Carlos Abad, Dennis Jegielka, Allen Aloysius and Sebastian Recknagel
{"title":"同位素稀释光谱法分析柏林地表水中硝酸盐和亚硝酸盐的痕量痕量分析及其应用","authors":"Carlos Abad, Dennis Jegielka, Allen Aloysius and Sebastian Recknagel","doi":"10.1039/D5JA00252D","DOIUrl":null,"url":null,"abstract":"<p >Accurate nitrate and nitrite data support water-quality regulation, yet routine methods rely on external calibration and rarely achieve SI traceability. We report a calibration-free determination of nitrate and nitrite by combining isotope dilution with high-resolution continuum-source graphite furnace molecular absorption spectrometry (ID-HR-CS-GF-MAS). A <small><sup>15</sup></small>N-enriched nitrate spike (its concentration verified by reverse isotope dilution against the standard reference material NIST 3185) provides the SI link, and it is gravimetrically added to samples; nitrate and residual nitrite are converted in situ to nitric oxide (NO), whose 215 nm band is recorded at a pixel resolution of <em>λ</em>/Δ<em>λ</em> ≈ 140 000. The 0.2127 nm shift between <small><sup>14</sup></small>NO and <small><sup>15</sup></small>NO electronic spectra is resolved, and a three-latent-variable partial least squares regression model yields the <small><sup>15</sup></small>N/<small><sup>14</sup></small>N ratio with 0.3% precision. Instrumental LoD values of 4.8 ng (<small><sup>14</sup></small>N) and 3.2 ng (<small><sup>15</sup></small>N) translate to a method LoD of 4.8 ng of nitrogen (equivalent to 1.05 mg L<small><sup>−1</sup></small> NO<small><sub>3</sub></small><small><sup>−</sup></small> for a 20 μL aliquot). The furnace program allows for successive drying/pyrolysis loops, so additional 20 μL aliquots can be layered onto the graphite platform. Alternatively, a 10 mL anion-exchange solid-phase extraction step concentrates nitrate and nitrite fivefold, allowing for the analysis of even lower sample concentrations. Results for four certified reference materials (2.9 to 1000 mg L<small><sup>−1</sup></small> NO<small><sub>3</sub></small><small><sup>−</sup></small>) agreed with certified values, giving relative expanded uncertainties of 2 to 4%. Analysis of twenty Berlin surface-water samples revealed concentrations ranging from 0.10 to 7.3 mg L<small><sup>−1</sup></small> NO<small><sub>3</sub></small><small><sup>−</sup></small>, indicating that the Panke River and Teltow Canal are the primary sources of nitrogen. ID-HR-CS-GF-MAS thus delivers ID-MS-level accuracy in a few minutes per run with bench-top optics, and, with optional on-platform or SPE pre-concentration, extends SI-traceable nitrate/nitrite monitoring into the low-ng regime.</p>","PeriodicalId":81,"journal":{"name":"Journal of Analytical Atomic Spectrometry","volume":" 10","pages":" 2692-2701"},"PeriodicalIF":3.1000,"publicationDate":"2025-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://pubs.rsc.org/en/content/articlepdf/2025/ja/d5ja00252d?page=search","citationCount":"0","resultStr":"{\"title\":\"SI-traceable total analysis of nitrate and nitrite by isotope dilution optical spectroscopy and its application to Berlin surface waters\",\"authors\":\"Carlos Abad, Dennis Jegielka, Allen Aloysius and Sebastian Recknagel\",\"doi\":\"10.1039/D5JA00252D\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >Accurate nitrate and nitrite data support water-quality regulation, yet routine methods rely on external calibration and rarely achieve SI traceability. We report a calibration-free determination of nitrate and nitrite by combining isotope dilution with high-resolution continuum-source graphite furnace molecular absorption spectrometry (ID-HR-CS-GF-MAS). A <small><sup>15</sup></small>N-enriched nitrate spike (its concentration verified by reverse isotope dilution against the standard reference material NIST 3185) provides the SI link, and it is gravimetrically added to samples; nitrate and residual nitrite are converted in situ to nitric oxide (NO), whose 215 nm band is recorded at a pixel resolution of <em>λ</em>/Δ<em>λ</em> ≈ 140 000. The 0.2127 nm shift between <small><sup>14</sup></small>NO and <small><sup>15</sup></small>NO electronic spectra is resolved, and a three-latent-variable partial least squares regression model yields the <small><sup>15</sup></small>N/<small><sup>14</sup></small>N ratio with 0.3% precision. Instrumental LoD values of 4.8 ng (<small><sup>14</sup></small>N) and 3.2 ng (<small><sup>15</sup></small>N) translate to a method LoD of 4.8 ng of nitrogen (equivalent to 1.05 mg L<small><sup>−1</sup></small> NO<small><sub>3</sub></small><small><sup>−</sup></small> for a 20 μL aliquot). The furnace program allows for successive drying/pyrolysis loops, so additional 20 μL aliquots can be layered onto the graphite platform. Alternatively, a 10 mL anion-exchange solid-phase extraction step concentrates nitrate and nitrite fivefold, allowing for the analysis of even lower sample concentrations. Results for four certified reference materials (2.9 to 1000 mg L<small><sup>−1</sup></small> NO<small><sub>3</sub></small><small><sup>−</sup></small>) agreed with certified values, giving relative expanded uncertainties of 2 to 4%. Analysis of twenty Berlin surface-water samples revealed concentrations ranging from 0.10 to 7.3 mg L<small><sup>−1</sup></small> NO<small><sub>3</sub></small><small><sup>−</sup></small>, indicating that the Panke River and Teltow Canal are the primary sources of nitrogen. ID-HR-CS-GF-MAS thus delivers ID-MS-level accuracy in a few minutes per run with bench-top optics, and, with optional on-platform or SPE pre-concentration, extends SI-traceable nitrate/nitrite monitoring into the low-ng regime.</p>\",\"PeriodicalId\":81,\"journal\":{\"name\":\"Journal of Analytical Atomic Spectrometry\",\"volume\":\" 10\",\"pages\":\" 2692-2701\"},\"PeriodicalIF\":3.1000,\"publicationDate\":\"2025-08-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://pubs.rsc.org/en/content/articlepdf/2025/ja/d5ja00252d?page=search\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Analytical Atomic Spectrometry\",\"FirstCategoryId\":\"92\",\"ListUrlMain\":\"https://pubs.rsc.org/en/content/articlelanding/2025/ja/d5ja00252d\",\"RegionNum\":2,\"RegionCategory\":\"化学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"CHEMISTRY, ANALYTICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Analytical Atomic Spectrometry","FirstCategoryId":"92","ListUrlMain":"https://pubs.rsc.org/en/content/articlelanding/2025/ja/d5ja00252d","RegionNum":2,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"CHEMISTRY, ANALYTICAL","Score":null,"Total":0}
引用次数: 0
摘要
准确的硝酸盐和亚硝酸盐数据支持水质调节,但常规方法依赖外部校准,很少实现SI可追溯性。我们报道了用同位素稀释与高分辨率连续源石墨炉分子吸收光谱法(ID-HR-CS-GF-MAS)相结合的免校准测定硝酸盐和亚硝酸盐的方法。15n富集的硝酸盐峰(其浓度通过对标准参考物质NIST 3185的反向同位素稀释验证)提供SI链接,并以重量方式添加到样品中;硝酸盐和残余亚硝酸盐在原位转化为一氧化氮(NO),其215 nm波段以λ/Δλ≈140 000的像素分辨率记录。利用三潜变量偏最小二乘回归模型求解了14NO和15NO之间的0.2127 nm位移,得到了精度为0.3%的15N/14N比值。4.8 ng (14N)和3.2 ng (15N)的仪器LoD值转化为4.8 ng氮的方法LoD(相当于1.05 mg L−1 NO3−对于20 μL的溶液)。熔炉程序允许连续的干燥/热解循环,因此额外的20 μL等分可以分层到石墨平台上。另外,10ml阴离子交换固相萃取步骤浓缩硝酸盐和亚硝酸盐五倍,允许分析更低的样品浓度。四种认证标准物质(2.9 ~ 1000 mg L−1 NO3−)的结果与认证值一致,相对扩展不确定度为2% ~ 4%。对柏林20个地表水样本的分析显示,NO3 -的浓度在0.10至7.3 mg L - 1之间,表明潘克河和泰尔托运河是氮的主要来源。因此,ID-HR-CS-GF-MAS可以在几分钟内提供id - ms级的精度,并且可以选择平台上或SPE预浓缩,将si可追溯的硝酸盐/亚硝酸盐监测扩展到低浓度状态。
SI-traceable total analysis of nitrate and nitrite by isotope dilution optical spectroscopy and its application to Berlin surface waters
Accurate nitrate and nitrite data support water-quality regulation, yet routine methods rely on external calibration and rarely achieve SI traceability. We report a calibration-free determination of nitrate and nitrite by combining isotope dilution with high-resolution continuum-source graphite furnace molecular absorption spectrometry (ID-HR-CS-GF-MAS). A 15N-enriched nitrate spike (its concentration verified by reverse isotope dilution against the standard reference material NIST 3185) provides the SI link, and it is gravimetrically added to samples; nitrate and residual nitrite are converted in situ to nitric oxide (NO), whose 215 nm band is recorded at a pixel resolution of λ/Δλ ≈ 140 000. The 0.2127 nm shift between 14NO and 15NO electronic spectra is resolved, and a three-latent-variable partial least squares regression model yields the 15N/14N ratio with 0.3% precision. Instrumental LoD values of 4.8 ng (14N) and 3.2 ng (15N) translate to a method LoD of 4.8 ng of nitrogen (equivalent to 1.05 mg L−1 NO3− for a 20 μL aliquot). The furnace program allows for successive drying/pyrolysis loops, so additional 20 μL aliquots can be layered onto the graphite platform. Alternatively, a 10 mL anion-exchange solid-phase extraction step concentrates nitrate and nitrite fivefold, allowing for the analysis of even lower sample concentrations. Results for four certified reference materials (2.9 to 1000 mg L−1 NO3−) agreed with certified values, giving relative expanded uncertainties of 2 to 4%. Analysis of twenty Berlin surface-water samples revealed concentrations ranging from 0.10 to 7.3 mg L−1 NO3−, indicating that the Panke River and Teltow Canal are the primary sources of nitrogen. ID-HR-CS-GF-MAS thus delivers ID-MS-level accuracy in a few minutes per run with bench-top optics, and, with optional on-platform or SPE pre-concentration, extends SI-traceable nitrate/nitrite monitoring into the low-ng regime.