Half-Life Calculator

–remaining fraction = 2^(-t/T) - enter time and half-life
IsotopeHalf-lifeKnown for
Carbon-145,730 yearsradiocarbon dating archaeology
Iodine-1318.02 daysthyroid treatment and diagnostics
Technetium-99m6.01 hoursthe workhorse of medical imaging
Cobalt-605.27 yearscancer radiotherapy sources
Cesium-13730.17 yearsChernobyl and Fukushima fallout
Strontium-9028.79 yearsbone-seeking fallout product
Radium-2261,600 yearsthe Curies’ original element
Plutonium-23924,110 yearsweapons and reactor fuel
Americium-241432 yearssmoke detector ionization sources
Potassium-401.25 billion yearsdating rocks, and bananas
Uranium-2384.47 billion yearsthe Earth’s dating clock
Thorium-23214.0 billion yearsolder than most of the universe’s stars
Half-lives in the table are the standard published values maintained in the NNDC nuclear data sheets at Brookhaven National Laboratory. The decay law is pure exponent: what remains after time t is 2^(-t/T) of the starting amount - 25% after two half-lives, 12.5% after three, and it never reaches zero, which is why “how long until it’s all gone” has no answer, only “how long until it barely matters.” Radiocarbon dating reads the same law backwards: living things hold a constant Carbon-14 ratio, and the ratio left in something dead counts the years since. Bottom line: after ten half-lives - 57,300 years for Carbon-14 - just 0.1% remains, which is why carbon dating runs out of signal around 50,000 years and hands older rocks to Uranium-238. Element-level data: periodic table list, weights molar mass calculator, constants physical constants table.

Radioactive decay follows one line of math: after each half-life, half of what remained is gone - so the remainder is 2^(-t/T), never zero. This calculator runs that exponent for twelve common isotopes (half-lives from the Brookhaven NNDC data) or any custom value, and answers in percent and fraction.

The same law reads backward as dating: Carbon-14’s 5,730-year half-life turns a measured ratio into an age, which is how archaeology dates charcoal and how the Uranium-238 clock dates rocks a billion years old.

How to use

  1. Pick an isotope (the half-life fills itself) or choose custom and type a half-life with matching units.
  2. Enter elapsed time; the chips load the classic cases - two Carbon-14 half-lives, one Iodine-131, four Cobalt-60 quarter-lives.
  3. Read the fraction line for the exact multiplier and how many half-lives the elapsed time represents.

Frequently asked questions

Why does radioactive material never fully disappear?

Because the decay removes half per half-life, the remainder is a geometric sequence: 1/2, 1/4, 1/8... approaching but never reaching zero. That is why regulations use practical targets - ten half-lives leaves 0.1%, the standard rule of thumb for when a source is stored rather than feared.

How does carbon dating use this calculator?

Living things exchange carbon constantly, holding a steady Carbon-14 ratio with the atmosphere. At death the exchange stops and the ratio decays on a 5,730-year clock: a wooden artifact showing 25% of the living ratio is two half-lives old - about 11,460 years. The calculator’s C-14 chip runs exactly this.

What is the decay constant lambda?

The exponent’s other face: lambda = ln(2) / T½, about 0.693 divided by the half-life, so N(t) = N₀ · e^(-λt). Same curve, different spelling - textbooks use lambda, this calculator uses the 2^(-t/T) form because half-lives are what tables publish.

Why do medical isotopes have such short half-lives?

By design: Technetium-99m’s 6 hours means the imaging dose fades before the patient leaves the hospital, while Iodine-131’s 8 days is long enough to concentrate in the thyroid and short enough to stop soon after. The therapeutic window is half-life selection.

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