Abstract
We describe a quantitative model for air-driven fluidization in a vertically vibrated granular system and use experimental results and simulations to evaluate it. The model involves a mechanism for vibrationally induced interstitial gas flow [L.I. Reyes, I. Sánchez, G. Gutiérrez, Physica A, cond-mat/0502376, in press] that can generate fluid-like states that produce density-dependent segregation of large objects, through a buoyancy force. A criterion for the onset of fluidization analogous to that of a gas-fluidized static bed is used. We calculate the vertical displacement of a large sphere occurring within one period of oscillation, in specific parts of the cycle where the granular system behaves like a regular fluid.
| Original language | English |
|---|---|
| Pages (from-to) | 83-87 |
| Number of pages | 5 |
| Journal | Physica A: Statistical Mechanics and its Applications |
| Volume | 356 |
| Issue number | 1 |
| DOIs | |
| State | Published - Oct 1 2005 |
| Externally published | Yes |
| Event | Nonequilibrium Statistical Mechanics and Nonlinear Physics (MEDYFINOL'04) - Duration: Dec 2 2004 → Dec 4 2004 |
ASJC Scopus Subject Areas
- Statistics and Probability
- Condensed Matter Physics
Keywords
- Buoyancy
- Fluidization
- Granular
- Segregation
Disciplines
- Statistics and Probability
- Condensed Matter Physics
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