Supplement of Effects of Liquid–Liquid Phase Separation and Relative Humidity on the Heterogeneous OH Oxidation of Inorganic-Organic Aerosols: Insights from Methylglutaric Acid/Ammonium Sulfate Particles Hoi Ki Lam1, Rongshuang Xu1, Jack Choczynski2, James F. Davies2, Dongwan Ham3, Mijung Song3, Andreas Zuend4, Wentao Li5, Ying-Lung Steve Tse5, Man Nin Chan 1,6 1Earth System Science Programme, Faculty of Science, The Chinese University of Hong Kong, Hong Kong, China 2Department of Chemistry, University of California Riverside, Riverside, CA, USA 3Department of Earth and Environmental Sciences, Jeonbuk National University, Jeollabuk-do, Republic of Korea 4Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, Québec, Canada 5Departemnt of Chemistry, The Chinese University of Hong Kong, Hong Kong, China’ 6The Institute of Environment, Energy and Sustainability, The Chinese University of Hong Kong, Hong Kong, China Corresponding author:
[email protected] Table S1. Composition, viscosity, diffusion coefficient and mixing time scale of aqueous droplets containing 3-MGA and ammonium sulfate (AS) in an organic- to-inorganic dry mass ratio (OIR) = 1 at different RH predicted by the AIOMFAC-LLE. RH (%) 55 60 65 70 75 80 85 88 Salt-rich phase (Phase α) Mass fraction of 3-MGA 0.00132 0.00372 0.00904 0.0202 / / Mass fraction of AS 0.658 0.616 0.569 0.514 / / Mass fraction of H2O 0.341 0.380 0.422 0.466 / / Organic-rich phase (Phase β) Mass fraction of 3-MGA 0.612 0.596 0.574 0.546 / / Mass fraction of AS 0.218 0.209 0.199 0.190