Sediment creep triggered by porous flow

16 Feb 2020 Houssais Morgane Maldarelli Charles Morris Jeffrey F.

Quasi-2D experiments of a submerged sediment layer creeping downward were performed, varying the channel tilt and a porous flow under the respective thresholds for yielding. Logarithmic decay rates of the deformation are observed, with the rate increasing with both control parameters... (read more)

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Categories


  • SOFT CONDENSED MATTER
  • DISORDERED SYSTEMS AND NEURAL NETWORKS
  • MATERIALS SCIENCE
  • APPLIED PHYSICS
  • GEOPHYSICS