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RD&D-Programme 2004 - SKB

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comprehensive and gives evidence of a good understanding of relationships between initial<br />

properties and long-term processes, and that there is no reason to assume that a buffer with<br />

acceptable properties cannot be found.<br />

However, SKI points out that it is difficult on the basis of <strong>SKB</strong>’s account in the RD&Dprogramme<br />

to make independent judgements of individual areas due to couplings and<br />

repercussions on other areas.<br />

17.1 Initial state of the buffer<br />

17.1.1 Variables<br />

In SR 97, the buffer was described by a set of variables, see Table 17-1.<br />

The initial state, i.e. the value these variables were assumed to have at the time of deposition,<br />

was described in the main report of SR 97, section 6.4 /17-1/. The research programme around<br />

the initial state for the different variables in the buffer is described in the following.<br />

Table 17-1. Variables for the buffer and the backfill.<br />

Variable<br />

Geometry<br />

Pore geometry<br />

Radiation intensity<br />

Temperature<br />

Montmorillonite<br />

content<br />

Water content<br />

Gas contents<br />

Hydrovariables<br />

Swelling pressure<br />

Montmorillonite<br />

composition<br />

Pore water<br />

composition<br />

Impurity levels<br />

Definition<br />

Geometric dimensions of buffer/backfill. A description of e.g. interfaces on the inside towards<br />

the canister and on the outside towards the geosphere.<br />

Pore geometry as a function of time and space in buffer and backfill. The porosity, i.e. the<br />

fraction of the volume that is not occupied by solid material, is often given.<br />

Intensity of α, β, γ and neutron radiation as a function of time and space in buffer and backfill.<br />

Temperature as a function of time and space in buffer and backfill.<br />

Montmorillonite content as a function of time and space in buffer and backfill.<br />

Water content as a function of time and space in buffer and backfill.<br />

Gas contents (including any radionuclides) as a function of time and space in buffer and backfill.<br />

Flows and pressures for water and gas as a function of time and space in buffer and backfill.<br />

Swelling pressure as a function of time and space in buffer and backfill.<br />

Chemical composition of the montmorillonite (including any radionuclides) in time and space<br />

in buffer and backfill. This variable also includes material sorbed to the montmorillonite surface.<br />

Composition of the pore water (including any radionuclides and dissolved gases) in time<br />

and space in buffer and backfill.<br />

Levels of impurities in time and space in buffer and backfill. Impurities also include<br />

other minerals than montmorillonite. In backfill, crushed rock is counted as an impurity.<br />

17.1.2 Geometry<br />

The geometry of the buffer is determined by the dimensions of the canister and the thickness<br />

of the buffer material required to obtain the desired function. In SR 97 and RD&D 2001, the<br />

dimensions of the canister were given and the dimensions of the buffer were set at 35 cm on<br />

the sides of the canister, 50 cm underneath the canister and 150 cm above the canister. These<br />

dimensions still apply to KBS-3V, while there are small differences for KBS-3H.<br />

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

SKI points out that <strong>SKB</strong> must make the choice of an optimal buffer (properties and availability)<br />

before a permit application is submitted. Kasam takes a positive view of <strong>SKB</strong>’s plans to conduct<br />

studies of alternative buffer materials in order to get an alternative reference to bentonite with a<br />

high montmorillonite content.<br />

RD&D-<strong>Programme</strong> <strong>2004</strong> 195

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