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

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In summary, the half-life of carbon-14 is 5730 years and if a sample initially contains 26 g of carbon-14, after 22,920 years it would contain 1/16 of the original amount. This is because the original amount has halved 4 times, with each halving resulting in 1/2 of the previous amount. Using the exponential decay function for carbon-14, Q=Q_0 e^(-0.000121t), we can calculate the final mass of carbon-14 after a given amount of time. This knowledge can be applied to determine the age of organic materials such as dinosaur bones.
  • #1
ConcealedDreamer
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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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  • #2
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...
 
  • #3
I did 26 divided by 4, does that work? Or do I keep halving it? As in 1.625?
 
  • #4
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
 
  • #5
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 [tex] Ae^{-kt} [/tex]

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

So try that, plug in 26g for [tex] Q_0 [/tex] and 22,920 years for [tex] t [/tex],
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? :uhh:
 

What is Carbon-14?

Carbon-14 is a radioactive isotope of the element carbon, with an atomic mass of 14. It is formed in the upper atmosphere when cosmic rays interact with nitrogen atoms, and is constantly produced in small amounts.

How is Carbon-14 used in dating?

Carbon-14 is used in radiocarbon dating, a method used to determine the age of organic materials. As living organisms absorb carbon from the atmosphere, they also absorb a small amount of Carbon-14. When an organism dies, it stops absorbing Carbon-14 and the amount present in its tissues begins to decay at a predictable rate. By measuring the remaining amount of Carbon-14 in a sample, scientists can determine how long ago the organism died.

What is the half-life of Carbon-14?

The half-life of Carbon-14 is approximately 5,730 years. This means that after 5,730 years, half of the initial amount of Carbon-14 in a sample will have decayed into nitrogen. After another 5,730 years, half of the remaining Carbon-14 will have decayed, and so on.

Can Carbon-14 be used to date all materials?

No, Carbon-14 dating can only be used on organic materials. Inorganic materials, such as rocks and minerals, do not contain Carbon-14 and therefore cannot be dated using this method.

Why is Carbon-14 considered a reliable dating method?

Carbon-14 dating is considered reliable because the rate of decay of Carbon-14 is constant and well understood. Additionally, scientists can use other methods, such as tree-ring dating, to cross-check and verify the accuracy of Carbon-14 dating results.

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