Friction modifies the quasistatic mechanical response of a confined, poroelastic medium
T\'erence Desclaux, Callum Cuttle, Chris W. MacMinn, Olivier Liot

TL;DR
This paper develops a theoretical framework to understand how wall friction influences the quasistatic mechanical response of confined poroelastic media, revealing effects like hysteresis, slip fronts, and altered energy dissipation.
Contribution
The study introduces a novel model incorporating Coulomb friction into poroelasticity, highlighting its impact on stress evolution, hysteresis, and energy dissipation during slow deformations.
Findings
Friction causes hysteresis and slip fronts during unloading.
Friction modifies the apparent mechanical properties of the medium.
Frictional effects depend on loading type and geometry.
Abstract
The mechanical response of elastic porous media confined within rigid geometries is central to a wide range of industrial, geological, and biomedical systems. However, current models for these problems typically overlook the role of wall friction, and particularly its interaction with confinement. Here, we develop a theoretical framework to describe the interplay between the mechanics of the medium and Coulomb friction at the confining walls for slow, quasistatic deformations in response to two canonical uniaxial forcings: piston-driven loading (i.e., an imposed effective stress at the top boundary) and fluid-driven loading (i.e., an imposed fluid pressure at the top boundary) followed by unloading. We find that, during compression, the stress field evolves according to a quasistatic advection-diffusion equation, extending classical poroelasticity results. The magnitude of friction is…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsThermoelastic and Magnetoelastic Phenomena · Nonlocal and gradient elasticity in micro/nano structures · High-pressure geophysics and materials
