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Lead-206 is a stable isotope of lead that is the end product of the radioactive decay series of uranium-238. This means that over a very long period, uranium transforms into lead-206 through a series of radioactive decay steps.123

The concept of half-life is crucial here. A half-life is the time it takes for half of a radioactive substance to decay into a different form. While lead-206 itself is stable, the isotopes that decay into it, like lead-210, have measurable half-lives. This decay process is utilized in lead-210 dating, a method used to determine the age of materials, particularly recent sediments, by measuring the ratio of lead-210 to lead-206.41

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