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radiocarbon dating |
Also found in: Wikipedia, Hutchinson | 0.02 sec. |
carbon-14 datingor radiocarbon datingMethod of determining the age of once-living material, developed by U.S. physicist Willard Libby in 1947. It depends on the decay of the radioactive isotope carbon-14 (radiocarbon) to nitrogen. All living plants and animals continually take in carbon: green plants absorb it in the form of carbon dioxide from the atmosphere, and it is passed to animals through the food chain. Some of this carbon is radioactive carbon-14, which slowly decays to the stable isotope nitrogen-14. When an organism dies it stops taking in carbon, so the amount of carbon-14 in its tissues steadily decreases. Because carbon-14 decays at a constant rate, the time since an organism died can be estimated by measuring the amount of radiocarbon in its remains. The method is a useful technique for dating fossils and archaeological specimens from 500 to 50,000 years old and is widely used by geologists, anthropologists, and archaeologists. radiocarbon dating a technique for determining the age of organic materials, such as wood, based on their content of the radioisotope 14C acquired from the atmosphere when they formed part of a living plant. The 14C decays to the nitrogen isotope 14N with a half-life of 5730 years. Measurement of the amount of radioactive carbon remaining in the material thus gives an estimate of its age radiocarbon dating [¦rad·ē·ō′kär·bən ′dād·iŋ] (nucleonics) How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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| Rogers, very recently deceased, who discovered that in the very area used to provide samples for the radiocarbon test, the Shroud linen had been mended. Ongoing radiocarbon tests may reduce that age estimate slightly, according to Trinkaus. Other labs will conduct radiocarbon tests to date the findings. |
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