The transition from brittle faulting to cataclastic flow: Permeability evolution

Triaxial compression experiments were conducted to investigate influences of stress and failure mode on axial permeability of five sandstones with porosities ranging from 15% to 35%. In the cataclastic flow regime, permeability and porosity changes closely track one another. A drastic decrease in permeability was triggered by the onset of shear‐enhanced compaction caused by grain crushing and pore collapse. The compactive yield stress C * maps out a boundary in stress space separating two different types of permeability evolution. Before C * is attained, permeability and porosity both decrease with increasing effective mean stress, but they are independent of deviatoric stresses. However, with loading beyond C *, both permeability and porosity changes are strongly dependent on the deviatoric and effective mean stresses. In the brittle faulting regime, permeability and porosity changes are more complex. Before the onset of shear‐induced dilation C ', both permeability and porosity decrease with increasing effective mean stress. Beyond C ', permeability may actually decrease in a dilating rock prior to brittle failure. After the peak stress has been attained, the development of a relatively impermeable shear band causes an accelerated decrease of permeability. Permeability evolution in porous sandstones is compared with that in low‐porosity crystalline rocks. A conceptual model for the coupling of deformation and fluid transport is proposed in the form of a deformation‐permeability map.