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Fire 2

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Fire 2


Fire is a topic on which most people can comment. Fire is a widespread phenomenon. Most of us have seen fires in natural vegetation, or their effects; stark, blackened vegetation or a smoke pall. Because fires such as these can have damaging economic and social effects, can spoil forestry timber, can burn down houses and farms, and can kill people and animals, there has been a lot written about wildfires. Added to this wide perception of the damage that can be caused by wildfires, there has been increasing publicity given, since the 1950's, to the active use of fire as a management tool, particularly in protecting against severe wildfires. The introduction of a policy of deliberate burning as a management tool has a fascinating history, especially in the United States Forest Service, but the ecological effects of prescribing a fixed burning regime on large tracts of land are increasingly being questioned (Lyons, 1985, 3).

To an ecologist, fire can be treated as just one of the many factors in an environment. It compares with droughts, floods, hurricanes and other physical disturbances because of the direct impact it makes on organisms. Unlike these physical factors, however, fire as a disturbing force is itself influenced by the biota, particularly the plant community. Alteration of the vegetation by any number of factors can influence the nature of a subsequent fire. Fire has similarities to grazing as a force on vegetation because of such feedback effects (Whelan, 1995, 20).

Fire History

When cavemen learned to make and use fire, they could start to live in civilized ways. With fire, they were able to cook their food so that it was easier to eat and tasted better. By the light of torches, men could more easily find their way at night. They could also improve their wooden tools by hardening the points in fire. With fire to keep them warm, they could live in the colder regions and spread out over the Earth ([CD-ROM], 1996).

It is supposed that early people got fire accidentally from trees set ablaze by lightning or from spouting volcanoes. Then they carefully kept it burning in huts or caves. As far back as the study has gone, primitive peoples have never been found without fire for warmth and cooking. Fire also protected them from wild beasts ([CD-ROM], 1996).

In time people discovered how to create fire by rubbing dry sticks together. Then they invented bow drills to aid the process. When they began to chip flint to make axes, they found that hot sparks came from the stone. From this they later developed the flint-and-steel method of fire making. Later it was found that fire could be made by focusing the sun's rays with a lens or curved mirror ([CD-ROM], 1996).

People remained ignorant of the true character of fire until 1783. In that year the great French chemist Antoine Lavoisier investigated the properties of oxygen and laid the foundation for modern chemistry ([CD-ROM], 1996).

Lavoisier showed that ordinary fire is due to the chemical process called oxidation, which is the combination of a substance with oxygen. He disproved the earlier "phlogiston" theory. The phlogiston theory held that when an object was heated or cooled it was due to a mysterious substance (phlogiston) that flowed into or out of the object in question ([CD-ROM], 1996).

Since fires are due to oxidation, they need air to burn properly, and a flame will go out after it has used up the oxygen in a closed vessel. Almost anything will combine with oxygen if enough time is allowed. Iron will rust if exposed long to damp air, and the rust is simply oxidized iron. When the chemical combination is so rapid that it is accompanied by a flame, it is called combustion ([CD-ROM], 1996).

Ignition Point or Kindling Temperature

Heat is required to start combustion. The degree of temperature at which a substance will catch fire and continue to burn is called its ignition point or its kindling point. A substance that can be ignited in the air is said to be flammable (or inflammable). The flash point of a flammable liquid is lower than its ignition point. The flash point is the temperature at which it gives off sufficient vapor to flash, or flame suddenly, in the air. It is not the temperature at which the substance will continue to burn ([CD-ROM], 1996).

When primitive peoples rubbed two sticks together to kindle a fire, they discovered without knowing it that the ignition point of wood is usually quite high. They had to use enough energy to create a good deal of heat before flames appeared. The tip of a match is composed of chemicals that, under ordinary circumstances, have a low ignition point. The heat created by scratching it once on a rough surface is enough to start combustion. It must be remembered, however, that the temperature needed to sustain combustion can vary with the condition of the substance and the pressure of the air or other gases involved, as well as with laboratory test methods ([CD-ROM], 1996).

Lowering the Temperature Puts Out Fire

After a fire has started, it will be self-supporting only when the temperature created by the combustion of the burning substance is as high or higher than its ignition point. This is one of the most important laws of fire. Some very hard woods, such as ebony, require a great deal of heat to burn. If the end of a stick of ebony is placed in a coal fire, it will burn. When it is drawn out, the fire of the smoldering ebony itself is lower in temperature than the ignition point of the wood. The flames thus will die (Lyons, 1985, 5).

This principle explains why a match can be blown out. One's breath carries away the heat, and the temperature falls below the ignition point of the matchstick. The stream of water from a firefighter's hose cools the burning walls of a building with a similar result (Lyons, 1985, 5).

The heat of a fire depends on the speed with which chemicals combine with oxygen. This speed depends generally on the quantity of oxygen present. If a lit match is touched to a small piece of iron wire, it will not burn. If a tip of a match is fastened to the end of the wire, struck, and plunged quickly into a jar of pure oxygen, the wire will catch fire and burn, with bright sparks shooting off briskly (Lyons, 1985, 6).

Fire Without Flame

Fire may burn either with or without flames. A flame always indicates that heat has forced gas from a burning substance. The flames come from the combination of this gas with oxygen in the air. When a coal fire flames, it does so because gas is being forced from the coal, and the carbon and hydrogen in the gas combine with oxygen. If kept from burning, such gas can be stored. Manufactured gas is forced from coal in airtight kilns, or retorts. The product left after the gas is extracted from coal is called coke. Coke will burn without flame because no gas is driven off. In order to burn, the carbon in the coke combines directly with oxygen (Lyons, 1985, 8).

It is the gas given off by the heated wax in a candle that produces the bright flame. When a burning candle is blown out, for example, a thin ribbon of smoke will arise. If a lighted match is passed through this smoke an inch (2.5 centimeters) above the wick, a tiny flame will run down and relight the candle (Lyons, 1985, 8).

The brightest flames are not always the hottest. Hydrogen, which combines with oxygen when burning to form water, has an almost invisible flame even under ordinary circumstances. When it is absolutely pure and the air around it is completely free of dust, the hydrogen flame cannot be seen even in a dark room (Lyons, 1985, 9).

Whenever a flammable gas is mixed with air in exactly the quantities necessary for complete combination, it will burn so fast as to create an explosion. This is what takes place in a gasoline engine. The carburetor provides the air mixture, and the electric spark sets it on fire.

The small explosions that sometimes occur after the burners of a gas stove are turned off are from the gas remaining in the pipe. Air creeps in through the air valve until the mixture becomes explosive, and the tiny flame that remains on the burner fires back (Lyons, 1985, 9).

Legends and Worship of Fire

Tribal legends of the North American Indians say various animals showed the Indians' ancestors how to make fire. Other early peoples said that fire came down from heaven in magic ways. According to a myth of ancient Greece, Prometheus, a member of the giant race of Titans, stole fire from the sun and carried it to the Earth. There is much evidence that primitive peoples used fire for some time before they learned how to kindle it. When they captured fire, they tended it carefully so that it would not go out ([CD-ROM] 1996).

Gradually the legends of the magic origin of fire and the tending of perpetual fires were associated with religious practices. Fire worship was often associated with sun worship. Fire was said to be the earthly representative of the sun-god. Sacred fires were preserved in temples by the Egyptians, Greeks, and Romans. Priests or certain special people watched the fires. Among the most famous were the Vestal Virgins in the Temple of Vesta in Rome. The Mayas and Aztecs kept sacred fires burning on top of high pyramids or fire altars. The Iranian religion Zoroastrianism maintains a sacred fire that must be fed at least five times a day ([CD-ROM] 1996).

The history of fire is the history of progress. As people have learned how to tame fire and make it their servant, they have been able to develop the forces of nature. Fire has yielded the power of steam. It has extracted metals from rocks. It has helped make rubber from the gum of a tree and hard brick from soft clay. It is essential to a wide variety of manufacturing processes ([CD-ROM] 1996).

Forest Fires on the Home Front

Forest fires are a natural part of a forest's life cycle. Indeed, the extreme weather and forest fires we are experiencing this spring and summer are not unique -- Canadians have endured forest loss, flooding and heat waves for many, many years. But what is new and alarming is the frequency at which these events are now occurring. In the last fifteen years, we have experienced five of the seven worst forest fire years in recorded Canadian history. And, not surprisingly, in that same period we have lived through eight of the warmest years on record (UNEP, [On-line], 1998).

Canadians can continue to expect more fires, more often and earlier in the season. While there are fluctuations in forest fire activity from year to year, the trend is clearly upward. Since the early eighties, there has been a two-fold increase in forest fire activity. From 1920 to 1980, the average annual amount of forest loss due to fire was about one million hectares. Since then,

the average has been around 2.2 million hectares (...

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