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Pressure-Dependent Friction on Granular Slopes Close to Avalanche.
Jérôme Crassous1, Antoine Humeau2,3, Samuel Boury1,4
1Université Rennes 1, Institut de Physique de Rennes (UMR UR1-CNRS 6251), Campus de Beaulieu, F-35042 Rennes, France.
Object stability on inclined granular surfaces depends on surface deformation. Heavy and light objects are stable, while intermediate weights cause sliding due to surface changes, impacting friction laws.
Area of Science:
- Physics
- Geophysics
- Robotics
Background:
- Understanding granular material dynamics is crucial for predicting object stability.
- Avalanche thresholds in granular media are complex phenomena influenced by various factors.
- Friction in granular systems deviates from classical models under certain conditions.
Purpose of the Study:
- To investigate the influence of surface deformations on object sliding near the avalanche threshold.
- To determine how object weight affects stability and friction on inclined granular surfaces.
- To explore potential applications in locomotion for devices and animals.
Main Methods:
- Experimental setup involving objects sliding on inclined granular surfaces.
- Controlled variation of object weight to observe surface deformation effects.
- Measurement of friction coefficients and analysis of stability criteria.
Main Results:
- Object stability is primarily driven by surface deformations, not solely by weight.
- Heavy objects create stabilizing deformations (footprints), while light objects cause minimal disturbance.
- Intermediate object weights induce surface deformations leading to sliding, with friction minimal at a characteristic pressure.
- Observed friction coefficients deviate from Amontons-Coulomb laws.
Conclusions:
- Surface deformation is a key factor in granular object stability, overriding simple frictional models.
- The relationship between pressure, deformation, and friction is non-monotonic.
- Findings have implications for designing legged robots and understanding animal locomotion on granular terrains.
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