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RD&D-Programme 2004 - SKB

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2<br />

In Sea (mol)<br />

3<br />

Water Sea (mol/m 3 )<br />

1<br />

In Bay (mol)<br />

Concentration (mol/kg) 2<br />

Water Bay (mol/m<br />

In<br />

Sea<br />

3 )<br />

Sedimentation<br />

Water Bay<br />

(1)<br />

Conclusion<br />

Concentration (mol/kg)<br />

Resuspension<br />

Burial<br />

Sediments Bay<br />

(2)<br />

In<br />

Concentration (mol/m 3 )<br />

Bay<br />

In<br />

Out<br />

Sedimentation<br />

Water Sea<br />

(4)<br />

In<br />

Out<br />

Concentration<br />

(mol/kg)<br />

Resuspension<br />

Sediments Sea<br />

(5)<br />

Conclusion<br />

1<br />

Out (mol)<br />

In<br />

Concentration<br />

(mol/m 3 )<br />

Conclusion<br />

Deep Sediments Bay<br />

(3)<br />

Figure 20-1. Coast model from SR 97 constructed in Tensit. The graphic environment for<br />

constructing the model is similar to a conceptual formalization of the most important processes<br />

and state variables /20-30/.<br />

20.5 Transport processes<br />

The transport processes determine which ecosystems and organisms will be exposed to radionuclides<br />

and how great the dilution will be. Much of this is handled with current models, under<br />

the provision that the radionuclides are dissolved in water.<br />

A certain fraction of the radionuclides in the environment will be bound to particles, humus<br />

complexes and organisms. The transport of radionuclides in the biosphere is therefore dependent<br />

to a great extent on particle transport. Particle transport can be passive, as in the case of<br />

sedimentation and resuspension, or active, as in the case of transport via swimming organisms,<br />

food ingestion, trade, etc.<br />

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

It was described in RD&D 2001 that the water exchange models for coastal waters were<br />

improved in the Safe project /20-31, 20-32/, and that there is a model that covers the entire<br />

Baltic Sea and provides boundary conditions for the local coastal models /20-31/.<br />

In RD&D 2001 it is pointed out that the surface hydrology is important for understanding what<br />

transport pathways and dispersal and dilution processes affect contaminated water after it has<br />

left the rock. Several comments from the regulatory authorities have wished for deeper studies.<br />

In its review, for example, SSI said that in preparation for the safety assessments accompanying<br />

the permit applications, <strong>SKB</strong> should develop its analysis of radionuclide transport in the<br />

transition between geosphere and biosphere. Kasam wished to see a deeper understanding<br />

of the hydrological relationships between a deep repository and different ecosystems.<br />

See also section 20.2.<br />

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

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