Second generation ‘diamond-in-water’ ablation – a step forward in trace element and isotopic composition analysis

IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Yaakov Weiss, Gonzalo Guadaño, Janne M. Koornneef, Yael Kempe, Ofir Tirosh, Gareth R. Davies
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引用次数: 0

Abstract

A second generation diamond-in-water laser ablation system combined with mass spectrometry measurements is presented for trace elements and radiogenic isotopic analyses of microinclusion-bearing diamonds. Ablation was conducted using a Nd: YV04 laser (532 nm, 136 µJ/pulse, 25 ns pulse duration, 2000 Hz repetition rate) in a closed ultra-clean glass cuvette filled with milli-Q water (18.2 MΩ cm). Multiple experiments indicate a highly stable and precise ablation process that proceeded at an average rate of 0.75 ± 0.41 mg/h. Triple Quadrupole inductively coupled plasma mass spectrometer (ICP-MS) trace element analyses of the ablated material reveal primitive mantle normalized patterns that are similar to previously analyzed microinclusion-bearing diamonds. Results comparable with previous ablation analyses of individual diamonds, and results of BHVO-2G and BCR-2G standards determined using this new ablation technique confirm its accuracy. Furthermore, the reference material results provide a means to estimate the uncertainty for the elemental concentrations in the diamonds, suggesting that it is generally below 10% for most elements of interest, and likely under 15% for all elements. The new ablation system produces enough material for successful Sr, Nd, and Pb isotope analyses by combined wet-chemistry and thermal ionization mass spectrometer (TIMS) using 1011 or 1013 Ω resistors. The Sr–Nd–Pb isotope values of BHVO-2G and BCR-2G ablated, purified using ion chromatography and measured by the same technique validate its accuracy. Low total procedural blank levels (Sr average of 71 ± 21 pg; Nd of 0.42 ± 0.25 pg Nd; Pb of 9.4 ± 3.6 pg) have little impact on the measured isotope values, but a blank correction can be applied if necessary.

第二代“水中钻石”烧蚀-微量元素和同位素组成分析的一个进步
提出了第二代水中金刚石激光烧蚀与质谱测量相结合的方法,用于微包裹体金刚石的微量元素和放射性成因同位素分析。使用Nd: YV04激光器(532 nm, 136µJ/脉冲,25 ns脉冲持续时间,2000 Hz重复频率)在一个封闭的超净玻璃试管中进行烧蚀,试管中充满毫微米q水(18.2 MΩ cm)。多次实验表明,在0.75±0.41 mg/h的平均速率下,烧蚀过程非常稳定和精确。三重四极电感耦合等离子体质谱(ICP-MS)对烧蚀材料的微量元素分析显示,原始地幔归一化模式与先前分析的含微包裹体钻石相似。与以往单个钻石的烧蚀分析结果相比较,以及使用这种新烧蚀技术确定的BHVO-2G和BCR-2G标准的结果证实了其准确性。此外,参考物质的结果提供了一种方法来估计钻石中元素浓度的不确定度,表明大多数感兴趣的元素的不确定度通常低于10%,而所有元素的不确定度可能低于15%。新的烧蚀系统产生足够的材料,使用1011或1013 Ω电阻器,通过湿化学和热电离质谱仪(TIMS)成功分析Sr, Nd和Pb同位素。对BHVO-2G和BCR-2G的Sr-Nd-Pb同位素值进行了烧蚀、离子色谱纯化和相同技术测量,验证了其准确性。低总程序空白水平(Sr平均值为71±21 pg, Nd平均值为0.42±0.25 pg, Pb平均值为9.4±3.6 pg)对测量的同位素值影响不大,但必要时可以进行空白校正。
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来源期刊
Mineralogy and Petrology
Mineralogy and Petrology 地学-地球化学与地球物理
CiteScore
2.60
自引率
0.00%
发文量
0
审稿时长
1 months
期刊介绍: Mineralogy and Petrology welcomes manuscripts from the classical fields of mineralogy, igneous and metamorphic petrology, geochemistry, crystallography, as well as their applications in academic experimentation and research, materials science and engineering, for technology, industry, environment, or society. The journal strongly promotes cross-fertilization among Earth-scientific and applied materials-oriented disciplines. Purely descriptive manuscripts on regional topics will not be considered. Mineralogy and Petrology was founded in 1872 by Gustav Tschermak as "Mineralogische und Petrographische Mittheilungen". It is one of Europe''s oldest geoscience journals. Former editors include outstanding names such as Gustav Tschermak, Friedrich Becke, Felix Machatschki, Josef Zemann, and Eugen F. Stumpfl.
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