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Gas Diffusion Method: a Simple and Rapid Method for δ~(15)N - NH_4 Determination in Water Samples

机译:气体扩散法:一种简单快速的测定水中样品中δ〜(15)N-NH_4的方法

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摘要

Isotope tracer analysis is one of the most expected methods for studying the nitrogen cycle in aquatic environments in determining the sources and processes of nitrogen compounds. Previously, several researches proposed the analytical procedure for δ~(15)N - NH_4, those methods have been still insufficient for practical application in technical reasons. In this study, Gas diffusion method was developed for recovering ammonium followed by analysis of stable isotope ratios. This method was an enhancement of the liquid phase diffusion method, in which NH3 in base condition is trapped in acidic filter through gas phase instead of liquid phase as the original method suggested. The results demonstrated that, for environmental water samples having concentration more than 1 ppm, isotope ratios were determined with high precision, ± 0.41 ‰, after five days of sample diffusion. In summary, this method could shorten time threefold and need sample volume less than 80 times comparing to the liquid phase diffusion method.
机译:同位素示踪分析是研究水生环境中氮循环以确定氮化合物来源和过程的最理想方法之一。以前,已有一些研究提出了δ〜(15)N-NH_4的分析方法,但由于技术原因,这些方法仍不足以实际应用。在这项研究中,开发了一种气体扩散法来回收铵,然后分析稳定的同位素比。该方法是对液相扩散法的增强,在液相扩散法中,碱性条件下的NH3通过气相而不是液相吸附到酸性过滤器中,这是原始方法所建议的。结果表明,对于浓度大于1 ppm的环境水样品,在样品扩散5天后,可以以±0.41‰的高精度确定同位素比。综上所述,与液相扩散法相比,该方法可将时间缩短三倍,所需样品量不到80倍。

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  • 会议地点 Sapporom(JP)
  • 作者单位

    Special Master's program on River Basin Environmental Science, University of Yamanashi, Yamanashi, 400-8511, Japan;

    Interdisciplinary Centre for River Basin Environment, University of Yamanashi, Yamanashi, 400-8511, Japan;

    Interdisciplinary Centre for River Basin Environment, University of Yamanashi, Yamanashi, 400-8511, Japan;

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  • 正文语种 eng
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