What Is the Age of Rock Using Potassium-Argon Dating?

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SUMMARY

The discussion centers on potassium-argon dating, a method used to date solidified lava flows by measuring the ratio of argon-40 (40Ar) to potassium-40 (40K). The half-life of 40K is 1.28 billion years, and the calculation of the rock's age is based on the formula N(t) = N(0)(1/2)^(t/t1/2). The user initially miscalculated the age of the rock as 4.1 billion years due to confusion about the decay process, but clarified that N(t) represents the remaining potassium-40 atoms, not argon atoms. Correcting this misunderstanding is crucial for accurate dating results.

PREREQUISITES
  • Understanding of radioactive decay and half-life concepts
  • Familiarity with potassium-argon dating methodology
  • Basic knowledge of logarithmic functions and their applications in decay equations
  • Ability to interpret isotopic ratios in geological samples
NEXT STEPS
  • Study the principles of radioactive decay and half-life calculations
  • Learn about the applications and limitations of potassium-argon dating
  • Explore the use of isotopic ratios in geochronology
  • Investigate alternative dating methods such as uranium-lead dating
USEFUL FOR

Geologists, students in earth sciences, and researchers interested in dating geological formations and understanding the age of volcanic rocks.

bmxicle
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Homework Statement


The technique known as potassium-argon dating is used to date old lava flows. The potassium isotope 40K has a 1.28 billion year half-life and is naturally present as very low levels. 40K decays by beta emission into 40Ar. 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 is trapped inside and cannot escape. A geologist brings you a piece of solidified lava in which you find the 40Ar/40K ratio to be 0.12. What is the age of the rock


Homework Equations


N(t) = N(0)(1/2)t/t1/2
r = ln2/t1/2[/SUP]


The Attempt at a Solution


Here's what i have so far.
NAr is the number of argon atoms in the sample
NK is the number of pottasium atoms in the sample
K0 is the original number of pottassium atoms in the sample.

NAr/NK =0.12 ===> NAr = 0.12NK
Nk0 = NAr + Nk
These two equations combined give NK0 = 1.12Nk
and since Nk = NAr/0.12
===> NK0 = NAr1.12/0.12

Plugging this into the equation gives:

NAr = NAr1.12/0.12(0.5)t/t1/2
0.12/1.12 = (0.5)t/t1/2
T = T1/2(ln(0.12/1.12)/ln(0.5))

This gives me 4.1 billion years which isn't right.
 
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bmxicle said:

Homework Equations


N(t) = N(0)(1/2)t/t1/2

What is N(t)?

ehild
 
ah sorry i guess that's not normal notation. N(t) is just the number of decayed particles as a function of time, so in this case it's NAr
 
Do you think that the number of Ar atoms is No at the beginning of the decay, and it decreases with time? Is not it just the opposite? ehild
 
I don't think that's what i have up there--and if i do that would explain the wrong answer. The number NK0 ie. the initial number of potassium atoms in the rock when the lava cooled is going to be equal to the number of Argon atoms (atoms that underwent decay) plus the number of undecayed potassium atoms Nk.
 
It is the number of the potassium atoms that decreases exponentially, so your N(t) means the number of 40K atoms still present at time t.

ehild
 
Yup that's what I was doing wrong; don't know why i got so flipped around on that. Thanks for your help.
 

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