How can the half-life of Carbon-14 help determine the age of organic materials?

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The discussion centers on calculating the remaining amount of carbon-14 in a sample after 22,920 years, given its half-life of 5,730 years. It is established that 22,920 years equals four half-lives. The process of halving is explained, emphasizing that after each half-life, the amount of carbon-14 reduces by half. Starting with 26 grams, the amount after four half-lives is calculated by halving the original amount four times, leading to the conclusion that the remaining mass is 1.625 grams. The exponential decay formula for carbon-14 is also mentioned, illustrating how to calculate the remaining quantity using the initial mass and time. Additionally, the relevance of carbon-14 dating in determining the age of organic materials, such as dinosaur bones, is highlighted.
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The half-life of carbon-14 is 5730 years. If a sample had 26 g of carbon-14, how much would it contain after 22,920 years (x 4)?
 
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calculate how many times the half-life time has past, you apparentely did so and that is 4 times, so that means that the original amount has halved 4 times...

after 1 time the half-life time you have half of the original amount
after 2 times the half-life time you have half of the half of the original amount so a quart
after 3 times...
 
I did 26 divided by 4, does that work? Or do I keep halving it? As in 1.625?
 
No if it halves 4 times, that does not mean yoiu have to divide by 4

take for example 20 to start with,
if you half that ones you have 10
if you halve it a second time you have 5
so after halving it two times you have what you had originally divided by 4

you have to keep halving, four times.
1/2 *1/2 *1/2 *1/2 = 1/16
so you have to divide by 16
 
Since biology is a subdiscipline of physics, and since we are in the physics forum. Here is another way to look at your question.
Radioactive decay of Carbon-14 follows an exponential decaying function of the form Ae^{-kt}

Carbon-14 follows the expontial decay: Q= Q_0 e^{-0.000121t}
where t - years, Q_0 - initial mass, Q - final mass.

So try that, plug in 26g for Q_0 and 22,920 years for t,
what do you get?

Ask you teacher/professor: Knowing the half-life of Carbon-14, how can that be used to calculate the age of dinosaur bones or other organic matter? :rolleyes:
 
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