A half-life is the time it takes for half of the radioactive nuclei in a sample to decay. Each isotope has its own half-life. Iodine-131 is about 8 days, carbon-14 is about 5,730 years, and uranium-238 is about 4.5 billion years. Ordinary changes in temperature, pressure, and chemical bonding have almost no effect on half-life, though electron capture can shift very slightly with chemical environment.
Decay is exponential, not linear. After one half-life, 1/2 of the sample remains, after two 1/4 remains, and after three 1/8 remains. The general formula is N=N0(21)n, where n=t/t1/2 is the number of half-lives. Half-life describes large groups of atoms, so you can't predict when any single atom will decay.
Radiocarbon dating relies on this. While an organism is alive, it exchanges carbon with its environment and keeps a carbon-14 ratio close to that of its surroundings. After death, its carbon-14 decays. Measuring what remains can estimate the age of once-living material up to about 50,000 years old.
Worked example. A sample contains 80.0 mg of iodine-131 (t1/2=8.0 days). How much remains after 24 days? The number of half-lives is n=24/8.0=3. The mass left is 80.0×(1/2)3=80.0/8=10.0 mg, so 70.0 mg has decayed.
Some honors classes also use N=N0e−λt with λ=0.693/t1/2, which also works when the time isn't a whole number of half-lives.
- Half-life ($t_{1/2}$): Half-life is the time it takes for half of the radioactive nuclei in a sample to decay.
- Decay constant ($\lambda$): The decay constant gives the probability per unit time that a radioactive nucleus will decay, and it equals 0.693/t1/20.693 / t_{1/2}0.693/t1/2.
- Radiometric dating: Radiometric dating estimates a material's age from a radioactive isotope's known half-life and measured isotope ratios, often the ratio of a parent isotope to its daughter product.
Check yourself. A piece of wood has 25% of the carbon-14 found in living trees. About how old is it? (Answer: 25% is (1/2)2, so two half-lives have passed. That's 2×5,730≈11,460 years.)