“…Despite this prominent role, SOA particle formation ranks among the least understood 5 processes in the atmosphere (Kanakidou et al, 2005;Hallquist et al, 2009;Goldstein and Galbally, 2007;Galbally et al, 2007;Weiss et al, 2008a), rooted in part in the limited knowledge about SOA chemical composition. Molecular studies (Yasmeen et al, 2010;Weiss et al, 2008b;Kleiber et al, 2009;Wang et al, 2005b;Gao et al, 2010;Mena-Carrasco et al, 2009;Huynh et al, 2003;Palaniappan et al, 2009;Greenham 10 et al, 1996;Sharma et al, 2003;Tolocka et al, 2004;Grassian, 2009;Docherty et al, 2005;Heaton et al, 2009) aimed at bridging this knowledge gap support the hypothesis that the products formed from the gas phase oxidization of biogenic volatile organic compounds react with one another to form species with lower and lower vapor pressures, ultimately leading to SOA particle formation. Heterogeneous processes such as 15 physisorption and surface reactions are important for conditions of condensational particle growth.…”