Chemical reactions are the heart of chemistry.
People have always known that they exist. The Ancient Greeks were the firsts to
speculate on the composition of matter. They thought that it was possible that
individual particles made up matter. Later, in the Seventeenth Century, a
German chemist named George Ernst Stahl was the first to postulate on chemical
reaction, specifically, combustion. He said that a substance called phlogiston
escaped into the air from all substances during combustion. He explained that a
burning candle would go out if a candle snuffer was put over it because the air
inside the snuffer became saturated with phlogiston. According to his ideas,
wood is made up of phlogiston and ash, because only ash is left after
combustion. His ideas soon came upon some contradiction. When metal is burned,
its ash has a greater mass than the original substance. Stahl tried to cover
himself by saying that phlogiston will take away from a substances mass or that
it had a negative mass, which contradicted his original theories.
In
the Eighteenth Century Antoine-Laurent Lavoisier, in France, discovered an
important detail in the understanding of the chemical reaction combustion,
oxigine (oxygen). He said that combustion was a chemical reaction involving
oxygen and another combustible substance, such as wood.
The
large diversity of chemical reactions and approaches to their study results in
the existence of several concurring, often overlapping, ways of classifying
them. Below are examples of widely used terms for describing common kinds of
reactions. When a chemical reaction occurs, the reactants and the product must
get an equal amount of energy. The term combustion is usually used for only
large-scale oxidation of whole molecules, i.e. a controlled oxidation of a
single functional group is not combustion. The general application of
combustion reactio is fossil fuels.
Mankind
has used fossil fuels for a very long time. The Chinese used coal for heating
and metal smelting around 500 BC. Roman historians describe coal being used for
heating residences in Britannia during the roman occupation. During the
industrial revolution in the 18th century more large-scale mining operations of
coal started and oil was later introduced as a replacement for coal. Coal
fueled Great Britain’s almost exponential growth of industry and combustion
provided energy for the first true worldwide empire. In the end of 18th century
was discovered that kerosene could be extracted from crude oil and by using
refining even more usable fuels could be obtained. The demand for oil was
greatly increased and after the First World War it became the primary fuel for
the industrialized world.
The
combustion of all fossil fuels follows a very similar reaction: Fuel (any hydrocarbon source) plus oxygen
yields carbon dioxide and water and energy. A simple combustion reaction
is given for methane. The combustion of methane means that it is possible to
burn it. The world and modern society are driven by the need to produce energy to
make products (manufacturing), to move around (transportation), to heat homes
and buildings, and to create light (electricity). At least 75% of these needs
are met by the combustion of fossil fuels. Energy is stored in chemical
compounds in the bonds that bind atoms to each other.
Fossil fuels are of great importance because they can be
burned (oxidized
to carbon
dioxide and water), producing significant amounts of energy. The use
of coal
as a fuel predates recorded history. Coal was used to run furnaces for the
melting of metal ore. Semi-solid hydrocarbons from seeps were also burned in
ancient times, but these materials were mostly used for waterproofing and embalming.
Commercial exploitation of petroleum,
largely as a replacement for oils from animal sources (notably whale oil)
for use in oil lamps began in the nineteenth century.
Natural gas, once flared-off as an un-needed
byproduct of petroleum production, is now considered a very valuable resource.
Heavy crude oil, which is much more viscous
than conventional crude oil, and tar sands,
where bitumen
is found mixed with sand and clay, are becoming more important as sources of
fossil fuel. Oil shale
and similar materials are sedimentary rocks containing kerosene, a complex mixture of high-molecular weight organic
compounds, which yield synthetic crude oil when heated.
These materials have yet to be exploited commercially.
These fuels are employed in internal combustion engines, fossil fuel power stations and other uses.
Prior to the latter half of the eighteenth century, windmills
or watermills
provided the energy needed for industry such as milling flour, sawing wood
or pumping water, and burning wood or peat provided domestic
heat. The wide-scale use of fossil fuels, coal at first and petroleum later, to
fire steam engines,
enabled the Industrial Revolution. At the same time, gas lights
using natural gas or coal gas were coming into wide use. The invention of the internal combustion engine and its use in automobiles
and trucks
greatly increased the demand for gasoline and diesel oil, both made from fossil fuels. Other
forms of transportation, railways and aircraft
also required fossil fuels. The other major use for fossil fuels is in generating electricity and the petrochemical
industry. Tar,
a leftover of petroleum extraction, is used in construction of roads.
Early combustion techniques: The
first, coal ovens were very similar to ordinary wood ovens and were used for
heat generation. The typical design was a bed of stone, on which coal was
placed and ignited. More coal was added to the fire when the original coal was
combusted. Ash and soot remained in a pile together with unburned coal and had
to be removed from time to time. The second, critical and supercritical steam boilers: with
the invention of electricity generators combustion was quickly adapted to drive
steam boilers for power generation. The supercritical systems will result in
slightly less fuel consumption due to the higher efficiency. The term boiler is
a bit misleading as no actual boiling takes place in a supercritical system.
The third, fixed-bed or stoker
combustion: the primitive ovens were soon improved and refined
once more large scale-coal combustion became important for heat and electricity
production. This resulted in the so-called fixed-bed systems or Stoker systems.
The fourth, pulverized coal combustion:
if coal particles are made
fine enough, they will burn almost as easily and efficiently as a gas. This
idea has resulted in the concept of pulverized coal combustion, which is the
most wide just principle of combustion world wide today.
The
fifth, cyclone furnace combustion: cyclone
furnaces are an improved version of cyclone
furnace combustion systems that requires less processing of the fuel and
can use a wider array of different coal types. With a cyclone furnace it is possible
to burn low-grade coal with high water and ash content. The coal is first
crushed, into smaller pieces, and can be stored in containers or transported
directly into the combustion area. The pieces do not have to be as small as in cyclone furnace combustion. The
furnace itself is basically a large cylinder jacketed with water pipes that
absorb some of the heat to make steam and protect the burner from melting. The
sixth, cogeneration and polygeneration
plants: fossil-fired power plants can also operate in
cogeneration mode. This means that both useful electricity and heat is produced
instead of only electricity. However this is only feasible if the power plant
is located close to the consumers to the heat can be transported without being
lost. Usually the heat is used for industrial processes, hot water generation
or residential heating. By capturing the heat instead of cooling it away more
useful energy can be produced from the same amount of fuel. The seventh, fluidized-bed combustion: by
suspending a solid fuel on an upward-blowing jet of air a so-called fluidized
bed can be obtained. The result is a turbulent mixing of gas and solids, which
provide more effective chemical reactions and heat transfer. The behavior
resembles to a bubbling fluid and gives a rapid mixing of particles. Compared
to cyclone combustion the temperature is lower. Fluidized-bed combustion is of particular value for low-grade, high
ash coals that are difficult to pulverize and might have varying combustion
properties. The eighth, integrated
gasification combined cycle: the integrated gasification combined cycle design creates a synthesis
gas from coal or any other carbon source and burns the gas in a high efficiency
gas turbine. It is also easier to clean out impurities and noxious materials
from the syngas compared to cleaning the exhaust vapor from ordinary combustion
of coal. The ninth, combustion of oil:
Today only a very small percentage of the worlds electricity comes
from combustion of oil. After the oil crisis in the 1980-ies most oil-fired
power plants have shut down due to high oil prices. The tenth, combustion of gas: natural gas
is burned in gas turbines.
Finally, emissions from fossil combustion Coal combustion is by far
the dominating source of carbon dioxide emissions from power generation. Almost
60% of the world total CO2 emissions from power generation come from coal-fired
power plants. However there are also more problems with combustion of fossil
fuels than just the released carbon dioxide. Coal is mostly composed of organic
matter, but inorganic compounds are also present. It is primary the inorganic
material that is deemed responsible for health, environmental and technological
problems related to coal combustion. Some of these inorganic trace elements are
even naturally radioactive. Sulphur constitutes of a major part of the
unhealthy elements in coal. During combustion if can react with oxygen and form
sulphur dioxide, which is toxic and leads to acid rain. Nowadays
desulphurization is standard procedure for most coal-fired power plants and the
emissions have been drastically reduced. Nitrogen can form NOx during
combustion. Nitrous oxides are toxic and believed to aggregate asthmatic
conditions. Eventually it can produce ground-level ozone, which in unhealthy and
irritating. It can also react with water and form nitric acid, which leads to
acid rain. NOx formation is generally prevented in modern combustion power
plants by various methods such as scrubbing. Smog can be formed from Sox, NOx,
volatile organic compounds, peroxyacyl nitrates and aldehydes resulting from
incomplete combustion. It is an unhealthy mixture of fog and smoke, which cause
problems in urban areas with much combustion. With proper flue gas treatment
the possibility for smog creation is reduced to very small numbers.
Will the supplies of
fuels we use today come to an end? Fossil energy sources by their very nature
are a limited resource, though some are far more abundant than others. We are currently in an energy
crisis. Fossil fuels are the lifeblood of our society and for many others
around the world. Our supply has a finite end, which is why we are willing to
go to war for it and make friends with those we really hate. The former Soviet
Union and many of the countries in the Middle East are in our good favor
strictly because of their oil reserves. Our foreign aid has a legitimate
purpose. Even with our newfound friends, fossil fuels will run out and the use
of them will soon take the lives of many people. These are important reasons to
find other means of getting the energy we need to continue our society as we
know it.
So what are our options? Alternative forms of energy are currently under
development even though most of them are only in their inital stages. With
increased government and public support, we may be able to speed up the
development of these technologies and help free ourselves from the usage of
fossil fuels. Oil companies will have to be dealt with because with the future
shortages of fossil fuels, they would stand to reap enormous profits. To
prevent this, oil and other energy resource providing companies should be
encouraged to develop these technologies for the sake of ethics if not for
long-term profit gains when all fossil fuel resources are exhausted.
Sources:
House,
James E. Inorganic Chemistry. 2008.
Canada: Elsevier
Huheey,
James. Inorganic Chemistry. 1993.
USA: Harper Collins College Piblishers
Sugiyarto,
KH. Kimia Anorganik 1. 2004.
Yogyakarta: FMIPA UNY
Bartok, William;
Sarofim, Adel F. 1991. Fossil Fuel Combustion: A Source Book.
New York: John Wiley & Sons, Inc.,
Seidel, Stephen. Can We Delay a Greenhouse Warming?.
1983. Washington, D.C.: Strategic Studies Staff, Office of Policy Analysis
http://www.visionlearning.com/library/module_viewer.php?mid=54
http://www.scienceclarified.com/Ci-Co/Combustion.html
http://www.green-planet-solar-energy.com/fossil-fuels.html
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