What is a half-life?
The time for exactly half of a radioactive sample to decay. After n half-lives, N = N₀/2ⁿ.
Calculate remaining radioactive atoms after time t. N = N₀ (½)^(t/t½) — exponential decay.
N = N₀(½)^(t/t₁∕₂)
| Symbol | Quantity | SI Unit |
|---|---|---|
| N | Remaining quantity | same as N₀ |
| N₀ | Initial quantity | atoms or Bq |
| t | Elapsed time | any unit |
| t₁/₂ | Half-life | same time unit |
| λ | Decay constant = ln2/t½ | s⁻¹ |
This radioactive half-life calculator is built for quick physics checks and worked-problem review. Enter values in the units shown beside each input, then compare the result with the formula and variable table before using it in a longer solution. The calculator does the arithmetic, but the physics still depends on choosing a model that matches the situation.
Start by identifying the system, the known quantities, and the quantity you want to find. If a value is given in a non-SI unit, convert it before substitution. A correct numerical answer with mixed units can still be physically wrong, especially when squared units, inverse seconds, charges, temperatures, or distances are involved.
The formula N = N₀(½)^(t/t₁∕₂) is a model, not a universal description of every possible case. It assumes the quantities in the variable table are the relevant quantities for the problem and that hidden effects are either negligible or already included in the inputs. If friction, drag, relativistic speeds, changing fields, non-constant temperature, or geometry-specific effects matter, check whether a more complete model is needed.
Use the result as a magnitude and units check. Ask whether the answer has the right sign, whether it grows or shrinks when an input changes, and whether the limiting cases make sense. Setting an input to zero, doubling a quantity, or using a very large value is often enough to catch a formula choice or unit mistake before it reaches a final answer.
Carbon-14: t½ = 5,730 years. 1,000 atoms, t = 11,460 years. Find N.
Step 1: t / t½ = 11460/5730 = 2.0 half-lives
Step 2: N = 1000 × (½)² = 1000/4
Answer: N = 250 atoms
The time for exactly half of a radioactive sample to decay. After n half-lives, N = N₀/2ⁿ.
Yes — carbon-14 (t½ = 5,730 years) is used to date organic materials up to ~50,000 years old.