Physics

Physics

Problem

A zircon crystal contains 3.0×10173.0\times10^{17} atoms of 238U^{238}\text{U} and 4.5×10174.5\times10^{17} atoms of 206Pb^{206}\text{Pb}. Laboratory analysis shows that 0.5×10170.5\times10^{17} of the lead atoms were present when the crystal formed. Assuming all additional 206Pb^{206}\text{Pb} arose from the decay of 238U^{238}\text{U} (half-life 4.5×109 years4.5\times10^{9}\,\text{years}), the best estimate of the crystal’s age is a) 2.6×109 years2.6\times10^{9}\,\text{years} b) 6.6×109 years6.6\times10^{9}\,\text{years} c) 5.5×109 years5.5\times10^{9}\,\text{years} d) 4.5×109 years4.5\times10^{9}\,\text{years}
Intuitive explanation

Radioactive dating works by tracking how much of a parent isotope has decayed into a daughter product over time. Here, uranium-238 decays into lead-206, so the extra lead beyond what was originally present tells you how many uranium atoms have decayed. Use the decay constant and the ratio of remaining uranium to decayed uranium to find the elapsed time—this is the core of the radioactive dating method.

Intuitive explanation

Radioactive dating works by tracking how much of a parent isotope has decayed into a daughter product over time. Here, uranium-238 decays into lead-206, so the extra lead beyond what was originally present tells you how many uranium atoms have decayed. Use the decay constant and the ratio of remaining uranium to decayed uranium to find the elapsed time—this is the core of the radioactive dating method.

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