National Research Council of Canada, 1200 Montreal Road, K1A 0R6 Ottawa, Ontario, Canada.
Consiglio Nazionale delle Ricerche (CNR), Istituto di Chimica dei Composti Organometallici, UOS di Pisa, Via Moruzzi 1, 56124 Pisa, Italy.
J Chromatogr A. 2018 Sep 28;1569:193-199. doi: 10.1016/j.chroma.2018.07.055. Epub 2018 Jul 18.
In this study, we propose a novel approach for the determination of total dissolved nitrogen (TDN) in seawater combining high-precision isotope dilution GC-MS with persulfate digestion. A 2 mL sample aliquot was digested with an alkaline solution of persulfate to convert nitrogen containing compounds to nitrate. Digested samples were spiked with NO internal standard and treated with aqueous triethyloxonium to convert the analyte into volatile EtONO. This derivative was readily separated from the matrix under gaseous form and could be sampled from the headspace before GC-MS analysis. The resulting chromatograms showed a stable flat baseline with EtONO as the only eluting peak (retention time 2.75 min on a DB 5.625 column). Such an approach provides specificity and obviates the shortcomings of current detection methods employed to analyze seawater samples after digestion with persulfate. In negative chemical ionization mode, the method reached a detection limit of 0.5 μmol/kg TDN (7 ng/g N) and could be applied to quantify seawater samples with 1-25 μmol/kg TDN. On the upper end of the range, quantitation could be repeated within 1%, whereas on a 6 μmol/kg TDN sample repeatability was 2.3% on eight measurements. The method was employed in two proficiency testing exercises providing results in agreement with consensus values. We investigated the impact of reagent blank and we implemented a blank-matching optimal design to account for such contribution. Finally, we performed a study on the yield of persulfate oxidation for organic and inorganic nitrogen compounds typically present in seawater. Whilst nitrite and ammonium are fully converted to nitrate, more complex organic molecules showed recoveries varying from 70% to 100%.
在本研究中,我们提出了一种新的方法来测定海水中的总溶解氮(TDN),该方法结合了高精度同位素稀释 GC-MS 和过硫酸盐消解。取 2ml 样品与过硫酸盐的碱性溶液混合消解,将含氮化合物转化为硝酸盐。消解后的样品用 NO 内标物进行标记,并与三乙氧基氧化铵水溶液反应,将分析物转化为挥发性的 EtONO。该衍生物在气态下很容易与基质分离,并可在气相色谱-质谱分析前从顶空采样。所得色谱图显示出稳定的平坦基线,只有 EtONO 作为唯一洗脱峰(在 DB-5 625 柱上保留时间为 2.75 分钟)。这种方法提供了特异性,并避免了当前用于分析过硫酸盐消解后的海水样品的检测方法的缺点。在负离子化学电离模式下,该方法的检测限达到 0.5 μmol/kg TDN(7 ng/g N),可用于定量 1-25 μmol/kg TDN 的海水样品。在该范围内的较高端,定量可以在 1%以内重复,而在 6 μmol/kg TDN 样品上,八个测量值的重复性为 2.3%。该方法在两项能力验证测试中得到了应用,结果与共识值一致。我们研究了试剂空白的影响,并实施了空白匹配最佳设计以考虑到这种贡献。最后,我们对过硫酸盐氧化有机和无机氮化合物的产率进行了研究,这些化合物通常存在于海水中。亚硝酸根和铵盐完全转化为硝酸盐,而更复杂的有机分子的回收率则在 70%至 100%之间变化。