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.
Title resolution pending
2 Pith papers cite this work. Polarity classification is still indexing.
2
Pith papers citing it
fields
cond-mat.soft 2verdicts
UNVERDICTED 2representative citing papers
Quaking occurs only for volume fraction above material-parameter-determined φ_c independent of rate; inertia suppresses it, narrowing the regime with increasing shear speed.
citing papers explorer
-
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.
-
Quaking in Soft Granular Particles with Speed-dependent Friction: Role of Critical Volume Fraction and Inertia
Quaking occurs only for volume fraction above material-parameter-determined φ_c independent of rate; inertia suppresses it, narrowing the regime with increasing shear speed.