Problem set · Sharp, Principles of Stable Isotope Geochemistry, 1st ed. (2007) · Answers →
The working standard CO2 used on a certain mass spectrometer has a δ18O value of 38.72 per mil relative to VSMOW. If a sample of CO2 has a δ18O value of −14.57 per mil relative to this working standard,
[Worksheet constructed. Each row is one conversion with equation (2.3); in row 4, first convert the working standard to the VPDB scale in C4 using the KA and KB constants.]
Related interactive plots: delta algebra, scale conversions.
A 32S/34S ratio of 21.56 was reported for a sample of seawater sulfate in the early days of stable isotope geochemistry, when sulfur isotope compositions were reported as absolute ratios. Given that the absolute sulfur isotope ratio of Cañón Diablo Troilite (CDT) is 22.22, what is δ34S (CDT) of this sulfate sample?
[Worksheet constructed.]
There was a computer crash after an important nitrogen sample was analyzed on the mass spectrometer. No information was saved, other than the voltages of the masses 28 and 29 (N2) for the sample and the standard. (See the table in the worksheet.) Assuming that the reference gas has a δ15N value of −0.57‰ relative to AIR, what is the δ15N value of the sample relative to AIR?
[Worksheet constructed; voltages as printed.]
Vapor in oxygen isotope equilibrium with liquid water at 10 °C has a δ18O value of −13.42‰. What is the δ18O value of the water? α18O(l–v) = 1.0101 at 10 °C.
Quartz from the silica–carbonate rock in Trench 14 at the proposed disposal site for nuclear waste at Yucca Mountain, Nevada, has a δ18O value of 24.4‰. Given that
[Worksheet constructed.]
Related interactive plot: 1/T² thermometer.
The term ε is commonly defined for phases a and b as εa–b = 1000(αa–b − 1). For δb = δa − 10, show that the equality εa–b = δa − δb is valid when δ is close to zero, but invalid if δ is very different from 0 (e.g., 100‰).
[Worksheet constructed.]
Correct the following sentences:
Write an expression for the sulfur isotope exchange reaction between pyrite and sphalerite.
Derive equation (2.3), δX–B = δX–A + δA–B + 0.001·δX–A·δA–B, using the definitions of α and δ.
Give three isotopologues of water with the same mass.
In this chapter, it is stated that “A sample with a δ18O value of +19.7‰ has an 18O/16O ratio that is 19.7 per mil, or 1.97 percent, higher than that of the standard.” If the standard VSMOW has an 18O/16O ratio of 2005.20·10−6, calculate the 18O/16O ratio of the sample, using the stated expression. Show that you get the same answer as when you use the definition of delta, given in equation (2.1).
[Worksheet constructed.]
The Merriam–Webster dictionary gives the following definition of an isotope: “any of two or more species of atoms of a chemical element with the same atomic number and nearly identical chemical behavior but with differing atomic mass or mass number and different physical properties”. What is wrong with this definition? How could you improve on it?
For a laboratory experiment, you wish to make a liter of water with a δD value of +500‰, starting with a mixture of normal water (δD = −90‰) and pure D2O. How much D2O must you add to 1 liter of water?
[Worksheet constructed; the mole and density constants for the volume conversion are supplied as parameter cells and are not printed in the problem.]
Transcribed from Z. Sharp, Principles of Stable Isotope Geochemistry, 1st ed. (Pearson Prentice Hall, 2007), end-of-chapter problem set (published source). Reference-scale names are written VSMOW, VPDB and VCDT where the original used SMOW, PDB and CDT, with the original numerical constants unchanged; historical usages (e.g. Craig's definition of SMOW) are kept as printed.
The source PDF's text layer scrambles mathematics, so equations and some values were reconstructed during transcription. Bracketed notes and anything tagged reconstructed or check vs print are editorial (constructed), not part of the original, and the warn-tagged items should be verified against the print copy.