final practice questions and was unable to answer the first five or so questions. The
powerpoint on stratigraphy doesn't really explain how to solve these types of problems
very well. I looked over the slides a few times and am still confused. Thanks.
A: Radioactive decay occurs at a constant rate. As a result, you can use it like a clock. The rate of decay is measured in half lives. The half life of carbon is roughly 5000 years. Carbon-14 decays into Nitrogen-14. Carbon-14 is called the parent isotope, Nitrogen-14, the daughter isotope.
Say you have 16 atoms of carbon 14. After ~5000 years, half of the carbon has decayed away, so there are 8 atoms of carbon 14, 8 atoms of nitrogen. What about after 10,000 years? How many atoms of Carbon 14? (Answer: 4). How many total atoms of N-14? (Answer: 12 = 8 oldones, 4 new ones). After 15,000 years?
A Problem: You have find a fossil snail shell. It has carbon in it, so you can date it using Carbon-14 (C-14) methods. Let’s say you find that you have 15 grams of nitrogen-14 (N-14), and 1 gram of carbon 14. Assume all N-14 that’s there is the result of carbon 14 decay. So, when the snail was alive, it didn’t have any N-14 in it. How old is the snail?
Answer:
OK: how much C 14 was there to start?
15 + 1 grams = 16 grams.
How much carbon is left?
1 out of 16 original grams.
How many half lives is that?
Half-life #1: Carbon goes from 16 -> 8
Half-life #2: 8 -> 4
Half-life #3: 4 -> 2
Half-life #4: 2 -> 1
Four half-lives, each 5000 years: 4x5000 = 20,000 years.
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