Electron capture is a type of radioactive decay in which an inner orbital electron is captured by the nucleus of its own atom. This process decreases the atomic number by one and usually results in the emission of an X-ray photon or Auger electron.
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Electron capture reduces the atomic number by one while keeping the mass number unchanged.
It is commonly observed in proton-rich nuclei where it helps achieve a more stable neutron-to-proton ratio.
The captured electron usually comes from the K-shell (innermost shell) of the atom.
The process often results in the emission of either an X-ray photon or an Auger electron as the atom rearranges itself to fill the vacancy left by the captured electron.
Electron capture can be represented by: $p + e^- \rightarrow n + \nu_e$, where $p$ is a proton, $e^-$ is an electron, $n$ is a neutron, and $\nu_e$ is an electron neutrino.
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Related terms
Positron Emission: A type of radioactive decay where a proton inside a nucleus is converted into a neutron, releasing a positron and a neutrino.