利用螯合树脂和电感耦合等离子体质谱法测定海水中的氧化还原钒V(IV)和V(V)

IF 2.3 3区 地球科学 Q2 OCEANOGRAPHY
Erika Kurahashi, Sandra Poehle, Andrea Koschinsky
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引用次数: 0

摘要

使用螯合树脂 Chelex-100 进行固相萃取,开发了一种改进的离线分离海水中钒氧化还原物种 V(V) 和 V(IV) 的方法。对柱形、洗脱液、洗脱体积、样品 pH 值和流速进行了测试和优化,从而建立了一种简单的离线分离方法。利用电感耦合等离子体质谱法(ICP-MS)和使用氦气的动能辨别模式(KED)进行分析,精确测定了盐基溶液中的氧化还原钒。掺杂了 V(V) 和 V(IV) 的溶液中,V(V) 的平均回收率为 92%,V(IV) 的平均回收率为 96%。在 0.6 摩尔/千克的氯化钠溶液中,V(V) 的方法检测限为 0.87 毫摩尔/千克,V(IV) 的方法检测限为 0.47 毫摩尔/千克。对海水中氧化还原物种 V(IV)在有氧室和无氧室中的稳定性测试表明,V(IV)物种在海水中可保存 24 小时以上,在正常氧化环境中可再保存 14 天。我们开发了一种无需调节样品溶液 pH 值的方法,从而降低了改变两种氧化还原物种天然组分的风险。我们将所提出的方法应用于 GEOTRACES GA08 研究巡航期间在东南大西洋采集的开阔海域和沿岸海水样本。在纳米比亚海岸附近(水深 43-2997 米)的样本中发现,V(V) 浓度为 29-37 nmol/kg,V(IV) 浓度为 1.5-2.2 nmol/kg。与近海海水相比,在含氧量极低的近海沿岸海水中检测到的 V(IV)浓度更高(水深 200 米处为 2.4 nmol/kg)。新获得的结果表明,不仅溶解氧浓度,生物地球化学参数(如生物活性)也可能在解释海水中 V 氧化还原物种的分布方面发挥重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determination of vanadium redox species V(IV) and V(V) in seawater using chelating resin and inductively coupled plasma mass spectrometry

An improved off-line separation method of vanadium redox species V(V) and V(IV) in seawater using a solid phase extraction with chelating resin Chelex-100 was developed. Column shape, eluting solution, elution volume, pH of sample, and flow rate were tested and optimized to establish a simple offline separation method. Analyses with inductively coupled plasma mass spectrometry (ICP-MS) combining with a Kinetic Energy Discrimination mode (KED) using helium gas achieved precise determination of vanadium redox species in saline matrix solutions. Average recovery of solutions doped with both V(V) and V(IV) was 92% for V(V) and 96% for V(IV). The method detection limit was 0.87 nmol/kg for V(V) and 0.47 nmol/kg for V(IV) obtained from 0.6 mol/kg NaCl solution. Stability tests of redox species V(IV) in seawater with/without an aerobic chamber revealed that V(IV) species were preserved in seawater for over 24 h and possibly further 14 days in normal oxidizing atmosphere. We developed a method that does not require pH adjustment of sample solution, which reduces the risk of changing the natural fractions of both redox species. The proposed method was applied to selected samples from open ocean and coastal seawater collected in the South-East Atlantic Ocean during GEOTRACES research cruise GA08. Concentrations of 29–37 nmol/kg of V(V) and 1.5–2.2 nmol/kg of V(IV) in samples off-shore the Namibian coast (43–2997 m water depth) were found. Higher concentrations of V(IV) were detected in near-shore coastal seawater characterized by very low oxygen content (2.4 nmol/kg at 200 m water depth) relative to those from off-shore seawater. The newly obtained results suggest that not only dissolved oxygen concentration but also biogeochemical parameters (e.g. biological activity) may play an important role to explain the distribution of redox species of V in seawater.

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来源期刊
CiteScore
4.60
自引率
4.20%
发文量
144
审稿时长
18.3 weeks
期刊介绍: Deep-Sea Research Part I: Oceanographic Research Papers is devoted to the publication of the results of original scientific research, including theoretical work of evident oceanographic applicability; and the solution of instrumental or methodological problems with evidence of successful use. The journal is distinguished by its interdisciplinary nature and its breadth, covering the geological, physical, chemical and biological aspects of the ocean and its boundaries with the sea floor and the atmosphere. In addition to regular "Research Papers" and "Instruments and Methods" papers, briefer communications may be published as "Notes". Supplemental matter, such as extensive data tables or graphs and multimedia content, may be published as electronic appendices.
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