
Radioactive materials naturally change over time through a process known as radioactive decay. One of the most important ways scientists describe this process is through the concept of half-life.
Half-life calculations allow researchers to determine how long it takes for a radioactive substance to decay, estimate the age of objects, and understand nuclear reactions occurring in nature and in laboratories. From nuclear medicine to carbon dating, half-life plays a central role in modern science.
This guide explains what half-life is, how it works, and how scientists calculate it in nuclear reactions.
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