Petroleum that occurs naturally under normal
conditions of temperature and pressure in the ground in a
gaseous state. Most natural gas is methane, followed by
ethane, propane, butane, and pentane, with common impurities
of inorganic gases including nitrogen, carbon dioxide,
and hydrogen sulfide. Natural gas has an origin similar to
other hydrocarbons, being derived from the decomposition of
buried organic matter. It is simply the lighter end member of
the spectrum of compositions of hydrocarbons, and being a
gas, it has only gaseous hydrocarbons (C1-C5) with no C6+
compounds. All types of organic matter can contribute to the
formation of natural gas, when buried and heated to more
than 320°F (160°C). Some natural gas is generated during the
decomposition of coal and petroleum when they are heated
above 320°F, whereas other gas is produced along with the
generation of other hydrocarbons. An additional type of natural
gas is biogenic methane, produced at shallow levels by
the biodegradation of petroleum, and when bacteria reduce
carbon dioxide to methane in shallow sediments. Natural gas
is abundant in shallow crustal reservoirs and is useful as a
fossil fuel. It generally burns much cleaner than petroleum or
coal and so is increasingly being sought as an energy source.
Reserves of natural gas are huge and may greatly exceed the
remaining reserves of petroleum in the world.
See also HYDROCARBON; PETROLEUM.
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