Radioactive Dating with Potassium Argon

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SUMMARY

The forum discussion focuses on potassium-argon dating, a technique utilized to date ancient lava flows using the potassium isotope ^{40}{\rm K}, which has a half-life of 1.28 billion years. The decay of ^{40}{\rm K} into ^{40}{\rm Ar} is significant because argon escapes from molten lava but becomes trapped once solidified. The calculated ^{40}{\rm Ar}/^{40}{\rm K} ratio of 0.350 leads to a dating result of approximately 1.94 billion years. The discussion highlights the importance of understanding decay rates and ratios in radioactive dating.

PREREQUISITES
  • Understanding of radioactive decay principles
  • Familiarity with the half-life concept
  • Knowledge of natural isotopes, specifically ^{40}{\rm K} and ^{40}{\rm Ar}
  • Basic logarithmic calculations for decay equations
NEXT STEPS
  • Study the principles of radioactive decay and half-life calculations
  • Learn about the applications of potassium-argon dating in geology
  • Explore other radioactive dating methods, such as carbon dating
  • Investigate the significance of isotopic ratios in dating techniques
USEFUL FOR

Geologists, students studying geology or radiometric dating, and researchers interested in dating volcanic rocks and understanding geological time scales.

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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 ^{40}{\rm K} has a 1.28 billion year half-life and is naturally present at very low levels. ^{40}{\rm K} decays by beta emission into ^{40}{\rm Ar}. 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 ^{40}{\rm K} is trapped inside and cannot escape. A geologist brings you a piece of solidified lava in which you find the ^{40}{\rm Ar}/^{40}{\rm K} 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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Bit of a tricky question. What you can do however is say that:

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

N_0 = N_{Ar} + N

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

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