Radioactive decay occurs when an unstable nucleus spontaneously disintegrates by emitting particles or electromagnetic waves. There are three main types of radioactive emissions: alpha particles, beta particles, and gamma rays. Each type has distinct properties in terms of charge, speed, penetrating power, and interaction with electric and magnetic fields. Radioactive decay continues in a nucleus until it reaches a stable configuration. The rate of decay is random but consistent, allowing the calculation of half-life, the time for half the radioactive nuclei to decay. Common radioactive isotopes and their half-lives are listed.