Abstract

The phenomenon called “flashover” or “eruptive fire” in forest fires is characterized by a sudden change in fire behavior: everything seems to burst into flames instantly and firefighters are overwhelmed by a sort of eruption, spreading at a speed at far several meters per second. Unfortunately it has cost several lives in the past. The reasons for such an accident always create controversy in the research field. Different theories are highlighted and especially two major axes are currently subject to discussion because they are very popular among people involved in fire-fighting. The one with regard to VOCs emissions is the best-known among firemen. Under great heat, during summer or with a fire approaching, plants emit VOCs and the more the temperature grows, the more the amount of VOCs emitted grows. Under specific conditions (essentially topographical, meteorological and atmospheric), the cloud of gas can accumulate in an appropriate zone. The concentration of VOCs may therefore reach the Lower Explosive Limit, triggering the burst of the cloud when in contact with the fire. The second theory depends on physical considerations. An example is based on a convective flow created by the fire itself. When a fire spreads on a slope, it creates an aspiration phenomenon in a way to supply the fire with oxygen. The more this phenomenon is important, the more the flames tilt and increase the rate of speed, needing even more oxygen and thus induced flow. This vicious circle can stabilize or have an erratic behavior to trigger off a fire eruption. This article presents these two theories, and especially the new advances on this research subject.

Highlights

  • Flashovers are complex phenomena that are met in specific cases of fires in enclosed areas

  • If a flashover in an enclosed space is well known (NFPA 921, 2011) especially in fire safety science (NFPA 555, 2000), the Generalized Blaze flash (GBF) must be compared to blowup fires, defined by Butler et al (1998) as a rapid transition from a surface fire exhibiting relatively low intensity to a fire burning in the whole vegetation complex, from surface to canopy and demonstrating dramatically larger flame heights, higher energy release rates, and faster rates of spread

  • A Generalized Blaze Flash consists in a practically instantaneous ignition of a forest area in the whole vegetation and several explanations of its triggering are considered in the literature

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Summary

General Information on VOC Emissions

Still subject to discussion, a steady-state forest fire can abruptly change its behavior While it predictably spread, firefighters could be led to believe that they master the situation, its features suddenly change: it increases in intensity, and speed, so that in a flash, all the plants blaze. Oxygen content (i.e. oxidant) is too low to allow the flame to continue to grow The values of these limits depend on initial temperature and pressure. The flashpoint is the minimum temperature required by the vapors, emitted by the heated substance, to ignite hot gases. The second characteristic is the auto-ignition temperature (AIT) This is the minimum temperature in which a product or mixture ignites willingly with air by spontaneous combustion.

VOCs’ Role
Plants and VOC
Configurations Which Raise the Accumulation of VOCs
Physical Issues
Flow Attachment
Convective Flow Induced by the Fire
VOCs’ Theory
Findings
Fire Properties’ Theory
Conclusion
Full Text
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