Number of C-14 atoms in old piece of wood

In summary: E.g. after 5 half-lives, there would be a residue of 1/5 of the original amount. After 10 half-lives, there would be a residue of 1/10 of the original amount.
  • #1
kmoh111
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0

Homework Statement


I'm working a homework problem that states:

A very old specimen of wood contained 1012 atoms of 14C in 1986.
• How many 14C atoms did it contain in the year 9474 B.C.?
• How many 14C atoms did it contain in 1986 B.C.?



Homework Equations



N(t) = N(0)exp^(-lambda*t)


The Attempt at a Solution



For C-14, lambda = ln2/T1/2 = 0693/5730 yrs = .000121 yr-1

Since we do not know N0, I took the ratio of C-14 atoms in 1986 (A.D.) to C-14 atoms in 9474 B.C.:

Let t1 reflect the time from t0 to 1986.
Let t2 reflect the time from t0 to 9474 B.C.
then the ratio of N(t1)/N(t2) is:

N0 * e-lambda*t1
-----------------------------------------------------
N0 * e-lambda*t2

N0 cancels and we know that N(t1) = 1012 atoms.

Solving for N(t2) gives us:

1012
----------------------------------------------------
e-lambda(t2-t1)

We know that the difference t2 - t1 is equal to 1986 + 9474 = 11460 yrs. Plugging the numbers and solving for N(T2), gives us

1012
----------------------------
e(-0.693(11460/5730))

N(t2) = 4 x 1012 ===> number of C-14 atoms in 9474 B.C.

Is this the correct approach? I used the approach for the second part of the question for number of C-14 atoms in 1986 B.C.. I got 1.6 x 1012 atoms.

Thanks for the help.
 
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  • #2
Well...*technically* [tex]N(t1) = N_0 * e^{-\lambda*t1} [/tex], so you shouldn't have canceled out the N0, although it does not affect your final answer.
 
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  • #3
Perhaps an easier approach would be to note that the time elapsed, 11,460 years, is about 2 half-lives, 2.01 to be precise. What fraction of the original sample is left after 2 half-lives have gone by? If you know the fraction remaining, you can easily find the original amount.

In general, I find it easier to answer this kind of problem using the half-life as a unit of time because the fraction remaining after n half-lives is

f = 2-n.
 

Related to Number of C-14 atoms in old piece of wood

What is the significance of the number of C-14 atoms in an old piece of wood?

The number of C-14 atoms in an old piece of wood is significant because it can provide information about the age of the wood. C-14 is a radioactive isotope that decays at a predictable rate, so by measuring the amount of C-14 remaining in the wood, scientists can determine how long ago the tree was alive and therefore the age of the wood.

How do scientists determine the number of C-14 atoms in an old piece of wood?

Scientists use a technique called radiocarbon dating to determine the number of C-14 atoms in an old piece of wood. This involves measuring the amount of C-14 present in a sample and comparing it to the amount of C-14 in a living organism. By knowing the rate of decay of C-14, scientists can calculate the age of the wood.

Can the number of C-14 atoms in an old piece of wood be used to date other organic materials?

Yes, radiocarbon dating can be used to date other organic materials such as bones, shells, and fabric. However, it is not effective for dating materials older than 50,000 years as the amount of C-14 becomes too small to accurately measure.

How accurate is the number of C-14 atoms in an old piece of wood for determining its age?

Radiocarbon dating is considered to be a highly accurate method for determining the age of organic materials. However, the accuracy can be affected by factors such as contamination, sample size, and the calibration curve used. Generally, radiocarbon dating can provide an age estimate within a range of a few hundred years to a few thousand years.

Why do scientists use the number of C-14 atoms in an old piece of wood instead of other dating methods?

Radiocarbon dating is a useful method for determining the age of organic materials because it is based on a constant rate of decay and can provide accurate results for relatively recent materials. Other dating methods, such as dendrochronology (tree ring dating) or potassium-argon dating, are useful for dating older materials but may not be as accurate for younger materials.

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