Radionuclide

A radionuclide (radioactive nuclide, radioisotope, radioactive isotope, or unstable isotope) is a nuclide that is unstable and known to undergo radioactive decay into a different nuclide, which may be another radionuclide (see decay chain) or be stable.

Radioactive decay is a random process at the level of single atoms: it is impossible to predict when one particular atom will decay. For a collection of atoms of a single nuclide, their average decay rate can be measured, and its half-life (t1/2) calculated. Half-lives vary by 55 orders of magnitude and have no known limits.

All chemical elements have radionuclides - even the lightest, hydrogen, has a well-known radionuclide, tritium (though helium, lithium, and boron have none with half-life over a second). Elements heavier than lead (Z > 82), and the elements technetium and promethium, have only radionuclides and do not exist in stable forms, though bismuth can be treated as stable with the half-life of its natural isotope being over a trillion times longer than the current age of the universe.

Radiation emitted by radionuclides is almost always ionizing radiation and exposure above a certain level can cause damage to living organisms.

Production and effects

Artificial production methods of radionuclides include neutron sources such as nuclear reactors, as well as particle accelerators such as cyclotrons.

The radiation from radionuclides generally has a harmful effect on organisms including humans, although low levels of exposure occur naturally. The degree of harm depends on the nature and extent of the radiation (alpha, beta, gamma, or neutron), the amount and nature of exposure (close contact, inhalation or ingestion), and the element's biochemical properties (toxicity).