“…The reduction in CH 4 permeability is attributed to (1) chain rigidification of polymer near the bulk of zeolite, which remarkably reduces the penetration of gas molecules on that region, (2) partial pore blockage of zeolites by polymer chains, which occurs when the polymer chains penetrate in to the zeolite pores and obstruct them partially (Bastani et al, 2013;Li et al, 2005) and (3) the slower diffusion of large gases such as CH 4 in zeolite channels compared with polymer chains (Zhang et al, 2008;Jia et al, 1991). All these factors make CH 4 as a less adsorbable and condensable gas (d KT,CH4 = 3.8 Å, T c,CH4 = 191 K) which permeated more slowly compared with CO 2 (d KT,CO2 = 3.3 Å, T c,CO2 = 304 K) which led to a higher selectivity (Ebadi Amooghin et al, 2010;Sanaeepur et al, 2012;Xiao et al, 2009). Additionally, considerable increase in CO 2 permeability can be attributed to the more interactions of polar CO 2 molecules with polar surface of calcined ZSM-5.…”