Carbon-14 and Radiocarbon Dating
Category: Science & Technology | GS Paper III
SEO Title: Carbon-14 Dating: Half-Life, Principle, Applications and Limitations in Archaeology
UPSC Notes
Carbon-14 is a radioactive isotope of carbon used to estimate the age of organic materials.
Half-life: Approximately 5,730 years.
Formation: Cosmic-ray neutrons interact with nitrogen-14 in the upper atmosphere, producing carbon-14.
Entry into living organisms: Carbon-14 enters the food chain through atmospheric carbon dioxide and biological processes.
Radioactive decay: Carbon-14 decays by beta emission into nitrogen-14.
Radiocarbon dating: Developed by Willard Libby, who received the Nobel Prize in Chemistry in 1960.
Age range: Commonly useful for organic samples up to around 50,000 years old.
Modern technique: Accelerator Mass Spectrometry (AMS) can measure very small quantities of carbon-14.
Calibration: Tree rings and other chronological records improve dating accuracy.
Applications: Archaeology, biological research and tracing carbon movement.
Limitation: It is not the standard method for dating ancient rocks; uranium–lead and potassium–argon methods are used for suitable geological materials.
Key Pointers for Prelims
Carbon-14 half-life: 5,730 years.
Scientist: Willard Libby.
Best suited to organic remains.
Radiocarbon dates require calibration.
The source mentions archaeological samples from Keeladi, Tamil Nadu.
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