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Stable hydrogen isotopic analysis of nanomolar molecular hydrogen by automatic multi-step gas chromatographic separation

机译:通过自动多步气相色谱分离技术对纳摩尔分子氢进行稳定的氢同位素分析

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摘要

We have developed a new automated analytical system that employs a continuous flow isotope ratio mass spectrometer to determine the stable hydrogen isotopic composition (δD) of nanomolar quantities of molecular hydrogen (H_2) in an air sample. This method improves previous methods to attain simpler and lower-cost analyses, especially by avoiding the use of expensive or special devices, such as a Toepler pump, a cryogenic refrigerator, and a special evacuation system to keep the temperature of a coolant under reduced pressure. Instead, the system allows H_2 purification from the air matrix via automatic multi-step gas chromatographic separation using the coolants of both liquid nitrogen (77 K) and liquid nitrogen + ethanol (158 K) under 1 atm pressure. The analytical precision of the δD determination using the developed method was better than 4° for >5 nmol injections (250 mL STP for 500 ppbv air sample) and better than 15° for 1 nmol injections, regardless of the δD value, within 1 h for one sample analysis. Using the developed system, the δD values of H_2 can be quantified for atmospheric samples as well as samples of representative sources and sinks including those containing small quantities of H_2, such as H _2 in soil pores or aqueous environments, for which there is currently little δD data available. As an example of such trace H_2 analyses, we report here the isotope fractionations during H_2 uptake by soils in a static chamber. The δD values of H_2 in these H_2-depleted environments can be useful in constraining the budgets of atmospheric H_2 by applying an isotope mass balance model.
机译:我们开发了一种新的自动化分析系统,该系统采用连续流同位素比质谱仪确定空气样品中纳摩尔量的分子氢(H_2)的稳定氢同位素组成(δD)。此方法改进了以前的方法,以实现更简单且成本更低的分析,尤其是避免使用昂贵或特殊的设备(例如,Toepler泵,低温冰箱和特殊的抽真空系统,以使冷却剂的温度保持在减压状态) 。相反,该系统允许在1个大气压下使用液氮(77 K)和液氮+乙醇(158 K)的冷却剂通过自动多步气相色谱分离从空气基质中纯化H_2。在1 h内,无论采用何种δD值,使用发达的方法测定δD的分析精度均优于4°(> 5 nmol进样(500 ppbv空气样品为250 mL STP)和1 nmol进样的15°以上。进行一次样品分析。使用开发的系统,H_2的δD值可用于大气样品以及代表性来源和汇样品的定量,包括那些含有少量H_2的样品,例如土壤孔隙或水环境中的H_2,目前这些样品很少可用δD数据。作为这种痕量H_2分析的一个例子,我们在这里报告了静态室内土壤吸收H_2期间的同位素分馏。在这些贫乏H_2的环境中,H_2的δD值可通过应用同位素质量平衡模型来约束大气H_2的预算。

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