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Names | |||
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Preferred IUPAC name
Methane[1] | |||
Systematic IUPAC name
Carbane (never recommended[1]) | |||
Other names
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Identifiers | |||
3D model (JSmol)
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3DMet | |||
1718732 | |||
ChEBI | |||
ChEMBL | |||
ChemSpider | |||
ECHA InfoCard | 100.000.739 | ||
EC Number |
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59 | |||
KEGG | |||
MeSH | Methane | ||
PubChem CID
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RTECS number |
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UNII | |||
UN number | 1971 | ||
CompTox Dashboard (EPA)
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Properties | |||
CH4 | |||
Molar mass | 16.043 g·mol−1 | ||
Appearance | Colorless gas | ||
Odor | Odorless | ||
Density | |||
Melting point | −182.456 °C (−296.421 °F; 90.694 K)[3] | ||
Boiling point | −161.5 °C (−258.7 °F; 111.6 K)[3] | ||
Critical point (T, P) | 190.56 K (−82.59 °C; −116.66 °F), 4.5992 MPa (45.391 atm) | ||
22.7 mg/L[4] | |||
Solubility | Soluble in ethanol, diethyl ether, benzene, toluene, methanol, acetone and insoluble in water | ||
log P | 1.09 | ||
Henry's law
constant (kH) |
14 nmol/(Pa·kg) | ||
Conjugate acid | Methanium | ||
Conjugate base | Methyl anion | ||
−17.4×10−6 cm3/mol[5] | |||
Structure | |||
Td | |||
Tetrahedral at carbon atom | |||
0 D | |||
Thermochemistry[6] | |||
Heat capacity (C)
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35.7 J/(K·mol) | ||
Std molar
entropy (S⦵298) |
186.3 J/(K·mol) | ||
Std enthalpy of
formation (ΔfH⦵298) |
−74.6 kJ/mol | ||
Gibbs free energy (ΔfG⦵)
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−50.5 kJ/mol | ||
Std enthalpy of
combustion (ΔcH⦵298) |
−891 kJ/mol | ||
Hazards[7] | |||
GHS labelling: | |||
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Danger | |||
H220 | |||
P210 | |||
NFPA 704 (fire diamond) | |||
Flash point | −188 °C (−306.4 °F; 85.1 K) | ||
537 °C (999 °F; 810 K) | |||
Explosive limits | 4.4–17% | ||
Related compounds | |||
Related alkanes
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Related compounds
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Supplementary data page | |||
Methane (data page) | |||
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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Methane (US: /ˈmɛθeɪn/ METH-ayn, UK: /ˈmiːθeɪn/ MEE-thayn) is a chemical compound with the chemical formula CH4 (one carbon atom bonded to four hydrogen atoms). It is a group-14 hydride, the simplest alkane, and the main constituent of natural gas. The abundance of methane on Earth makes it an economically attractive fuel, although capturing and storing it is hard because it is a gas at standard temperature and pressure.
Naturally occurring methane is found both below ground and under the seafloor and is formed by both geological and biological processes. The largest reservoir of methane is under the seafloor in the form of methane clathrates. When methane reaches the surface and the atmosphere, it is known as atmospheric methane.[9]
The Earth's atmospheric methane concentration has increased by about 160% since 1750, with the overwhelming percentage caused by human activity.[10] It accounted for 20% of the total radiative forcing from all of the long-lived and globally mixed greenhouse gases, according to the 2021 Intergovernmental Panel on Climate Change report.[11] Strong, rapid and sustained reductions in methane emissions could limit near-term warming and improve air quality by reducing global surface ozone.[12]
Methane has also been detected on other planets, including Mars, which has implications for astrobiology research.[13]
Methane is a retained name (see P-12.3) that is preferred to the systematic name 'carbane', a name never recommended to replace methane, but used to derive the names 'carbene' and 'carbyne' for the radicals H2C2• and HC3•, respectively.