USGS46 Greenland Ice Core Water – A New Isotopic Reference Material for δ 2 H and δ 18 O Measurements of Water

Ice core from Greenland was melted, filtered, homogenised, loaded into glass ampoules, sealed, autoclaved to eliminate biological activity, and calibrated by dual‐inlet isotope‐ratio mass spectrometry. This isotopic reference material ( RM ), USGS46, is intended as one of two secondary isotopic refe...

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Bibliographic Details
Published in:Geostandards and Geoanalytical Research
Main Authors: Coplen, Tyler B., Qi, Haiping, Tarbox, Lauren, Lorenz, Jennifer, Buck, Bryan
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2013
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1751-908x.2013.00267.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1751-908X.2013.00267.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1751-908X.2013.00267.x
Description
Summary:Ice core from Greenland was melted, filtered, homogenised, loaded into glass ampoules, sealed, autoclaved to eliminate biological activity, and calibrated by dual‐inlet isotope‐ratio mass spectrometry. This isotopic reference material ( RM ), USGS46, is intended as one of two secondary isotopic reference waters for daily normalisation of stable hydrogen (δ 2 H) and stable oxygen (δ 18 O) isotopic analysis of water with a mass spectrometer or a laser absorption spectrometer. The measured δ 2 H and δ 18 O values of this reference water were −235.8 ± 0.7‰ and −29.80 ± 0.03‰, respectively, relative to VSMOW on scales normalised such that the δ 2 H and δ 18 O values of SLAP reference water are, respectively, −428 and −55.5‰. Each uncertainty is an estimated expanded uncertainty ( U = 2 u c ) about the reference value that provides an interval that has about a 95‐percent probability of encompassing the true value. This reference water is available in cases containing 144 glass ampoules that are filled with either 4 ml or 5 ml of water per ampoule.