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采用预浓缩技术进行在线浓度调整,以提高元素分析仪/连续流同位素比率质谱仪对低硫含量样品的信号。

Signal improvement in elemental analyzer/continuous flow isotope ratio mass spectrometry for samples with low sulfur contents using a pre-concentration technique for on-line concentration adjustment.

作者信息

Fritzsche Florian, Tichomirowa Marion

机构信息

Institute of Soil Science and Soil Geography, University of Bayreuth, 95440 Bayreuth, Germany.

出版信息

Rapid Commun Mass Spectrom. 2006;20(11):1679-82. doi: 10.1002/rcm.2488.

Abstract

Elemental analyzer/continuous flow isotope ratio mass spectrometry (EA/CF-IRMS) has become a standard procedure for the determination of delta(34)S values. Common procedures are, however, frequently less than satisfactory for organic as well as for mineral samples with very low concentrations of sulfur (<2000 ppm). Here we present a method which employs cold trapping of SO(2) to adjust the gas concentration for subsequent isotope signature determination. Analytical accuracy is comparable with common EA/CF-IRMS analysis without trapping, showing a precision of better than +/-0.4 per thousand in delta(34)S (1 SD). The virtual absence of memory effects was established by analyzing adjacent samples exhibiting a large difference in delta(34)S and by prolonged freezing of the carrier gas, yielding virtually no S concentration peak. The method was tested using less than 15% (6 microg) of the S required for a conventional isotope analysis at comparable signal intensity. Even smaller samples can be analyzed with high precision. This facilitates the on-line delta(34)S determination in small biological and mineral samples, minimizing matrix effects in various materials including sandstone, soil, and plant samples.

摘要

元素分析仪/连续流同位素比率质谱仪(EA/CF-IRMS)已成为测定δ(34)S值的标准方法。然而,对于有机样品以及硫浓度极低(<2000 ppm)的矿物样品,常用方法常常不尽人意。在此,我们提出一种方法,该方法采用对SO₂进行冷阱捕集来调整气体浓度,以便后续测定同位素特征。分析精度与不采用捕集的常规EA/CF-IRMS分析相当,δ(34)S(1 SD)的精密度优于±0.4‰。通过分析δ(34)S差异很大的相邻样品以及对载气进行长时间冷冻,证实几乎不存在记忆效应,几乎没有产生硫浓度峰。在可比的信号强度下,使用的硫量不到传统同位素分析所需硫量的15%(6微克)对该方法进行了测试。甚至更小的样品也能高精度分析。这便于对小型生物和矿物样品进行在线δ(34)S测定,最大限度地减少包括砂岩、土壤和植物样品在内的各种材料中的基质效应。

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