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1 ES 6216 – Isotope Geochemistry Problem Set 2 Distributed 9/11 ...

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<strong>ES</strong> <strong>6216</strong> – <strong>Isotope</strong> <strong>Geochemistry</strong> <strong>Problem</strong> <strong>Set</strong> 2<br />

<strong>Distributed</strong> 9/<strong>11</strong>/12<br />

Due 9/25/12<br />

1. a. What magnetic field strength would be required to focus a beam of CO 2 + ions on<br />

a collector of a mass spectrometer whose analyzer tube as a radius of 31.45cm,<br />

assuming a voltage of 1000V?<br />

b. Change your magnetic field strength by -10%, what voltage puts the CO 2 ions<br />

into the collector?<br />

2. Estimate the Earth’s potassium content in ppm by weight from data for Ar in the atmosphere.<br />

[helpful numbers: mass atmosphere = 5.3 x 10 21 g, Ar = 1.29% of atmosphere]<br />

3. Calculate the K-Ar age for a feldspar sample which yielded the following data:<br />

K = 0.157 wt. %<br />

40 Ar = 7.37 x 10 -7 cc STP/g<br />

[helpful number: 1 mole of gas = 22.4 liters at STP]<br />

4. The data in the table below are for various mineral and chemical separates from the<br />

Shergotty meteorite, which is believed to be a fragment ejected from Mars. Shergotty has an<br />

igneous texture, and the age information from various radioactive decay systems is believed<br />

to reflect the time of crystallization of this material on Mars. Construct an isochron and<br />

determine the age and initial ratio of Shergotty. Express the intial ratio in terms of both molar<br />

ratios and ∈ Nd (t). Assuming that Sm/Nd for Mars is similar to that for Earth, what does this<br />

say about the source materials from which the Shergotty magma was derived? Use CHUR<br />

isotope ratios provided in lecture notes.<br />

Sample #<br />

147 Sm/ 144 Nd<br />

143 Nd/ 144 Nd<br />

1 0.31489 0.512420<br />

2 0.31510 0.512420<br />

3 0.29640 0.512370<br />

4 0.26490 0.512250<br />

5 0.07660 0.5<strong>11</strong>810<br />

6 0.37700 0.512530<br />

7 0.33600 0.512450<br />

8 0.28000 0.512227<br />

9 0.32070 0.512410<br />

10 0.14180 0.512010<br />

<strong>11</strong> 0.20930 0.512090<br />

5. What was the 235 U/ 238 U ratio when the earth formed 4.6 billion years ago?<br />

6. Assuming the activity ratio ( 234 U/ 238 U) in seawater has not changed over the past few hundred<br />

thousand years, what is the ( 234 U/ 238 U) activity ratio in an undisturbed coral with an age of<br />

85,000y and a U concentration of 2.8ppm?<br />

1


) Assuming that no Th was incorporated into its skeleton when it precipitated, how<br />

many 230 Th atoms does a 1g sample of this coral contain?<br />

c) The analytical precision for a U-Th age is typically limited by measurement of the<br />

230 Th atoms, and typically one is lucky to recover 0.05% of the total 230 Th atoms during<br />

a typical mass spec run. What will be a minimum 2σ relative error on the U-Th age for<br />

your 1g coral sample?<br />

7. Suppose a radioactive gaseous element in the atmosphere has a half-life of 6yrs. Its daughter,<br />

also radioactive, has a half-life of one month. Because the daughter is not gaseous, it adsorbs<br />

onto aerosol particles and is removed by physical processes, mainly precipitation. If the<br />

activity ratio for these two isotopes (daughter/parent) in the atmosphere is observed to be 0.3<br />

in steady state, what is the lifetime of the daughter with respect to physical removal from the<br />

atmosphere?<br />

8. The following activity ratios were measured in a manganese nodule. Estimate the growth rate<br />

of the nodule, assuming that the amount of U-supported 230 Th is negligible.<br />

Depth (mm)<br />

230 Th/ 232 Th<br />

0-0.3 43.7± 1.8<br />

0.3-0.5 26.2 ± 0.6<br />

0.5-0.85 10.4 ± 0.3<br />

2

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