Calculating 238U/235U Ratio for Earth's Age

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In summary, you used the half-life of 238U and 235U to calculate the ratio of the number of nuclei at present to the number of nuclei at the time of the Earth's formation. You then used the equation N(t)=N0*e^-lambda*t to calculate the number of nuclei at a given time. You then attempted to solve for the ratios of 238U and 235U in the past by multiplying the numerator and denominator of the current ratio by the appropriate multipliers. However, you ran into difficulty because you did not take into account the last column of the table. You ended up with 199.54/60.46 for the ratio of U-238 and U-
  • #1
planesinspace
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Homework Statement


The Age of the Earth is 4.5 × 109 y. Use the information given in the following table to
calculate the ratio of the number of 238U nuclei at the present time to the number of 235U nuclei
at the time of the formation of the Earth.

Isotope Half-life Current natural abundance(%)
238U 4.468 ×109 y 99.274
235U 7.04 ×108 y 0.72




Homework Equations


I used T1/2= ln(2)/lamda to work out lambda for both 235 and 238Uranium.

I converted time in years to seconds by no. of years * 3.156x10^7 ( I saw it done in my book don't really understand it but anyway :) )

I used N(t)=N0*e^-lambda*t to work out the number of radioactive nuclei at a given time.


The Attempt at a Solution



So basically just using those two equations I came to
238U N(t) and present to be = 0.498N0
and 235UN(t) at beginning, (hence t=0) to be N0,
so i said the ratio is 0.498... However upon doing this I realized I didnt take into account the last column of the table given in the quetsion, and seeing as the question says taking into account the following information, I figure I have gone about this the wrong way...
Any help much appreciated :)
 
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  • #2
You have the current U-238/U-235 ratio of 99.274/0.72 . You can take this to represent a ratio of individual nuclei, rather than percentages. From the half-life information, you can figure out a multiplier for how many times more of each isotope there would have been 4.5 Gyr ago. If you multiply the numerator and denominator of your current ratio by the appropriate multipliers, you will have the ratio for that time in the past.
 
  • #3
Ok well to work out the multipliers, I am not sure I have done it right, for 238U I divided 4.5e9 by 4.468e9 to see how many times it goes into it, then i multiplied that by two? because were going backwards from halfing them... and i did the same for 235U, is this the right method? I ended up with 238U past : 199.970009 and 235U past : 9.204.
 
  • #4
You are correct in dividing 4.5·10^9 by 4.468·10^9 to find the number of U-238 half-lives, which is 1.0072. But you would then raise 2 to that power to get the number of times more U-238 that there was 4.5 Gyr ago. (The amount is halved with each passing half-life, so it would be doubled in going back into the past with each half-life.)

Similarly, you would find that there are 6.392 U-235 half-lives, so this is the power by which you would raise 2 to find the multiplier for the U-235 abundance for 4.5 Gyr in the past.

Your abundance ratio for 4.5 billion years ago will have a number close to 200 on top for U-238, but the denominator for U-235 will be substantially larger than 9...
 
  • #5
So I ened up with 199.54/60.46 for the ratio of them in the past.
So do I just put the number of u238 present (99.274) over 60.46?
It seems a pretty pointless calculation..
 

Related to Calculating 238U/235U Ratio for Earth's Age

1. How is the 238U/235U ratio used to determine the age of the Earth?

The 238U/235U ratio is used as a natural clock in geochemistry and geochronology studies. This ratio can be measured in rocks and minerals, and by comparing it to a known standard, scientists can calculate the age of the sample.

2. What is the significance of the 238U/235U ratio in Earth's history?

The 238U/235U ratio has remained relatively constant throughout Earth's history, making it a reliable tool for determining the age of the planet. This ratio is also used to study geological processes and the evolution of the Earth's crust and mantle.

3. How is the 238U/235U ratio measured?

The 238U/235U ratio is measured using a mass spectrometer, which separates isotopes based on their mass-to-charge ratio. The ratio is then calculated by comparing the intensities of the 238U and 235U isotopes in the sample.

4. Can the 238U/235U ratio be used to determine the age of other celestial bodies?

Yes, the 238U/235U ratio can be used to determine the age of other celestial bodies, such as the Moon and meteorites. However, the ratio may differ slightly due to different formation processes and radioactive decay rates.

5. Are there any limitations to using the 238U/235U ratio to calculate the age of the Earth?

Yes, there are some limitations to this method. For instance, if the sample has been subjected to extreme temperatures or chemical processes, the 238U/235U ratio may have been altered, leading to inaccurate age calculations. It is also important to use multiple samples and methods to ensure the accuracy of the results.

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