Coupled CFD-DEM simulations show frictional instability arises from coupled evolution of pore pressure, drainage, dilation/compaction, hydraulic connectivity, and granular fabric rather than pore pressure alone.
Comparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts , volume =
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Investigating frictional instability due to pressurization in granular media: insights from coupled computational fluid dynamics discrete element method
Coupled CFD-DEM simulations show frictional instability arises from coupled evolution of pore pressure, drainage, dilation/compaction, hydraulic connectivity, and granular fabric rather than pore pressure alone.