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Published February 18, 2020 | Supplemental Material
Journal Article Open

Stable Isotope Analysis of Intact Oxyanions Using Electrospray Quadrupole-Orbitrap Mass Spectrometry

Abstract

The stable isotopes of sulfate, nitrate, and phosphate are frequently used to study geobiological processes of the atmosphere, ocean, as well as land. Conventionally, the isotopes of these and other oxyanions are measured by isotope-ratio sector mass spectrometers after conversion into gases. Such methods are prone to various limitations on sensitivity, sample throughput, or precision. In addition, there is no general tool that can analyze several oxyanions or all the chemical elements they contain. Here, we describe a new approach that can potentially overcome some of these limitations based on electrospray hyphenated with Quadrupole Orbitrap mass spectrometry. This technique yields an average accuracy of 1–2‰ for sulfate δ³⁴S and δ¹⁸O and nitrate δ¹⁵N and δ¹⁸O, based on in-house and international standards. Less abundant variants such as δ¹⁷O, δ³³S, and δ³⁶S, and the ³⁴S–¹⁸O "clumped" sulfate can be quantified simultaneously. The observed precision of isotope ratios is limited by the number of ions counted. The counting of rare ions can be accelerated by removing abundant ions with the quadrupole mass filter. Electrospray mass spectrometry (ESMS) exhibits high-throughput and sufficient sensitivity. For example, less than 1 nmol sulfate is required to determine ¹⁸O/³⁴S ratios with 0.2‰ precision within minutes. A purification step is recommended for environmental samples as our proposed technique is susceptible to matrix effects. Building upon these initial provisions, new features of the isotopic anatomy of mineral ions can now be explored with ESMS instruments that are increasingly available to bioanalytical laboratories.

Additional Information

© 2020 American Chemical Society. Received: October 1, 2019; Accepted: January 21, 2020; Published: February 3, 2020. We thank the reviewers for comments. We are grateful for assistance provided by Roxana Eggleston-Rangel and Brett Lomenick, and thank George Rossmann as well as the companies Peñoles, Crimidesa, Saltex, Airborne Industrial Minerals, and Searles Valley Minerals for providing sulfates. This study was using ESMS instrumentation at the Proteome Exploration Laboratory (supported by Beckman Institute, and NIH 1S10OD02001301). C.N. is a fellow of the Hanse-Wissenschaftskolleg. The authors declare no competing financial interest.

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