Radioactive decay is a process by which an unstable atomic nucleus loses energy by emitting radiation. During this transformation, the nucleus of a radioactive element decays into a different element or a different isotope, releasing particles such as alpha particles, beta particles, or gamma rays. This release of particles leads to a change in the atomic structure of the radioactive substance.
A few key points about radioactive decay include:
- It is a random process at the level of single atoms, meaning it is impossible to predict when a particular atom will decay.
- However, with a large number of atoms, decay rates become predictable and are described by the half-life.
- Radioactive decay follows first-order kinetics, where the rate of decay is directly proportional to the number of undecayed nuclei present.
Understanding radioactive decay is crucial when studying elements with unstable nuclei, as it dictates how quickly a material will break down over time.