Radioactive decay is a process by which an unstable atomic nucleus loses energy by radiation. During this process, the nucleus transmits particles or energy, transforming into a different element or isotope. The decay is spontaneous and results from the nuclear instability of certain isotopes, known as radioisotopes.
Common types of radioactive decay include:
- Alpha decay (emission of an alpha particle).
- Beta decay (emission of a beta particle and an antineutrino).
- Gamma decay (emission of gamma radiation).
In beta decay, the emitted particles allow the nucleus to achieve a more stable configuration. This helps in the transformation of elements and contributes to the natural radioactive processes found in the environment, medical applications, and the dating of archaeological findings.