Theoretical determination of the size of the emergency planning zones pertinent to a postulated severe accident of the SAFARI-1 research reactor at NECSA due to gaseous releases
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North-West University (South Africa)
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Abstract
In South Africa the requirement for emergency planning at nuclear
installations is a statutory requirement. Emergency planning consists of two
distinct functions, preparedness and response. The preparedness functions
deals proactively with issues such as threat quantification, the infrastructure
and resources to manage the threat, and aspects of mitigating the
consequences to the worker, public and environment. The response function ,
on the other hand, deals with actions and organisations implemented during
the event. Preparedness therefore is the planning and preparation function
and response is the actual implementation of all the planned activities.
Due to the public sensitivity to effects of radiological and nuclear
emergencies, it is of the utmost importance to be appropriately prepared to
manage any unplanned event, even those of very low probabilities, before it
manifests. Preparedness commences with threat identification and threat
quantification. The design of the facility should eliminate most of the threats.
However, those of very low frequencies would not be accounted for by design.
It is for these events that the emergency plan must be in place.
At SAFARl-1 , the research reactor at Necsa, changes were made to the
composition of the fuel elements. These changes would affect on the
quantities of radioactive material that could be released under remote
circumstances. That necessitated a recalculation of the extent of planning
and the size of the zone for which this planning is performed. The emergency
planning zone at question is that in which urgent protective actions may
require implementation. Off-site consequences are included.
The perimeter of the radial zone was derived to be at the level at which
sheltering, as a protective action, is to be implemented. Calculation of the
zone size was performed with acceptable codes, PC COSYMA and lnterras.
The input data required for the use of the code, include amongst other, the
source term and meteorological information.
The outputs of the codes were compared with work done previously on fuel
elements containing 200g U-235. It was concluded, from the results of this
work, that the size of the urgent protective may be reduced to less than one
kilometre from the point of release, if all the assumptions that were made are
valid and all the uncertainties regarding the source term and dispersion
modelling are acceptable. However more work is required on the validation of
the model, the verification of assumptions and uncertainties regarding the
source term.
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MSc, North-West University, Mahikeng Campus
