Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-10T06:11:14.431Z Has data issue: false hasContentIssue false

Total Uncertainty of Radiocarbon Measurements of Marine Dissolved Organic Carbon and Methodological Recommendations

Published online by Cambridge University Press:  09 February 2016

Ellen R M Druffel*
Affiliation:
Department of Earth System Science, University of California Irvine, Irvine, California 92697-3100, USA
Sheila Griffin
Affiliation:
Department of Earth System Science, University of California Irvine, Irvine, California 92697-3100, USA
Brett D Walker
Affiliation:
Department of Earth System Science, University of California Irvine, Irvine, California 92697-3100, USA
Alysha I Coppola
Affiliation:
Department of Earth System Science, University of California Irvine, Irvine, California 92697-3100, USA
Danielle S Glynn
Affiliation:
Department of Earth System Science, University of California Irvine, Irvine, California 92697-3100, USA
*
1Corresponding author. Email: edruffel@uci.edu.

Abstract

We report results of duplicate measurements of dissolved organic carbon concentrations ([DOC] as μM) and Δ14C in seawater in order to assess the total uncertainty of reported [DOC] and Δ14C measurements via the UV oxidation method. In addition, pure International Atomic Energy Agency standards analyzed over a 4-yr period are evaluated. We find the total uncertainty of Δ14C measurements to be ±4.0. However, in samples that were thawed, subsampled, and refrozen prior to UV oxidation, the total uncertainty of Δ14C measurements is on the order of ±10. The [DOC] measurements of these samples were also higher by 1.8 ± 0.3 μM. The reason(s) for these documented increases in total [DOC] and Δ14C uncertainty are unclear. In order to minimize any effects on sample measurements, we recommend the following: 1) regular monitoring of duplicate samples, DOC standards, and diluent (Milli-Q™) water for Δ14C and [DOC] measurements; 2) thawing a sample immediately and only once prior to UV oxidation; 3) avoid the use of DOC-leachable plumbing (such as PVC pipe) in both water systems feeding and within Milli-Q systems; and 4) consider the use of DOC-free diluents (i.e. pre-UV oxidized Milli-Q or sample water).

Type
Radiocarbon Reservoir Effects
Copyright
Copyright © 2013 by the Arizona Board of Regents on behalf of the University of Arizona 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Beaupré, SR, Druffel, ERM. 2009. Constraining the propagation of bomb-radiocarbon through the dissolved organic carbon (DOC) pool in the northeast Pacific Ocean. Deep-Sea Research I 56(10):1717–26.Google Scholar
Beaupré, SR, Druffel, ERM, Griffin, S. 2007. A low-blank photochemical extraction system for concentration and isotopic analyses of marine dissolved organic carbon. Limnology and Oceanography 5:174–84.Google Scholar
Griffin, S, Beaupré, SR, Druffel, ERM. 2010. An alternate method of diluting dissolved organic carbon seawater samples for 14C analysis. Radiocarbon 52(2–3):1224–9.Google Scholar
Southon, J, Santos, GM, Druffel-Rodriguez, K, Druffel, E, Trumbore, S, Xu, X, Griffin, S, Ali, S, Mazon, M. 2004. The Keck Carbon Cycle AMS laboratory, University of California, Irvine: initial operation and a background surprise. Radiocarbon 46(1):41–9.Google Scholar
Vogel, JS, Southon, JR, Nelson, DE. 1987. Catalyst and binder effects in the use of filamentous graphite for AMS. Nuclear Instruments and Methods in Physics Research B 29(1–2):50–6.CrossRefGoogle Scholar
Williams, PM, Druffel, ERM. 1987. Radiocarbon in dissolved organic carbon in the central North Pacific Ocean. Nature 330(6145):246–8.Google Scholar
Williams, PM, Oeschger, H, Kinney, P. 1969. Natural radiocarbon activity of the dissolved organic carbon in the north-east Pacific Ocean. Nature 224(5216):256–8.Google Scholar