Beta decay is a fascinating type of nuclear decay that involves a neutron changing into a proton. This transformation occurs when a nucleus is unstable due to an imbalance in the number of protons and neutrons. In beta decay, as seen in the case of radioisotope \[^{100}_{43}\text{Tc}\] it emits a beta particle and an antineutrino.
- The beta particle emitted is essentially an electron, represented by \( \beta^{-} \).
- The antineutrino, represented by \( \bar{u}_e \), is a nearly massless and neutral particle emitted during the process.
As the neutron decays into a proton, the atomic number of the element increases by one, changing the element itself into another element with one higher atomic number, which in this case is \[^{100}_{44}\text{Mo}\].
This pathway is prevalent in many heavy, neutron-rich isotopes and is a natural process that helps unstable atomic nuclei attain stability.