In physics, the term "half-life" refers to the time it takes for half of a quantity of a substance to undergo a change or decay. This concept is commonly used in the context of radioactive decay, but it can also be applied to other processes in physics and chemistry.

Let's focus on radioactive decay to illustrate the concept. Radioactive isotopes are unstable atoms that spontaneously transform into more stable ones by emitting particles or electromagnetic radiation. The half-life of a radioactive isotope is the time it takes for half of a sample of that isotope to decay.

For example, if you start with a certain amount of a radioactive substance, after one half-life, half of that substance will have decayed, and you'll be left with half of the original amount. After two half-lives, only one-fourth of the original substance will remain, and so on.

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