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The term half-life is applied to the time it takes half of a sample of a radioactive substance to decay. It really is as simple as that, but we'd better add a few things to make it clear. Let's look a bit more closely.

Radioactive materials or substance are unstable. That is, the nuclei of the atoms of radioactive materials are unstable, and they will want to undergo a change that will allow them to get to a more stable state. Radioactive decay is the term we apply to the nuclear decay of these materials.

Radioactive materials undergo decay at a given rate. If we have an atom of a radioactive material it will eventually decay, but we cannot be sure when a specific atom will actually decay. But we can do a statistical analysis of a large sample and get an accurate answer. By carefully measuring decay events and making statistical calculations, we have arrived at some very accurate figures for the half-lives of radioactive materials. They vary widely from the tiniest fractions of a second to many billions of years.

Here are some common radioisotopes and their half-lives:

  • Uranium-238 has a half-life of 4.468 x 109 years. That's 4.468 billion years.
  • Plutonium-239 has a half-life of 24,100 years.
  • Cobalt-60 has a half-life of 5.2714 years.
  • Radon-222 has a half-life of 3.8235 days.
  • Carbon-14 has a half-life of 5,730 (+/- 40) years.

The half-life is the time it takes for one-half of something (usually a radioactive isotope) to decay.
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