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Information on the concept of radiometric dating and details about specific radioactive isotopes and their half-lives. It includes a problem-solving assignment where students are asked to determine the age of moon rocks based on the percentage of parent and daughter isotopes present.
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Age of Moon Rocks by Radiometric Dating
Parent Isotope Daughter Isotope Half-life Thorium-232 Lead-208 14 billion years Uranium-238 Lead-206 4.47 billion years Potassium-40 Argon-40 1.25 billion years Uranium-235 Lead-207 704 million years Carbon-14 Nitrogen-14 5,730 years
A radioactive substance is one that is unstable. It will eventually decay to a simpler form. The rate at which a radioactive substance decays is described by its half-life. The half-life is the amount of time that must pass before half of the original radioactive substance has decayed away.
The table above shows a few radioactive substances (the “parent”), what stable form they can decay to (the “daughter”), and how long the half-life is. Note that there are several intermediate stages between each parent-daughter pair.
For example, imagine that you have a 1 gram rock of potassium-40 in it. After 1.25 billion years (i.e., one half-life) there will be 0.5 grams remaining. After 2.5 billion years (two half-lives) there will be 0.25 grams left. After 3.75 billion years (three half-lives) there will be 0.125 grams left. The rest of the rock will be daughter products.
We describe this situation mathematically by:
current amount original amount
where t is the elapsed time since the rock formed, and thalf is the half-life of the parent, given in the table. The fraction current amount/original amount is a number between 0 and 1. If only 10% of a parent remains, then this fraction equals 0.10.
Imagine that you are analyzing Moon rocks returned by the Apollo missions. You detect small amounts of uranium- and its lead daughter product.