Beta decay is a type of radioactive decay where a beta particle (electron or positron) is emitted from an atomic nucleus. This occurs in nuclei with an excess of neutrons or protons, leading to a more balanced neutron-to-proton ratio.
During beta decay, one of the following transformations occurs:
- A neutron turns into a proton, emitting an electron and an antineutrino.
- A proton turns into a neutron, emitting a positron and a neutrino.
In the case of tritium, beta decay involves the transformation of a neutron into a proton. This nuclear rearrangement results in the emission of a beta particle and an antineutrino.
Beta decay is fundamental in nuclear physics, significantly affecting isotope stability. It transforms the atomic nucleus into a more stable state by adjusting the neutron and proton counts, making it a critical concept in understanding nuclear reactions.