IAEA-CH-3

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€200.00
Producing Laboratory: TERC
Availability: In stock
Cellulose

IAEA-CH-3 is aimed at δ(13C) calibrations by EA-IRMS techniques.

IAEA-CH-3 was prepared in 1989 at the IAEA from large batch of cellulose harvested from approximately 40 years old trees originating from Sweden. Processed material was pressed into sheets and initially characterized for 14C value of IAEA-C3. Three kilograms of these sheets were milled to fine powder, homogenized and characterised for δ(13C) value of IAEA-CH-3. The final calibration of the material was performed in 2004 by a small group of experienced laboratories together with the re-calibration of most of the other organic carbon stable isotope reference materials available at IAEA [1].

AnalyteReference ValueUnitCombined standard uncertainty with k=1
δ(13C)-24.72VPDB-LSVEC0.04

Note: For δ(13C), currently two scales exist and are in use: VPDB and VPDB-LSVEC.  δ(13C) values reported on the VPDB and VPDB-LSVEC scale can differ, with maximum reported differences (VPDB minus VPDB-LSVEC) of +0.3 ‰ for materials with carbon isotope delta values around –45 ‰ and negligible difference (below current analytical combined uncertainty) at carbon isotope delta values close to zero [https://doi.org/10.1002/rcm.10018)]. 

End users should state the values of reference materials used to normalize isotope data following the minimum requirements established by IUPAC [https://doi.org/10.1515/pac-2021-1108] and in the case of carbon, whether they are publishing δ(13C) values on the VPDB scale or the VPDB-LSVEC scale. Users should ensure that in one calibration they only use values for reference materials assigned on one scale. 

References:

  1. COPLEN, T.B., BRAND, W.A., GEHRE, M., GRÖNING, M., MEIJER, H.A.J., TOMAN, B., VERKOUTEREN, R.M., New guidelines for δ13C measurementsAnal. Chem. 78 (2006) 2439-2441.
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