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RD&D-Programme 2004 - SKB

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19.2.11 Advection/mixing – groundwater chemistry<br />

This section deals with the mixing that occurs due to the fact that the water moves at varying<br />

velocity in the fracture system in the rock and how the process influences the groundwater<br />

chemistry. The next section deals with advection and dispersion in connection with radionuclide<br />

transport.<br />

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

Mixing calculations, utilizing for example the code M3, that were originally carried out with<br />

data from the Äspö area have been supplemented by calculations including data from other<br />

investigated sites in Sweden and Finland. It turns out that the mixing pattern is similar, but the<br />

proportions of the different “typical waters” vary from site to site. However, there are clear<br />

similarities in the probable hydrological and chemical evolution undergone by the sites. Modern<br />

meteoric and glacial water can always be identified. Often, though not always, deep saline water<br />

is present, and in coastal locations modern and old seawater is always present.<br />

Results from the modelling exercise within the international Task 5 Äspö Task Force on<br />

Modelling of Groundwater Flow and Transport of Solutes showed that it is possible to numerically<br />

handle the advection/mixing process on a large scale and thereby utilize both hydrological<br />

and chemical data.<br />

SKI points out that <strong>SKB</strong> should also report the calculated salinity evolution for scenarios that<br />

involve extensive climate changes over long periods of time.<br />

Newfound knowledge since RD&D 2001<br />

New models for groundwater flow have been developed, see also section 19.2.3 concerning<br />

groundwater flow.<br />

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

The computer code M3, which is used for statistical processing by multivariate analysis, has<br />

been developed with support from <strong>SKB</strong>. M3 is planned to undergo a number of updates and<br />

verifications within the next six years.<br />

One of the models developed for groundwater flow (Darcy Tools) will be evaluated in a recently<br />

started project. The purpose is to model the conditions around Äspö by including both chemical<br />

parameters and hydrological data, see 19.2.3.<br />

Within the site investigations, site-specific mixing calculations will be important for understanding<br />

the evolution of the water on the site. Calculations of salinity evolution in connection with<br />

extensive climate changes over long periods of time will be carried out within the framework of<br />

the next few safety assessments. An attempt will be made to link hydrochemistry with hydrogeological<br />

data and calculations in coming site modellings and safety assessments.<br />

19.2.12 Advection/mixing – radionuclide transport<br />

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

No questions for further research were identified in RD&D-<strong>Programme</strong> 2001 or its review.<br />

RD&D-<strong>Programme</strong> 2001 dealt with flow-related transport parameters under the two headings<br />

“Groundwater transport” and “Radionuclide transport – molecular diffusion and matrix<br />

diffusion”.<br />

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

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