Oxygen isotope exchange with quartz during pyrolysis of silver sulfate and silver nitrate

Andrew J Schauer; Shelley A Kunasek; Eric D Sofen; Joseph Erbland; Joel Savarino; Ben W Johnson; Helen M Amos; Robina Shaheen; Mariana Abaunza; Terri L Jackson; Mark H Thiemens; Becky Alexander

doi:10.1002/rcm.6332

Oxygen isotope exchange with quartz during pyrolysis of silver sulfate and silver nitrate

Rapid Commun Mass Spectrom. 2012 Sep 30;26(18):2151-7. doi: 10.1002/rcm.6332.

Authors

Andrew J Schauer¹, Shelley A Kunasek, Eric D Sofen, Joseph Erbland, Joel Savarino, Ben W Johnson, Helen M Amos, Robina Shaheen, Mariana Abaunza, Terri L Jackson, Mark H Thiemens, Becky Alexander

Affiliation

¹ Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA. aschauer@uw.edu

PMID: 22886811
DOI: 10.1002/rcm.6332

Abstract

Rationale: Triple oxygen isotopes of sulfate and nitrate are useful metrics for the chemistry of their formation. Existing measurement methods, however, do not account for oxygen atom exchange with quartz during the thermal decomposition of sulfate. We present evidence for oxygen atom exchange, a simple modification to prevent exchange, and a correction for previous measurements.

Methods: Silver sulfates and silver nitrates with excess (17)O were thermally decomposed in quartz and gold (for sulfate) and quartz and silver (for nitrate) sample containers to O(2) and byproducts in a modified Temperature Conversion/Elemental Analyzer (TC/EA). Helium carries O(2) through purification for isotope-ratio analysis of the three isotopes of oxygen in a Finnigan MAT253 isotope ratio mass spectrometer.

Results: The Δ(17)O results show clear oxygen atom exchange from non-zero (17)O-excess reference materials to zero (17)O-excess quartz cup sample containers. Quartz sample containers lower the Δ(17)O values of designer sulfate reference materials and USGS35 nitrate by 15% relative to gold or silver sample containers for quantities of 2-10 µmol O(2).

Conclusions: Previous Δ(17)O measurements of sulfate that rely on pyrolysis in a quartz cup have been affected by oxygen exchange. These previous results can be corrected using a simple linear equation (Δ(17)O(gold) = Δ(17)O(quartz) * 1.14 + 0.06). Future pyrolysis of silver sulfate should be conducted in gold capsules or corrected to data obtained from gold capsules to avoid obtaining oxygen isotope exchange-affected data.