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Radioactive decay calculator: half-life, remaining amount and carbon dating

Work out how much of a radioactive isotope remains after a given time, or date a sample from the share left, with common isotopes built in.

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What to calculate

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Results

Amount remaining

88.606

Time elapsed (age)

1,000.00

Exponential decay Each half-life halves what is left, whatever the starting amount.
Share remaining
88.606%
Share decayed
11.394%
Half-lives elapsed
0.175
Time to fall to 1%
38,069.30
Decay constant λ (per year)
0.000121

Amount left after other times

Amount remainingShare remaining
100 years current98.79898.798%
1,000 years current88.60688.606%
5,730 years current50.00050.000%
10,000 years current29.82929.829%
20,000 years current8.8988.898%
50,000 years current0.2360.236%

How radioactive decay works

A radioactive isotope has unstable nuclei that change into other elements by emitting radiation. Each nucleus decays at random, but in a large sample the pattern is very regular: in a fixed time, the half-life, half of the remaining nuclei decay. That makes radioactivity a reliable clock, used to date fossils and rocks and to plan medical treatments.

The formulas

  • Remaining amount N = N0 × (1/2)^(t ÷ t½)
  • Equivalently N = N0 × e^(−λt), with the decay constant λ = ln 2 ÷ t½
  • Age from the share remaining t = t½ × log2(N0 ÷ N)
  • Activity, in becquerels or curies, follows the same curve as the number of nuclei

Worked example: carbon-14

A sample starts with 100 units of carbon-14 (half-life 5,730 years). How much is left after 1,000 years?

  1. Half-lives elapsed: 1,000 ÷ 5,730 = 0.175.
  2. Remaining: 100 × 0.5^0.175 = 88.6.
  3. 11.4% has decayed.
  4. It takes about 38,000 years to fall below 1%.

Radiocarbon dating

While alive, plants and animals take in carbon with the same carbon-14 share as the atmosphere. After death, the carbon-14 decays and is not replaced. Measuring the share left gives the age:

Carbon-14 left Age (years)
90% about 870
75% about 2,380
50% 5,730
25% 11,460
10% about 19,000
1% about 38,000

Beyond roughly 50,000 years, too little is left to measure. Labs also calibrate raw ages against tree rings and other records, because atmospheric carbon-14 has varied over time.

Half-lives of common isotopes

Isotope Half-life Use or source
Technetium-99m 6.0 hours Medical imaging
Iodine-131 8.0 days Thyroid treatment, nuclear accidents
Cobalt-60 5.3 years Radiotherapy, sterilization
Tritium 12.3 years Glow-in-the-dark signs, fusion research
Cesium-137 30.1 years Fallout from Chernobyl and Fukushima
Carbon-14 5,730 years Archaeological dating
Uranium-238 4.47 billion years Dating the age of the Earth

Practical rules of thumb

  • After 7 half-lives, less than 1% remains; after 10, less than 0.1%.
  • Short half-lives mean intense but brief radioactivity, which is why medical isotopes like technetium-99m are chosen.
  • Long half-lives mean weak but lasting radioactivity: uranium-238 has decayed only by about half since the Earth formed.

Frequently asked questions

How do you calculate radioactive decay?

Remaining amount = initial amount × (1/2)^(t ÷ half-life). After two half-lives, a quarter is left; after ten, about 0.1%.

How does carbon-14 dating work?

Living things keep a steady level of carbon-14. After death it decays with a half-life of 5,730 years, so the share left gives the age: 25% left means about 11,460 years.

What is the decay constant?

λ = ln 2 ÷ half-life, the fraction of nuclei that decay per unit of time. For carbon-14 it is about 0.000121 per year.

How long until a radioactive substance is gone?

Never completely, but after 10 half-lives less than 0.1% is left. Iodine-131, with an 8-day half-life, falls below 0.1% after about 80 days.

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Results are estimates provided for information purposes. They do not replace professional advice.