2002
DOI: 10.1016/s1568-2692(02)80042-0
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3-D numerical modelling of mud and radionuclide transport in the Chernobyl Cooling Pond and Dnieper - Boog Estuary

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Cited by 10 publications
(9 citation statements)
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“…The exchange processes between water and solids in most models are described in the frame of a one-step reversible reaction of sorption/ desorption on the surface of particles (e.g. [18,26,27]); however, the mobility of radionuclides can be affected by a slow sorption process which ''fixes'' the ion to the solids due to the penetration of ions into the structure of sediment particles and interlattice spacing [20,22,33,35]. These processes were taken into account using two-step fast and slow reversible reactions [9,20,25,36].…”
Section: Introductionmentioning
confidence: 99%
“…The exchange processes between water and solids in most models are described in the frame of a one-step reversible reaction of sorption/ desorption on the surface of particles (e.g. [18,26,27]); however, the mobility of radionuclides can be affected by a slow sorption process which ''fixes'' the ion to the solids due to the penetration of ions into the structure of sediment particles and interlattice spacing [20,22,33,35]. These processes were taken into account using two-step fast and slow reversible reactions [9,20,25,36].…”
Section: Introductionmentioning
confidence: 99%
“…In 2002, RODOS (Real-time On-line Decision Support)which developed by European Commission has added THREETOX 3-D hydraulic model which includes sediment transportation and radionuclide transportation. In the paper [6,7], Margvelashvily has rebuilt the dispersion of Cs-137 and Sr-90 diffusion in the estuaries and shelf seas.After FUKUSHIMA nuclear accidents, researches of Daisuke Tsumune simulate the distribution of Cs-137 in the sea by Regional Ocean Modeling system [8].…”
Section: Research Developmentsmentioning
confidence: 99%
“…This section will present the modifications made to include the computation of suspended sediment in POM. The governing equation for suspended sediment transport in sigma coordinate is: (1) where C is the concentration of the suspended sedimentary material, U, V and w are current velocities in x, y and a direction respectively, ws is settling velocity (downward direction) of the considered sediment type; H is the bottom depth; D is total depth; and Kx, Ky, KH are diffusion coefficients. Here we set Kx=Ky=Ah, where Ah is horizontal eddy diffusivity used in POM.…”
Section: The Model Systemmentioning
confidence: 99%