During the development of the International Thermonuclear Experimental Reac
tor (ITER) fusion reactor, many efforts are done to minimise the amount of
radioactive waste that will arise from the decommissioning of a nuclear fus
ion power plant. Nevertheless, the most active waste types will have to be
disposed in a repository. The impact of possible future human actions on th
e performance of the repository has to be evaluated. The most active waste
types are selected from the inventory of fusion plant model PM-2 with low-a
ctivation martensitic steel as main material. After a cooling period of 100
years, the fusion waste is assumed to be disposed off in a repository loca
ted in the boom clay layer at the Mol site (Belgium). A systematic approach
for the identification of the relevant intrusion scenarios is applied. Thr
ee scenarios resulting from borehole drilling are identified as relevant, c
ore inspection, residence and unsealed borehole. This paper will focus on t
he analysis of the most drastic human intrusion scenario, i.e. the core ins
pection scenario. The maximum dose is calculated for waste arising from Be-
coatings. In the case of a routine inspection, the dose to a geological wor
ker is always under 0.5 Sv. This value, under which serious deterministic h
ealth effects are unlikely, can be considered as a reference level for acut
e exposure. In the case of the very pessimistic close inspection variant a
maximum dose of 0.4 Sv is calculated if the intrusion occurs immediately af
ter the disposal. After 60 000 years, the dose becomes lower than 3.5 mSv,
which is the average annual background dose. The results of an alternative
approach, considering a fusion-specific repository and wells drilling as th
e main intrusion scenario, are also included in this paper. Finally, a comp
arison of the consequences due to intrusion scenarios calculated for fusion
and fission waste is presented. For the most active fission waste types it
lasts 1 million years before the close inspection dose drops under 0.5 Sv.
(C) 2001 Elsevier Science B.V. All rights reserved.