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RD&D-Programme 2004 - SKB

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pumped through the fracture for a long period. In the experiments, between 20 and 40 percent<br />

of the injected neptunium accompanied the groundwater in the form of uncomplexed neptunyl<br />

ion (NpO 2+ ) (same breakthrough as HTO). The longer the residence time in the fracture, the<br />

lower the concentrations of pentavalent neptunium were observed in the eluate. No plutonium<br />

was found in the eluate, while americium was found in concentrations on the order of 10 –11 mol/l<br />

/19-83/. Similar experiments have also been conducted in above-ground laboratories. Within the<br />

framework of RNR Actinide, batch sorption tests have also been performed in above-ground<br />

laboratories with the same actinides as in the field tests and fracture-filling material/crushed<br />

granite. These tests showed a clear time dependence for sorption of the actinides in question.<br />

Some knowledge of sorption has also emerged from the True experiments. These results are<br />

described below in section 19.2.26.<br />

Knowledge of sorption and sorption mechanisms is being compiled in the ongoing EU project<br />

Retrock /19-62/. The final report for Retrock will be completed during <strong>2004</strong>.<br />

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

Within the framework of actinide migration in a drill core with a longitudinal fracture, a test will<br />

be conducted with uranium and technetium using the same experimental set-up as for actinide<br />

migration (see above).<br />

It has emerged from various joint international projects, such as Geotrap within the OECD/NEA<br />

and Retrock within the EU, that a more process-oriented description of the retention processes<br />

that are often lumped together under the heading of sorption may be needed for the purposes of<br />

safety assessment as well. The processes that are principally of interest besides pure sorption<br />

are precipitation, co-precipitation and surface precipitation. The processes that are normally<br />

included in sorption are mainly ion exchange and surface complexation processes.<br />

Process-based models can provide better process understanding and be used to bound simplified<br />

models based on distribution coefficients at equilibrium (K d values). <strong>SKB</strong> plans to evaluate<br />

the need for process-oriented sorption modelling specifically for safety assessment during the<br />

current three-year period. If a need to develop this type of modelling capacity emerges, work<br />

will be initiated. An obvious advantage of models of this type is that they can be used to study<br />

how retention is affected by changes in groundwater chemistry, such as pH changes. A new<br />

task has also been proposed for the Äspö Task Force on Modelling of Groundwater Flow and<br />

Transport of Solutes that would involve reinterpreting the True-1 experiments with a more<br />

process-oriented modelling strategy for retention. <strong>SKB</strong> is also continuing to support more<br />

fundamental studies of surface complexation.<br />

During the current period, a licenciate project will be conducted to develop methods for<br />

determining K d values on intact pieces of rock with the aid of electrical methods. A problem<br />

with traditional measurements of K d values is that they are done either on crushed rock material<br />

or via diffusion tests on intact pieces of rock, which is more relevant but takes a very long time.<br />

The idea of the planned project is to investigate whether an electrical potential can be used to<br />

speed up the penetration of sorbing nuclides in intact pieces of rock. In preliminary tests with<br />

non-sorbing substances, the penetration rate increased by around a factor of 1,000 /19-84,<br />

19-85/.<br />

In the site investigation programme, sorption measurements on site-specific materials are<br />

also being carried out in the laboratory. These investigations are described in greater detail in<br />

/19-73/.<br />

RD&D-<strong>Programme</strong> <strong>2004</strong> 263

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