Astronomy Assignment: Determining the Age of Moon Rocks using Radiometric Dating, Assignments of Astronomy

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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Pre 2010

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Astr 138 Assignment #6 - Due Thurs Oct 27, 2005
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 =1
2t/thalf (1)
where tis 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-238
and its lead daughter product.
1. In a ro ck from the lunar highlands, you determine that 55% of the original uranium-238 remains, the other 45% has
decayed. What is the age of this rock?
2. In a ro ck from the lunar lowlands, you determine that 63% of the original uranium-238 remains. What is the age of
this rock?
3. Which ro ck is older, highland or lowland? How do your results compare with the density of craters in the highlands
versus the lowlands? Are your age results surprising, or expected?

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Astr 138 Assignment #6 - Due Thurs Oct 27, 2005

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

)t/thalf

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.

  1. In a rock from the lunar highlands, you determine that 55% of the original uranium-238 remains, the other 45% has decayed. What is the age of this rock?
  2. In a rock from the lunar lowlands, you determine that 63% of the original uranium-238 remains. What is the age of this rock?
  3. Which rock is older, highland or lowland? How do your results compare with the density of craters in the highlands versus the lowlands? Are your age results surprising, or expected?