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Microrollers flow uphill as granular media

Author

Listed:
  • Samuel R. Wilson-Whitford

    (Lehigh University)

  • Jinghui Gao

    (Lehigh University)

  • Maria Chiara Roffin

    (Lehigh University
    Nottingham Trent University)

  • William E. Buckley

    (Lehigh University)

  • James F. Gilchrist

    (Lehigh University)

Abstract

Pour sand into a container and only the grains near the top surface move. The collective motion associated with the translational and rotational energy of the grains in a thin flowing layer is quickly dissipated as friction through multibody interactions. Alternatively, consider what will happen to a bed of particles if one applies a torque to each individual particle. In this paper, we demonstrate an experimental system where torque is applied at the constituent level through a rotating magnetic field in a dense bed of microrollers. The net result is the grains roll uphill, forming a heap with a negative angle of repose. Two different regimes have been identified related to the degree of mobility or fluidisation of the particles in the bulk. Velocimetry of the near surface flowing layer reveals the collective motion of these responsive particles scales in a similar way to flowing bulk granular flows. A simple granular model that includes cohesion accurately predicts the apparent negative coefficient of friction. In contrast to the response of active or responsive particles that mimic thermodynamic principles, this system results in macroscopic collective behavior that has the kinematics of a purely dissipative granular system.

Suggested Citation

  • Samuel R. Wilson-Whitford & Jinghui Gao & Maria Chiara Roffin & William E. Buckley & James F. Gilchrist, 2023. "Microrollers flow uphill as granular media," Nature Communications, Nature, vol. 14(1), pages 1-6, December.
  • Handle: RePEc:nat:natcom:v:14:y:2023:i:1:d:10.1038_s41467-023-41327-1
    DOI: 10.1038/s41467-023-41327-1
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    References listed on IDEAS

    as
    1. Morgane Houssais & Carlos P. Ortiz & Douglas J. Durian & Douglas J. Jerolmack, 2015. "Onset of sediment transport is a continuous transition driven by fluid shear and granular creep," Nature Communications, Nature, vol. 6(1), pages 1-8, May.
    2. Pierre Jop & Yoël Forterre & Olivier Pouliquen, 2006. "A constitutive law for dense granular flows," Nature, Nature, vol. 441(7094), pages 727-730, June.
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