Hillier Aimee, Mussell-Webber Eric, Hopkinson Emily, Wilson Freya, Nehrbass-Ahles Christoph, Brewer Paul J, Worton David R, Rennick Christopher, Arnold Tim, Moossen Heiko, Rothe Michael, Geilmann Heike, Dylag Caroline, Hill-Pearce Ruth E
National Physical Laboratory, Hampton Road, Teddington, Middlesex TW11 0LW, U.K.
Department of Physical Geography and Ecosystem Science, Lund University, Lund 223 62, Sweden.
Anal Chem. 2025 Jun 24;97(24):12513-12520. doi: 10.1021/acs.analchem.4c06540. Epub 2025 Jun 9.
Measurements of the stable carbon isotope ratio in methane (δC-CH) are used in determining the source of CH emissions on local, regional, and global scales. To achieve the required level of data comparability for atmospheric monitoring networks, accurate gas reference materials of δC-CH in air are required with high levels of reproducibility. We describe a method to determine the δC-CH of CH in synthetic air reference materials reported against the Vienna Pee Dee Belemnite (VPDB) scale. The measurement principle converts CH into carbon dioxide (CO) via direct combustion using a platinum catalyst. Subsequently, the CO resulting from CH combustion was analyzed for δC-CO using OIRS (optical isotope ratio spectroscopy) against CO in synthetic air reference materials traceable to the δC scale. The δC-CH of four nominally 410 μmol mol CH in synthetic air reference materials, prepared in pairs from two CH sources with distinct δC-CH were certified with an average δC-CH of -39.07‰ and -51.91‰. Measurement reproducibility within 0.17‰ was demonstrated between measurements of the two reference materials from each CH source. Agreement to traceable measurements of the pure CH was achieved within reported measurement reproducibility. Combined expanded uncertainties (= 2) between 0.4 and 1.5‰ have been demonstrated. The sensitives of the conversion system to flow rate have been assessed and found to have a negligible impact on the certification of δC-CH. Thus, we demonstrate that a combustion system coupled to OIRS measurement of CO can provide a means of useful measurement of δC-CH traceable to VPDB.
甲烷中稳定碳同位素比率(δC-CH)的测量被用于确定地方、区域和全球尺度上CH排放的来源。为了达到大气监测网络所需的数据可比性水平,需要具有高重现性的空气中δC-CH的准确气体标准物质。我们描述了一种测定合成空气标准物质中CH的δC-CH的方法,该方法以维也纳皮迪-贝列姆石(VPDB)标度为参照进行报告。测量原理是使用铂催化剂通过直接燃烧将CH转化为二氧化碳(CO₂)。随后,针对源自CH燃烧的CO₂,使用可溯源至δC标度的合成空气标准物质中的CO₂,通过光同位素比率光谱法(OIRS)分析其δC-CO₂。对由两种具有不同δC-CH的CH源成对制备的四种标称410 μmol/mol CH的合成空气标准物质的δC-CH进行了认证,其平均δC-CH分别为-39.07‰和-51.91‰。在对每个CH源的两种标准物质的测量之间,证明测量重现性在0.17‰以内。在报告的测量重现性范围内,与纯CH的可溯源测量结果达成了一致。已证明合成扩展不确定度(= 2)在0.4‰至1.5‰之间。评估了转化系统对流速的敏感性,发现其对δC-CH的认证影响可忽略不计。因此,我们证明了与CO₂的OIRS测量相结合的燃烧系统能够提供一种可溯源至VPDB测量δC-CH的有用方法。