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首页> 外文期刊>Journal of Analytical Atomic Spectrometry >Temporal changes of size distribution of mass and relative intensity for ablated particles during laser ablation inductively coupled plasma mass spectrometry
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Temporal changes of size distribution of mass and relative intensity for ablated particles during laser ablation inductively coupled plasma mass spectrometry

机译:激光烧蚀电感耦合等离子体质谱过程中烧蚀颗粒的质量尺寸分布和相对强度的时间变化

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摘要

To investigate elemental fractionation during laser ablation-inductively coupled plasma mass spectrometry (LA-ICPMS) we measured mass fractions of ablated particles and chemical composition of ablated particles in this study. Temporal changes of fractionation indexes (FIs) were investigated under laser defocus conditions which caused a large variation of size distribution of abated particles. It was a useful technique for understanding the relationship between temporal changes of FIs and the size of ablated particles. Ablated particles were fractionated by aerodynamic diameters (<0.06, 0.06-0.22. 0.22-2.2, and >2.2 μm) with a low-pressure impactor and were digested with HNO_3 and HF; then As, Rb, Rh, La, Gd, Yb, W, Re, and Th were measured by ICPMS. Under 0.5 mm defocus and 1.0 mm defocus conditions, the mass fractions (ablated particle mass at 1-5 min divided by that at 0-1 min) of ablated particles larger than 0.22 nm were larger than the mass fractions of ablated particles smaller than 0.22 nm. Volatile elements such as As and Rb were enriched in particles smaller than 0.22 nm, owing to the large aspect ratio of the crater under defocus conditions. However, the magnitude of the enrichment for volatile elements did not change as ablation progressed. Therefore, we concluded that large particles could not be decomposed completely in the ICP and the FI peak observed at 2-3 min was caused by changes in elemental behavior due to changes in ablated particles larger than 0.22 nm.
机译:为了研究激光烧蚀-电感耦合等离子体质谱法(LA-ICPMS)中的元素分离,我们在本研究中测量了烧蚀颗粒的质量分数和烧蚀颗粒的化学成分。研究了激光散焦条件下分馏指数(FIs)随时间的变化,这引起了烧蚀颗粒尺寸分布的较大变化。这是一种有用的技术,可用于了解FI的时间变化与烧蚀颗粒大小之间的关系。用低压冲击器按空气动力学直径(<0.06、0.06-0.22、0.22-2.2和> 2.2μm)对烧蚀的颗粒进行分级分离,并用HNO_3和HF进行消解;然后通过ICPMS测量As,Rb,Rh,La,Gd,Yb,W,Re和Th。在0.5 mm离焦和1.0 mm离焦条件下,大于0.22 nm的烧蚀颗粒的质量分数(1-5分钟处的烧蚀颗粒质量除以0-1 min处的质量分数)大于小于0.22 nm的烧蚀颗粒的质量分数纳米由于火山口在散焦条件下的高长宽比,挥发性元素(例如As和Rb)富含小于0.22 nm的颗粒。但是,随着消融的进行,挥发性元素的富集幅度没有改变。因此,我们得出的结论是,较大的颗粒无法在ICP中完全分解,并且在2-3分钟观察到的FI峰是由于大于0.22 nm的烧蚀颗粒的变化引起的元素行为变化而引起的。

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  • 来源
    《Journal of Analytical Atomic Spectrometry》 |2016年第3期|809-814|共6页
  • 作者单位

    Faculty of Science and Engineering, Department of Applied Chemistry, Chuo University, 1-13-27 Kasuga, Bunkyo-ku, Tokyo 112-8551, Japan;

    Faculty of Science and Engineering, Department of Applied Chemistry, Chuo University, 1-13-27 Kasuga, Bunkyo-ku, Tokyo 112-8551, Japan;

    Faculty of Science and Engineering, Department of Applied Chemistry, Chuo University, 1-13-27 Kasuga, Bunkyo-ku, Tokyo 112-8551, Japan;

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