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RD&D-Programme 2004 - SKB

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<strong>Programme</strong><br />

<strong>SKB</strong> does not consider sorption in bentonite to be a prioritized research area. However, existing<br />

data will be updated prior to each new safety report.<br />

17.2.27 Speciation of radionuclides<br />

The speciation of radionuclides is of importance for sorption and diffusion in the buffer. It<br />

is influenced by what speciation the nuclide had at the boundary to the buffer, i.e. inside the<br />

canister, but also by the chemical conditions in the buffer.<br />

The speciation process is discussed in section 15.2.14 and the evolution of the chemical<br />

environment in the buffer in section 17.2.23. In SR-Can, the same types of speciation<br />

calculations are carried out for e.g. the buffer environment as in SR 97.<br />

17.2.28 Radionuclide transport – colloid transport through bentonite<br />

The buffer is supposed to prevent colloids with radionuclides from escaping from a damaged<br />

canister.<br />

Conclusions in RD&D 2001 and its review<br />

In SKI’s opinion, <strong>SKB</strong> should investigate the importance for the safety assessment of the fact<br />

that organic colloids can diffuse through the buffer, as well as whether the same phenomenon<br />

applies to inorganic colloids.<br />

Newfound knowledge since RD&D 2001<br />

Diffusion of organic colloids in bentonite has been studied in a doctoral thesis /17-28/. The<br />

purpose of the thesis was to obtain knowledge of the sorption and diffusion of organic colloids<br />

in compacted bentonite, and to investigate whether bentonite is an effective barrier to colloids.<br />

The transport properties of radionuclides in bentonite may be altered in the presence of colloids<br />

due to the fact that speciation and sorption processes are altered. It was found that humic acids,<br />

unlike bentonite colloids, are stable in granitic groundwaters. Despite the fact that humic acids<br />

give rise to charged and relatively large aggregates, they diffuse easily through compacted<br />

bentonite (diffusivity D e about 10 –11 m/s). The experiments show that humic acid diffuses in the<br />

entire pore volume, i.e. both intralamellarly and in the spaces between particles. The transport of<br />

Eu(III) and Co(II) in bentonite increases significantly in the presence of humic colloids, while<br />

the transport of Sr(II) is unaffected.<br />

<strong>Programme</strong><br />

It is important that colloids that are formed inside the canister be filtered in the bentonite.<br />

According to /17-28/, it is clear that organic colloids are not filtered by the bentonite in the same<br />

way as inorganic colloids. Understanding of the properties of colloids in bentonite will require<br />

further research.<br />

226 RD&D-<strong>Programme</strong> <strong>2004</strong>

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