“…Our fugacity-based modeling shows that 3-ring PAHs (Acy, Ace, Flo, Phe and Ant) tend to evaporate from soil to air with escaping diffusive fluxes ranging from 0.79 to 713 μg m −2 yr −1 , whereas 5-and 6-ring PAHs (BaP, DahA, IcdP and BghiP) are likely to deposit from air to soil with deposition fluxes varying between 0.99 and 10.2 μg m − 2 yr − 1 (Table 2). These results were consistent with the findings of several previous studies, conducted in Beijing , Tibetan Plateau (Wang et al, 2014), Dalian (Wang et al, 2008) and Zhejiang Province (Zhong and Zhu, 2013) of China, and in Turkey (Bozlaker et al, 2008), that soil is a secondary source of low molecular weight PAHs, but a sink of high molecular weight PAHs. It is interesting to note that the mean escaping or deposition fluxes of Flu and Pyr ranged from 1.3 to 1.41 or from 0.17 to 1.7 μg m −2 yr −1 (Table 2), and the soilair fugacity fractions of Flu and Pyr ranged from 0.27 to 0.67 (Table S6), approximately within the range of 0.30-0.70 used to suggest the soilair equilibrium state of a target compound in a region (Harner et al, 2001;Meijer et al, 2003).…”