Publicatie Laka-bibliotheek:
Safety consequences of the release of radiation induced stored energy (1994)
| Auteur | ECN, Prij |
| Datum | augustus 1994 |
| Classificatie | 6.01.5.51/40 (AFVAL - OPSLAG OP LAND (oa ZOUT/KLEI)) |
| Voorkant |
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Uit de publicatie:
Safety consequences of the release of radiation induced stored energy ABSTRACT Due to the disposal of high level waste (HLW) in a salt formation gamma energy will be deposited in the rock salt. Most of this energy will be converted into heat, whilst a small part will create defects in the salt crystals. It has been shown that energy is stored in the damaged crystals. Due to uncertainties in the models and differences inthe disposal concepts the estimated values for the stored energy range from 10 to 1000 J/g in the most heavily damaged crystals close to the waste containers. The amount of radiation damage decays exponentially with increasing distance from the containers and at distances larger than 0.2 m the stored energy can be neglected. Given the uncertainties in the model predictions and in the possible release mechanism this report concludes that at this moment an instantaneous release of stored energy cannot be excluded completely. Therefore the thermo-mechanical consequences of a postulated instanteous release of an extremely high amount of radiation induced stored penergy have been estimated. These estimations are based on the quasi-static solutions for line and point sources. To account for the dynamic effects and the occurrence of fractures an amplification factor has been derived from mining experience with explosives. A validation of this amplification factor has been given using post experimental observations of two nuclear explosions in a salt formation. For some typical disposal concepts in rock salt the extent of the fractured zone has been estimated. It appeared that the radial extent of the fractured zone is limited to 5 m. Given the much larger distance between the individual boreholes and the distance between the boreholes and the boundary of the salt formation (more than 100 m), it is concluded that the probability of a release of radiation induced stored energy creating a pathway for the nuclides from the containers to the groundwater, is extremely low. The radiological consequences of a groundwater intrusion scenario induced by this very unprobable pathway are bounded by the 'standard' groundwater intrusion-extrusion scenario used in the performance assessment (smaller than 10-8 Sv/a).
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