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📘 About the Half-Life
The half-life of a radioactive isotope is the time it takes for half of its atoms to decay. After one half-life 50% remains, after two 25%, after three 12.5%, and so on. This half-life calculator gives the amount left after any time.
The same maths applies to any first-order reaction in chemistry and to how drugs are cleared from the body. Use the same time unit (seconds, days or years) for both the half-life and the time elapsed.
🧮 Formula
Half-life does not depend on how much you start with — every sample of carbon-14 halves in 5,730 years.
✏️ Worked examples
Carbon-14 after 11,460 years
You get| Amount remaining (N) | 25 |
| Percent remaining | 25% |
| Amount decayed | 75 |
| Number of half-lives | 2 |
| Decay constant λ (per time unit) | 0.000120968 |
After two half-lives, 25 g of 100 g of carbon-14 remains.
Try this example →Iodine-131 (t½ = 8 days) after 30 days
You get| Amount remaining (N) | 7.43254 |
| Percent remaining | 7.43% |
| Amount decayed | 92.5675 |
| Number of half-lives | 3.75 |
| Decay constant λ (per time unit) | 0.0866434 |
Only 7.43% of the iodine-131 is left after 30 days.
Try this example →🧭 How to use this calculator
What you enter
- Starting amount (N₀)Grams, atoms, % or counts — the answer uses the same unit.
- Half-life (t½)Any time unit; use the same unit for time.
- Time elapsed (t)
What you get
- Amount remaining (N)
- Percent remaining
- Amount decayed
- Number of half-lives
- Decay constant λ (per time unit)
💡 Half-lives of some isotopes
- Polonium-214: 164 microseconds
- Iodine-131: 8.02 days
- Cobalt-60: 5.27 years
- Carbon-14: 5,730 years
- Plutonium-239: 24,110 years
- Uranium-238: 4.47 billion years
❓ Frequently asked questions
What is half-life?
The time taken for half of the radioactive nuclei in a sample, or half of a first-order reactant, to decay.
What is the half-life formula?
N = N₀(½)^(t/t½). The decay constant is λ = 0.693/t½.
How much remains after 3 half-lives?
Does half-life depend on temperature or amount?
No. Radioactive half-life is unaffected by temperature, pressure or the size of the sample.