A063-0011
Modeling Kinetically-Limited IEPOX-SOA Uptake via Volatility based and Compositionally defined Glass Transition Temperatures

Wednesday, 9 December 2020
Poster
William Vizuete1, Sara Farrell2, Quazi Rasool3, Havala Olson Taylor Pye4, Yue Zhang5, Ying-Hsuan Lin6, Yuzhi Chen1, Chi-Tsan Wang1, Haofei Zhang7, Ryan Schmedding2, Manabu Shiraiwa8 and Jason D Surratt9, (1)University of North Carolina at Chapel Hill, Chapel Hill, NC, United States, (2)University of North Carolina at Chapel Hill, Chapel Hill, United States, (3)Pacific Northwest National Laboratory, Richland, WA, United States, (4)US EPA, Durham, United States, (5)University of North Carolina at Chapel Hill, Department or Environmental Sciences and Engineering, Gillings School of Global Public Health, Chapel Hill, NC, United States, (6)University of California, Riverside, Riverside, CA, United States, (7)University of California Riverside, Department of Chemistry, Riverside, CA, United States, (8)Max-Planck-Institut für Chemie, Mainz, Germany, (9)UNC-Environment Sci & Eng, Chapel Hill, NC, United States
Abstract:
A major assumption in air quality models are that the organic and inorganic constituents found in aerosols are homogenously mixed. In recent years studies have shown that these aerosols can in fact form organic coatings with an inorganic core. This core-shell morphology has implications on human health, cloud condensation nuclei, and secondary organic aerosol formation and aging via multiphase chemical processes. A recent implementation in the Community Multi-Scale Air Quality Model (CMAQ), version 5.2, uses glass transition temperature (Tg) and composition of the bulk aerosol along with the relative humidity to determine phase state and organic-inorganic separation of the aerosol. When conditions were favorable for phase separation, the Tg of the bulk aerosol was used to predict the viscosity and thus diffusivity of the organic shell. The Tg of the bulk aerosol was determined via the aerosol liquid water (ALW) in the organic shell (assumed to be 10 percent of total ALW) and Tg of the individual species contributing to the organic shell - determined via their atomic oxygen-to-carbon (O/C) ratio and molecular weight. This study aims to implement the aforementioned phase state determinations and Tg equations into the latest iteration of CMAQ, version 5.3 - which parameterizes organic ALW based on hygroscopicity parameters. Furthermore, a renaissance of laboratory-based studies on organic aerosol Tg have developed new equations based on O/C ratios, saturation concentrations, and elemental compositions. Taking advantage of these new implementations, and new ALW estimates in CMAQ 5.3, this study evaluates various Tg parameterizations effect on phase state and multi-phase chemistry reactions of IEPOX-derived SOA. Model output for each parameterization will be compared to each other and to observational data collected from routine monitoring and intensive field campaigns. This research aims to support future model development of CMAQ and to inform future experimental work further investigating how oxygenated organic coatings can impact multiphase chemistry.