“…However, large discrepancies were reported between NOM surface areas derived from CO 2 adsorption and N 2 adsorption, primarily because of the activated diffusion phenomenon (Aochi and Farmer, 2005;de Jonge and Mittelmeijer-Hazeleger, 1996;Li and Werth, 2001;Ran et al, 2013;Ravikovitch et al, 2005;Xing and Pignatello, 1997). Carbon dioxide at 273 K and benzene at 295 K have been used as alternative gases for probing the surface properties of carbonaceous materials (Corley et al, 1996;de Jonge and Mittelmeijer-Hazeleger, 1996;Gan et al, 1972;Kwon and Pignatello, 2005;Larsen et al, 1995;Ravikovitch et al, 2005;Reucroft and Sethuraman, 1987;Walker and Kini, 1965;Xing and Pignatello, 1997). Glassy forms of NOM including humin, kerogen and coals have internal microporosity that apparently is not accessed by N 2 at 77 K due to activation diffusion.…”