Radiochemistry
Radiocarbon dating is a scientific method used to determine the age of organic materials by measuring the amount of carbon-14 they contain. This technique relies on the principles of beta decay, where unstable isotopes of carbon are transformed into stable nitrogen over time. The process involves analyzing the ratio of carbon-14 to carbon-12 in a sample, allowing researchers to estimate when the organism died, making it a crucial tool in fields such as archaeology and geology.
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