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Dynamics of a grain-scale intruder in a two-dimensional granular medium with and without basal friction

Ryan Kozlowski, C. Manuel Carlevaro, Karen E. Daniels, Lou Kondic, Luis A. Pugnaloni, Joshua E. S. Socolar, Hu Zheng, and Robert P. Behringer
Phys. Rev. E 100, 032905 – Published 25 September 2019

Abstract

We report on a series of experiments in which a grain-sized intruder is pushed by a spring through a two-dimensional granular material composed of photoelastic disks in a Couette geometry. We study the intruder dynamics as a function of packing fraction for two types of supporting substrates: A frictional glass plate and a layer of water for which basal friction forces are negligible. We observe two dynamical regimes: Intermittent flow, in which the intruder moves freely most of the time but occasionally gets stuck, and stick-slip dynamics, in which the intruder advances via a sequence of distinct, rapid events. When basal friction is present, we observe a smooth crossover between the two regimes as a function of packing fraction, and we find that reducing the interparticle friction coefficient causes the stick-slip regime to shift to higher packing fractions. When basal friction is eliminated, we observe intermittent flow at all accessible packing fractions. For all cases, we present results for the statistics of stick events, the intruder velocity, and the force exerted on the intruder by the grains. Our results indicate the qualitative importance of basal friction at high packing fractions and suggest a possible connection between intruder dynamics in a static material and clogging dynamics in granular flows.

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  • Received 4 June 2019
  • Corrected 23 March 2021

DOI:https://doi.org/10.1103/PhysRevE.100.032905

©2019 American Physical Society

Physics Subject Headings (PhySH)

Polymers & Soft MatterNonlinear Dynamics

Corrections

23 March 2021

Correction: The value for the interparticle friction coefficient μ was incorrectly reported in Table 1 and has been fixed.

Authors & Affiliations

Ryan Kozlowski1,*, C. Manuel Carlevaro2, Karen E. Daniels3, Lou Kondic4, Luis A. Pugnaloni5, Joshua E. S. Socolar1, Hu Zheng1,6, and Robert P. Behringer1

  • 1Department of Physics, Duke University, Durham, North Carolina 27708, USA
  • 2Instituto de Física de Líquidos y Sistemas Biológicos, CONICET, 59 789, 1900 La Plata, Argentina and Dpto. Ing. Mecánica, Universidad Tecnológica Nacional, Facultad Regional La Plata, Av. 60 Esq. 124, La Plata, 1900, Argentina
  • 3Department of Physics, North Carolina State University, Raleigh, North Carolina 27695, USA
  • 4Department of Mathematical Sciences and Center for Applied Mathematics and Statistics, New Jersey Institute of Technology, Newark, New Jersey 07102, USA
  • 5Dpto. de Física, Fac. Ciencias Exactas y Naturales, Universidad Nacional de La Pampa, CONICET, Uruguay 151, 6300 Santa Rosa (La Pampa), Argentina
  • 6Department of Geotechnical Engineering, College of Civil Engineering, Tongji University, Shanghai, 200092, China

  • *Corresponding author: rhk11@phy.duke.edu

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Issue

Vol. 100, Iss. 3 — September 2019

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