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    Measurement of Low 14C Activities in a Liquid Scintillation Counter in the Zagreb Radiocarbon Laboratory

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    Author
    Horvatinčić, Nada
    Barešić, Jadranka
    Krajcar Bronić, Ines
    Obelić, Bogomil
    Issue Date
    2004-01-01
    Keywords
    absolute age
    absorption method
    archaeology
    benzene synthesis method
    C 14
    carbon
    carbon dioxide
    Croatia
    errors
    Europe
    instruments
    isotopes
    liquid scintillation methods
    measurement
    methods
    radioactive isotopes
    Southern Europe
    Zagreb Croatia
    Zagreb Radiocarbon Laboratory
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    Citation
    Horvatinčić, N., Barešić, J., Bronić, I. K., & Obelić, B. (2004). Measurement of low 14C activities in a liquid scintillation counter in the Zagreb Radiocarbon Laboratory. Radiocarbon, 46(1), 105-116.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 18th International Radiocarbon Conference held in Wellington, New Zealand, September 1-5, 2003.
    URI
    http://hdl.handle.net/10150/654845
    DOI
    10.1017/S0033822200039412
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Two methods of chemical preparation of radiocarbon samples are implemented in the Zagreb Radiocarbon Laboratory for measurement by a new liquid scintillation counter (LSC), Quantulus 1220(TM): a CO2 absorption method (LSC-A) and a benzene synthesis method (LSC-B). For samples prepared by both methods, the optimal counting windows for measurement in LSC were determined. The total efficiency of LSC-A is 65% and that of the LSC-B is 83%, while the corresponding 14C dating limits are 31,800 yr and 52, 160 yr, respectively. 14C activities measured by the LSC-A and LSC-B methods were compared with those measured by the gas proportional counter (GPC) method (efficiency 75%, 14C dating limit 37,500 yr). The results obtained by the LSC-A method have larger errors than those measured by the GPC method, but LSC-A is quick, inexpensive, simple, and requires less carbon than the GPC method. Thus, LSC-A is suitable for 14C measurements of geological, hydrological, and environmental samples. On the other hand, the results obtained by the LSC-B method give smaller errors and a larger 14C dating range. Therefore, LSC-B is more suitable for 14C dating of archaeological samples.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200039412
    Scopus Count
    Collections
    Radiocarbon, Volume 46, Number 1 (2004)

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