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A simple approach to determine the diffusivity of americium in granite

  • Lai-Wu Song , Xiao-gui Feng , J. Liang , Ying-jie Zhang und J. Wang
Veröffentlicht/Copyright: 4. Dezember 2009

Abstract

The diffusivities of the key radionuclides in host rock are important for the performance assessment of repositories. One of the conventional methods for determining the diffusivities of radionuclides is to grind the rock tablet layer by layer and then to measure the radioactivity remaining on the rock tablet before each grinding cycle. Since grinding hard rock samples, especially those with radioactivity, is very difficult, we developed a new approach to determine the diffusivity of americium in granite. The new approach mainly includes two parts: one is to measure the radioactivities from both sides of a rock disk sample by autoradiography with phosphor imaging technique; the other is to study the relationship between the radioactivities and the apparent diffusivity of americium in granite by computer modelling. Because the high contamination risk of grinding radioactive rock samples has been avoided, the new approach is much simpler than the conventional method. It may be a better choice of measuring the diffusivities of radionuclides in rock, especially for those laboratories in which grinding radioactive rock samples is inconvenient.


* Correspondence address: Institue of Nuclear and New Energy Technology, Tsinghua University, P.O. Box 1021, 102201 Beijing, Volksrepublik China,

Published Online: 2009-12-04
Published in Print: 2009-10

© by Oldenbourg Wissenschaftsverlag, München, Germany

Heruntergeladen am 25.10.2025 von https://www.degruyterbrill.com/document/doi/10.1524/ract.2009.1651/html
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