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Methane

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Properties
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General
NameMethane
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\nLewis Structure:\n H \n | \n H-C-H\n | \n H \n
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Chemical formulaCH4
Formula weight16.04 amu
SynonymsMarsh gas; Methyl hydride
CAS number74-82-8
Phase behavior
Melting point90.6 K (-182.5°C)
Boiling point111 K (-162°C)
Triple point90.67 K (-182.48°C)
\n 0.117 bar
Critical point190.6 K (-82.6°C)
\n 46 bar
ΔfusH1.1 kJ/mol
ΔvapH8.17 kJ/mol
\nGas properties
ΔfH0gas-74.87 kJ/mol
S0gas188 J/mol·K
Cp35.69 J/mol·K
Safety
Acute effectsAsphyxia; in severe cases unconsciousness, cardiac arrest or CNS injury. The compound is transported as a cryogenic liquid, exposure to this will obviously cause frostbite.
Chronic effects???
Flash point-188°C
Autoignition temperature600°C\n
Explosive limits5-15%
More info
PropertiesNIST WebBook\n
MSDSHazardous Chemical Database
\n\nSI units were used where possible. Unless otherwise stated, standard conditions were used.\n

Disclaimer and references\n\n

The simplest hydrocarbon, methane is a gas with a chemical formula of CH4. \nA principal component of natural gas, methane is a significant fuel. Burning one molecule of methane in the presence of oxygen releases one molecule of CO2 (carbon dioxide) and two molecules of H2O (water):\n: CH4 + 2O2 → CO2 + 2H2O Due to the heat and attack by the active species, the methane reacts to a methyl radical (CH3), which reacts to formaldehyde (HCHO or H2CO). The formaldehyde reacts to a formal radical (HCO), which then forms carbon monoxide (CO). The process is called oxidative pyrolysis: \n:CH4 + O2 CO + H2 + H2O \nFollowing oxidative pyrolysis, the H2 oxidizes, forming H2O, replenishing the active species, and releasing heat. This occurs very quickly, usually in less than a millisecond. \n:H2 + ½ O2 H2O \nFinally, the CO oxidizes, forming CO2 and releasing more heat. This process is generally slower than the other chemical steps, and typically requires a few to several milliseconds to occur. \n:CO + ½ O2 CO2 The strength of the carbon-hydrogen covalent bond in methane is among the strongest in all hydrocarbons, and thus its use as a chemical feedstock is limited. The search for catalysts which can facilitate C-H bond activation in methane and other low alkanes is an area of research with considerable industrial significance. Pure methane is odorless, but when used as a fuel is usually mixed with small quantities of strongly-smelling sulfur compounds such as ethyl mercaptan to enable the detection of leaks. Methane is a greenhouse gas with a global warming potential of 21 (meaning that it has 21 times the warming ability of carbon dioxide). Methane results from the decomposition of certain organic matters in the absence of oxygen. It is therefore also classified as a biogas. Principal sources are\n* decomposition of organic wastes\n* natural sources (marshes) : 23 %\n* fossil fuel extraction : 20 % See Coal bed methane extraction\n* the processes of digestion of animals (cattle) : 17 %\n* bacteria found in rice plantations : 12 %\n* biomass anaerobic heating or combustion 80% of the world emissions are of human source. They come primarily from agricultural and other human activities. During the past 200 years, the concentration of this gas in the atmosphere doubled, passing from 0.8 to 1.7 ppm.

See also

\n*
methyl group, a functional group similar to methane\n*methanogen\n*methanogenesis\n*Methane clathrate\n*Coal bed methane extraction\n*Alkane Category: Alkanes\ncategory: greenhouse gases \n\n\n\n\n\n\n

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