Neutrino detection involves capturing these elusive particles using specialized instruments like neutrino telescopes or detectors.Neutrino detection is the process of capturing and measuring neutrinos, subatomic particles that interact extremely weakly with matter. Because neutrinos have no electric charge and very small mass, they pass through ordinary matter almost undisturbed, making them notoriously difficult to detect. Neutrino detectors are typically large-volume instruments—such as underground tanks of water or ice, or arrays of photodetectors—that look for the rare interactions of neutrinos with atomic nuclei or electrons. These interactions produce charged particles that emit light (Cherenkov radiation) or sound, which can be recorded and analyzed.
The neutrino was first detected in 1956 by Clyde Cowan and Frederick Reines, who used a nuclear reactor as a neutrino source and a liquid scintillator detector. The first solar neutrinos were detected by Ray Davis in the 1960s in the Homestake experiment, which used a chlorine-based detector.
Most detectors rely on the inverse beta decay or elastic scattering processes. For example, in a water Cherenkov detector, a neutrino can interact with a proton, producing a positron and a neutron. The positron moves faster than light in water, emitting a cone of blue Cherenkov light that is captured by photomultiplier tubes. The pattern and timing of the light reveal the neutrino's energy and direction. Other detectors use liquid scintillators, which emit light when excited by charged particles, or radio antennas that detect signals from neutrino-induced cascades in ice. To reduce background noise, detectors are placed deep underground or under ice, shielded from cosmic rays.
Neutrino detectors are used to study astrophysical sources like the Sun, supernovae, and active galactic nuclei, as well as to monitor nuclear reactors and verify nuclear non-proliferation. They also provide a unique probe of the Earth's interior through neutrino tomography.
The IceCube Neutrino Observatory, buried in a cubic kilometer of Antarctic ice, uses thousands of optical sensors to detect neutrinos, and in 2013 it identified the first high-energy neutrinos of astrophysical origin, likely from distant blazars.
| N | variable | number of detected neutrino events — count |
| L | variable | neutrino luminosity of the source — luminosity watt |
| d | variable | distance from source to detector — distance metre |
| A | variable | effective area of the detector — area square metre |
| t | variable | exposure time — time second |
| ⟨E_ν⟩ | variable | mean neutrino energy — energy joule |












