Radioactive Isotope

A radioactive isotope (radioisotope) is an isotope of an element that possesses excess nuclear energy, rendering it unstable. To achieve stability, it undergoes radioactive decay, emitting radiation in the form of particles (e.g., alpha, beta) or electromagnetic waves (e.g., gamma rays). This process transforms the nuclide into a different isotope or element, often releasing significant energy.

Key Characteristics

  • Instability: Arises from an imbalance between protons and neutrons in the nucleus.
  • Half-life (): The time required for half of the radioactive atoms in a sample to decay.
  • Applications: Used in medicine (imaging, therapy), industry (tracing, sterilization), archaeology (radiometric dating), and energy production.

Notable Radioisotopes & Observations

Iron-60 ()

is a rare, long-lived radioisotope produced in supernova explosions. Its detection in terrestrial archives provides critical evidence regarding the solar system’s interaction with the interstellar medium.

Other Common Radioisotopes

  • Carbon-14 (): Used for dating organic materials up to ~50,000 years old.
  • Uranium-235 () & Uranium-238 (): Primary fuels for nuclear reactors and weapons; parent isotopes for uranium-lead dating.
  • Potassium-40 (): A naturally occurring radioisotope found in potassium; contributes to background radiation and used in potassium-argon dating.
  • Cobalt-60 (): Widely used in medical radiotherapy and industrial radiography.

See Also