Apparent pore-pressure diffusivity in granular flows is not constant but emerges from diffusion-compaction coupling, controlled by a dimensionless ratio that makes mobility thickness-dependent.
Roche, Bulletin of Volcanology74(2012)
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Diffusion compaction coupling controls pore pressure dynamics in granular fluid flows
Apparent pore-pressure diffusivity in granular flows is not constant but emerges from diffusion-compaction coupling, controlled by a dimensionless ratio that makes mobility thickness-dependent.