Methane is a hydrocarbon gas involved in planetary cooling, atmospheric chemistry, and surface geology.Methane is an invisible gas that escapes from the ground in swamps and from the stomach of a cow as it digests grass. Imagine the methane molecule as a tiny tetrahedral hedgehog: a carbon atom in the center holds four hydrogen 'spines'. It is lighter than air, so like a balloon, it rises into the sky if set free.
The history of methane begins with alchemical observations of 'flammable air' in swamps. In 1776, Alessandro Volta scientifically described it, isolating it from bottom sediments. In the 19th century, Michael Faraday liquefied methane, and John Tyndall in 1859 proved its greenhouse properties. The modern era is associated with the study of methane hydrates on the ocean floor and its role in the climate system.
Methane traps heat through vibrational-rotational transitions: its molecule has several normal modes (symmetric and asymmetric C-H stretching, H-C-H bending vibrations) that actively absorb infrared radiation at wavelengths of about 3.3 μm and 7.7 μm. In the atmosphere, it is oxidized by hydroxyl radicals (OH•) over ~9 years, turning into CO₂ and water vapor. According to Planck’s radiation law, the absorption intensity depends on temperature, and the Doppler effect broadens spectral lines in a turbulent atmosphere.
Methane is called swamp gas because it bubbles up in bogs — that’s how bacteria finish off plant remains without oxygen, like tiny chefs making an invisible soup.























