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The thermodynamic processes can be classified into reversible and irreversible processes. The processes that can be restored to their initial state are called reversible processes. It is only possible if the process is in quasi-static equilibrium, i.e., it takes place in infinitesimally small steps, and the system remains at equilibrium However, these are ideal processes and do not occur naturally. An ideal system undergoing a reversible process is always in thermodynamic equilibrium within...
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(Ir)reversibility in dense granular systems driven by oscillating forces.

Ronny Möbius1, Claus Heussinger

  • 1Institute for Theoretical Physics, Georg-August University of Göttingen, Friedrich-Hund Platz 1, 37077 Göttingen, Germany. claus.heussinger@theorie.physik.uni-goettingen.de.

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Computer simulations reveal how granular particle systems behave under oscillating forces. Friction alters particle movement, transitioning from ordered motion to diffusion and distinct phase transitions at varying densities.

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Area of Science:

  • Physics
  • Computational Science
  • Materials Science

Background:

  • Granular materials exhibit complex behaviors under external forces.
  • Understanding energy dissipation is crucial for modeling dense particle systems.

Purpose of the Study:

  • To investigate the effects of different dissipation mechanisms on dense granular systems driven by oscillating forces.
  • To compare Stokes' drag with non-linear frictional forces on particle dynamics.

Main Methods:

  • Utilizing computer simulations to model highly dense granular particle systems.
  • Implementing and comparing Stokes' drag, inter-particle friction, and particle-wall friction as dissipation mechanisms.
  • Analyzing particle motion, density transitions, and phase behaviors.

Main Results:

  • Stokes' drag results in periodic particle motion even at high densities.
  • Inter-particle friction disrupts periodic motion, leading to particle diffusion and an "interacting absorbing state."
  • Particle-wall friction induces a discontinuous phase transition with diverging relaxation time.

Conclusions:

  • Dissipation mechanisms significantly alter the dynamics of driven granular systems.
  • Frictional forces are key to transitioning between ordered and diffusive particle motion.
  • The study highlights distinct phase transitions in granular matter influenced by density and friction.