A daughter nuclide is the product that remains after a radioactive isotope undergoes decay. It can be either stable or continue to undergo further radioactive decay.
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Daughter nuclides are formed as a result of alpha, beta, or gamma decay processes.
The stability of a daughter nuclide determines whether it will undergo further radioactive decay.
In some decay chains, multiple daughter nuclides are produced before reaching a stable state.
The identity of the daughter nuclide depends on the type of particle emitted during the decay process.
Radiometric dating techniques use daughter nuclides to determine the age of materials.
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Related terms
Parent Nuclide: The original unstable radioactive isotope that undergoes decay to form a daughter nuclide.
Half-Life: The time required for half of the atoms in a sample of a radioactive isotope to decay.