Methane

Methane
General
Other names	Marsh gas
Molecular formula	CH4
SMILES	C
Molar mass	16.04 g/mol
Appearance	colourless gas
CAS number	[74-82-8]
Properties
Density and phase	0.717 kg/m3, gas
Solubility in water	3.5 mL g/100 ml (17°C)
Melting point	−182.5°C (90.6 K) at 1 atm 25 °C (298 K) at 1.5 GPa
Boiling point	−161.6°C (111.55 K)
Triple point	90.7 K, 0.117 bar
Structure
Molecular shape	tetrahedral
Symmetry group	Td
Dipole moment	Zero
Hazards
MSDS	External MSDS
EU classification	Highly flammable (F+)
NFPA 704	4 1 0
R-phrases	R12
S-phrases	S2, S9, S16, S33
Flash point	−188°C
Autoignition temperature	537°C
Explosive limits	5–15%
Supplementary data page
Structure and properties
Thermodynamic data
Spectral data	UV, IR, NMR, MS
Related compounds
Related alkanes	Ethane Propane
Related compounds	Methanol Chloromethane
Except where noted otherwise, data are given for materials in their standard state (at 25 °C, 100 kPa) Infobox disclaimer and references

The simplest hydrocarbon, methane, is a gas with a chemical formula of CH₄. Pure methane is odorless, but when used commercially is usually mixed with small quantities of odorants, strongly-smelling sulfur compounds such as ethyl mercaptan to enable the detection of leaks.

A 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):

CH₄ + 2O₂ → CO₂ + 2H₂O

Methane is a greenhouse gas with a global warming potential over 100 years of 23 (IPCC Third Assessment Report) i.e. when averaged over 100 years each kg of CH₄ warms the earth 23 times as much as the same mass of CO₂.

Earth's mantle has huge amounts of methane and the main reservoir. Large amounts of methane also are emitted to atmosphere through Mud volcanoes which are connected with deep geological faults.

Methane has a wide range of thermodynamic stability.

Properties

At room temperature and pressure, methane is a colourless, odourless gas. It has boiling point of −162°C at 1 atmosphere pressure and is highly flammable.

Potential health effects

Methane is not toxic by any route. The immediate health hazard is that it may cause thermal burns. It is flammable and may form mixtures with air that are flammable or explosive. Methane is violently reactive with oxidizers, halogens, and some halogen compounds. Methane is an asphyxiant and may displace oxygen in a workplace atmosphere. Asphyxia may result if the oxygen concentration is reduced to below 18% by displacement. The concentrations at which flammable or explosive mixtures form are much lower than the concentration at which asphyxiation risk is significant. When structures are built on or near landfills, methane off-gas can penetrate the building interior and expose occupants to significant levels of methane. Some buildings have specially engineered recovery systems below their basements, to actively capture such fugitive off-gas and vent it away from the building. An example of this type of system is in the Dakin building, Brisbane, California.

Reactions of methane

The reactions with methane are: combustion, hydrogen activation, and halogen reaction.

Combustion

In the combustion of methane several steps are involved:

Methane forms a methyl radical (CH₃), which reacts with oxygen forming formaldehyde (HCHO or H₂CO). The formaldehyde gives a formyl radical (HCO), which then forms carbon monoxide (CO). The process is called oxidative pyrolysis:

CH₄ + O₂ → CO + H₂ + H₂O

Following oxidative pyrolysis, the H₂ oxidizes, forming H₂O, replenishing the active species, and releasing heat. This occurs very quickly, usually in less than a millisecond.

H₂ + ½O₂ → H₂O

Finally, 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.

CO + ½O₂ → CO₂

Hydrogen activation

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. Despite the high activation barrier for breaking the C-H bond, CH₄ is still the principal starting material for manufacture of hydrogen. 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.

Reactions with halogens

Methane undergoes reactions with all the halogens given correct conditions. The reactions occur as follows:

CH₄ + X₂ → CH₃X + HX

Where X is either fluorine (F), chlorine (Cl), bromine (Br) or sometimes iodine (I).

This mechanism for this process is called free radical substitution and it occurs as follows:

Initiation:

X₂ → 2Xˑ

Propagation:

CH₄ + Xˑ → ˑCH₃ + HX

ˑCH₃ + ˑX₂ → CH₃X + Xˑ

Termination:

2Xˑ → X₂

ˑCH₃ + X → CH₃X

ˑCH₃ + ˑCH₃ → CH₃CH₃

Uses

Fuel

For more on the use of methane as a fuel, see: natural gas

Methane is an important fuel for electrical generation. Compared to other hydrocarbon fuels, burning methane produces less carbon dioxide for each unit of heat released. Also, methane's heat of combustion is about 902 kJ/mol, which is lower than any other hydrocarbon, but if a ratio is made with the atomic weight (16 g/mol) divided by the heat of combustion (902 kJ/mol) it is found that methane, being the simplest hydrocarbon, actually produces the most heat per gram than other complex hydrocarbons. In many cities, methane is piped into homes for domestic heating and cooking purposes. In this context it is usually known as natural gas.

Industrial uses

Methane is used in industrial chemical processes and may be transported in liquid or refrigerated liquid form. While leaks from a liquid container are initially heavier than air, the gas is lighter than air. Gas pipelines distribute large amounts of natural gas, of which methane is a significant component.

In the chemical industry, methane is the feedstock of choice for the production of hydrogen, methanol, acetic acid, and acetic anhydride. When used to produce any of these chemicals, methane is first converted to synthesis gas, a mixture of carbon monoxide and hydrogen, by steam reforming. In this process, methane and steam react on a nickel catalyst at high temperatures (700–1100 °C).

CH₄ + H₂O → CO + 3H₂

The ratio of carbon monoxide to hydrogen in synthesis gas can then be adjusted via the water gas shift reaction to the appropriate value for the intended purpose.

CO + H₂O ⇌ CO₂ + H₂

Less significant methane-derived chemicals include acetylene, prepared by passing methane through an electric arc, and the chloromethanes (chloromethane, dichloromethane, chloroform, and carbon tetrachloride), produced by reacting methane with chlorine gas. However, the use of these chemicals is declining, acetylene as it is replaced by less costly substitutes, and the chloromethanes due to health and environmental concerns.

Sources of methane

Natural gas fields

The major source of methane is extraction from geological deposits known as natural gas fields. It is associated with other hydrocarbon fuels and sometimes accompanied by helium and nitrogen. The gas at shallow levels (low pressure) is formed by anaerobic decay of organic matter deep under the Earth's surface. In general, sediments buried deeper and at higher temperatures than those which give oil generate natural gas.

Alternative sources

Apart from gas fields an alternative method of obtaining methane is via biogas generated by the fermentation of organic matter including manure, wastewater sludge, municipal solid waste, or any other biodegradable feedstock, under anaerobic conditions. Industrially, methane can be created from common atmospheric gases and hydrogen (produced, perhaps, by electrolysis) through chemical reactions such as the Sabatier process, Fischer-Tropsch process. Coal bed methane extraction is a method for extracting methane from a coal deposit.

Methane in Earth's atmosphere

Methane concentrations graph

Computer models showing the amount of methane (parts per million by volume) at the surface (top) and in the stratosphere (bottom).

Methane in the earth's atmosphere is an important greenhouse gas with a Global warming potential of 23 over a 100 year period. Its concentation has increased by about 150% since 1750 and it accounts for 20% of the total radiative forcing from all of the long-lived and globally mixed greenhouse gases [1].

The average concentration of methane at the Earth's surface in 1998 was 1,745 ppb [2]. Its concentration is higher in the northern hemisphere as most sources (both natural and human) are larger. The concentrations vary seasonally with a minimum in the late summer.

Methane is created near the surface, and it is carried into the stratosphere by rising air in the tropics. Uncontrolled build-up of methane in Earth's atmosphere is naturally checked—although human influence can upset this natural regulation—by methane's reaction with a molecule known as the hydroxyl radical, a hydrogen-oxygen molecule formed when single oxygen atoms react with water vapor.

Early in the Earth's history—about 3.5 billion years ago—there was 1,000 times as much methane in the atmosphere as there is now. The earliest methane was released into the atmosphere by volcanic activity. During this time, Earth's earliest life appeared. These first, ancient bacteria added to the methane concentration by converting hydrogen and carbon dioxide into methane and water. Oxygen did not become a major part of the atmosphere until photosynthetic organisms evolved later in Earth's history. With no oxygen, methane stayed in the atmosphere longer and at higher concentrations than it does today.

Emissions of methane

Houweling et al. (1999) give the following values for methane emissions [3]:

Origin	CH4 emission (Tg/yr)
Natural emissions
Wetlands (incl rice production)	225
Ocean	20
Termites	15
Hydrates	10
Natural total	290
Anthropogenic emissions
Energy	110
Landfills	40
Ruminants	115
Waste treatment	25
Biomass Burning	40
Anthropogenic total	330

Slightly over half of the total emission is due to human activity [4].

Living Plants (e.g. forests) have recently been identified as a potentially important source of methane. The recent paper calculated emissions of 62–236 Tg yr^-1, and "this newly identified source may have important implications". [5], [6]. However the authors stress "our findings are preliminary with regard to the methane emission strength".[7]

Removal processes

The major removal mechanism of methane from the atmosphere is by reaction with the hydroxyl radical (·OH), which may be produced when a cosmic ray strikes a molecule of water vapor:

$CH_{4}+\cdot OH\to \cdot CH_{3}+H_{2}O$

This reaction in the troposphere gives a methane lifetime of 9.6 years. Two more minor sinks are soil sinks (160 year lifetime) and stratospheric loss by reaction with $\cdot OH$, $\cdot Cl$ and $\cdot O^{1}D$ in the stratosphere (120 year lifetime), giving a net lifetime of 8.4 years. [8]

Sudden release from methane clathrates

At high pressures, such as are found on the bottom of the ocean, methane forms a solid clathrate with water, known as methane hydrate. An unknown, but possibly very large quantity of methane is trapped in this form in ocean sediments. The sudden release of large volumes of methane from such sediments into the atmosphere has been suggested as a possible cause for rapid global warming events in the earth's distant past, such as the Paleocene-Eocene thermal maximum of 55 million years ago.

One source estimates the size of the methane hydrate deposits of the oceans at ten million million tons (10 exagrams). Theories suggest that should global warming cause them to heat up sufficiently, all of this methane could again be suddenly released into the atmosphere. Since methane is twenty-three times stronger (for a given weight, averaged over 100 years) than CO₂ as a greenhouse gas; this would immensely magnify the greenhouse effect, heating Earth to unprecedented levels.

Extraterrestrial Methane

Methane has been detected or is believed to exist in several locations of the solar system. It is believed to have been created by abiotic processes, with the possible exception of Mars.

• Jupiter
• Mars
• Saturn
  • Iapetus
  • Titan
  • Enceladus
• Neptune
  • Triton
• Uranus
  • Ariel
  • Miranda
  • Oberon
  • Titania
  • Umbriel
• Comet Halley
• Comet Hyakutake
• 2003 UB313

Traces of methane gas are present in the thin atmosphere of the Earth's Moon.

Methane has also been detected in interstellar clouds.

See also

• Alkane, a type of hydrocarbon of which methane is simplest member.
• Methane clathrate, form of water ice which contains methane.
• Methanogen, archaea that produce methane as a metabolic by-product.
• Methanogenesis, the formation of methane by microbes.
• Methanotroph, bacteria that are able to grow using methane as their only source of carbon and energy.
• Methyl group, a functional group similar to methane

External links

• Methane thermodynamics
• Inorganic Methane

• International Chemical Safety Card 0291
• Methane Hydrates
• Computational Chemistry Wiki
• Molview from bluerhinos.co.uk See Methane in 3D

• European Chemicals Bureau

 

Alkanes

methane CH4

|

ethane C2H6

|

propane C3H8

|

butane C4H10

|

pentane C5H12

|

hexane C6H14

heptane C7H16

|

octane C8H18

|

nonane C9H20

|

decane C10H22

|

undecane C11H24

|

dodecane C12H26

ar:ميثان bg:Метан ca:Metà cs:Methan cy:Llosgnwy da:Metan de:Methan el:Μεθάνιο es:Metano eo:Metano fr:Méthane ga:Meatán hr:Metan is:Metan it:Metano he:מתאן la:Methanum lb:Methan lv:Metāns lt:Metanas hu:Metán nl:Methaan ja:メタン no:Metan nn:Metan pl:Metan pt:Metano ru:Метан sh:Metan simple:Methane sk:Metán sl:Metan sr:Метан fi:Metaani sv:Metan vi:Mêtan tr:Metan zh:甲烷