Half-life is constant for a given isotope and is unaffected by temperature, pressure or the amount of material.
After half-lives, the fraction of the original activity remaining is .
| Half-lives | Fraction remaining |
|---|---|
| 1 | 1/2 |
| 2 | 1/4 |
| 3 | 1/8 |
| 4 | 1/16 |
Half-lives range from fractions of a second (for some artificial isotopes) to billions of years (e.g. uranium-238: 4.5 billion years).
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