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The number of <sup>238</sup> U atoms in ...

The number of 238 U atoms in an ancient rock equals the number of 206 Pb atoms. The half-life of decay of 238 U is 4.5x109 years. Estimate the age of the rock assuming that all the 206 Pb atoms are formed from the decay of 238U.

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Since the number of `.^(205)Pb` atoms equals the number of `.^(238)U` atoms, half of the original `.^(238)U` atoms have decayed. It takes one half-life to decay half of the active nuclei. Thus, the sample is `4.5xx10^(9)y` old.
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.^(238)U decays with a half-life of 4.5 xx10^(9) years, the decay series eventually ending at .^(206)Pb , which is stable. A rock sample analysis shows that the ratio of the number of atoms of .^(206)Pb to .^(238)U is 0.0058. Assuming that all the .^(206)Pb is produced by the decay of .^(238)U and that all other half-lives on the chain are negligible, the age of the rock sample is (ln 1.0058 =5.78 xx10^(-3)) .

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