Half-Life Calculator
Half-Life Calculator
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Half-Life, Mean Lifetime, and Decay Constant Conversion
Enter one of these values and the calculator finds the other two.
Press Calculate to see the results.
Enter any three of the four values, quantity remaining, initial quantity, time and half-life, and this half-life calculator solves for the fourth. A second tool converts between half-life, mean lifetime and decay constant.
Leave blank the value you want to find. With the defaults, 100 units decaying to 10 units in 50 time units, the half-life is 50 × ln 2 ÷ ln 10 ≈ 15.05 time units. Any unit of time works, as long as the time and the half-life use the same one. The quantity can be a mass, a number of atoms, a radioactivity reading or a drug concentration.
Definition and Formula
The half-life of a substance is the time it takes for half of it to decay or disappear. After one half-life, 50% remains; after two, 25%; after three, 12.5%; and after ten, a little under 0.1%. The idea is most closely tied to radioactive decay, where each unstable nucleus has a fixed chance of decaying in any instant, regardless of its age or of what its neighbors do. Because that chance is constant, the number of nuclei falls by the same fraction in every equal time interval, which is exponential decay.
The same mathematics describes many other processes: the elimination of a drug from the bloodstream, the discharge of a capacitor, the cooling of a hot object toward room temperature, and the decline of a chemical reactant in a first-order reaction. Doctors use a drug's half-life to choose dosing intervals, and archaeologists use the 5,730-year half-life of carbon-14 to date organic remains up to about 50,000 years old.
Three equivalent constants describe the rate. The half-life t½ is the most intuitive. The mean lifetime τ is the average time a single particle survives before decaying, and it is longer than the half-life by a factor of 1 ÷ ln 2 ≈ 1.4427. The decay constant λ is the probability of decay per unit time, the reciprocal of τ. They are related by t½ = τ ln 2 = ln 2 ÷ λ.
Half-lives span an enormous range, from fractions of a second for some artificial isotopes to billions of years for uranium-238, which is why some radioactive waste stays hazardous for millennia while medical tracers are chosen to fade within hours or days.
| Isotope | Half-life | Use or source |
|---|---|---|
| Technetium-99m | 6.01 hours | Medical imaging |
| Iodine-131 | 8.02 days | Thyroid treatment |
| Cobalt-60 | 5.27 years | Radiotherapy, sterilization |
| Tritium (hydrogen-3) | 12.3 years | Glow-in-the-dark signs |
| Cesium-137 | 30.1 years | Fission product |
| Carbon-14 | 5,730 years | Radiocarbon dating |
| Plutonium-239 | 24,110 years | Nuclear fuel |
| Uranium-238 | 4.47 billion years | Dating rocks |
N(t) = N₀ · (1/2)^(t ÷ t½) = N₀ · e^(−t ÷ τ) = N₀ · e^(−λt)
- N₀
- the initial quantity
- N(t)
- the quantity remaining after time t
- t½
- the half-life
- τ
- the mean lifetime
- λ
- the decay constant
Derivation of the Relationship Between Half-Life Constants
Start from the exponential decay law N(t) = N₀e^(−λt). At t = t½, exactly half remains, so N₀ ÷ 2 = N₀e^(−λt½). Dividing by N₀ and taking natural logarithms gives −ln 2 = −λt½, so t½ = ln 2 ÷ λ. The mean lifetime is the average of t weighted by the decay rate, τ = ∫ t·λe^(−λt) dt from 0 to ∞, which works out to 1 ÷ λ. Combining the two gives t½ = τ ln 2.
Frequently asked questions
What is the half-life formula?
N(t) = N₀ × (1/2)^(t ÷ t½), where N₀ is the starting amount, t is the elapsed time and t½ is the half-life.
How do I find the half-life from two measurements?
Use t½ = t × ln 2 ÷ ln(N₀ ÷ Nt). For 100 falling to 10 over 50 units of time, that is about 15.05.
How much remains after three half-lives?
One eighth, or 12.5%, because each half-life halves the amount: 1/2 × 1/2 × 1/2.
What is the difference between half-life and mean lifetime?
Half-life is the time for half to decay. Mean lifetime is the average survival time of one particle and is about 1.4427 times the half-life.
What is the half-life of carbon-14?
About 5,730 years, which makes it useful for dating organic material up to roughly 50,000 years old.
Does the half-life formula work for chemical reactions?
Yes for first-order reactions: their half-life, t½ = ln 2 ÷ k, stays constant, so the formula on this page applies. For a second-order reaction with one reactant, t½ = 1 ÷ (k × [A]₀) depends on the starting concentration, so each successive half-life is twice as long as the one before and this calculator's constant-half-life model does not fit.
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