Chemistry & Materials Codexery

Methane

Simplest alkane, main component of natural gas, potent greenhouse gas.

Methane

Methane is a chemical compound with the formula CH₄, consisting of one carbon atom bonded to four hydrogen atoms. It is a group-14 hydride, the simplest alkane, and the main constituent of natural gas. Its abundance on Earth makes it an economically attractive fuel, though capturing and storing it is difficult because it is a gas at standard temperature and pressure. In the atmosphere, methane acts as a greenhouse gas, absorbing infrared radiation. It is also detected on other planets, including Mars, with implications for astrobiology.

chemical_formula
CH₄
molar_mass
16.0 g/mol
flammability_range
5.4%–17% in air
pKa_in_DMSO
56
primary_sources
geological and biological processes, methane clathrates under seafloor

Lore & Background

Methane is a tetrahedral molecule with four equivalent C–H bonds. Its electronic structure involves two bonding molecular orbitals from the overlap of carbon and hydrogen valence orbitals. At standard temperature and pressure, it is an odorless, colorless, and transparent gas; the familiar smell of natural gas comes from added odorants like tert-butylthiol. Solid methane exists in several modifications, with methane I being a plastic crystal where molecules can rotate freely. Methane's primary chemical reactions include combustion, steam reforming to syngas, and halogenation. It is an extremely weak acid with a pKa of 56 in DMSO, but its conjugate base is known in forms such as methyllithium. Positive ions derived from methane, such as methenium (CH₃⁺), methane cation (CH₄⁺), and methanium (CH₅⁺), have been observed in low-pressure gas mixtures and some detected in outer space. Naturally occurring methane is found below ground and under the seafloor, formed by geological and biological processes. The largest reservoir is under the seafloor as methane clathrates. When it reaches the surface and atmosphere, it is known as atmospheric methane.

Reader's Guide

Methane is significant as the simplest hydrocarbon and the primary component of natural gas, making it a crucial fuel for electricity generation, heating, cooking, and industrial uses. It produces less carbon dioxide per unit of heat than other hydrocarbon fuels, and its high heat of combustion per mass unit (55.7 kJ/g) makes it efficient. As a rocket propellant (methalox), it offers advantages over kerosene and hydrogen: it produces smaller exhaust molecules, reduces coking, is easier to store due to higher boiling point and density, and avoids hydrogen embrittlement. As a greenhouse gas, methane absorbs infrared radiation in Earth's atmosphere, contributing to climate change. Its detection on Mars has implications for astrobiology research. Industrial-scale oxidation of methane to methanol has not proven economical, though enzymatic and catalytic systems exist. Methane's reactions are generally difficult to control, and its C–H bond activation is a focus of catalyst research.

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