首页> 外文期刊>Environmental Science & Technology >Continuous Ice Core Melter System with Discrete Sampling for Major Ion,Trace Element and Stable Isotope Analyses
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Continuous Ice Core Melter System with Discrete Sampling for Major Ion,Trace Element and Stable Isotope Analyses

机译:具有主要离子,痕量元素和稳定同位素分析的离散采样的连续冰芯融化器系统

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摘要

We present a novel ice/firn core melter system that uses fraction collectors to collect discrete,high-resolution (<1 cm/sample possible),continuous,coregistered meltwater samples for analysis of eight major ions by ion chroma-tography (IC),>32 trace elements by inductively coupled plasma sectorfield mass spectrometry (ICP-SMS),and stable oxygen and hydrogen isotopes by isotope ratio mass spectrometry (IRMS).The new continuous melting with discrete sampling (CMDS)system preserves an archive of each sample,reduces the problem of incomplete particle dissolution in ICP-SMS samples,and provides more precise trace element data than previous ice melter models by using longer ICP-SMS scan times and washing the instrument between samples.CMDS detection limits are similar to or lower than those published for ice melter systems coupled directly to analytical instruments and are suitable for analyses of polar and mid-low-latitude ice cores.Analysis of total calcium and sulfur by ICP-SMS and calcium ion,sulfate,and methanesulfonate by IC from the Mt.Logan Prospector-Russell Col ice core confirms data accuracy and coregistration of the split fractions from each sample.The reproducibility of all data acquired by the CMDS system is confirmed by replicate analyses of parallel sections of the GISP2 D ice core.
机译:我们提出了一种新颖的冰/熔芯融化器系统,该系统使用馏分收集器收集离散的高分辨率(可能小于1 cm /样品)连续的,共配准的融化水样品,用于通过离子色谱法(IC)分析八种主要离子,电感耦合等离子体扇形质谱(ICP-SMS)可以检测到32种以上的痕量元素,同位素比率质谱(IRMS)可以检测出稳定的氧和氢同位素。新的具有不连续采样的连续熔化(CMDS)系统可以保存每个样品的档案,减少了ICP-SMS样品中颗粒不完全溶解的问题,并通过使用更长的ICP-SMS扫描时间并在样品之间洗涤仪器来提供比以前的融冰机模型更精确的痕量元素数据.CMDS检测限与那些或更低出版的直接与分析仪器耦合的融冰机系统,适用于极地和中低纬度冰芯的分析.ICP-SMS和calciu分析总钙和硫洛根山Prospector-Russell Col冰芯的IC分析得到的离子,硫酸根和甲磺酸根证实了每个样品中分离出的馏分的数据准确性和共存性CMDS系统获得的所有数据的再现性均通过平行分析的重复分析得以证实GISP2 D冰芯的各个部分。

著录项

  • 来源
    《Environmental Science & Technology》 |2006年第10期|p.3355-3361|共7页
  • 作者单位

    Climate Change Institute,Sawyer Environmental ResearchCenter,and Department of Earth Sciences,Bryand Global Sciences Building,University of Maine,Orono,Maine 04469;

    Climate Change Institute,Sawyer Environmental ResearchCenter,and Department of Earth Sciences,Bryand Global Sciences Building,University of Maine,Orono,Maine 04469;

    Climate Change Institute,Sawyer Environmental ResearchCenter,and Department of Earth Sciences,Bryand Global Sciences Building,University of Maine,Orono,Maine 04469;

    Climate Change Institute,Sawyer Environmental ResearchCenter,and Department of Earth Sciences,Bryand Global Sciences Building,University of Maine,Orono,Maine 04469;

    Climate Change Institute,Sawyer Environmental ResearchCenter,and Department of Earth Sciences,Bryand Global Sciences Building,University of Maine,Orono,Maine 04469;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境化学;
  • 关键词

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