Characterization of Atmospheric PM2.5 Inorganic Aerosols Using the Semi-Continuous PPWD-PILS-IC System and the ISORROPIA-II

Atmosphere

Thi-Cuc Le¹  Yun-Chin Wang¹  Chuen-Jinn Tsai¹  DavidY. H. Pui² 

[1]Institute of Environmental Engineering, National Chiao Tung University, Hsinchu 30010, Taiwan

[2]School of Energy and Environmental Engineering, University of Science and Technology Beijing, Beijing 100083, China

关键词: PPWD;    PILS;    PDS;    ISORROPIA-II;    precursor gas;    water-soluble inorganic ion;   

DOI  :  10.3390/atmos11080820

来源: DOAJ

【 摘 要 】

A semi-continuous monitoring system, a parallel plate wet denuder and particle into liquid sampler coupled with ion chromatography (PPWD-PILS-IC), was used to measure the hourly precursor gases and water-soluble inorganic ions in ambient particles smaller than 2.5 µm in diameter (PM_2.5) for investigating the thermodynamic equilibrium of aerosols using the ISORROPIA-II thermodynamic equilibrium model. The 24-h average PPWD-PILS-IC data showed very good agreement with the daily data of the manual 5 L/min porous-metal denuder sampler with R² ranging from 0.88 to 0.98 for inorganic ions (NH₄⁺, Na⁺, K⁺, NO₃⁻, SO₄²⁻, and Cl⁻) and 0.89 to 0.98 for precursor gases (NH₃, HNO₃, HONO, and SO₂) and slopes ranging from 0.94 to 1.17 for ions and 0.87 to 0.95 for gases, respectively. In addition, the predicted ISORROPIA-II results were in good agreement with the hourly observed data of the PPWD-PILS-IC system for SO₄²⁻ (R² = 0.99 and slope = 1.0) and NH₃ (R² = 0.97 and slope = 1.02). The correlation of the predicted results and observed data was further improved for NH₄⁺ and NO₃⁻ with the slope increasing from 0.90 to 0.96 and 0.95 to 1.09, respectively when the HNO₂ and NO₂⁻ were included in the total nitrate concentration (TN = [NO₃⁻] + [HNO₃] + [HONO] + [NO₂⁻]). The predicted HNO₃ data were comparable to the sum of the observed [HNO₃] and [HONO] indicating that HONO played an important role in the thermodynamic equilibrium of ambient PM_2.5 aerosols but has not been considered in the ISORROPIA-II thermodynamic equilibrium model.

【 授权许可】

Unknown