Radioactive Decay & Half-Life

Unstable atomic nuclei break apart at random, one by one, and there is no way to predict exactly when any single nucleus will decay. But across a large sample, the pattern is completely predictable: after one half-life, exactly half the original nuclei remain, and after each further half-life, half of what is left decays away.

The formula

N = N₀ · (½)^(t/t½)

  • N — remaining amount (g): the amount of the substance still remaining at time t
  • N₀ — initial amount (g): the amount present at the very start, when t equals zero
  • t — elapsed time (s): how much time has passed since the start
  • t½ — half-life (s): the time it takes for half of the sample to decay

Worked example

An 80 gram sample of a radioactive isotope has a half-life of 5 days. How much is left after 10 days?

  • N₀ = 80 g
  • t½ = 5 days
  1. N = N₀ · (½)^(t/t½)
  2. N = 80 g · (½)^(10/5) = 80 g · (½)²

N = 20 g

Test yourself

The same 80 gram sample keeps decaying. How much is left after 15 days?
  • 40 g
  • Correct answer: 10 g
  • 26.7 g

Right! Three half-lives: 80 g → 40 g → 20 g → 10 g.

After 3 half-lives have passed, what fraction of the original sample is still left?
  • Correct answer: 1/8
  • 1/3
  • 1/6

Correct! One half times one half times one half equals one eighth.

Where you see this

Archaeologists date ancient wood and bone by carbon-14, whose half-life of 5,730 years steadily drops its concentration after death — measuring what is left reads the calendar. Hospitals use the same decay law with short-lived tracers that glow through the body and fade within a day.

Common mistakes

The arithmetic error is treating each half-life as subtracting a fixed amount — it multiplies by one half, so three half-lives leave one eighth (½ × ½ × ½), never zero and never three-halves gone: an 80 g sample goes 80 → 40 → 20 → 10 g. The conceptual error is expecting single nuclei to obey the law — any one nucleus decays at a random, unknowable moment; only large samples become predictable.

How it connects

Decay is probability done with nuclei — the same law-of-large-numbers logic as thermodynamics' entropy — and it hands the next lesson its question: WHY are some nuclei unstable and others not? The answer, binding energy, also brings back relativity's c² to price the difference.

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