A unit of energy equal to the energy gained by an electron accelerated through one volt.The electronvolt (eV) is a unit of energy that, despite its name, is not confined to electronics. It is defined as the kinetic energy gained by a single electron when it is accelerated through an electric potential difference of one volt. In practice, this is an extremely tiny amount of energy — about 1.6 × 10⁻¹⁹ joules — which makes it the natural measuring stick for the microscopic world of atoms, molecules, and subatomic particles.
The electronvolt was introduced in the early 20th century as a convenient unit for describing the energies of charged particles in vacuum tubes and early particle accelerators. Its exact origin is not well documented, but it became standard with the development of atomic and nuclear physics.
The definition stems directly from the relationship between electric potential energy and charge. When a particle with a charge equal to that of an electron (about 1.6 × 10⁻¹⁹ coulombs) moves across a potential difference of one volt, it gains or loses exactly one electronvolt of energy. Because this unit is so small, physicists routinely use multiples: keV (thousand), MeV (million), and GeV (billion) for particle physics, and even TeV for the highest-energy cosmic rays.
The electronvolt is the standard energy unit in particle physics, astrophysics, and materials science — from describing the binding energy of electrons in atoms (a few eV) to the energies of particles in cosmic rays (up to 10²⁰ eV). It is also used to specify the energy resolution of detectors and the thresholds of nuclear reactions.
A single photon of visible light carries about 2 to 3 electronvolts of energy, which is why the electronvolt is a convenient unit for describing optical and ultraviolet phenomena.



