“…Upward migration of CO 2 will occur whenever appropriate (sub-) vertical permeability is available, and/or when the capillary entry pressure of the caprock is exceeded (Krooss et al, 2004;Zweigel et al, 2004;Gibson-Poole et al, 2004;Moreno et al, 2004). Three main potential pathways for CO 2 release have been recognized (Zweigel et al, 2004;Espie, 2004), (1) leakage through the caprock (Lindeberg and Bergmo, 2003;Krooss et al, 2004), (2) migration along sub-vertical faults or fracture zones (Pruess and García, 2002;Rutqvist and Tsang, 2002;Hillis, 2003, 2004), and (3) escape through boreholes Bachu et al, 2004;Duguid et al, 2004).…”