Journal
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY
Volume 34, Issue 1, Pages 147-159Publisher
ROYAL SOC CHEMISTRY
DOI: 10.1039/c8ja00281a
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- UK Government Department for Business, Energy & Industrial Strategy (BEIS) [13</SUP>C-depleted glycines]
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Variations in the stable isotopic composition of carbon are commonly expressed as (C-13) values, and are used in diverse fields, including biology, environmental sciences, food and drug authentication and forensic applications. Progress in these fields requires accurate and comparable stable carbon isotope ratio measurements between laboratories and over time. Yet concerns about comparability of measurement results for stable carbon isotopes have been raised due to both replacement of one primary reference material by another and, more recently, due to the increase of (C-13) values of the second primary reference material (LSVEC) when exposed to the atmosphere. Establishing traceability to the SI as a stable metrological reference system can be a sustainable solution in ensuring accuracy and metrological traceability of measurement results. To address the shortage of reference materials certified for carbon isotope ratios traceable to the SI, a new reference material LGC171-KT has been produced in this study. This consists of three glycine solutions with certified n(C-13)/n(C-12) isotope amount ratios of 0.010642, 0.010821 and 0.011227 with expanded uncertainties (k = 2) of 0.000030, 0.000030 and 0.000032, respectively, and indicative (C-13)(VPDB) values of -42.22 parts per thousand, -24.66 parts per thousand and +12.55 parts per thousand with expanded uncertainties (95% confidence) of 0.34 parts per thousand, 0.24 parts per thousand and 0.22 parts per thousand, respectively. A strategy for the development and characterisation steps has been described in detail and includes an improved approach for evaluating results of homogeneity testing. The n(C-13)/n(C-12) isotope amount ratio for the zero point of the VPDB scale was also re-determined and the current best estimate, based on all available results, was determined to be 0.011117 with expanded uncertainty of 0.000039 (k = 2.6).
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