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Radiation Protection Dosimetry Advance Access published online on May 24, 2008

Radiation Protection Dosimetry, doi:10.1093/rpd/ncn162
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© The Author 2008. Published by Oxford University Press. All rights reserved. For Permissions, please email: journals.permissions@oxfordjournals.org

MOBILITY DETERMINATION OF LEAD ISOTOPES IN GLASS FOR RETROSPECTIVE RADON MEASUREMENTS

Mikko Laitinen1,*, Iiro Riihimäki1, Jörgen Ekman2, A. R. Ananda Sagari1, Lennart B. Karlsson2, Somjai Sangyuenyongpipat1, Sergey Gorelick1, Heikki Kettunen1, Heikki Penttilä1, Ragnar Hellborg3, Timo Sajavaara1, Johan Helgesson2 and Harry J. Whitlow1

1 Department of Physics, University of Jyväskylä (JYLF), P.O. Box 35, FIN-40014 Jyväskylä, Finland
2 School of Technology and Society, Malmö University, SE-205 06 Malmö, Sweden
3 Department of Physics, Lund university, P.O. Box 119, SE-22100 Lund, Sweden

* Corresponding author: mikko.laitinen{at}jyu.fi

Received December 22, 2007, amended April 8, 2008, accepted April 17, 2008

In retrospective radon measurements, the 22-y half life of 210Pb is used as an advantage. 210Pb is often considered to be relatively immobile in glass after alpha recoil implanted by 222Rn progenies. The diffusion of 210Pb could, however, lead to uncertain wrong retrospective radon exposure estimations if 210Pb is mobile and can escape from glass, or lost as a result of cleaning-induced surface modification. This diffusion was studied by a radiotracer technique, where 209Pb was used as a tracer in a glass matrix for which the elemental composition is known. Using the ion guide isotope separator on-line technique, the 209Pb atoms were implanted into the glass with an energy of 39 keV. The diffusion profiles and the diffusion coefficients were determined after annealing at 470–620°C and serial sectioning by ion sputtering. In addition, the effect of surface cleaning on diffusion was tested. From the Arrhenius fit, the activation enthalpy (H) was determined, which is equal to 3.2 ± 0.2 eV, and also the pre-exponential factor D0, in the order of 20 m2s–1. This result confirms the assumption that over a time period of 50 y 209Pb (and 210Pb) is effectively immobile in the glass. The boundary condition obtained from the measurements had the characteristic of a sink, implying loss of 209Pb in the topmost surface at high temperatures.


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