AP® Physics 2: Algebra-Based · Unit 15 · Topic 15.7
Half-Life and Decay Curves
Half-life is the time it takes for half of a radioactive sample to decay. No single atom's decay is predictable, but huge numbers of atoms decaying at a fixed rate produce a smooth, repeatable curve.
A single radioactive nucleus has no memory and no clock. It might decay in the next second or sit stable for a thousand years, and nothing about its past tells you which. That unpredictability is real, not just a gap in our knowledge. But a sample of atoms is not one atom, it is trillions of them, and each one has the same fixed probability of decaying per unit time. With numbers that large, randomness at the individual level averages into near-perfect regularity at the group level. That regularity is the half-life: the time for half of whatever nuclei remain to decay, no matter how much or how little you started with.
Because the same fraction decays every half-life, the amount remaining follows N = N0 (1/2)t/half-life, where N0 is the starting amount and t is elapsed time. Plot surviving nuclei against time and you get a curve that drops fast at first, then levels off, cutting itself in half again and again: after one half-life you have 50 percent left, after two 25 percent, after three 12.5 percent, and so on, never quite reaching zero. This is exponential decay, the same mathematical shape whether you are tracking atoms, radioactive dose, or drug concentration in the body.
This idea connects directly to carbon-14 dating, which reads age off this exact curve. Carbon-14 decays at a fixed, known half-life while stable carbon-12 does not change. Measuring the ratio of remaining carbon-14 to carbon-12 in a bone tells you what fraction of the original carbon-14 survives, and the decay equation converts that fraction straight into elapsed time since the organism died.
Key terms
- Half-life
- The time required for half of the radioactive nuclei in a sample to decay.
- Exponential decay
- A decrease where the quantity shrinks by the same fraction over each equal time interval.
- N0
- The initial amount or number of radioactive nuclei present at time zero.
- Carbon-14 dating
- A method that estimates age by comparing remaining radioactive carbon-14 to stable carbon-12 in a sample.
Watch it explained
- How it worksHow does a fixed fraction decaying per unit time produce that same falling curve every time?
- How it worksGraph the number of surviving nuclei over five half-lives and mark each halving.
- Worked exampleFind how much of a 80 g sample with a 6 day half-life is left after 24 days.
- Going furtherHow does carbon-14 dating read the age of a bone off this exact decay curve?
Check yourself
End of topic.