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Hydrogen-isotope analysis of nanomole (picoliter) quantities of H_2O

机译:纳摩尔(微升)H_2O的氢同位素分析

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摘要

We describe a technique for on-line reduction of water vapor carried in a He stream followed by continuous-flow mass spectrometry of evolved H_2 gas. This technique is appropriate for analysis of D/H ratios of ~10~(-9) to ~5 * 10~(-8) moles of water and has an external precision (1σ) typically varying between ±1.0 and 2.0‰. for specific ranges in sample size, temperature of the reduction reaction, and method of introducing evolved vapor into the mass spectrometer, this technique involves negligible analytical corrections (~0 to 3‰) beyond those inherent to gas-source mass spectrometry of molecular hydrogen. We present an analysis of the D/H ratio of water released by stepped heating of a 10-mg fragment of the Shergottite-Nahklite-Chassignite meteorite ALH84001 and ~1 to 2 μg of a terrestrial hydrous mineral (thermonatrite) as examples of possible applications making use of this technique.
机译:我们描述了一种在线还原He气流中所携带的水蒸气的技术,然后对所产生的H_2气体进行连续流质谱分析。此技术适用于分析D / H比为〜10〜(-9)到〜5 * 10〜(-8)摩尔水,并且其外部精度(1σ)通常在±1.0至2.0‰之间变化。对于样品大小,还原反应温度和将逸出的蒸气引入质谱仪的方法的特定范围,该技术所涉及的分析校正可忽略不计(约0到3‰),这超出了分子氢气体源质谱法固有的校正范围。我们通过逐步加热10mg的Shergottite-Nahklite-Chassignite陨石ALH84001碎片和约1-2μg的陆地含水矿物质(水辉石),对水的D / H比进行分析。利用这种技术。

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