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An Analog Macroscopic Technique for Studying Molecular Hydrodynamic Processes in Dense Gases and Liquids
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Dense granular flow around a penetrating object: experiment and hydrodynamic model.

A Seguin1, Y Bertho, P Gondret

  • 1Univ Paris-Sud, Univ Paris 6, CNRS, Lab FAST, Bâtiment 502, Campus Univ, F-91405 Orsay, France.

Physical Review Letters
|August 27, 2011
PubMed
Summary

We studied fluid flow around a cylinder in dense granular matter. Drag force depends linearly on pressure and cylinder size, not velocity, at low granular Reynolds numbers.

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Area of Science:

  • Physics of granular materials
  • Fluid dynamics
  • Hydrodynamics

Background:

  • Understanding granular flow is crucial in various industrial and geological processes.
  • Characterizing the forces acting on objects within granular media is complex.
  • Existing models often struggle to accurately predict flow behavior in dense granular systems.

Purpose of the Study:

  • To experimentally investigate the bidimensional flow field around a cylinder penetrating dense granular matter.
  • To measure the drag force experienced by the cylinder.
  • To validate a hydrodynamic model based on extended kinetic theory for dense granular flow.

Main Methods:

  • Experimental setup for observing 2D flow patterns around a cylinder.
  • Drag force measurements during cylinder penetration.
  • Application of a hydrodynamic model using extended kinetic theory for dense granular flow.

Main Results:

  • Observed flow localization in the granular matter adjacent to the cylinder.
  • Drag force was found to be independent of velocity.
  • Drag force scaled linearly with pressure and cylinder diameter, and weakly with grain size.
  • The observed regime is valid at low granular Reynolds numbers.

Conclusions:

  • The extended kinetic theory-based hydrodynamic model accurately reproduces experimental flow localization and drag force scalings.
  • The drag force in this regime is primarily governed by pressure and geometry, not velocity.
  • This study provides a validated model for predicting forces in dense granular flows under specific conditions.