Preprints
https://doi.org/10.5194/cpd-5-463-2009
https://doi.org/10.5194/cpd-5-463-2009
13 Feb 2009
 | 13 Feb 2009
Status: this preprint was under review for the journal CP but the revision was not accepted.

How to treat climate evolution in the assessment of the long-term safety of disposal facilities for radioactive waste: examples from Belgium

M. Van Geet, M. De Craen, D. Mallants, I. Wemaere, L. Wouters, and W. Cool

Abstract. In order to protect man and the environment, long-lasting, passive solutions are needed for the different categories of radioactive waste. In Belgium, three main categories of conditioned radioactive waste (termed A, B and C) are defined by radiological and thermal power criteria. It is expected that Category A waste – low and intermediate level short-lived waste – will be disposed in a near-surface facility, whereas Category B and C wastes – high-level and other long-lived radioactive waste – will be disposed in a deep geological repository. In both cases, the long-term safety of a given disposal facility is evaluated. Different scenarios and assessment cases are developed illustrating the range of possibilities for the evolution and performance of a disposal system without trying to predict its precise behaviour. Within these scenarios, the evolution of the climate will play a major role as the time scales of the evaluation and long term climate evolution overlap. In case of a near-surface facility (Category A waste), ONDRAF/NIRAS is considering the conclusions of the IPCC, demonstrating that a global warming is nearly unavoidable. The consequences of such a global warming and the longer term evolutions on the evolution of the near-surface facility are considered. In case of a geological repository, in which much longer time frames are considered, even larger uncertainties exist in the various climate models. Therefore, the robustness of the geological disposal system towards the possible results of a spectrum of potential climate changes and their time of occurrence will be evaluated. The results of climate modelling and knowledge of past climate changes will merely be used as guidance of the extremes of climate changes to be considered and their consequences.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
M. Van Geet, M. De Craen, D. Mallants, I. Wemaere, L. Wouters, and W. Cool
 
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
M. Van Geet, M. De Craen, D. Mallants, I. Wemaere, L. Wouters, and W. Cool
M. Van Geet, M. De Craen, D. Mallants, I. Wemaere, L. Wouters, and W. Cool

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