Studying wildfire spread using stationary burners
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Abstract
A method for performed experiments using stationary gas burners and liquid
fuel-soaked wicks to study flame geometry and buoyant instabilities important to
fundamental wildland fire behaviour has been developed. This thesis focuses on
experiments performed with stationary fires to carefully study instabilities observed
in spreading fires that suggest they play a critical role in fire spread.
Two types of flow conditions were used to perform experiments similar to
wildfire spread conditions: sloped fuel surface and forced-flow (wind aided). Small-
scale inclined experiments for performed at the University of Maryland with liquid-
fuel soaked wicks and large-scale experiments at the USDA Forest Service Missoula
Fire Sciences Laboratory with a gas-burner. These experiments were performed with
over a range of heat-release-rates and burner sizes for angles from 0 to 60 degrees
from the horizontal. Forced-flow experiments were performed in a large-scale wind
tunnel at the Missoula Fire Laboratory and at the University of Maryland with a
well characterized wind blower with gas-burners. These experiments were performed
for a range of heat-release-rates and burner sizes in wind speeds from 0.2 to 3.0 ms−1
The flame geometry was determined using high-speed videography. Important
two-dimensional flame geometry parameters such as centerline flame length and
flame tilt angle were measured from these images.
Flame intermittency and pulsation close to the surface was measured using
high-speed videography and micro-thermocouples. A method was developed to
track the extension of the flame close to the surface which would come in direct
contact with unburnt fuels ahead of the fire. These methods showed that the pul-
sation frequency is complicated suggesting large scale structures in the flow. Using
these frequency the stationary experiments follow similar Strouhal-Froude scaling
for flame pulsations in spreading fires.
Stream-wise streaks in the flow were observed and measured using high-speed
videography. Streak spacing has been observed to be associated with possible
Gotler votice structures in the fire. The spacing for streaks at the base of the
flame for these startionary experiments appear to be dependent on the boundary-
layer conditions and could possibly scale with the centerline flame length similar to
flame towers observed in spreading fires.