Radiocarbon mass balance for a Magnox nuclear power station

Annals of Nuclear Energy, Volume 75, 2015, Pages 665–671.

M.P. Metcalfe1, R.W. Mills2

  1.  National Nuclear Laboratory, Stonehouse Park, Bristol Road, Stonehouse, Gloucestershire GL10 3UT, United Kingdom.
  2. National Nuclear Laboratory, Central Laboratory, Sellafield, Seascale, Cumbria CA20 1PG, United Kingdom.

 

Abstract

Nuclear power generation in the United Kingdom is based principally on graphite-moderated gas-cooled reactors. The mass of irradiated graphite associated with these reactors, including material from associated experimental, prototype and plutonium production reactors, exceeds 96,000 tonnes. One of the principal long-lived radionuclides produced during graphite irradiation is radiocarbon (C-14). Its potential as a hazard must be taken into account in decommissioning and graphite waste management strategies. While C-14 production processes are well-understood, radionuclide distributions and concentrations need to be characterised. A common misconception is that generic statements can be made about C-14 precursors and their location. In fact, the composition of the original manufactured material, the chemical environment of the graphite during service and its irradiation history will all influence C-14 levels. The analysis presented here provides the first assessment of the principal C-14 activation pathways for a UK Magnox reactor. Activation modelling has been used to predict C-14 production rates in both the graphite core and the carbon dioxide coolant over a selected period of operation and the results compared with monitored site C-14 discharges. Principal activation routes have been identified, which should inform future graphite waste management strategies relating to radiocarbon.

 

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