Meteoric Radiation Decay Question Check

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SUMMARY

The discussion revolves around estimating the age of a meteorite sample using the decay of radioactive potassium-40 (40-K) into argon-40 (40-Ar). The half-life of 40-K is established at 1.3 billion years, and the decay ratio indicates that for every 100 40-K nuclei, 11 decay into 40-Ar. The correct formula to use is N(40-Ar + 40-Ca)/N(40-K) = e^(λt_Formation) - 1, where the ratio of argon to calcium is 11:89. The final conclusion is that the initial calculation of 1.3 billion years was incorrect due to the misinterpretation of the decay ratio.

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  • Understanding of radioactive decay and half-life concepts
  • Familiarity with the decay chain of potassium-40 to argon-40 and calcium-40
  • Knowledge of exponential functions and natural logarithms
  • Ability to manipulate equations involving ratios and decay constants
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  • Study the principles of radioactive dating using potassium-argon methods
  • Learn about the mathematical derivation of decay equations in nuclear physics
  • Explore the implications of half-life in geological time scales
  • Investigate the significance of isotopic ratios in geochronology
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Students in geology, physics, or chemistry, particularly those studying radiometric dating methods and the principles of radioactive decay.

TFM
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Homework Statement



I have done a question, but I am not sure wether the answer I got is correct:

A meteorite sampleis found to have some 40-Ar trapped in a small volume deep inside it, which also contains exactly the same amount of radioactive 40-K. Assuming that when the meteorite was formed there was no trapped argon, that every 100 40-K nuclei decay into 11 40-Argon nuclei (and 89 40-Ca, which play no further part in this question) and that the half life of 40-K is 1.3x10^9 years, estimate the age of the meteorite in years.

Homework Equations



\frac{N(^{40}Ar)}{N()^{40}K} = e^{\lambda t_{Formation}} - 1

t_{1/2} = \frac{ln2}{\lambda}

The Attempt at a Solution



Rearranging the formula, I get:

\frac{N(^{40}Ar)}{N(^{40}K)} = e^{(\frac{ln2}{t_{1/2}}) t_{Formation}} - 1

I considered the ratio to be 50:50, or 1:1, since there was equal numbers. Put in all the variables into the above equation, and I got a nice number of 1.3 billion years. It seems a fair enough answer.

My problem is, I don't seem to have taken into consideration the fact that only 11 of the 100 potassium atoms decay into Argon. and the fact that the time is the half-life shows that this should be the answer when the Potassium only forms argon, since half-life is the time for half the atoms to decay, it means from the half that have decaysed, really, only 11% should be argon.

Have I made a mistake somewhere/used the wrong formula?

TFM
 
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TFM said:
… since half-life is the time for half the atoms to decay, it means from the half that have decaysed, really, only 11% should be argon.

Hi TFM! :smile:

The question isn't very clear, but I think you're right: if you start with 200 atoms of K, then after one half-life you have 100 of K, 11 of Ar, and 89 of Ca. :smile:

So your \frac{N(^{40}Ar)}{N()^{40}K} = e^{\lambda t_{Formation}} - 1

should say \frac{N(^{40}Ar\,+\,^{40}Ca)}{N()^{40}K} = e^{\lambda t_{Formation}} - 1,

and then you use N(Ar)/N(Ca) = 11/89. :smile:
 

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