A Proof‐of‐Principle Study for <i>δ</i> <sup>15</sup> N Measurements of Aqueous Dissolved Nitrate With a Modified LC‐IRMS Interface

ABSTRACT Rationale The analysis of nitrogen isotopes in aqueous dissolved nitrate is an effective method for identifying pollution sources and offers the potential to study the nitrogen cycle. However, the measurement of nitrogen isotope ratios of nitrate still requires extensive sample preparation or derivatization. Methods In this study, a modified commercially available liquid chromatography–isotope ratio mass spectrometer (LC‐IRMS) interface is presented that enables automated measurement of δ 15 N signatures from nitrate by online reduction of nitrate in two consecutive steps. First, vanadium(III) chloride is used as a reducing agent to convert NO 3 − to N x O y under acidic conditions. The mix of nitrogen oxides is then transferred into a stream of helium and reduced to nitrogen (N 2 ) analysis gas via a hot copper reactor. Prior to the online conversion of aqueous nitrate into elemental nitrogen, the sample was chromatographically separated from potential matrix effects on a PGC column. Results Precision was achieved at a level below 1.4‰ by injecting 10 μL of 50 mg L −1 N, using five different nitrate standards and reference materials. These materials spanned a range of more than 180‰ in δ 15 N. To demonstrate the applicability of the method, we measured water samples from an enrichment experiment, where isotopically enriched ammonium chloride was administered into a small river over the course of 2 weeks. In contrary to our expectation, the δ 15 N values of river nitrate showed values between +0.4 ± 0.4‰ and +4.1 ± 0.3‰, varying over a small range of 3.7‰. Conclusions Our study showed that the measurement of nitrate nitrogen isotope ratios with a modified LC‐IRMS system is possible but that further modifications and improvements would be necessary for a robust and user‐friendly instrument.

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Publication Details

Journal
Rapid Communications in Mass Spectrometry
Published
2024-11-26
DOI
https://doi.org/10.1002/rcm.9950
Citations
1
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
0.35

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article

A Proof‐of‐Principle Study for δ 15 N Measurements of Aqueous Dissolved Nitrate With a Modified LC‐IRMS Interface

Klaus Kerpen, Torsten C. Schmidt, Christian K. Feld, Maik A. Jochmann et al.
1 citations
Rapid Communications in Mass Spectrometry
Groundwater and Isotope Geochemistry
0.35
article

A Proof‐of‐Principle Study for δ 15 N Measurements of Aqueous Dissolved Nitrate With a Modified LC‐IRMS Interface

Klaus Kerpen, Torsten C. Schmidt, Christian K. Feld, Maik A. Jochmann, Tobias Hesse, Felix Niemann, Julian Enß, Milen Nachev, Daniel Köster, Shaista Khaliq
article en
1 citations

Abstract

ABSTRACT Rationale The analysis of nitrogen isotopes in aqueous dissolved nitrate is an effective method for identifying pollution sources and offers the potential to study the nitrogen cycle. However, the measurement of nitrogen isotope ratios of nitrate still requires extensive sample preparation or derivatization. Methods In this study, a modified commercially available liquid chromatography–isotope ratio mass spectrometer (LC‐IRMS) interface is presented that enables automated measurement of δ 15 N signatures from nitrate by online reduction of nitrate in two consecutive steps. First, vanadium(III) chloride is used as a reducing agent to convert NO 3 − to N x O y under acidic conditions. The mix of nitrogen oxides is then transferred into a stream of helium and reduced to nitrogen (N 2 ) analysis gas via a hot copper reactor. Prior to the online conversion of aqueous nitrate into elemental nitrogen, the sample was chromatographically separated from potential matrix effects on a PGC column. Results Precision was achieved at a level below 1.4‰ by injecting 10 μL of 50 mg L −1 N, using five different nitrate standards and reference materials. These materials spanned a range of more than 180‰ in δ 15 N. To demonstrate the applicability of the method, we measured water samples from an enrichment experiment, where isotopically enriched ammonium chloride was administered into a small river over the course of 2 weeks. In contrary to our expectation, the δ 15 N values of river nitrate showed values between +0.4 ± 0.4‰ and +4.1 ± 0.3‰, varying over a small range of 3.7‰. Conclusions Our study showed that the measurement of nitrate nitrogen isotope ratios with a modified LC‐IRMS system is possible but that further modifications and improvements would be necessary for a robust and user‐friendly instrument.

Rapid Communications in Mass SpectrometryVol. 39(3)
Deutsche Gesetzliche Unfallversicherung (DE), Landesamt für Natur, Umwelt und Klima Nordrhein-Westfalen (DE), University of Duisburg-Essen (DE)
Deutsche Forschungsgemeinschaft
Clean water and sanitation
Openalex Percentile: Top 34%
Groundwater and Isotope Geochemistry
0.35
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