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Updated: Mar 8, 2026

An Analog Macroscopic Technique for Studying Molecular Hydrodynamic Processes in Dense Gases and Liquids
Published on: December 4, 2017
Macroscopic liquid-state molecular hydrodynamics
R G Keanini1, Peter T Tkacik1, Eric Fleischhauer1
1The University of North Carolina at Charlotte, Department of Mechanical Engineering and Engineering Science, Charlotte, NC, 28223, USA.
Granular materials vibrated at low amplitudes mimic liquid dynamics. New macroscopic models connect grain behavior to molecular hydrodynamics, enabling study of complex fluid phenomena.
Area of Science:
- Physics
- Soft Matter Physics
- Statistical Mechanics
Background:
- Molecular hydrodynamics in liquids are challenging to study directly at the molecular scale.
- Granular materials offer potential as macroscopic analogs for molecular systems.
- Previous models have not fully bridged granular dynamics with molecular hydrodynamics.
Purpose of the Study:
- To establish granular materials as experimental analogs for liquid-state molecular hydrodynamics.
- To develop new macroscopic statistical mechanics models for granular systems.
- To connect observable granular dynamics to fundamental hydrodynamic processes.
Main Methods:
- Experimental studies of confined, high-restitution granular piles under low-amplitude vibration.
- Theoretical modeling recasting microscale statistical mechanics into a self-consistent macroscale form.
- Derivation of continuum equations for viscous, liquid-like granular flow from the new models.
Main Results:
- Observed granular dynamics (single-grain and collective) that mimic molecular liquid behaviors.
- Demonstrated hydrodynamic organization on near-collision time scales.
- Showcased long-time scale excitation of collective modes and emergence of viscous flow.
Conclusions:
- Vibrated granular systems provide accessible analogs for studying liquid hydrodynamics.
- Novel macroscopic models successfully link granular physics to molecular hydrodynamic principles.
- The derived continuum equations allow for physically consistent interpretation of granular flow.
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