Radioactive Decay (Half-Life) Calculator
Calculate radioactive decay, remaining material, and activity after a given time.
Supports common isotopes with known half-lives.
Radioactive decay is the spontaneous process by which an unstable atomic nucleus loses energy by emitting radiation. The rate of decay is characterized by the half-life — the time it takes for half of the radioactive atoms to decay.
Decay formula:
N(t) = N₀ × (1/2)^(t / t½)
Where:
- N(t) = amount remaining after time t
- N₀ = initial amount
- t = elapsed time
- t½ = half-life of the isotope
Decay constant:
λ = ln(2) / t½ ≈ 0.693 / t½
Activity formula:
A(t) = A₀ × e^(-λt)
Activity is measured in becquerels (Bq) or curies (Ci). 1 Ci = 3.7 × 10¹⁰ Bq.
Common isotope half-lives:
| Isotope | Half-Life | Common Use |
|---|---|---|
| Carbon-14 | 5,730 years | Radiocarbon dating |
| Iodine-131 | 8.02 days | Thyroid treatment |
| Cobalt-60 | 5.27 years | Cancer radiotherapy |
| Cesium-137 | 30.17 years | Industrial gauges |
| Uranium-238 | 4.47 billion years | Geology dating |
| Radon-222 | 3.82 days | Indoor air concern |
| Phosphorus-32 | 14.3 days | Lab research |
| Technetium-99m | 6.01 hours | Medical imaging |
Practical example: If you start with 100 grams of Iodine-131 (half-life = 8.02 days):
- After 8.02 days: 50 g remains
- After 16.04 days: 25 g remains
- After 24.06 days: 12.5 g remains
- After 80.2 days (~10 half-lives): only 0.098 g remains
Number of half-lives:
n = t / t½
After n half-lives, the fraction remaining is (1/2)^n.
Tip: After about 10 half-lives, less than 0.1% of the original material remains. This is often used as a practical threshold for when a radioactive source is considered “decayed away.”
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This calculator runs entirely in your browser, so the numbers you enter stay on your device. The math behind it is written by hand and tested against worked examples and standard references before the page goes live.
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