A decay process where a nucleus absorbs an inner-shell electron, converting a proton to a neutron.Electron capture is a type of radioactive decay in which an atomic nucleus absorbs one of its own inner-shell electrons, typically from the K or L shell. This process converts a proton into a neutron and emits a neutrino. It is a competing process to beta-plus decay and is common in proton-rich nuclei. Electron capture plays a crucial role in stellar nucleosynthesis, particularly in the late stages of massive stars, and in the synthesis of elements in supernovae.
Electron capture was first proposed by Hideki Yukawa in 1935, and the process was experimentally observed by Luis Alvarez in 1937. Alvarez's work confirmed the theoretical prediction and earned him recognition in the field of nuclear physics.
The nucleus captures an electron that is close to it, usually from the innermost electron shell. The captured electron combines with a proton to form a neutron, and a neutrino is emitted. The atomic number decreases by one, while the mass number remains unchanged. The resulting atom is left with a vacancy in its electron shell, which is filled by an outer electron, leading to the emission of X-rays or Auger electrons.
Electron capture is used in medical imaging, such as in PET scans where certain isotopes decay via electron capture, and in the study of neutrino properties. It also influences the cooling of neutron stars and the production of elements in stellar environments.
Electron capture is the only decay mode that can occur for a free proton inside a nucleus, and it is responsible for the 'missing' lithium in the universe, as it destroys lithium-7 in stars.









