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关于反硝化法进行氮同位素分析时校正必要性的讨论。

Discussion on the need for correction during isotopic analysis of nitrogen by the denitrifier method.

作者信息

Hu Jing, Pan Mengyan, Li Yuliang, Xing Meng, Cao Yunning, Yang Kaili, Liu Weiguo

机构信息

State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences No. 97, Yanxiang Road Xi'an 710061 China.

Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region, Ministry of Education, School of Water and Environment, Chang'an University Xi'an 710054 China

出版信息

RSC Adv. 2023 May 5;13(20):13834-13839. doi: 10.1039/d3ra00371j. eCollection 2023 May 2.

Abstract

The nitrogen and oxygen isotopes of NO are effectively used to trace the main nitrogen sources and migration processes in the atmosphere, water and soil. NO can be converted into NO by the bacterial denitrification method, which is an advanced method with high sensitivity. However, due to the existence of a small but inevitable blank during the whole experimental process, the N isotopic signal of NO produced by denitrification superimposes on that of the N blank. Currently, the standard curve correction method is used to correct measured nitrogen isotope results to mitigate blank interference. It has been reported that high variability of the nitrogen isotope results have been produced by the denitrifier method by conducting an interlaboratory comparison of denitrifier methods and other methods on standards and environmental samples, and to reduce this problem, the nitrogen isotope calibration process with a standard curve is examined in depth in this paper, which uses PreCon-GC-IRMS to determine the nitrogen isotopes in NO. We demonstrate for the first time that reliable results can be obtained without correction for samples with nitrogen isotope composition ranging from -9.9 to 19.5‰, which covers the natural sample range. This study establishes the double test approach for the bacterial denitrification method, ensuring the accuracy and long-term stability of different batches of nitrogen isotope results.

摘要

一氧化氮(NO)的氮和氧同位素被有效地用于追踪大气、水和土壤中的主要氮源及迁移过程。通过细菌反硝化法可将NO转化为NO,这是一种灵敏度高的先进方法。然而,由于整个实验过程中存在虽小但不可避免的空白值,反硝化产生的NO的氮同位素信号会叠加在氮空白值的信号上。目前,采用标准曲线校正法对测得的氮同位素结果进行校正,以减轻空白干扰。通过对标准物质和环境样品的反硝化法及其他方法进行实验室间比对,已有报道称反硝化法产生的氮同位素结果具有较高的变异性。为减少这一问题,本文深入研究了使用PreCon-GC-IRMS测定NO中氮同位素的标准曲线氮同位素校准过程。我们首次证明,对于氮同位素组成范围为-9.9至19.5‰(涵盖天然样品范围)的样品,无需校正即可获得可靠结果。本研究建立了细菌反硝化法的双重测试方法,确保了不同批次氮同位素结果的准确性和长期稳定性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f79c/10161198/7255086b0504/d3ra00371j-f1.jpg

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