Evolution of Permeability during Fracturing Processes in Rocks under Conditions of Geological Storage of CO₂

  • Fujii Takashi
    Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology (AIST)
  • Funatsu Takahiro
    Western Australian School of Mines, Curtin University
  • Oikawa Yasuki
    Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology (AIST)
  • Sorai Masao
    Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology (AIST)
  • Lei Xinglin
    Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology (AIST)

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タイトル別名
  • Evolution of Permeability during Fracturing Processes in Rocks under Conditions of Geological Storage of CO<sub>2</sub>

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We investigated experimentally the change in permeability in three different types of soft rocks including mudstone, sandstone, and tuff from the Fureoi and Takinoue formations, which are representative of the CCS demonstration site at Tomakomai in Japan, and another type of mudstone from the Besho Fm. (B-M). Permeability during deformation, shear fracturing, and post-failure slipping is estimated from measured flow rate and differential pore pressure. In addition, the morphologies of the shear fracture zones were examined using the X-ray CT scanning technique. All the samples exhibit typical brittle-fracturing behaviors, except for the B-M sample which does not show a major shear fracture. During the fracturing process, the permeability increased by one to three orders of magnitude. Further changes in the post-failure slipping and stress relaxation regimes show strong dependence on the type of rocks. Observed changes in permeability can be interpreted as results of fracturing creation, shear zone smoothing, closure and reactivation of fractures under different stress regimes.

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