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Particle acidity and sulfate production during severe haze events in China cannot be reliably inferred by assuming a mixture of inorganic salts

  • Gehui Wang*
  • , Fang Zhang
  • , Jianfei Peng
  • , Lian Duan
  • , Yuemeng Ji
  • , Wilmarie Marrero-Ortiz
  • , Jiayuan Wang
  • , Jianjun Li
  • , Can Wu
  • , Cong Cao
  • , Yuan Wang
  • , Jun Zheng
  • , Jeremiah Secrest
  • , Yixin Li
  • , Yuying Wang
  • , Hong Li
  • , Na Li
  • , Renyi Zhang
  • *Corresponding author for this work
  • CAS - Institute of Earth Environment
  • Chinese Academy of Sciences
  • College of Global Change and Earth System Science
  • Beijing Normal University
  • Departments of Atmospheric Sciences and Chemistry
  • Texas A&M University
  • Peking University
  • State Environmental Protection Key Lab
  • East China University of Science and Technology
  • Guangdong Key Laboratory of Environmental Catalysis and Health Risk Control
  • Guangdong University of Technology
  • State Key Laboratory of Loess and Quaternary Geology
  • Jet Propulsion Laboratory, California Institute of Technology
  • Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control
  • Nanjing University of Information Science & Technology
  • State Key Laboratory of Environmental Criteria and Risk Assessment
  • Chinese Research Academy of Environmental Sciences
  • Key Laboratory of Songliao Aquatic Environment
  • Jilin Jianzhu University

Research output: Contribution to journal › Article › peer-review

Abstract

Atmospheric measurements showed rapid sulfate formation during severe haze episodes in China, with fine particulate matter (PM) consisting of a multi-component mixture that is dominated by organic species. Several recent studies using the thermodynamic model estimated the particle acidity and sulfate production rate, by treating the PM exclusively as a mixture of inorganic salts dominated by ammonium sulfate and neglecting the effects of organic compounds. Noticeably, the estimated pH and sulfate formation rate during pollution periods in China were highly conflicting among the previous studies. Here we show that a particle mixture of inorganic salts adopted by the previous studies does not represent a suitable model system and that the acidity and sulfate formation cannot be reliably inferred without accounting for the effects of multi-aerosol compositions during severe haze events in China. Our laboratory experiments show that SO2 oxidation by NO2 with NH3 neutralization on fine aerosols is dependent on the particle hygroscopicity, phase-state, and acidity. Ammonium sulfate and oxalic acid seed particles exposed to vapors of SO2, NO2, and NH3 at high relative humidity (RH) exhibit distinct size growth and sulfate formation. Aqueous ammonium sulfate particles exhibit little sulfate production, in contrast to aqueous oxalic acid particles with significant sulfate production. Our field measurements demonstrate significant contribution of water-soluble organic matter to fine PM in China and indicate that the use of oxalic acid in laboratory experiments is representative of ambient organic dominant aerosols. While the particle acidity cannot be accurately determined from field measurements or calculated using the thermodynamic model, our results reveal that the pH value of ambient organics-dominated aerosols is sufficiently high to promote efficient SO2 oxidation by NO2 with NH3 neutralization under polluted conditions in China.

Original languageEnglish
Pages (from-to)10123-10132
Number of pages10
JournalAtmospheric Chemistry and Physics
Volume18
Issue number14
DOIs
StatePublished - 17 Jul 2018

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