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Radiocarbon Dating of Iron Artifacts at the Erlangen AMS Facility

Published online by Cambridge University Press:  18 July 2016

Andreas Scharf ,
Wolfgang Kretschmer ,
Gerhard Morgenroth ,
Thomas Uhl ,
Karin Kritzler ,
Katja Hunger  and
Ernst Pernicka
Andreas Scharf*
Affiliation:
Physikalisches Institut Abt. IV, Erwin–Rommel–Str.1, Universität Erlangen, 91058 Erlangen, Germany. Email: [email protected].
Wolfgang Kretschmer
Affiliation:
Physikalisches Institut Abt. IV, Erwin–Rommel–Str.1, Universität Erlangen, 91058 Erlangen, Germany. Email: [email protected].
Gerhard Morgenroth
Affiliation:
Physikalisches Institut Abt. IV, Erwin–Rommel–Str.1, Universität Erlangen, 91058 Erlangen, Germany. Email: [email protected].
Thomas Uhl
Affiliation:
Physikalisches Institut Abt. IV, Erwin–Rommel–Str.1, Universität Erlangen, 91058 Erlangen, Germany. Email: [email protected].
Karin Kritzler
Affiliation:
Physikalisches Institut Abt. IV, Erwin–Rommel–Str.1, Universität Erlangen, 91058 Erlangen, Germany. Email: [email protected].
Katja Hunger*
Affiliation:
Institut für Archäometrie, Gustav–Zeuner–Str. 5, TU Bergakademie Freiberg, 09599 Freiberg, Germany.
Ernst Pernicka*
Affiliation:
Physikalisches Institut Abt. IV, Erwin–Rommel–Str.1, Universität Erlangen, 91058 Erlangen, Germany. Email: [email protected].
*
Corresponding author. Email: [email protected].
Email: [email protected].
Email: [email protected].
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Abstract

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One problem in preparing iron for radiocarbon dating is the low carbon content which makes the sample size needed too large for some sample combustion systems. Also, the metallic character of the samples complicates sample combustion or oxidation. The Erlangen accelerator mass spectrometry group uses an elemental analyzer for the sample combustion, directly followed by a reduction facility. As the carbon content and sample size for iron samples are unsuitable for combustion in an elemental analyzer, 2 alternative approaches are to (a) avoid oxidation and reduction, or (b) extract the carbon from the iron, prior to combustion. Therefore, 2 different pathways were explored. One is direct sputtering of the unprocessed iron sample in the ion source. The other is the complete chemical extraction of carbon from the iron sample and dating of the carbonaceous residue. Also, different methods for cleaning samples and removing contamination were tested. In Erlangen, a Soxhlet extraction is employed for this purpose. Also, the sampling of the iron sample by drilling or cutting can be a source of contamination. Thus, the measurement of iron drill shavings yielded ages that were far too high. The first results for iron samples of known age from 2 archaeological sites in Germany are presented and discussed.

Type
Articles
Information
Radiocarbon , Volume 46 , Issue 1: Proceedings of the 18th International Radiocarbon Conference (Part 1 of 2), Conference Editors: Nancy Beavan Athfield, Rodger J Sparks , 2004 , pp. 175 - 180
Copyright
Copyright © 2004 by the Arizona Board of Regents on behalf of the University of Arizona 

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