To simulate the radionuclide flux from the Dnieper-Bug Estuary into the Bla
ck Sea the three-dimensional time-dependent flow and transport code THREETO
X was used. The prognostic variables of the model are the three components
of the velocity field, temperature, salinity, surface elevation, suspended
sediment concentration and the rajionuclide concentrations in the solute, s
uspended sediments and bottom deposition. The dispersion of Cs-137 and Sr-9
0 in the estuary and adjacent shelf area of the Black Sea over the first tw
o years following the Chernobyl accident was reconstructed. The fluxes of r
adionuclides from the Dnieper-Bug Estuary into the Black Sea were estimated
. The results are in reasonable agreement with the available measurements.
It is shown that the differences between the Cs-137 and Sr-90 distributions
specific to the Dnieper-Bug Estuary were due to the different geochemical
behaviours of these radionuclides. The deviation from a linear correlation
between salinity and dissolved Cs-137 concentration in the estuary was show
n to be due to exchange processes with contaminated bottom sediments, (C) 1
999 Elsevier Science Ltd. All rights reserved.