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14C Background Levels in An Accelerator Mass Spectrometry System

Published online by Cambridge University Press:  18 July 2016

J S Vogel ,
D E Nelson  and
J R Southon
J S Vogel
Affiliation:
Department of Archaeology, Simon Fraser University Burnaby, British Columbia V5A 1S6 Canada
D E Nelson
Affiliation:
Department of Archaeology, Simon Fraser University Burnaby, British Columbia V5A 1S6 Canada
J R Southon
Affiliation:
Department of Archaeology, Simon Fraser University Burnaby, British Columbia V5A 1S6 Canada
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Abstract

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The levels and sources of the measurement background in an AMS 14C dating system have been studied in detail. The relative contributions to the total background from combustion, graphitization, storage, handling, and from the accelerator were determined by measuring the C concentrations in samples of anthracite coal ranging in size from 15μg to 20mg. The results show that, for the present system, the uncertainty in the background is greater than that due to measurement precision alone for very old or for very small samples. While samples containing 100μg of carbon can yield useful 14C dates throughout the Holocene, 200 to 500μg are required for dating late Pleistocene materials. With the identification of the procedures that introduce contamination, the level and uncertainty of the total system background should both be reducible to the point that 100μg of carbon would be sufficient for dating most materials.

Type
Research Article
Information
Radiocarbon , Volume 29 , Issue 3 , 1987 , pp. 323 - 333
Copyright
Copyright © The American Journal of Science 

References

Boutton, T W, Wong, W W, Hachey, D L, Lee, L S, Cabrera, M P and Klein, P D, 1983, Comparison of quartz and Pyrex tubes for combustion of organic samples for stable carbon isotope analysis: Anal Chem, v 55, p 1832–1833.CrossRefGoogle Scholar
de Boer, J H, 1968, The dynamical character of adsorption: Oxford, Clarendon Press.Google Scholar
Dozier, W D, Drake, J M and Klafter, J M, 1986, Self-diffusion of a molecule in porous Vycor glass: Phys Rev Letters, v 56, no. 2, p 197–200.CrossRefGoogle ScholarPubMed
Eitel, W, 1966, Silicate science, vol 4: New York, Academic Press.Google Scholar
Emmett, P H and DeWitt, T W, 1943, The low temperature adsorption of nitrogen, oxygen, argon, hydrogen, n-butane, and carbon dioxide on porous glass and on partially hydrated chabazite: Jour Am Ceramic Soc, v 65, no. 7, p 1253–1262.Google Scholar
Nelson, D E and Hobson, K A, Simon Eraser University radiocarbon dates I: Radiocarbon, v 24, no. 3, p 344–351.CrossRefGoogle Scholar
Nelson, D E, Southon, J R, Vogel, J S, Korteling, R and Ku, T-L, 1984, Progress in 14-C and 10-Be dating at SFU: Nuclear Instruments & Methods, v B5, p 136–143.Google Scholar
Nelson, D E, Vogel, J S, Southon, J R and Brown, T A, 1986, Accelerator radiocarbon dating at SFU, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, v 28, no. 2A, p 215–222.Google Scholar
Nordberg, M E, 1944, Properties of some Vycor brand glasses: Jour Am Ceramic Soc, v 27, no. 10, p 299–305.Google Scholar
Schwertz, F A, 1949, Fluid flow study of porous glass: Jour Am Ceramic Soc, v 32, no. 12, p 390–393.CrossRefGoogle Scholar
Vogel, J S, Southon, J R, Nelson, D E and Brown, T A, 1984, Performance of catalytically condensed carbon for use in accelerator mass spectrometry: Nuclear Instruments & Methods, v B5, p 289–293.Google Scholar