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RD&D-Programme 2004 - SKB

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19.2.26 Integrated modelling – radionuclide transport<br />

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

It was observed in RD&D 2001 regarding model studies that the one-dimensional description<br />

of transport and the dispersion formulation should be evaluated with the aid of more complex<br />

models. It was further observed that Farf31 should be compared with models with a higher<br />

process complexity for retention. The reference was specifically to models with heterogeneity<br />

in diffusion and sorption properties in the matrix. Finally, it was observed that Farf31 should<br />

be updated with respect to how input data are formulated so that information regarding the<br />

transport resistance can be used directly in the model.<br />

In RD&D 2001, it was observed with regard to field studies that further evaluation of True<br />

Block Scale results should be done.<br />

In its evaluation of RD&D 2001, SKI supported the development of transport models for<br />

radionuclides that can take heterogeneity (variable penetration depth) in matrix properties<br />

into account. Further, SKI wanted to see a report that summarized conceptual assumptions,<br />

mathematical formulations and scientific support for Farf31. SKI also observes that if the results<br />

from True indicate that retention can only be described in the context of transport in a threedimensional<br />

network of fractures, <strong>SKB</strong> should describe the simplification errors that can result<br />

from an application in the one-dimensional Farf31 model.<br />

Newfound knowledge since RD&D 2001<br />

Model studies<br />

In the international Äspö Task Force on Modelling of Groundwater Flow and Transport of<br />

Solutes, Task 4 has been completed and Task 6 is in progress. Task 4 dealt with numerical<br />

modelling of the True-1 experiments; Task 6 deals with upscaling of transport to time and space<br />

scales that are relevant to the needs of the safety assessment.<br />

The modelling in Task 4 has been evaluated, and it turned out that most of the modelling groups<br />

utilized similar conceptualization of the retention processes /19-99/. All groups included matrix<br />

diffusion and equilibrium sorption as the dominant mechanisms in the modelling of the experiment.<br />

However, the predictions exhibit a progressively increasing spread for the more strongly<br />

sorbing tracers (for example cesium). Remaining uncertainties in modelling and evaluation of<br />

results are judged to be mainly due to incomplete knowledge of the flow field in the experiment.<br />

In Task 6, modelling results have been presented for the two initial phases. In these phases,<br />

transport has been modelled in a single fracture (length scale 10 metres) for experimental time<br />

scales and for time scales of relevance to a safety assessment. The purpose of these two exercises<br />

has been to evaluate how different conceptualizations and models behave when the time<br />

scale increases. Final results have not yet been presented. In Task 6C, a fracture network model<br />

with associated retention parameterization has been constructed on a 200-metre scale for use in<br />

the later parts of Task 6 /19-100/. The method presented in this report has also served as a basis<br />

for formulating a strategy for the modelling of transport properties within the site investigation<br />

/19-101/.<br />

An evaluation of how retention mechanisms in connection with radionuclide transport should<br />

be incorporated in modelling in safety assessment has also been done within the EU project<br />

Retrock. Specifically, a number of open questions and recommendations have been compiled.<br />

The final report is expected to be finished in <strong>2004</strong>, but it can already be concluded that most of<br />

the questions and recommendations presented are covered by activities in the geosphere part of<br />

this RD&D-programme.<br />

A validity document for <strong>SKB</strong>’s code for radionuclide transport in the geosphere, Farf31, has<br />

been published /19-102/. The document discusses numerical verification of the code and then<br />

concludes regarding validation that the code is suitable for its stated purposes. These purposes<br />

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

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