Radioactive isotopes, also known as radioisotopes, are atoms that emit radiation as they decay into a more stable form. Unlike stable isotopes, radioactive isotopes have an imbalance in the number of protons and neutrons that makes them unstable. This radioactivity often stems from having too many protons, too many neutrons, or a mix of both, which disrupts the energy balance within the nucleus.
The stability of isotopes greatly depends on how their nucleus is composed and how well it can resist decay.
- Radioactive isotopes decay over time, emitting energy in the form of radiation, such as alpha, beta, or gamma rays.
- The process by which they decay is random but quantifiable in terms of half-life, the time it takes for half of the radioactive atoms in a sample to decay.
- Isotopes that are closer to having equal numbers of protons and neutrons tend to be more stable.
When assessing whether an isotope might be radioactive, scientists often compare the neutron-to-proton ratio and consult known magic numbers, which reflect particularly stable configurations.