Abstract

Standards for reporting C-14 age determinations are discussed. All dates should be related either directly or indirectly to the NBS oxalic acid standard. Corrections for isotopic fractionation are also desirable. For some materials, particularly marine shell, corrections for reservoir effect are necessary, but these should always be reported separately from the conventional radiocarbon age. The statistical uncertainty (plus or minus one standard deviation) expresses counting errors, inaccuracies in voltage, pressure, temperature, dilution, and should include errors in C-13 ratios. Errors can be significant when isotope ratios are estimated rather than measured directly. The error in the conventional C-14 half life is not included. The article includes tables indicating what data should be reported.

Keywords

Isotope dilutionStandard deviationOxalic acidMeasurement uncertaintyEnvironmental scienceIsotopeFractionationRadiocarbon datingDilutionSystematic errorStandard errorChemistryEnvironmental chemistryStatisticsChromatographyMathematicsGeologyMass spectrometryNuclear physicsThermodynamicsPhysics

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Publication Info

Year
2003
Type
article
Volume
37
Issue
1
Pages
18A-26A
Citations
4919
Access
Closed

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Minze Stuiver, Henry Polach (2003). Characterizing aquatic dissolved organic matter.. PubMed , 37 (1) , 18A-26A.