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Full text: Modelling of marine dispersion and transfer of radionuclides accidentally released from land based facilities

77 DESCRIPTION OF THE NRPA BOX MODEL The Norwegian Radiation Protection Authority’s (NRPA) box model uses a modified approach for compartmental modelling [I-1–3] which allows for dispersion of radionuclides over time. The box structures for surface, mid-depth and deep water layers have been developed based on the description of polar, Atlantic and deep waters in the Arctic Ocean and the Northern Seas and site specific information for the boxes generated from the 3-D hydrodynamic model NAOSIM [I-4]. The structure of the NRPA’s box model is presented in Figure I-1. The NRPA box model includes the processes of advection of radioactivity between compartments, sedimentation, di?usion of radioactivity through pore water in sediments, particle mixing, pore water mixing and a burial process of radioactivity in deep sediment layers. Radioactive decay is calculated for all compartments and the contamination of biota is further calculated from the radionuclide concentrations in filtered seawater in the di?erent water regions. Doses to humans are calculated on the basis of seafood consumption, in accordance with available data for seafood catches and assumptions about human diet in the respective areas. Dose rates to biota are developed on the basis of calculated radionuclide concentrations in marine organisms, water and sediment, using dose conversion factors. Its structure, for the Baltic Sea only, is presented in Figure I-2. The equations of the transfer of radionuclides between the boxes are of the form: ??? ?? = ? ??,?????? ? ??? +??,??? ? ? ??? ? ??,?????? ? ??? + ??,??? ? ????? (? ? ??) + ??; ? ? ?? ? ??? (I-1) ?? = 0; ? ? ?? (I-2) where ki,i = 0 for all i, Ai and Aj are activities (Bq) at time t in boxes i and j; ki,j and kj,i are rates of transfer (y?1) between boxes i and j; ki is an e?ective rate of transfer of activity (y?1) from box i taking into account loss of material from the compartment without transfer to another, for example due to radioactive decay; Qi is an input of radionuclides into box i (Bq/y); n is the number of boxes in the system, Ti is the time of availability for box i (the first time when box i is open for dispersion of radionuclides) and ? is a unit function: ?(?) = ?1 ? ? ??0 ? < ?? (I-3) The times of availability: ?? = ?????(??,??)??? ? ??,? ?,? (I-4)
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