Decay products are extremely important in understanding radioactive decay and the management of radioactive waste.
In practice nearly all decay products are themselves radioactive. The result of this is that most radionuclides do not have simply a decay product, but rather a decay chain, leading eventually to a stable nuclide. For elements above lead in atomic number, this is nearly always an isotope of lead. Lead is generally the stable point at which decay chains stop.
In many cases members of the decay chain are far more radioactive than the original nuclide. Thus, although uranium is not dangerously radioactive when pure, some pieces of naturally-occurring pitchblende are quite dangerous owing to their radium content. Similarly, thoriumgas mantles are very slightly radioactive when new, but become far more radioactive after only a few months of storage.
Although it cannot be predicted whether any given atom of a radioactive substance will decay at any given time, the decay products of a radioactive substance are extremely predictable. Because of this, decay products are important to scientists in many fields who need to know the quantity or type of the parent product. Such studies are done to measure pollution levels (in and around nuclear facilities) and for other matters.
In nuclear physics, a decay product, also known as a daughterproduct, daughterisotope or daughternuclide, is a nuclide resulting from the radioactive decay of a parent isotope or precursor nuclide.
The daughterproduct may be stable or it may decay to form a daughterproduct of its own.
The daughter of a daughterproduct is sometimes called a granddaughter product.
When a material incorporates both the parent and daughternuclides at the time of formation, it may be necessary to assume that the initial proportions of a radioactive substance and its daughter are known.
The daughterproduct should not be a small-molecule gas that can leak out of the material, and it must itself have a long enough half-life that it will be present in significant amounts.
Measuring the decay products of an extinct radionuclides with a mass spectrometer and using isochronplots it is possible to determine relative ages between different events in the early history of the solar system.