The antimatter counterpart of the neutrino, a neutral elementary particle produced in beta decay.An antineutrino is the antimatter counterpart of the neutrino — a neutral, nearly massless elementary particle that is produced in beta decay, where a neutron transforms into a proton, an electron, and an antineutrino. Antineutrinos are famously elusive: they interact only via the weak force and gravity, so they can pass through vast amounts of matter (even the entire Earth) with a high probability of not interacting at all. Despite their ghostly nature, antineutrinos are produced in enormous quantities by nuclear reactors, the Sun, supernovae, and natural radioactive decays in the Earth's crust, making them valuable probes of processes that are otherwise hidden from view.
The antineutrino was first hypothesized by Wolfgang Pauli in 1930 as a 'desperate remedy' to explain the continuous energy spectrum of beta decay. It was experimentally confirmed in 1956 by Clyde Cowan and Frederick Reines, who detected antineutrinos from a nuclear reactor, earning Reines the Nobel Prize in Physics in 1995.
In beta decay, a down quark inside a neutron changes into an up quark, emitting a W⁻ boson, which then decays into an electron and an antineutrino. The antineutrino carries away a small amount of energy and lepton number, ensuring conservation laws are satisfied. Detecting antineutrinos typically relies on the inverse beta decay process, where an antineutrino interacts with a proton to produce a positron and a neutron — a reaction that yields a characteristic delayed coincidence signal, allowing sensitive detectors to pick out these rare events from background noise.
Antineutrino detectors are used for nuclear reactor monitoring (safeguards and non-proliferation), geoneutrino studies to map the Earth's interior heat production, and supernova early-warning systems.
Every second, about 10²⁰ antineutrinos from the Sun pass through each human body, yet only a handful interact with it over a lifetime.













