Radioactive decay is a natural process by which an unstable atomic nucleus loses energy by emitting radiation. This radiation can come in the form of alpha particles, beta particles, or gamma rays. During radioactive decay, the nucleus changes from a higher energy state to a lower energy state.
There are various types of radioactive decay, but the common ones include alpha decay and beta decay. In alpha decay, the nucleus emits an alpha particle, which consists of 2 protons and 2 neutrons. This type of decay reduces the atomic mass and the atomic number of the element.
Beta decay, our primary focus, involves the transformation of neutrons or protons in the nucleus, leading to the emission of beta particles. Radioactive decay plays a crucial role in the natural transmutation of elements, changing them over time into different elements or isotopes:
- Transmutation of elements
- Emission of radiation
- Natural process of energy loss
Understanding these processes is key to illustrations of how certain elements transition from one form to another over long periods.