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Euradwaste '08 - EU Bookshop - Europa

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3. Results<br />

3.1 Impact of the thermal output of the waste on the repository's dimensions<br />

The minimum lengths of the galleries for disposal of SF and HLW are derived from heat dissipation<br />

calculations by ensuring that the temperature limitations are respected; in the disposal concepts considered<br />

in this study these are that the temperature has to remain below 100 °C in the bentonite<br />

buffer for granite and at the interface between the gallery liner and the host formation for clay. As<br />

the thermal output of the ILW canisters is negligible, the length of the ILW galleries is determined<br />

by the number and size of the disposal containers. An overview of the estimated lengths of the SF<br />

and HLW disposal galleries is given in Table 1.<br />

Table 1: Estimated lengths of the SF and HLW disposal galleries<br />

Fuel cycle scenario<br />

Granite<br />

A1 A2 A3 B1 B2<br />

SF + HLW gallery length (m/TWhe) 8.89 11.12 5.52 3.63 4.49<br />

relative SF + HLW gallery<br />

length<br />

Clay<br />

(-) 1.00 1.25 0.62 0.41 0.51<br />

allowable thermal output (50 a) (W/m) 353 332-376 365 379 379<br />

SF + HLW gallery length (m/TWhe) 5.92 5.74 3.48 1.88 2.89<br />

relative SF + HLW gallery<br />

length<br />

(-) 1.00 0.97 0.59 0.32 0.49<br />

3.2 Evaluation of the radiological impact in the case of the reference scenario<br />

The dose to a member of the reference group in the case of the reference scenario, which is associated<br />

with radionuclide transport in groundwater, was calculated by making a number of simplifying<br />

assumptions. For granite it was assumed that the canisters will fail between 1300 and 10 000 years,<br />

and that waste matrix lifetimes are 72 000 years for HLW, 10 million years for uranium oxide SF<br />

and 1 million years for MOX SF. For clay the canister lifetime was assumed to be 2000 years, and<br />

the waste matrix lifetimes 100 000 years for HLW and 200 000 years for SF. For granite sorption<br />

on the buffer and on minerals of the host formation was taken into account, whereas for clay sorption<br />

on the buffer was neglected. The calculated doses, normalised per produced electricity, are<br />

shown in Figs. 3 and 4 for a repository in granite and clay respectively. The radiotoxicity released<br />

from the repository into the environment was also calculated. Table 2 compares the radiotoxicity<br />

released over a 10 million years period with the initial radiotoxicity in the disposed waste. In most<br />

recent safety cases, a time cut-off of 1 million years is used; however for the purpose of Red-Impact<br />

it was considered more appropriate to consider a longer time scale of 10 million years to illustrate<br />

that also at the very long-term no considerable change in the radiological impact has to be expected<br />

from P&T.<br />

Table 2: Comparison between initial radiotoxicity in the disposed SF and HLW (50 years cooling<br />

prior to disposal) and the radiotoxicity released from the geological repository into the environment<br />

over a 10 million years period.<br />

Fuel cycle<br />

Initial radiotoxicity (50 Released radiotoxicity (10<br />

a)<br />

Ma) Containment factor<br />

(Sv/TWhe) (Sv/TWhe) (-)<br />

145

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