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COMPLETE DOCUMENT (1862 kb) - OECD Nuclear Energy Agency

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Figure II.34 Cavern-convection scenario, evolution of individual dose rate<br />

for the most important nuclides (I-129*: refers to full 129 I inventory in spent fuel)<br />

10 -6<br />

Total<br />

Dose rate (Sv/year)<br />

10 -7<br />

10 -8<br />

10 -9<br />

10 -10<br />

I-129<br />

Np-chain<br />

Se-79<br />

10 -5 10 3 10 4 10 5 10 6<br />

I-129*<br />

U-Ra-chain<br />

Am-chain<br />

Th-chain<br />

10 -11<br />

C-14<br />

10 -12<br />

Tc-99<br />

Time (year)<br />

In 1988, a comparative performance study (PAGIS) was undertaken within the framework of<br />

the European Commission in order to assess the long-term impact of the disposal of HLW resulting<br />

from a conceptual 10 GWe reactor park operated for 30 years. The equivalent of 8 180 tHM glass<br />

canisters (about 900 m 3 vitrified HLW) were considered as the radioactive source term (fission<br />

products, minor actinides and corrosion products). The calculations were refined in the PACOMA [193]<br />

and EVEREST [194] projects.<br />

The actinides Am and Cm and the daughter product 240 Pu decay completely within the first<br />

10 m of the clay layer. This is not the case with 237 Np or with uranium if it were disposed of. The<br />

maximum annual dose due to the presence of 237 Np is about 0.02 µSv/year when the use of drinking<br />

water from a well in the upper aquifer near the clay layer is considered as the main pathway. According<br />

to the same scenario, the doses due to 135 Cs and 99 Tc amount to 0.015 µSv/year and 0.15 µSv/year,<br />

respectively. Figure II.36 shows the contribution of the different nuclides.<br />

In a climate change scenario, where water underlying the clay layer might be used for drinking<br />

purposes, the dose to man due to 129 I would reach the tolerance level of 0.2 mSv/year if all the iodine<br />

waste (as AgI) recovered from the effluents of the reprocessing plant were stored in the clay repository.<br />

Since 95 to 99% of 129 I is separated from the HLW during the reprocessing operations and<br />

discharged in the ocean, only 1 to 5% is supposed to be associated with the cladding materials, so the<br />

dose resulting from the leaching and migration of 129 I in the near field comes from MLW and would<br />

amount to 30 µSv/year. Partitioning of 129 I during reprocessing and washing of the hulls in order to<br />

minimise the residual quantities of iodine is therefore very important. Conventional transmutation of<br />

iodine waste by n-γreaction in LWRs has proved not to be very effective. Selective transmutation<br />

228

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