Technical note: On the reliability of laboratory beta-source calibration for luminescence dating

The dose rate of the 90Sr / 90Y beta source used in most luminescence readers is a laboratory key parameter. There is a well-established body of knowledge about parameters controlling accuracy and precision of the calibration value but some hard-to-explain inconsistencies still exist. Here, we have...

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Main Authors: Mauz, Barbara (Author) , Martin, Loïc (Author) , Discher, Michael (Author) , Tribolo, Chantal (Author) , Kreutzer, Sebastian (Author) , Bahl, Chiara (Author) , Lang, Andreas (Author) , Mercier, Norbert (Author)
Format: Article (Journal)
Language:English
Published: 23 Jun 2021
In: Geochronology
Year: 2021, Volume: 3, Issue: 1, Pages: 371-381
ISSN:2628-3719
DOI:10.5194/gchron-3-371-2021
Online Access:Verlag, kostenfrei, Volltext: https://doi.org/10.5194/gchron-3-371-2021
Verlag, kostenfrei, Volltext: https://gchron.copernicus.org/articles/3/371/2021/
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Author Notes:Barbara Mauz, Loïc Martin, Michael Discher, Chantal Tribolo, Sebastian Kreutzer, Chiara Bahl, Andreas Lang, and Norbert Mercier

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520 |a The dose rate of the 90Sr / 90Y beta source used in most luminescence readers is a laboratory key parameter. There is a well-established body of knowledge about parameters controlling accuracy and precision of the calibration value but some hard-to-explain inconsistencies still exist. Here, we have investigated the impact of grain size, aliquot size and irradiation geometry on the resulting calibration value through experiments and simulations. The resulting data indicate that the dose rate of an individual beta source results from the interplay of a number of parameters, most of which are well established by previous studies. Our study provides evidence for the impact of aliquot size on the absorbed dose in particular for grain sizes of 50-200 µm. For this grain-size fraction, the absorbed dose is enhanced by ∼ 10 %-20 % as aliquot size decreases due to the radial increase of dose rate towards the centre of the aliquot. The enhancement is most variable for 50-100 µm grains mounted as aliquots of < 8 mm size. The enhancement is reversed when large grains are mounted as small aliquots due to the edge effect by which the dose induced by backscattered electrons is reduced. While the build-up of charge dictates the increase of absorbed dose with the increase of grain size, this principle becomes more variable with changing irradiation geometry. We conclude that future calibration samples should consist of subsamples composed of small, medium, large and very large quartz grains, each obtaining several gamma doses. The calibration value measured with small, medium and large aliquots is then obtained from the inverse slope of the fitted line, not from a single data point. In this way, all possible irradiation geometries of an individual beta source are covered, and the precision of the calibration is improved. 
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