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Half-life and radioactive decay calculator

Find the remaining quantity after a given time, the decay constant, and the time to reach any fraction of the original amount.

Quantity remaining
29.8292 of 100
Fraction remaining29.829%
Half-lives elapsed1.7452
Decay constant λ0.000120968
Mean lifetime8266.64
Time to 1% remaining38069.3

Quantities keep whatever unit you entered (grams, atoms, becquerels). Times keep the unit you used for the half-life.

Radioactive decay is a random process at the level of individual atoms, but entirely predictable in bulk. The half-life is the time for half of any quantity to decay, and it is the same regardless of how much you started with.

N(t) = N₀ · e^(−λt)   λ = ln(2) / t½   N(t) = N₀ · (½)^(t/t½)

Nothing ever fully decays

Each half-life removes half of what remains, so the quantity approaches zero without reaching it. After ten half-lives about 0.1% is left; after twenty, one part in a million. This is why waste storage timescales are usually quoted as ten or twenty half-lives rather than as a point of complete disappearance.

Half-life is unaffected by conditions

Temperature, pressure and chemical state have essentially no effect, because decay is a nuclear process and chemistry happens in the electron shells. This is what makes radiometric dating reliable and why a sample cannot be made to decay faster.

Dating

Carbon-14 has a half-life of 5730 years, which suits archaeological timescales up to roughly 50,000 years. Beyond that too little remains to measure and longer-lived isotopes are used: potassium-40 at 1.25 billion years and uranium-238 at 4.5 billion years are the standard tools for dating rocks.

The same maths elsewhere

Drug elimination from the bloodstream, capacitor discharge and the cooling of a hot object all follow the identical exponential form. Only the constant changes.