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Euradwaste '08 - EU Bookshop - Europa

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one study, the compartment structures should be identical, or at least as similar as possible, in order<br />

to allow a comparison of the results. Since performance indicators are not based on a safety statement<br />

they do not require any reference value and their use is more flexible. Performance indicators<br />

are very important for the understanding of the modelled processes and they can be used for optimising<br />

the repository system. Finally not every applied performance indicator may be used in the<br />

safety case, but most of them give valuable arguments for increasing the confidence in the safety of<br />

a repository system.<br />

With respect to the work concerning safety and performance indicators several test cases have been<br />

defined and applied to host rocks such as clay and rock salt, for which the use of safety and performance<br />

indicators has hardly been investigated in detail yet. The general approach is based on the<br />

SPIN methodology. Preliminary results suggest that this methodology works well for all kinds of<br />

host rock. Some new indicators have been identified, which are tested within PAMINA with results<br />

still pending. It is evident, that performance indicators give a good insight to the functioning of the<br />

system. In this context it was observed that performance indicators applied to specific radionuclides<br />

are useful for identifying influential processes. Finally it is noted that performance indicators are<br />

dependent on repository systems and host rocks.<br />

4. RTDC4<br />

In RTD component 4 several benchmark exercises are carried out, in which quantitative comparisons<br />

are made of approaches that, on the one hand, rely on simplifying assumptions and models,<br />

and on the other hand, on complex models that take into account a more complete process conceptualization<br />

in space and time. The main objective is to evaluate the added value of using more complex<br />

and more realistic modelling approaches not yet fully accounted for in PA. This RTD component<br />

comprises of three work packages.<br />

The first work package focuses on processes which determine the evolution of the near field of a<br />

repository in salt as host rock. One aspect being investigated is the convergence process of rock<br />

salt, which determines the advective flow of radionuclides in case of a repository completely filled<br />

with solution. For several test cases results are compared from different approaches to model this<br />

complex process which depends on many parameters. Also the brine intrusion process into a backfilled<br />

drift and the radionuclide transport by density driven exchange are investigated for salt as<br />

host rock.<br />

Specific benchmarks have been set up to study the reactive transport of radionuclides for clay as<br />

host rock. One exercise investigates Cs migration, considering all competitive effects on sorption<br />

processes. Both empirical and thermodynamic models are defined for geochemical modelling. Another<br />

exercise focuses on heavy elements behaviour with regard to sorption and precipitation processes.<br />

Also, benchmarks are carried out for sensitivity analysis on “Kd” and “solubility limit” models<br />

/ geochemical transport with respect to radionuclide migration in the near field. In case of granite<br />

as host rock benchmark calculations using the reactive transport code CORE and GoldSim as PA<br />

code aim to draw conclusions on the usefulness and the need of implementing fully reactive transport<br />

in PA models instead of the Kd and solubility limit approach commonly used in PA.<br />

The second work package is to investigate the usefulness of codes dealing with geometric complex<br />

representations of the geosphere in comparison to coarse or simplified 1D representations often<br />

used in PA codes for modelling the transport behaviour of radionuclides in the far field. Part of this<br />

work is described in the following for a repository located in rock salt. Typically, the water in the<br />

aquifer that is in contact with the cap rock of the salt dome is highly saline, while other aquifers at<br />

373

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