Drop 100 parent atoms in. Advance time one half-life at a time. The graph builds itself.
In a real sample, each atom decays at a random moment — but with millions of atoms, the average always halves each half-life.
| HL | Parent | Daughter | %P |
|---|
Notice: the % column halves each row (100 → 50 → 25 → 12.5 …). It never reaches zero.
A rock sample contains 12.5% of its original parent isotope. How many half-lives have passed? If the isotope is potassium-40 (HL = 1.25 billion years), what is the rock's age?
Use the simulator: advance until %P ≈ 12.5%. That gives you the number of half-lives directly. Multiply by 1.25 billion years.