Electron capture is a nuclear process where an unstable nucleus absorbs an electron, effectively making the electron a reactant rather than a product, as seen in beta decay. In beta decay, the electron is emitted, while in electron capture, it is taken in by the nucleus. This process can be represented by a specific reaction.
For example, consider francium-223 (Fr), which has an atomic number of 87. When francium-223 undergoes electron capture, it absorbs an electron, represented as follows:
Fr-223 + e- → Rn-223 + ν
In this reaction, the atomic mass remains the same (223), but the atomic number decreases by one (from 87 to 86), resulting in the formation of radon-223 (Rn). This illustrates how electron capture leads to a transformation of the element, contrasting with the emission seen in beta decay.
Understanding electron capture is crucial in nuclear chemistry, as it highlights the different pathways through which unstable nuclei can achieve stability. This process is significant in various applications, including radioactive decay series and the study of isotopes.