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Half-life, decay constant, mean lifetime and remaining amount.
Time and half-life must use the same unit — seconds, years, whatever you like. The arithmetic does not care which, only that they match.
| Half-lives | Time | Remaining | % left |
|---|
| Isotope | Half-life | Used for |
|---|---|---|
| Carbon-14 | 5,730 years | Radiocarbon dating |
| Uranium-238 | 4.47 billion years | Dating rocks and the Earth |
| Potassium-40 | 1.25 billion years | Potassium-argon dating |
| Iodine-131 | 8.02 days | Thyroid treatment and imaging |
| Technetium-99m | 6.01 hours | Medical imaging |
| Caesium-137 | 30.17 years | Fallout and contamination studies |
| Radon-222 | 3.82 days | Indoor air quality |
| Plutonium-239 | 24,110 years | Nuclear waste management |
Remaining quantity
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Amount that has decayed away
Half-life is independent of the starting quantity — one gram and one tonne of the same isotope halve in the same time. The same exponential law governs drug elimination and capacitor discharge, so the calculator is not limited to radioactivity.
The Half-Life Calculator solves exponential decay in any direction. Give any three of initial quantity, remaining quantity, elapsed time and half-life, and it finds the fourth, along with the decay constant and mean lifetime.
Solve exponential decay problems in whichever direction you need. Give any three of initial quantity, remaining quantity, elapsed time and half-life, and the fourth is calculated, along with the decay constant and mean lifetime.
Half-life is the time for a quantity to fall to half its value, and the reason it is such a useful description is that it does not depend on how much you started with — one gram and one tonne of the same isotope both halve in the same time. The same arithmetic covers a good deal more than radioactivity: drug elimination, capacitor discharge and radiocarbon dating all follow the identical exponential law, and a table of common isotopes is included for reference.
Remaining amount, elapsed time, half-life or starting quantity — whichever you leave out.
Both derived figures are shown, since problems often ask for one of them rather than the half-life itself.
Carbon-14, uranium-238, iodine-131 and others, so you have a reference value to hand.
The page notes that drug elimination and capacitor discharge follow the identical law.
Any consistent time unit works — the arithmetic does not care whether you use seconds or millennia.
Remaining amount, elapsed time, half-life or the initial quantity.
Any three of the four values. Units for time are yours to choose, as long as you are consistent.
The missing value, plus the decay constant and mean lifetime that follow from it.
Common isotopes are listed if you need a reference value rather than your own.
The amount remaining is N = N₀ × (1/2)^(t/T), where N₀ is the starting amount, t is elapsed time and T is the half-life. Equivalently N = N₀ × e^(−λt), with λ the decay constant.
The decay constant λ equals the natural logarithm of 2 divided by the half-life, roughly 0.693 ÷ T. Mean lifetime is the reciprocal, 1/λ.
Rearranging gives t = T × log₂(N₀/N). This is exactly how radiocarbon dating works, using carbon-14 with a half-life of 5,730 years.
Yes. Any process with a constant proportional rate of loss follows the same law, including drug elimination from the bloodstream and the discharge of a capacitor.
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