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Fire is the rapid oxidation of a material (the fuel) in the exothermic chemical process of combustion, releasing heat, light, and various reaction products. At a certain point in the combustion reaction, called the ignition point, flames are produced. The flame is the visible portion of the fire. Flames consist primarily of carbon dioxide, water vapor, oxygen and nitrogen. If hot enough, the gases may become ionized to produce plasma. Depending on the substances alight, and any impurities outside, the color of the flame and the fire's intensity will be different.

Fire, in its most common form, has the potential to result in conflagration, which can lead to physical damage, which can be permanent, through burning. Fire is a significant process that influences ecological systems worldwide. The positive effects of fire include stimulating growth and maintaining various ecological systems. Its negative effects include hazard to life and property, atmospheric pollution, and water contamination. When fire removes protective vegetation, heavy rainfall can contribute to increased soil erosion by water. Additionally, the burning of vegetation releases nitrogen into the atmosphere, unlike elements such as potassium and phosphorus which remain in the ash and are quickly recycled into the soil. This loss of nitrogen caused by a fire produces a long-term reduction in the fertility of the soil, which can be recovered as atmospheric nitrogen is fixed and converted to ammonia by natural phenomena such as lightning or by leguminous plants such as clover, peas, and green beans.

Fire is one of the four classical elements and has been used by humans in rituals, in agriculture for clearing land, for cooking, generating heat and light, for signaling, propulsion purposes, smelting, forging, incineration of waste, cremation, and as a weapon or mode of destruction.

Etymology

The word "fire" originated from Old English Fyr 'Fire, a fire', which can be traced back to the Germanic root *fūr-, which itself comes from the Proto-Indo-European *perjos from the root *paewr- 'fire'. The current spelling of "fire" has been in use since as early as 1200, but it was not until around 1600 that it completely replaced the Middle English term fier (which is still preserved in the word "fiery").

History

Fossil record

The fossil record of fire first appears with the establishment of a land-based flora in the Middle Ordovician period, 470 million years ago, permitting the accumulation of oxygen in the atmosphere as never before, as the new hordes of land plants pumped it out as a waste product. When this concentration rose above 13%, it permitted the possibility of wildfire. Wildfire is first recorded in the Late Silurian fossil record, 420 million years ago, by fossils of charcoalified plants. Apart from a controversial gap in the Late Devonian, charcoal is present ever since. The level of atmospheric oxygen is closely related to the prevalence of charcoal: clearly oxygen is the key factor in the abundance of wildfire. Fire also became more abundant when grasses radiated and became the dominant component of many ecosystems, around 6 to 7 million years ago; this kindling provided tinder which allowed for the more rapid spread of fire. These widespread fires may have initiated a positive feedback process, whereby they produced a warmer, drier climate more conducive to fire.

Human control of fire

Early human control

The ability to control fire was a dramatic change in the habits of early humans. Making fire to generate heat and light made it possible for people to cook food, simultaneously increasing the variety and availability of nutrients and reducing disease by killing pathogenic microorganisms in the food. The heat produced would also help people stay warm in cold weather, enabling them to live in cooler climates. Fire also kept nocturnal predators at bay. Evidence of occasional cooked food is found from 1 million years ago. Although this evidence shows that fire may have been used in a controlled fashion about 1 million years ago, other sources put the date of regular use at 400,000 years ago. Evidence becomes widespread around 50 to 100 thousand years ago, suggesting regular use from this time; resistance to air pollution started to evolve in human populations at a similar point in time. The use of fire became progressively more sophisticated, as it was used to create charcoal and to control wildlife from tens of thousands of years ago.

Fire has also been used for centuries as a method of torture and execution, as evidenced by death by burning as well as torture devices such as the iron boot, which could be filled with water, oil, or even lead and then heated over an open fire to the agony of the wearer.

By the Neolithic Revolution, during the introduction of grain-based agriculture, people all over the world used fire as a tool in landscape management. These fires were typically controlled burns or "cool fires", as opposed to uncontrolled "hot fires", which damage the soil. Hot fires destroy plants and animals, and endanger communities. This is especially a problem in the forests of today where traditional burning is prevented in order to encourage the growth of timber crops. Cool fires are generally conducted in the spring and autumn. They clear undergrowth, burning up biomass that could trigger a hot fire should it get too dense. They provide a greater variety of environments, which encourages game and plant diversity. For humans, they make dense, impassable forests traversable. Another human use for fire in regards to landscape management is its use to clear land for agriculture. Slash-and-burn agriculture is still common across much of tropical Africa, Asia and South America. For small farmers, controlled fires are a convenient way to clear overgrown areas and release nutrients from standing vegetation back into the soil. However, this useful strategy is also problematic. Growing population, fragmentation of forests and warming climate are making the earth's surface more prone to ever-larger escaped fires. These harm ecosystems and human infrastructure, cause health problems, and send up spirals of carbon and soot that may encourage even more warming of the atmosphere – and thus feed back into more fires. Globally today, as much as 5 million square kilometres – an area more than half the size of the United States – burns in a given year.

Later human control

There are numerous modern applications of fire. In its broadest sense, fire is used by nearly every human being on Earth in a controlled setting every day. Users of internal combustion vehicles employ fire every time they drive. Thermal power stations provide electricity for a large percentage of humanity by igniting fuels such as coal, oil or natural gas, then using the resultant heat to boil water into steam, which then drives turbines.

Use of fire in war

The use of fire in warfare has a long history. Fire was the basis of all early thermal weapons. The Byzantine fleet used Greek fire to attack ships and men.

The invention of gunpowder in China led to the fire lance, a flame-thrower weapon dating to around 1000 CE which was a precursor to projectile weapons driven by burning gunpowder.

The earliest modern flamethrowers were used by infantry in the First World War, first used by German troops against entrenched French troops near Verdun in February 1915. They were later successfully mounted on armoured vehicles in the Second World War.

Hand-thrown incendiary bombs improvised from glass bottles, later known as Molotov cocktails, were deployed during the Spanish Civil War in the 1930s. Also during that war, incendiary bombs were deployed against Guernica by Fascist Italian and Nazi German air forces that had been created specifically to support Franco's Nationalists.

Incendiary bombs were dropped by Axis and Allies during the Second World War, notably on Coventry, Tokyo, Rotterdam, London, Hamburg and Dresden; in the latter two cases firestorms were deliberately caused in which a ring of fire surrounding each city was drawn inward by an updraft caused by a central cluster of fires. The United States Army Air Force also extensively used incendiaries against Japanese targets in the latter months of the war, devastating entire cities constructed primarily of wood and paper houses. The incendiary fluid napalm was used in July 1944, towards the end of the Second World War, although its use did not gain public attention until the Vietnam War.

Fire management

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Controlling a fire to optimize its size, shape, and intensity is generally called fire management, and the more advanced forms of it, as traditionally (and sometimes still) practiced by skilled cooks, blacksmiths, ironmasters, and others, are highly skilled activities. They include knowledge of which fuel to burn; how to arrange the fuel; how to stoke the fire both in early phases and in maintenance phases; how to modulate the heat, flame, and smoke as suited to the desired application; how best to bank a fire to be revived later; how to choose, design, or modify stoves, fireplaces, bakery ovens, or industrial furnaces; and so on. Detailed expositions of fire management are available in various books about blacksmithing, about skilled camping or military scouting, and about domestic arts.

Productive use for energy

Burning fuel converts chemical energy into heat energy; wood has been used as fuel since prehistory. The International Energy Agency states that nearly 80% of the world's power has consistently come from fossil fuels such as petroleum, natural gas, and coal in the past decades. The fire in a power station is used to heat water, creating steam that drives turbines. The turbines then spin an electric generator to produce electricity. Fire is also used to provide mechanical work directly by thermal expansion, in both external and internal combustion engines.

The unburnable solid remains of a combustible material left after a fire is called clinker if its melting point is below the flame temperature, so that it fuses and then solidifies as it cools, and ash if its melting point is above the flame temperature.

Physical properties

Chemistry

Fire is a chemical process in which a fuel and an oxidizing agent react, yielding carbon dioxide and water. This process, known as a combustion reaction, does not proceed directly and involves intermediates. Although the oxidizing agent is typically oxygen, other compounds are able to fulfill the role. For instance, chlorine trifluoride is able to ignite sand.

Fires start when a flammable or a combustible material, in combination with a sufficient quantity of an oxidizer such as oxygen gas or another oxygen-rich compound (though non-oxygen oxidizers exist), is exposed to a source of heat or ambient temperature above the flash point for the fuel/oxidizer mix, and is able to sustain a rate of rapid oxidation that produces a chain reaction. This is commonly called the fire tetrahedron. Fire cannot exist without all of these elements in place and in the right proportions. For example, a flammable liquid will start burning only if the fuel and oxygen are in the right proportions. Some fuel-oxygen mixes may require a catalyst, a substance that is not consumed, when added, in any chemical reaction during combustion, but which enables the reactants to combust more readily.

Once ignited, a chain reaction must take place whereby fires can sustain their own heat by the further release of heat energy in the process of combustion and may propagate, provided there is a continuous supply of an oxidizer and fuel.

If the oxidizer is oxygen from the surrounding air, the presence of a force of gravity, or of some similar force caused by acceleration, is necessary to produce convection, which removes combustion products and brings a supply of oxygen to the fire. Without gravity, a fire rapidly surrounds itself with its own combustion products and non-oxidizing gases from the air, which exclude oxygen and extinguish the fire. Because of this, the risk of fire in a spacecraft is small when it is coasting in inertial flight. This does not apply if oxygen is supplied to the fire by some process other than thermal convection.

Fire can be extinguished by removing any one of the elements of the fire tetrahedron. Consider a natural gas flame, such as from a stove-top burner. The fire can be extinguished by any of the following:

• turning off the gas supply, which removes the fuel source;
• covering the flame completely, which smothers the flame as the combustion both uses the available oxidizer (the oxygen in the air) and displaces it from the area around the flame with CO₂;
• application of an inert gas such as carbon dioxide, smothering the flame by displacing the available oxidizer;
• application of water, which removes heat from the fire faster than the fire can produce it (similarly, blowing hard on a flame will displace the heat of the currently burning gas from its fuel source, to the same end); or
• application of a retardant chemical such as Halon (largely banned in some countries as of 2023) to the flame, which retards the chemical reaction itself until the rate of combustion is too slow to maintain the chain reaction.

In contrast, fire is intensified by increasing the overall rate of combustion. Methods to do this include balancing the input of fuel and oxidizer to stoichiometric proportions, increasing fuel and oxidizer input in this balanced mix, increasing the ambient temperature so the fire's own heat is better able to sustain combustion, or providing a catalyst, a non-reactant medium in which the fuel and oxidizer can more readily react.

Flame

A flame is a mixture of reacting gases and solids emitting visible, infrared, and sometimes ultraviolet light, the frequency spectrum of which depends on the chemical composition of the burning material and intermediate reaction products. In many cases, such as the burning of organic matter, for example wood, or the incomplete combustion of gas, incandescent solid particles called soot produce the familiar red-orange glow of "fire". This light has a continuous spectrum. Complete combustion of gas has a dim blue color due to the emission of single-wavelength radiation from various electron transitions in the excited molecules formed in the flame. Usually oxygen is involved, but hydrogen burning in chlorine also produces a flame, producing hydrogen chloride (HCl). Other possible combinations producing flames, amongst many, are fluorine and hydrogen, and hydrazine and nitrogen tetroxide. Hydrogen and hydrazine/UDMH flames are similarly pale blue, while burning boron and its compounds, evaluated in mid-20th century as a high energy fuel for jet and rocket engines, emits intense green flame, leading to its informal nickname of "Green Dragon".

The glow of a flame is complex. Black-body radiation is emitted from soot, gas, and fuel particles, though the soot particles are too small to behave like perfect blackbodies. There is also photon emission by de-excited atoms and molecules in the gases. Much of the radiation is emitted in the visible and infrared bands. The color depends on temperature for the black-body radiation, and on chemical makeup for the emission spectra.

The common distribution of a flame under normal gravity conditions depends on convection, as soot tends to rise to the top of a general flame, as in a candle in normal gravity conditions, making it yellow. In microgravity or zero gravity, such as an environment in outer space, convection no longer occurs, and the flame becomes spherical, with a tendency to become more blue and more efficient (although it may go out if not moved steadily, as the CO₂ from combustion does not disperse as readily in microgravity, and tends to smother the flame). There are several possible explanations for this difference, of which the most likely is that the temperature is sufficiently evenly distributed that soot is not formed and complete combustion occurs. Experiments by NASA reveal that diffusion flames in microgravity allow more soot to be completely oxidized after they are produced than diffusion flames on Earth, because of a series of mechanisms that behave differently in micro gravity when compared to normal gravity conditions. These discoveries have potential applications in applied science and industry, especially concerning fuel efficiency.

Typical adiabatic temperatures

The adiabatic flame temperature of a given fuel and oxidizer pair is that at which the gases achieve stable combustion.

• Oxy–dicyanoacetylene 4,990 °C (9,000 °F)
• Oxy–acetylene 3,480 °C (6,300 °F)
• Oxyhydrogen 2,800 °C (5,100 °F)
• Air–acetylene 2,534 °C (4,600 °F)
• Blowtorch (air–MAPP gas) 2,200 °C (4,000 °F)
• Bunsen burner (air–natural gas) 1,300 to 1,600 °C (2,400 to 2,900 °F)
• Candle (air–paraffin) 1,000 °C (1,800 °F).

Fire science

Fire science is a branch of physical science which includes fire behavior, dynamics, and combustion. Applications of fire science include fire protection, fire investigation, and wildfire management.

Fire ecology

Every natural ecosystem on land has its own fire regime, and the organisms in those ecosystems are adapted to or dependent upon that fire regime. Fire creates a mosaic of different habitat patches, each at a different stage of succession. Different species of plants, animals, and microbes specialize in exploiting a particular stage, and by creating these different types of patches, fire allows a greater number of species to exist within a landscape.

Prevention and protection systems

Wildfire prevention programs around the world may employ techniques such as wildland fire use and prescribed or controlled burns. Wildland fire use refers to any fire of natural causes that is monitored but allowed to burn. Controlled burns are fires ignited by government agencies under less dangerous weather conditions.

Fire fighting services are provided in most developed areas to extinguish or contain uncontrolled fires. Trained firefighters use fire apparatus, water supply resources such as water mains and fire hydrants or they might use A and B class foam depending on what is feeding the fire.

Fire prevention is intended to reduce sources of ignition. Fire prevention also includes education to teach people how to avoid causing fires. Buildings, especially schools and tall buildings, often conduct fire drills to inform and prepare citizens on how to react to a building fire. Purposely starting destructive fires constitutes arson and is a crime in most jurisdictions.

Model building codes require passive fire protection and active fire protection systems to minimize damage resulting from a fire. The most common form of active fire protection is fire sprinklers. To maximize passive fire protection of buildings, building materials and furnishings in most developed countries are tested for fire-resistance, combustibility and flammability. Upholstery, carpeting and plastics used in vehicles and vessels are also tested.

Where fire prevention and fire protection have failed to prevent damage, fire insurance can mitigate the financial impact.

See also

• Aodh (given name)
• Bonfire
• The Chemical History of a Candle
• Colored fire
• Control of fire by early humans
• Deflagration
• Fire (classical element)
• Fire investigation
• Fire lookout
• Fire lookout tower
• Fire making
• Fire pit
• Fire safety
• Fire triangle
• Fire whirl
• Fire worship
• Flame test
• Life Safety Code
• List of fires
• List of light sources
• Phlogiston theory
• Piano burning
• Prometheus, the Greek mythological figure who gave mankind fire
• Pyrokinesis
• Pyrolysis
• Pyromania
• Self-immolation

References

Notes

1. Slower oxidative processes like rusting or digestion are not included by this definition.

Citations

1. Glossary of Wildland Fire Terminology (PDF). National Wildfire Coordinating Group. October 2007. p. 70. Archived from the original (PDF) on 2008-08-21. Retrieved 2008-12-18.
2. Helmenstine, Anne Marie. "What is the State of Matter of Fire or Flame? Is it a Liquid, Solid, or Gas?". About.com. Archived from the original on 24 January 2009. Retrieved 2009-01-21.
3. Helmenstine, Anne Marie. "What is the State of Matter of Fire or Flame? Is it a Liquid, Solid, or Gas?". About.com. Archived from the original on 2009-01-24. Retrieved 2009-01-21.
4. Lentile, et al., 319
5. Morris, S. E.; Moses, T. A. (1987). "Forest Fire and the Natural Soil Erosion Regime in the Colorado Front Range". Annals of the Association of American Geographers. 77 (2): 245–54. doi:10.1111/j.1467-8306.1987.tb00156.x. ISSN 0004-5608.
6. "SCIENCE WATCH; Burning Plants Adding to Nitrogen". The New York Times. 1990-08-14. ISSN 0362-4331. Archived from the original on 2024-05-27. Retrieved 2023-11-02.
7. "How Do Wildfires Affect Soil? - Applied Earth Sciences". 2019-11-12. Archived from the original on 2024-05-27. Retrieved 2023-11-02.
8. "Fire". Online Etymology Dictionary. Archived from the original on 2024-05-27. Retrieved 2023-03-24.
9. Wellman, C. H.; Gray, J. (2000). "The microfossil record of early land plants". Philos Trans R Soc Lond B Biol Sci. 355 (1398): 717–31, discussion 731–2. doi:10.1098/rstb.2000.0612. PMC 1692785. PMID 10905606.
10. Jones, Timothy P.; Chaloner, William G. (1991). "Fossil charcoal, its recognition and palaeoatmospheric significance". Palaeogeography, Palaeoclimatology, Palaeoecology. 97 (1–2): 39–50. Bibcode:1991PPP....97...39J. doi:10.1016/0031-0182(91)90180-Y.
11. Glasspool, I.J.; Edwards, D.; Axe, L. (2004). "Charcoal in the Silurian as evidence for the earliest wildfire". Geology. 32 (5): 381–383. Bibcode:2004Geo....32..381G. doi:10.1130/G20363.1.
12. ^ Scott, AC; Glasspool, IJ (2006). "The diversification of Paleozoic fire systems and fluctuations in atmospheric oxygen concentration". Proceedings of the National Academy of Sciences of the United States of America. 103 (29): 10861–5. Bibcode:2006PNAS..10310861S. doi:10.1073/pnas.0604090103. PMC 1544139. PMID 16832054.
13. ^ Bowman, D. M. J. S.; Balch, J. K.; Artaxo, P.; Bond, W. J.; Carlson, J. M.; Cochrane, M. A.; d'Antonio, C. M.; Defries, R. S.; Doyle, J. C.; Harrison, S. P.; Johnston, F. H.; Keeley, J. E.; Krawchuk, M. A.; Kull, C. A.; Marston, J. B.; Moritz, M. A.; Prentice, I. C.; Roos, C. I.; Scott, A. C.; Swetnam, T. W.; Van Der Werf, G. R.; Pyne, S. J. (2009). "Fire in the Earth system". Science. 324 (5926): 481–4. Bibcode:2009Sci...324..481B. doi:10.1126/science.1163886. PMID 19390038. S2CID 22389421. Archived from the original on 2024-05-27. Retrieved 2024-01-26.
14. Retallack, Gregory J. (1997). "Neogene expansion of the North American prairie". PALAIOS. 12 (4): 380–90. Bibcode:1997Palai..12..380R. doi:10.2307/3515337. JSTOR 3515337.
15. Gowlett, J. A. J. (2016). "The discovery of fire by humans: a long and convoluted process". Philosophical Transactions of the Royal Society B: Biological Sciences. 371 (1696): 20150164. doi:10.1098/rstb.2015.0164. PMC 4874402. PMID 27216521.
16. Gowlett, J. A. J.; Wrangham, R. W. (2013). "Earliest fire in Africa: towards the convergence of archaeological evidence and the cooking hypothesis". Azania: Archaeological Research in Africa. 48 (1): 5–30. doi:10.1080/0067270X.2012.756754. S2CID 163033909.
17. Kaplan, Matt (2012). "Million-year-old ash hints at origins of cooking". Nature. doi:10.1038/nature.2012.10372. S2CID 177595396. Archived from the original on 1 October 2019. Retrieved 25 August 2020.
18. O'Carroll, Eoin (5 April 2012). "Were Early Humans Cooking Their Food a Million Years Ago?". ABC News. Archived from the original on 4 February 2020. Retrieved 10 January 2020. Early humans harnessed fire as early as a million years ago, much earlier than previously thought, suggests evidence unearthed in a cave in South Africa.
19. Francesco Berna; et al. (May 15, 2012). "Microstratigraphic evidence of in situ fire in the Acheulean strata of Wonderwerk Cave, Northern Cape province, South Africa". PNAS. 109 (20): E1215 – E1220. doi:10.1073/pnas.1117620109. PMC 3356665. PMID 22474385.
20. ^ Bowman, D. M. J. S.; et al. (2009). "Fire in the Earth system". Science. 324 (5926): 481–84. Bibcode:2009Sci...324..481B. doi:10.1126/science.1163886. PMID 19390038. S2CID 22389421. Archived from the original on 2024-05-27. Retrieved 2024-01-26.
21. Pyne, Stephen J. (1998). "Forged in Fire: History, Land and Anthropogenic Fire". In Balée, William (ed.). Advances in Historical Ecology. Historical Ecology Series. University of Columbia Press. pp. 78–84. ISBN 0-231-10632-7. Archived from the original on 2024-05-27. Retrieved 2023-03-19.
22. ^ Krajick, Kevin (16 November 2011). "Farmers, Flames and Climate: Are We Entering an Age of 'Mega-Fires'? – State of the Planet". Columbia Climate School. Archived from the original on 2012-05-26. Retrieved 2012-05-23.
23. "In Pictures: German destruction Archived 2019-12-13 at the Wayback Machine". BBC News.
24. "Flamethrower in action". nzhistory.govt.nz. Archived from the original on 2024-05-27. Retrieved 2023-11-02.
25. David P. Barash; Charles P. Webel (10 July 2008). Peace and Conflict Studies. SAGE. p. 365. ISBN 978-1-4129-6120-2. Archived from the original on 27 May 2024. Retrieved 2 September 2022.
26. Guillaume, Marine (2016-12-01). "Napalm in US Bombing Doctrine and Practice, 1942-1975" (PDF). The Asia-Pacific Journal. 14 (23). Archived (PDF) from the original on 2020-09-04.
27. Sterrett, Frances S., ed. (1995). Alternative fuels and the environment. Boca Raton: Lewis. ISBN 978-0-87371-978-0.
28. (October 2022), "World Energy Outlook 2022 Archived 2022-10-27 at the Wayback Machine", IEA.
29. "How electricity is generated". U.S. Energy Information Administration. Retrieved 2023-11-02.
30. ^ "What is fire?". New Scientist. Archived from the original on February 2, 2023. Retrieved November 5, 2022.
31. Lowe, Derek (February 26, 2008). "Sand Won't Save You This Time". Science. Archived from the original on February 19, 2023. Retrieved November 5, 2022.
32. NASA Johnson (29 August 2008). "Ask Astronaut Greg Chamitoff: Light a Match!". Archived from the original on 2021-12-11. Retrieved 30 December 2016 – via YouTube.
33. Inglis-Arkell, Esther (8 March 2011). "How does fire behave in zero gravity?". Archived from the original on 13 November 2015. Retrieved 30 December 2016.
34. Spiral flames in microgravity Archived 2010-03-19 at the Wayback Machine, National Aeronautics and Space Administration, 2000.
35. CFM-1 experiment results Archived 2007-09-12 at the Wayback Machine, National Aeronautics and Space Administration, April 2005.
36. LSP-1 experiment results Archived 2007-03-12 at the Wayback Machine, National Aeronautics and Space Administration, April 2005.
37. "Flame temperatures". www.derose.net. Archived from the original on 2014-04-17. Retrieved 2007-07-09.
38. Begon, M., J.L. Harper and C.R. Townsend. 1996. Ecology: individuals, populations, and communities, Third Edition. Blackwell Science Ltd., Cambridge, Massachusetts, US
39. Federal Fire and Aviation Operations Action Plan, 4.
40. "UK: The Role of Fire in the Ecology of Heathland in Southern Britain". International Forest Fire News. 18: 80–81. January 1998. Archived from the original on 2011-07-16. Retrieved 2011-09-03.
41. "Prescribed Fires". SmokeyBear.com. Archived from the original on 2008-10-20. Retrieved 2008-11-21.
42. Fire & Life Safety Education, Manitoba Office of the Fire Commissioner Archived December 6, 2008, at the Wayback Machine
43. Ward, Michael (March 2005). Fire Officer: Principles and Practice. Jones & Bartlett Learning. ISBN 9780763722470. Archived from the original on February 16, 2022. Retrieved March 16, 2019.
44. Baars, Hans; Smulders, Andre; Hintzbergen, Kees; Hintzbergen, Jule (2015-04-15). Foundations of Information Security Based on ISO27001 and ISO27002 (3rd revised ed.). Van Haren. ISBN 9789401805414. Archived from the original on 2021-04-11. Retrieved 2020-10-25.

Sources

• Haung, Kai (2009). Population and Building Factors That Impact Residential Fire Rates in Large U.S. Cities. Applied Research Project Archived 2012-03-08 at the Wayback Machine. Texas State University.
• Karki, Sameer (2002). Community Involvement in and Management of Forest Fires in South East Asia (PDF). Project FireFight South East Asia. Archived from the original (PDF) on February 25, 2009. Retrieved 2009-02-13.
• Kosman, Admiel (January 13, 2011). "Sacred fire". Haaretz.
• Lentile, Leigh B.; Holden, Zachary A.; Smith, Alistair M. S.; Falkowski, Michael J.; Hudak, Andrew T.; Morgan, Penelope; Lewis, Sarah A.; Gessler, Paul E.; Benson, Nate C (2006). "Remote sensing techniques to assess active fire characteristics and post-fire effects". International Journal of Wildland Fire. 3 (15): 319–345. doi:10.1071/WF05097. S2CID 724358. Archived from the original on 2014-08-12. Retrieved 2010-02-04.

Further reading

• Pyne, Stephen J. Fire : a brief history (University of Washington Press, 2001).
  • Pyne, Stephen J. World fire : the culture of fire on earth (1995) online
  • Pyne, Stephen J. Tending fire : coping with America's wildland fires (2004) online
  • Pyne, Stephen J. Awful splendour : a fire history of Canada (2007) online
  • Pyne, Stephen J. Burning bush : a fire history of Australia (1991) online
  • Pyne, Stephen J. Between Two Fires: A Fire History of Contemporary America (2015)
  • Pyne, Stephen J. California: A Fire Survey (2016)
• Safford, Hugh D., et al. "Fire ecology of the North American Mediterranean-climate zone." in Fire ecology and management: Past, present, and future of US forested ecosystems (2021): 337–392. re California and its neighbors online

External links

• How Fire Works at HowStuffWorks
• What exactly is fire? from The Straight Dope
• On Fire, an Adobe Flash–based science tutorial from the NOVA (TV series)
• "20 Things You Didn't Know About... Fire" from Discover magazine

• Fire
• Terrestrial plasmas
• Cooking techniques