THE EVOLUTION OF RESERVOIR FRACTURE PERMEABILITY DUE TO CO2 INJECTION
Image logs show no preferred fracture orientation, and fracture density is variable throughout each potential injection zone. In these two zones at the RSU#1 location, pore pressures are below the hydrostatic gradient, as measured from mini-DST and VIT tests. The magnitude of the vertical principal stress was calculated at specific depths by calculating the weight of overburden from density logs. The orientation of the maximum horizontal stress is 085°±15°, determined by orientation of wellbore breakouts. The magnitude of the minimum horizontal stress can be measured directly by Micro-Frac or extended leak-off tests, but these tests were not run to completion in RSU#1. Instead, horizontal stress magnitudes were constrained using methods developed by Barton, Zoback et al. (1988). Measured breakout widths from the RSU#1 were compared to predicted widths, which were calculated from laboratory rock strength measurements and other known geomechanical parameters.
Natural fractures at current subsurface conditions at the RSU are not critically stressed due to low pore pressure relative to in-situ stress. At injection pressures above formation pore pressure and below the fracture gradient, some fractures should become critically stressed. This would both increase reservoir permeability and introduce additional permeability anisotropy. This type of information can be used to optimize the CO2 injection strategy and modeling of the CO2 plume.