Radioactive Dating with Potassium Argon

In summary, the technique of potassium-argon dating is used to date old lava flows by measuring the ratio of ^{40}{\rm Ar}/^{40}{\rm K} in solidified lava. With a known half-life of 1.28 billion years, this ratio can be used to determine the age of the lava. Using the given ratio of 0.350, the calculated age of the lava is approximately 1.94 billion years. This method is similar to carbon dating, where the ratio of ^{14}{\rm C}/^{12}{\rm C} is used to determine the age of organic materials.
  • #1
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[SOLVED] Radioactive Dating with Potassium Argon

Homework Statement


The technique known as potassium-argon dating is used to date old lava flows. The potassium isotope [tex]^{40}{\rm K}[/tex] has a 1.28 billion year half-life and is naturally present at very low levels. [tex]^{40}{\rm K}[/tex] decays by beta emission into [tex]^{40}{\rm Ar}[/tex]. Argon is a gas, and there is no argon in flowing lava because the gas escapes. Once the lava solidifies, any argon produced in the decay of [tex]^{40}{\rm K}[/tex] is trapped inside and cannot escape. A geologist brings you a piece of solidified lava in which you find the [tex]^{40}{\rm Ar}/^{40}{\rm K}[/tex] ratio to be 0.350.

t = ? [billions of years]


Homework Equations


Any of these I suppose:
N = N_0 e^(-t/T)
T = time constant = 1/r
r = decay rate = [per seconds]
(t/2) = half-life = 1.28 billion years
Beta-plus decay: X becomes Y (A same, Z-1) + e^+1 + energy


The Attempt at a Solution


N = given ratio of Ar/K = .350
N_0 = 1

ln(1/2) = -(t/2) / T
T = -t/2 / ln(.5) = 1.846... years
r = 1 / T = 5.41 * 10^-10 [yr^-1]

.350 = 1e^(-rt)
t = ln .350 / -r = 1,938,653,661
t = 1.94 billion years

different attempt using
N = N_0 * (.5)^t/(t/2)
t/2 = given halflife, N = ratio = .350, N_0 = 1
t = 1.94 billion years

I'm guessing I shouldn't be putting in the ratio of Ar to K in for N. But my book only goes into details about Carbon-dating, so I'm not sure where to go from here.

Cheers.
 
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  • #2
Bit of a tricky question. What you can do however is say that:

[tex] N_{Ar}/N = 0.35 [/tex] where N is the amount of potassium after decay, and,

[tex] N_0 = N_{Ar} + N [/tex]

That should help you if you have some Carbon dating examples.
 
  • #3
Thanks that worked out flawlessly.
 

Related to Radioactive Dating with Potassium Argon

1. How does potassium argon dating work?

Potassium argon dating is a method used to determine the age of rocks and minerals based on the decay of radioactive potassium-40 to argon-40. The process involves measuring the amount of argon-40 present in a sample and calculating the amount of time it would take for that amount of argon to accumulate from the radioactive decay of potassium.

2. How accurate is potassium argon dating?

The accuracy of potassium argon dating depends on several factors such as the amount of sample available, the purity of the sample, and the precision of the measurement techniques. Generally, this method can provide accurate results within a range of a few thousand to a few million years.

3. Can potassium argon dating be used on any type of rock?

Potassium argon dating is most commonly used on volcanic rocks because they contain high levels of potassium and low levels of argon. This method can also be used on other types of rocks, but the results may not be as accurate due to potential contamination or lack of suitable minerals for analysis.

4. What are the limitations of potassium argon dating?

One limitation of potassium argon dating is that it can only be used to date rocks that are millions of years old. This method is not suitable for determining the age of very young rocks or recent geological events. Additionally, the technique can be affected by factors such as weathering and metamorphism, which can alter the amount of argon present in a sample.

5. How is potassium argon dating different from other dating methods?

Potassium argon dating is different from other dating methods because it relies on the decay of a single radioactive isotope rather than multiple isotopes. This method is also useful for dating very old rocks and has a wider range of applicability compared to other techniques such as carbon dating, which is only useful for organic materials up to 50,000 years old.

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