How Do Geologists Determine the Age of Rock Samples Using Isotopic Ratios?

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Discussion Overview

The discussion revolves around the methods geologists use to determine the age of rock samples through isotopic ratios and radioactive decay. Participants explore the calculations involved in using isotopic ratios of rubidium-strontium and uranium-lead systems, addressing a specific homework problem related to these concepts.

Discussion Character

  • Homework-related
  • Mathematical reasoning
  • Technical explanation

Main Points Raised

  • One participant outlines the process of calculating rock ages using isotopic ratios and decay rates, mentioning specific isotopes and their half-lives.
  • Another participant suggests that the original poster may be focusing on the wrong isotopes in their calculations and encourages deriving equations for the decay products over time.
  • There is a mention of converting half-lives to mean lives as a valid approach in the calculations.
  • One participant expresses confusion about the ratios being used and indicates they are still arriving at the same incorrect answer despite attempts to clarify their approach.
  • Another participant requests that the original poster show all working and reasoning to better understand the errors in their calculations.
  • A later reply indicates that the original poster eventually figured out their mistake, suggesting a misinterpretation of the ratios involved in the problem.
  • One participant acknowledges a slight mistake in their earlier comments regarding the ratios and reflects on the confusion caused by the order of the ratios used in the calculations.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the correct approach initially, as there is confusion regarding the isotopes and ratios. However, the original poster eventually resolves their misunderstanding, indicating some level of agreement on the need for clarity in the calculations.

Contextual Notes

There are limitations in the discussion regarding the assumptions made about the initial quantities of isotopes and the specific ratios used in the calculations, which remain unresolved.

molly16
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Homework Statement


Geologists are able to calculate ages of rock samples through measurements of certain isotopic rations combined with known radioactive decay rates (all such decays being considered to adhere to 1st order kinetic rate laws). Two such processes leading to stable isotopes are:

87Rb --> 87Sr
238Ur --> 206Pb

Half life of 87Rb is 4.90x10^10 years while half life of 238Ur is 4.51x10^9 years.The isotopic ratios are:

87Sr/87Rb = 0.051
206Pb/238Ur = 0.71

Assuming the time the rock was formed it contained no 87Sr or 206Pb Calculate the age of the rock indicated by the isotopic ratios.

Homework Equations



dA/dt = -k[A]

ln(A/Ao) = -kt

t1/2 = ln(2)/k

The Attempt at a Solution



I tried solving for the rate constant using t1/2 = ln(2)/k
and rearranging it to k = ln(2)/t1/2 = 1.41 x 10^-11

Then to solve for the time for the decay of 87Rb I plugged the value into the equation ln(A/Ao) = -kt

ln (A/Ao) = ln (87Sr/87Rb) = ln (0.051) = -(1.41x10^-11)t

then I solved for t which is t = 2.1x10^11 years for the decay of the 87Rb
but the answer is supposed to be t = 3.517x10^9 years

Can someone please explain this question to me and tell me what I'm doing wrong?
Thanks!
 
Last edited:
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I tried solving for the rate constant using t1/2 = ln(2)/k
... converting half-lives to mean lives, good.

Can someone please explain this question to me and tell me what I'm doing wrong?
If you have isotope X' and Y' and they decay to X and Y respecively, but at different rates, then, from the decay equations of X' and Y' you can get equations for how the amounts of X and Y change over time ... and thus how the ratio of X:Y changes with time.

You are given the ratio X:Y, and initial quantities of X and Y, and you have to find the time that has elapsed to turn the initial quantities into the final ratio.

I suspect you have been concentrating on the wrong isotope - on X':Y' instead of X:Y ... start by deriving the equation for the quantity of each decay product as a function of time.
 
Simon Bridge said:
... converting half-lives to mean lives, good.

I suspect you have been concentrating on the wrong isotope - on X':Y' instead of X:Y ... start by deriving the equation for the quantity of each decay product as a function of time.

so then
Ao = A (1-e^-kt)
Ao/A = 1-e^-kt
ln (Ao/A) = +kt

but I still get the same answer??
 
Please show all your working with your reasoning at each stage.
 
Simon Bridge said:
Please show all your working with your reasoning at each stage.

Ahh never mind I figured it out. Thanks.
 
Well done :)

For others googling here later:
I made a slight mistake earlier - you are given X:X' rather than X:Y.
I think your repeated mistake was that you were putting the ration as A/Ao or Ao/A... which was similar to my misreading.
 

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