator Award) [4964-RFA17-3/18-6]
  2. United States Environmental Protection Agency (EPA) [CR-83590201]

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Acidity has significant effects on the formation of reactive oxygen species (ROS) in atmospheric secondary organic aerosols (SOA). Different pH values result in distinct radical yields and composition in SOA. Isoprene SOA has higher radical yields at neutral pH, while superoxide is the dominant species at lower pH. Acidic conditions can suppress the decomposition of organic peroxide and enhance the molar yields of hydrogen peroxide (H2O2) in biogenic and aromatic SOA.
Reactive oxygen species (ROS) play a critical role in the chemical transformation of atmospheric secondary organic aerosols (SOA) and aerosol health effects by causing oxidative stress in vivo. Acidity is an important physicochemical property of atmospheric aerosols, but its effects on the ROS formation from SOA have been poorly characterized. By applying the electron paramagnetic resonance spin-trapping technique and the Diogenes chemiluminescence assay, we find highly distinct radical yields and composition at different pH values in the range of 1-7.4 from SOA generated by oxidation of isoprene, a-terpineol, a-pinene, beta-pinene, toluene, and naphthalene. We observe that isoprene SOA has substantial hydroxyl radical ((OH)-O-center dot) and organic radical yields at neutral pH, which are 1.5-2 times higher compared to acidic conditions in total radical yields. Superoxide (O-2(center dot-)) is found to be the dominant species generated by all types of SOAs at lower pH. At neutral pH, alpha-terpineol SOA exhibits a substantial yield of carboncentered organic radicals, while no radical formation is observed by aromatic SOA. Further experiments with model compounds show that the decomposition of organic peroxide leading to radical formation may be suppressed at lower pH due to acid-catalyzed rearrangement of peroxides. We also observe 1.5-3 times higher molar yields of hydrogen peroxide (H2O2) in acidic conditions compared to neutral pH by biogenic and aromatic SOA, likely due to enhanced decomposition of a-hydroxyhydroperoxides and quinone redox cycling, respectively. These findings are critical to bridge the gap in understanding ROS formation mechanisms and kinetics in atmospheric and physiological environments.

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