2015
DOI: 10.1002/rcm.7232
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A thoroughly validated spreadsheet for calculating isotopic abundances (2H, 17O, 18O) for mixtures of waters with different isotopic compositions

Abstract: RATIONALE: Oxygen and hydrogen stable isotopes are widely used tracers for studies on naturally occurring and laboratory mixtures of isotopically different waters. Although the mixing calculations are straightforward to perform, there are ample possibilities to make mistakes, especially when dealing with a large number of mixed fluids. To facilitate isotope mixing calculations and to avoid computational mistakes, a flexible tool to carry out these calculations is in demand. METHODS: We developed, in three inde… Show more

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Cited by 13 publications
(43 citation statements)
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References 26 publications
(32 reference statements)
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“…The clumped isotopic composition of pure N 2 O reference materials can be evaluated by equilibration with activated alumina at moderate temperatures, and this may be a viable approach for calibration of S p values. There is a need for common mass overlap corrections in mass spectrometric analysis and we encourage publication of spreadsheets to accomplish this task, as was recently done for the isotopic analysis of water by spectroscopic approaches . As mass overlap corrections for N 2 O are complicated and involve assumptions, such as equivalent isotopic fractionation during breakage of α and β nitrogen bonds during ionization, spectroscopic approaches may prove useful in evaluating the validity of such assumptions .…”
Section: Future Directionsmentioning
confidence: 99%
See 1 more Smart Citation
“…The clumped isotopic composition of pure N 2 O reference materials can be evaluated by equilibration with activated alumina at moderate temperatures, and this may be a viable approach for calibration of S p values. There is a need for common mass overlap corrections in mass spectrometric analysis and we encourage publication of spreadsheets to accomplish this task, as was recently done for the isotopic analysis of water by spectroscopic approaches . As mass overlap corrections for N 2 O are complicated and involve assumptions, such as equivalent isotopic fractionation during breakage of α and β nitrogen bonds during ionization, spectroscopic approaches may prove useful in evaluating the validity of such assumptions .…”
Section: Future Directionsmentioning
confidence: 99%
“…There is a need for common mass overlap corrections in mass spectrometric analysis 3,15 and we encourage publication of spreadsheets to accomplish this task, as was recently done for the isotopic analysis of water by spectroscopic approaches. 37 As mass overlap corrections for N 2 O are complicated and involve assumptions, such as equivalent isotopic fractionation during breakage of α and β nitrogen bonds during ionization, spectroscopic approaches may prove useful in evaluating the validity of such assumptions. 1,38 There is a need for additional pure N 2 O gas isotope reference materials because, although USGS51 and USGS52 differ markedly in S P , they have similar bulk δ 15 N and δ 18 O values.…”
Section: Future Directionsmentioning
confidence: 99%
“…By using the accurately determined dilution factor, we could in this way calibrate the  17 O of TLW reference waters using IAEA-609,608 and 607. All calculations of isotope abundances and -values were performed using a thoroughly validated Excel spreadsheet 36 . Based on the measurement uncertainties, the uncertainties in the values quoted for the IAEA waters, and the dilution uncertainties we attribute a -conservative-± 1 % relative uncertainty to our  17…”
Section: Preparation Of the Triply Labelled Watermentioning
confidence: 99%
“…Three new laboratory standards were prepared gravimetrically [22] using distilled tap water (δ 2 H VSMOW-SLAP = -77 ‰), and by adding 32-200 g of 99.9993 % deuterium oxide (Sigma-Aldrich, St. Louis, MO, USA) in order to span the δ 2 H range for 250-2000 mL electrolytically enriched samples obtained in typical tritium operations (estimated to be in the 6000-60,000 ‰ range for δ 2 H VSMOW-SLAP ). The laboratory standards were homogenized for 1 week prior to isotopic analysis and stored at 0.5 bar argon gas pressure in steel siphon-dispensing containers.…”
Section: H-enriched Calibration Standardsmentioning
confidence: 99%
“…Deuterium sampling consisted of taking a 0.5 mL sub-sample of the pre-electrolysis spike (natural abundance, after pre-distillation) and a 0.5 mL sub-sample from the 10-12 mL final electrolytically enriched post-distilled sample (extremely 2 H-enriched). All the [22] b N=number of measurements made by laser spectroscopy. Boldface is mean±SEM, with assigned δ values used in the IHL laboratory.…”
Section: Tritium Enrichment Unit Test Water Samplesmentioning
confidence: 99%