A simple approach to determine the diffusivity of americium in granite
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Lai-Wu Song
, Xiao-gui Feng , J. Liang , Ying-jie Zhang und J. Wang
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.
© by Oldenbourg Wissenschaftsverlag, München, Germany
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- New cross section measurements for production of the positron emitters 75Br and 76Br via intermediate energy proton induced reactions
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- UC oxidation with HNO2 in aqueous solutions of HNO3 and HClO4
- A simple approach to determine the diffusivity of americium in granite
- Synthesis and crystal structures of new complexes of Np(V) glycolate with 2,2′-bipyridine, [NpO2(C10H8N2)(OOC2H2OH)]·1.5H2O and [NpO2(C10H8N2)(OOC2H2OH)]·2.5H2O
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