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通过化学转化为一氧化二氮对有机氮的稳定氮同位素组成进行灵敏测定。

Sensitive determinations of stable nitrogen isotopic composition of organic nitrogen through chemical conversion into N2O.

作者信息

Tsunogai Urumu, Kido Tadasuke, Hirota Akinari, Ohkubo Satoru B, Komatsu Daisuke D, Nakagawa Fumiko

机构信息

Earth and Planetary System Science, Faculty of Science, Hokkaido University, N10W8 Kita-ku, Sapporo, Hokkaido 060-0810, Japan.

出版信息

Rapid Commun Mass Spectrom. 2008;22(3):345-54. doi: 10.1002/rcm.3368.

Abstract

We present a method for high-sensitivity nitrogen isotopic analysis of particulate organic nitrogen (PON) in seawater and freshwater, for the purpose of determining the aquatic nitrogen fixation rate through the 15N2 tracer technique for samples that contain a low abundance of organisms. The method is composed of the traditional oxidation/reduction methods, such as the oxidation of PON to nitrate (NO3*) using persulfate, the reduction of NO3* to nitrite (NO2*) using spongy cadmium, and further reduction of NO2* to nitrous oxide (N2O) using sodium azide. Then, N2O is purged from the water and trapped cryogenically with subsequent release into a gas chromatography column to analyze the stable nitrogen isotopic composition using continuous-flow isotope ratio mass spectrometry (CF-IRMS) by simultaneously monitoring the NO+ ion currents at masses 30, 31, and 32. The nitrogen isotopic fractionation was consistent within each batch of analysis. The standard deviation of sample measurements was less than 0.3 per thousand for samples containing PON of more than 50 nmolN, and 0.5 per thousand for those of more than 20 nmolN, by subtracting the contribution of blank nitrogen, 8 +/- 2 nmol at final N2O. By using this method, we can determine delta15N for lower quantities of PON better than by other methods, so we can reduce the quantities of water samples needed for incubation to determine the nitrogen fixation rate. In addition, we can expand the method to determine the nitrogen isotopic composition of organic nitrogen in general, such as that of total dissolved nitrogen (TDN; sum of NO3*, NO2*, ammonium, and DON), by applying the method to filtrates.

摘要

我们提出了一种用于海水和淡水中颗粒有机氮(PON)高灵敏度氮同位素分析的方法,目的是通过15N2示踪技术,针对生物丰度较低的样品测定水生固氮率。该方法由传统的氧化/还原方法组成,例如使用过硫酸盐将PON氧化为硝酸盐(NO3*),使用海绵镉将NO3还原为亚硝酸盐(NO2),以及使用叠氮化钠将NO2进一步还原为一氧化二氮(N2O)。然后,将N2O从水中吹扫出来并低温捕集,随后释放到气相色谱柱中,通过同时监测质量数为30、31和32的NO+离子流,使用连续流同位素比率质谱仪(CF-IRMS)分析稳定氮同位素组成。每批分析中的氮同位素分馏是一致的。对于含有超过50 nmolN的PON的样品,扣除空白氮(最终N2O中为8 +/- 2 nmol)的贡献后,样品测量的标准偏差小于0.3‰;对于含有超过20 nmolN的样品,标准偏差小于0.5‰。通过使用这种方法,我们能够比其他方法更好地测定较低含量PON的δ15N,因此可以减少用于培养以确定固氮率所需的水样量。此外,通过将该方法应用于滤液,我们可以将其扩展到一般有机氮的氮同位素组成测定,例如总溶解氮(TDN;NO3、NO2*、铵和溶解有机氮的总和)。

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