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采用超净方法控制污染,可靠地对格陵兰冰雪中的 Cd、U 和 Zn 浓度进行超痕量分析。

Reliable Ultra Trace Analysis of Cd, U and Zn Concentrations in Greenland Snow and Ice by Using Ultraclean Methods for Contamination Control.

机构信息

Division of Polar Paleoenvironment, Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon 21990, Korea.

Department of Ocean Sciences, Inha University, 100 Inha-ro, Michuhol-gu, Incheon 22212, Korea.

出版信息

Molecules. 2020 May 28;25(11):2519. doi: 10.3390/molecules25112519.

Abstract

This study presents ultraclean procedures used in the challenging task of determining trace elements at or below the pg/g concentration level encountered in Greenland snow and ice. In order to validate these ultraclean procedures, recent snowfall and Holocene ice from northwest Greenland were analyzed for Cd, U, and Zn concentrations. The total procedural blanks brought through the entire measurement procedure proved to be negligible, compared to trace element concentrations, measured in snow and ice samples. This validates the overall practicality of the proposed ultraclean procedures, thereby ensuring the reliable measurements of ultra-trace analysis. A comparison between our study and published data shows that improper procedures employed throughout all stages, from field sampling to analysis to elevate the concentrations by several orders of magnitude, relative to the reliable concentration ranges. The risk of contamination exposure for selected trace elements appears to increase in the order of U < As ≤ Pb < Cd < Zn. Reliable measurements of Cd, U, and Zn concentrations in snow and ice allowed us to interpret the data in terms of seasonal variations in the inputs of crustal and anthropogenic sources to Greenland ice sheet.

摘要

本研究提出了超净程序,用于解决在格陵兰冰雪中遇到的痕量元素在 pg/g 浓度水平或以下的挑战性任务。为了验证这些超净程序,分析了来自格陵兰西北部的近期降雪和全新世冰芯中的 Cd、U 和 Zn 浓度。与雪和冰样品中测量的痕量元素浓度相比,整个测量过程中的总程序空白可以忽略不计。这验证了所提出的超净程序的整体实用性,从而确保了超痕量分析的可靠测量。我们的研究与已发表数据的比较表明,从野外采样到分析再到将浓度提高几个数量级,所有阶段都采用了不适当的程序,相对于可靠的浓度范围而言,这会使浓度升高。选定痕量元素的污染暴露风险似乎按 U<As≤Pb<Cd<Zn 的顺序增加。雪和冰中 Cd、U 和 Zn 浓度的可靠测量使我们能够根据地壳和人为源对格陵兰冰盖输入的季节性变化来解释数据。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c2ce/7321221/3207a5e7b693/molecules-25-02519-g001.jpg

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