Abstract
We propose a simple empirical model to describe the Rayleigh-Taylor (RT) turbulent mixing of immiscible, miscible and stratified fluids. For immiscible fluids, the rate of momentum loss is an invariant of the flow, whereas the energy dissipation rate increases linearly with time. Turbulent diffusion, accounted for through temperature fluctuations, does not terminate mixing but slows it down significantly. A stratified density distribution can stabilize RT mixing.
Original language | English (US) |
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Article number | 081705 |
Pages (from-to) | 1-4 |
Number of pages | 4 |
Journal | Physics of Fluids |
Volume | 17 |
Issue number | 8 |
DOIs | |
State | Published - Aug 2005 |
ASJC Scopus subject areas
- Computational Mechanics
- Condensed Matter Physics
- Mechanics of Materials
- Mechanical Engineering
- Fluid Flow and Transfer Processes