Half-life

Science

Definition

The time required for half of a radioactive substance to decay into a different element or isotope. After each half-life, the remaining amount of the original substance is reduced by 50%. Half-life is constant for any given isotope regardless of conditions.

Examples

  • Carbon-14 has a half-life of 5,730 years, used to date archaeological artifacts
  • Uranium-238 has a half-life of 4.5 billion years, used to date rocks
  • Iodine-131 has an 8-day half-life, used in medical thyroid treatments
Key Fact

After n half-lives, remaining amount = initial amount × (1/2)ⁿ

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