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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >High-precision in situ U-238-U-234-Th-230 isotopic analysis using laser ablation multiple-collector ICPMS
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High-precision in situ U-238-U-234-Th-230 isotopic analysis using laser ablation multiple-collector ICPMS

机译:使用激光消融多收集器ICPMS的高精度原位U-238-U-234-Th-230同位素分析

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We have developed a method for the rapid, in situ measurement of U-Th isotopic compositions at the semimicro scale using laser ablation sampling, combined with multiple collector ICP magnetic sector mass spectrometry (MC-ICPMS). The system uses a Q-switched and frequency quadrupled 266 nm Nd:YAG laser to ablate samples containing 100 ppm levels of U at 150 mum scale resolution, corresponding to 1-4 ng U-238, similar to 70-200 fg of U-234 and 20-60 fg of Th-230 consumed per analysis. Synthetic glass standards and naturally occurring samples of zircon and opal, with U contents of 460, 260, and similar to 200 ppm, respectively, were used to assess the precision and accuracy of our laser ablation technique. Our initial experiments used argon as the plasma support gas. Thirty-seven laser analyses on the glass and 29 on the zircon give respective mean [U-234/U-238](act) of 0.17114 +/- 0.00022 and 1.0018 +/- 0.0014 (2 sigma (M)), indistinguishable from the MC-ICPMS solution nebulization values of 0.17094 +/- 0.00006 and 1.0011 +/- 0.0009 (2 sigma (M)), respectively. The usual within-run precision obtained for both glass and zircon is +/-3 parts per thousand at the 2 sigma (M) level. An additional 12 laser analyses on the opal give a mean [U-234/U-238](act) of 0.9997 +/- 0.0034, in excellent agreement with the expected secular equilibrium value of unity and a typical within-run precision of +/-8 parts per thousand (2 sigma (M)). Our Nd:YAG laser, coupled with an all Ar gas system, produces large elemental fractionation effects between U and Th. Both U-238/Th-232 and [Th-230/U-238](act) can be measured at the per mill level, but Th ion beams are suppressed relative to U. As a result, the Th/U ratios are systematically lower, and the apparent U-238-U-234-Th-230 ages are systematically younger than the true values. The U-Th fractionation is primarily controlled by ionization conditions in the plasma, transportation efficiency of ablated particles, and the composition of the sample matrix. The use of helium instead of Ar in the ablation cell significantly improves the relative sensitivity of Th, and entirely eliminates the elemental fractionation between U and Th, while retaining accuracy and precision in U isotope measurement. With He, mean values for [Th-230/U-238](act) Of 0.996 +/- 0.013 and U-238/Th-232 Of 1.625 +/- 0.092 were determined for the zircon standard, in excellent agreement with the solution nebulization values of 1.0042 +/- 0.0016 and 1.6288 +/- 0.0006 (2 sigma (M),), respectively. In an unknown sample, it is possible to determine correct values for [Th-230/U-238](act) and U-238/Th-232, with respective within-run uncertainties as good as 7 parts per thousand and 2 parts per thousand, by monitoring the isotopic composition of a well characterized, matrix-matched standard. For high-U material, the combined uncertainties in [U-234/U-238](act) and [Th-230/U-238](act) routinely translate to 2 sigma (M) errors in the U-238-U-234-Th-230 age of better than +/-2,500 years in 100,000-year-old samples. Copyright (C) 2000 Elsevier Science Ltd. [References: 38]
机译:我们已经开发了一种使用激光烧蚀采样结合多收集器ICP磁扇区质谱仪(MC-ICPMS)在半微尺度下快速,原位测量U-Th同位素组成的方法。该系统使用Q开关和频率四倍的266 nm Nd:YAG激光以150微米的分辨率烧蚀包含100 ppm水平U的样品,相当于1-4 ng U-238,类似于70-200 fg U-每次分析消耗234和20-60 fg Th-230。分别使用U含量分别为460、260和200 ppm的合成玻璃标准品和锆石和蛋白石的天然样品,来评估我们的激光烧蚀技术的精度和准确性。我们的初始实验使用氩气作为等离子体支撑气体。对玻璃进行37次激光分析,对锆石进行29次激光分析,得出[U-234 / U-238](act)的平均值分别为0.17114 +/- 0.00022和1.0018 +/- 0.0014(2 sigma(M)),与MC-ICPMS溶液雾化值分别为0.17094 +/- 0.00006和1.0011 +/- 0.0009(2 sigma(M))。在2 sigma(M)水平下,玻璃和锆石通常获得的批内精度为+/- 3千分之几。在蛋白石上进行的另外12次激光分析得出[U-234 / U-238](act)的平均值为0.9997 +/- 0.0034,与预期的长期长期平衡值一致,典型的内部运行精度为+ / -8千分之几(2 sigma(M))。我们的Nd:YAG激光器与全Ar气体系统相结合,可在U和Th之间产生较大的元素分馏效应。 U-238 / Th-232和[Th-230 / U-238](act)均可在每磨级下测量,但Th离子束相对于U受到抑制。结果,Th / U比为系统上较低,并且表观的U-238-U-234-Th-230年龄系统上比真实值年轻。 U-Th分级主要受血浆中的电离条件,烧蚀颗粒的传输效率以及样品基质的组成控制。在烧蚀池中使用氦气代替Ar可以显着提高Th的相对灵敏度,并完全消除U和Th之间的元素分离,同时保留U同位素测量的准确性和精度。用He测定锆石标准品的[Th-230 / U-238](act)平均值为0.996 +/- 0.013,U-238 / Th-232平均值为1.625 +/- 0.092,与溶液雾化值分别为1.0042 +/- 0.0016和1.6288 +/- 0.0006(2 sigma(M))。在未知样品中,可以确定[Th-230 / U-238](act)和U-238 / Th-232的正确值,并且各自的运行中不确定性分别为千分之七和二分之二通过监测特征明确的基质匹配标准品的同位素组成,确定每千分之一。对于高U材料,[U-234 / U-238](act)和[Th-230 / U-238](act)中的不确定性通常会转换为U-238-2中的2σ(M)误差。在100,000年的样本中,U-234-Th-230的年龄优于+/- 2,500年。版权所有(C)2000 Elsevier ScienceLtd。[参考:38]

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