Assessing the influence of NO_<i>x</i> concentrations and relative humidity on secondary organic aerosol yields from <i>α</i>-pinene photo-oxidation through smog chamber experiments and modelling calculations

• Main Authors: L. Stirnweis, C. Marcolli, J. Dommen, P. Barmet, C. Frege, S. M. Platt, E. A. Bruns, M. Krapf, J. G. Slowik, R. Wolf, A. S. H. Prévôt, U. Baltensperger, I. El-Haddad
• Format: Article
• Language: English
• Published: Copernicus Publications 2017-04-01
• Series: Atmospheric Chemistry and Physics
• Online Access: http://www.atmos-chem-phys.net/17/5035/2017/acp-17-5035-2017.pdf

Secondary organic aerosol (SOA) yields from the photo-oxidation of <i>α</i>-pinene were investigated in smog chamber (SC) experiments at low (23–29 %) and high (60–69 %) relative humidity (RH), various NO_<i>x</i> ∕ VOC ratios (0.04–3.8) and with different aerosol seed chemical compositions (acidic to neutralized sulfate-containing or hydrophobic organic). A combination of a scanning mobility particle sizer and an Aerodyne high-resolution time-of-flight aerosol mass spectrometer was used to determine SOA mass concentration and chemical composition. We used a Monte Carlo approach to parameterize smog chamber SOA yields as a function of the condensed phase absorptive mass, which includes the sum of OA and the corresponding bound liquid water content. High RH increased SOA yields by up to 6 times (1.5–6.4) compared to low RH. The yields at low NO_<i>x</i> ∕ VOC ratios were in general higher compared to yields at high NO_<i>x</i> ∕ VOC ratios. This NO_<i>x</i> dependence follows the same trend as seen in previous studies for <i>α</i>-pinene SOA. <br><br> A novel approach of data evaluation using volatility distributions derived from experimental data served as the basis for thermodynamic phase partitioning calculations of model mixtures in this study. These calculations predict liquid–liquid phase separation into organic-rich and electrolyte phases. At low NO_<i>x</i> conditions, equilibrium partitioning between the gas and liquid phases can explain most of the increase in SOA yields observed at high RH, when in addition to the <i>α</i>-pinene photo-oxidation products described in the literature, fragmentation products are added to the model mixtures. This increase is driven by both the increase in the absorptive mass and the solution non-ideality described by the compounds' activity coefficients. In contrast, at high NO_<i>x</i>, equilibrium partitioning alone could not explain the strong increase in the yields with RH. This suggests that other processes, e.g. reactive uptake of semi-volatile species into the liquid phase, may occur and be enhanced at higher RH, especially for compounds formed under high NO_<i>x</i> conditions, e.g. carbonyls.