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Jeudi, 13 Octobre 2011 12:00

Equation: Radiocarbon Dating

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  • 12:00 pm  | 
  • Wired October 2011

Illustration: Mario Hugo

Right now, 40,000 feet overhead, a cosmic ray is sending a neutron smashing into a nitrogen atom, smacking a proton out of its nucleus and forming an isotope called carbon-14. Armed with the equation below, archaeologists use these atoms to pinpoint how old the Dead Sea Scrolls are, or the drawings in Chauvet Cave, or Ötzi the Iceman.

Living things constantly consume carbon—through photosynthesis, for plants, and for animals, ingestion of those plants. The atmospheric ratio of carbon-14 to regular carbon-12 remains consistent at one part per trillion, so if something is alive, one-trillionth of its carbon atoms will be C-14. But once a plant or animal dies, its carbon-14 is no longer replenished. C-14 is radioactive and unstable, with a half-life of 5,730 years, which means that half the atoms will turn back into nitrogen over that period. That rate of decay is key to gauging age.

Amount of carbon-14 detected in the sample

Amount of carbon-14 in the sample at the time of death, which would have been a trillionth of the total carbon present

Half-life of carbon-14: 5,730 years

What we’re solving for: time elapsed since the thing—or the organic materials used to make the thing—died


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French (Fr)English (United Kingdom)

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