Carbon-14 after three half lives
N₀ = 100, t = 17,190 yr, t½ = 5,730 yrt/t½ = 17,190 / 5,730 = 3. N = 100 · (½)³ = 100 / 8 = 12.5. Start with 100 g and 12.5 g is left; start with 100% and 12.5% is left.
The amount left after radioactive decay, the time it took, or the half life.
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The Coddy physics course teaches the method: you solve each problem in steps on an interactive board, and it tells you which step went wrong.
A radioactive sample decays at a rate set by its half life, t½: the time it takes for half of the atoms to decay. Whatever amount you start with, half is left after one half life, a quarter after two, an eighth after three. The formula is N = N₀(½)^(t/t½), where N₀ is the starting amount, N the amount left and t the time that has passed.
The exponent t/t½ counts how many half lives have gone by, and it does not have to be a whole number. To go backwards to the time, take a base 2 logarithm: t = t½ · log₂(N₀/N). If 80 g has become 10 g, N₀/N = 8, log₂ 8 = 3, so three half lives have passed. The half life does not depend on how much you have: a gram and a tonne of iodine-131 both halve in 8.02 days.
The calculator solves the formula for whichever of the four you leave blank: the amount left, the starting amount, the time or the half life. The two amounts can be in any unit, grams, atoms, a percentage or becquerels of activity, as long as both use the same one. The times can be in seconds, minutes, hours, days or years (a year here is 365.25 days), and the time and the half life may use different units: both are converted to seconds first, and the answer is given in the unit you pick and in the others.
Three of the four: the starting amount N₀, the amount left N, the time t and the half life t½.
Hours with hours, years with years. 2 days is 48 hours; a year is 365.25 days.
N = N₀ · (½)^(t/t½). 100 g of carbon-14 after 17,190 years: 17,190 / 5,730 = 3, and 100 · (½)³ = 12.5 g.
t = t½ · log₂(N₀/N). From 100% to 25% is log₂ 4 = 2 half lives; for carbon-14 that is 2 · 5,730 = 11,460 years. On a calculator without log₂, use log₂ x = ln x / ln 2.
Rounded standard values. They run from minutes to billions of years, which is why the calculator takes times from seconds to years.
| Isotope | Half life | Where you meet it |
|---|---|---|
| Fluorine-18 | 110 minutes | PET scans |
| Technetium-99m | 6.01 hours | The most used tracer in medical scans |
| Radon-222 | 3.82 days | A gas that seeps from rocks into basements |
| Iodine-131 | 8.02 days | Thyroid treatment |
| Polonium-210 | 138 days | Alpha sources |
| Cobalt-60 | 5.27 years | Radiotherapy, sterilising medical equipment |
| Hydrogen-3 (tritium) | 12.3 years | Glowing exit signs and watch dials |
| Caesium-137 | 30.1 years | Fallout from Chernobyl and Fukushima |
| Radium-226 | 1,600 years | Old luminous paint |
| Carbon-14 | 5,730 years | Radiocarbon dating |
| Plutonium-239 | 24,100 years | Nuclear reactors |
| Uranium-235 | 704 million years | Nuclear fuel |
| Potassium-40 | 1.25 billion years | Bananas, the human body, dating rocks |
| Uranium-238 | 4.47 billion years | Dating the oldest rocks on Earth |
N₀ = 100, t = 17,190 yr, t½ = 5,730 yrt/t½ = 17,190 / 5,730 = 3. N = 100 · (½)³ = 100 / 8 = 12.5. Start with 100 g and 12.5 g is left; start with 100% and 12.5% is left.
N₀ = 80, N = 10, t = 24 dRearrange for the half life: t½ = t / log₂(N₀/N) = 24 / log₂ 8 = 24 / 3 = 8 days. That is close to iodine-131's 8.02 days. Set the half life box to days and the answer reads 8; it is also given in seconds, hours and years.
N₀ = 1, N = 0.25, t½ = 8 dt = t½ · log₂(N₀/N) = 8 · log₂ 4 = 8 · 2 = 16 days. A quarter is two halvings, so the time is two half lives.
N₀ = 100, t = 24 h, t½ = 6.01 hTechnetium-99m: t/t½ = 24 / 6.01 = 3.993 half lives, not a whole number, and that is fine. N = 100 · (½)^3.993 = 6.28, so 6.28% of the dose is left after a day.
N₀ = 100, N = 25, t½ = 5,730 yrA bone with 25% of the carbon-14 of living tissue: t = 5,730 · log₂(100 / 25) = 5,730 · 2 = 11,460 years old.
N = N₀(½)^(t/t½), where N₀ is the starting amount, N the amount left after a time t, and t½ the half life. The exponent t/t½ is the number of half lives that have passed.
Measure the amount at the start and after a known time, then use t½ = t / log₂(N₀/N). If 80 units fall to 10 in 24 days, log₂ 8 = 3, so the half life is 24 / 3 = 8 days.
Use t = t½ · log₂(N₀/N). The logarithm counts the halvings: from 100% to 12.5% is log₂ 8 = 3 half lives, so for a half life of 5,730 years the time is 17,190 years.
One eighth, 12.5%. Each half life halves what is left: 50% after one, 25% after two, 12.5% after three, 6.25% after four and 3.125% after five.
Yes. The formula only uses the ratio of the two amounts, so any unit works as long as the amount left and the starting amount use the same one. Activity in becquerels works too, since it falls with the same half life.
The decay constant λ is the fraction of atoms that decay per unit of time, and λ = ln 2 / t½. For carbon-14 it is 0.693 / 5,730 = 1.21 × 10⁻⁴ per year. The law can then be written N = N₀e^(−λt).
Living things take in carbon-14 and keep the same share as the air. When they die, it decays with a half life of 5,730 years. Measure the fraction left and t = 5,730 · log₂(N₀/N) gives the age: 25% left means 11,460 years.