“…The pressure is inversely proportional to the size of the pores, and only slight pressure is required for mercury to intrude into large macropores, whereas much greater pressure is required to force mercury into small pores. In porous medium, mercury intrusion is similar to air injection in a saturated soil in the drying process of a water retention curve (Prapaharan et al, 1987;Romero et al, 1999;Aung et al, 2001;Simms and Yanful, 2001;Zhang and Li, 2010;Mascarenha et al, 2011;Otalvaro et al, 2016). A PoreMaster 60 GT (Quantachrome Instruments) mercury porosimeter was used, and a surface tension and contact angle of mercury of 480 mN m -1 and 130°, respectively, were chosen.…”