Abstract
Whirling fire plumes are known to increase the danger of naturally occurring or post-disaster fires. In order for a fire whirl to exist, there must be an organized source of angular momentum to produce the large swirl velocities as air is entrained into the fire plume. These vorticity-driven fires occur over a large range of length and velocity scales, and significantly alter the entrainment and combustion dynamics. A new model is derived for a buoyant plume that incorporates angular rotation and neglects dissipation; the result is a form of the steady state Euler equations. Included is a general solution for large density and temperature variations. Results are presented that identify the mechanisms and their effects toward creating a fire whirl. (C) 2000 American Institute of Physics.
| Original language | English |
|---|---|
| Pages (from-to) | 2859-2867 |
| Number of pages | 9 |
| Journal | Physics of Fluids |
| Volume | 12 |
| Issue number | 11 |
| DOIs | |
| State | Published - 2000 |
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