“…At the field scale, NAPL migration is controlled by a complex combination of aquifer properties, NAPL properties, and other macro-scale features such as released volume of NAPL, local pumping effects and lithology (Mercer and Cohen, 1990;Divine et al, 2004). Therefore, sitespecific mathematical models are necessary for investigating the dissolution and transport of NAPL compounds, which largely depend on the nature of the contaminant source and the initial fuel composition (Ostendorf and Kampbell, 1991;Zhu and Sykes, 2000;Vaezihir et al, 2012).…”