摘要
Rationale: The nitrogen isotopic ratio of nitrate (δ15N-NO3 − value) is a critical parameter for understanding nitrogen biogeochemical cycling in aquatic systems. Current approaches to the determination of δ15N-NO3 − values involve time-intensive handling procedures, the use of toxic chemicals and complicated microbial incubation. Methods: A chemical reduction method for measuring the δ15N-NO3 − values of aquatic samples was established. Nitrate was first quantitatively reduced to nitrite in a column filled with copper-coated cadmium granules, and the produced nitrite further reduced to nitrous oxide gas with hydroxylamine hydrochloride. The nitrogen isotope ratio of the produced nitrous oxide was measured using a continuous-flow isotope ratio mass spectrometer coupled with a purge and cryogenic trap system. Results: The optimized experimental conditions were: solution acidity, H+ concentration of 0.46 M, pH = 0.34; dosage of hydroxylamine, molar ratio of NH2OH to NO2 − of 4; reaction temperature, 45°C; and reaction time, 14–16 h. No salt effect was found for this method. The reproducibility of the δ15N-NO3 − value for the laboratory standard was better than 0.3‰ for long-term measurements (20 nmol NO3 − requirement). Conclusions: This method provides a reliable approach for the determination of δ15N-NO3 − values at natural abundance. It provides (1) high measurement accuracy, (2) ease of operation, (3) environmental-friendly procedure (less toxic regents used), and (4) suitability for both freshwater and saline water samples.
| 源语言 | 英语 |
|---|---|
| 文章编号 | e8804 |
| 期刊 | Rapid Communications in Mass Spectrometry |
| 卷 | 34 |
| 期 | 13 |
| DOI | |
| 出版状态 | 已出版 - 15 7月 2020 |
| 已对外发布 | 是 |
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