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Chemical conversion of nitrate and nitrite to nitrous oxide for nitrogen and oxygen isotopic analysis in freshwater and seawater

机译:将硝酸盐和亚硝酸盐化学转化为一氧化二氮,以分析淡水和海水中的氮和氧同位素

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We present a novel method for nitrogen and oxygen natural isotopic abundance analysis of nitrate and nitrite of seawater and freshwater at environmental concentrations. The method involves the reduction of nitrate to nitrite using spongy cadmium with further reduction to nitrous oxide using sodium azide in an acetic acid buffer. For separate nitrite analysis, the cadmium reduction step is simply bypassed. Nitrous oxide is purged from the water sample and trapped cryogenically using an automated system with subsequent release into a gas chromatography column. The isolated nitrous oxide is then analyzed on a continuous flow isotope ratio mass spectrometer via an open split. This paper describes the basic protocol and reaction conditions required to obtain reproducible natural abundance level nitrogen and oxygen isotopic ratios from nitrate, nitrite, or both, and the results obtained to support these conclusions. A standard deviation less than 0.2 parts per thousand for nitrogen and 0.5 parts per thousand for oxygen was found for nitrate samples ranging in concentration from 40 to 0.5 mu M (better for nitrite), with a blank of 2 nmol for 50-mL samples. Nitrogen and oxygen isotopic fractionation and oxygen atom exchange were consistent within each batch of analysis. There was no interference from any seawater matrixes. Only one other method published to date can measure the nitrate oxygen isotopic abundance in seawater and none that do so for nitrite alone in the presence of nitrate. This method may prove to be simpler, faster, and obtain isotopic information for lower concentrations of nitrate and nitrite than other methods.
机译:我们提出了一种在环境浓度下对海水和淡水中的硝酸盐和亚硝酸盐进行氮和氧自然同位素丰度分析的新方法。该方法涉及使用海绵状镉将硝酸盐还原为亚硝酸盐,并使用叠氮化钠在乙酸缓冲液中进一步还原为一氧化二氮。对于单独的亚硝酸盐分析,只需跳过镉还原步骤。从水样本中清除一氧化二氮,并使用自动化系统将其低温捕集,然后释放到气相色谱柱中。然后在连续流同位素比质谱仪上通过开放式分流器对分离出的一氧化二氮进行分析。本文介绍了从硝酸盐,亚硝酸盐或两者中获得可重现的自然丰度水平的氮和氧同位素比所需的基本方案和反应条件,并获得了支持这些结论的结果。对于浓度范围为40至0.5μM(对于亚硝酸盐而言更好)的硝酸盐样品,发现氮的标准偏差小于千分之0.2,对于氧气而言,其标准偏差小于千分之千(对于亚硝酸盐而言更好),对于50 mL样品,空白为2 nmol。在每批分析中,氮和氧同位素分馏和氧原子交换均一致。没有任何海水基质的干扰。迄今为止,只有一种其他方法可以测量海水中硝酸盐氧同位素的丰度,而没有任何一种方法可以单独测量存在硝酸盐的亚硝酸盐。与其他方法相比,该方法可能被证明更简单,更快速,并且可以获得较低浓度的硝酸盐和亚硝酸盐的同位素信息。

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