Abstract
Over the period from 1986 to 2016 the data for the 90Sr and 137Cs horizontal and vertical distribution in the surface water and in the water column of the Black Sea, accordingly, were analyzed. The results of full-profile measurements of 137Cs in the deep water column were obtained in 2015 for the first time for the whole post-Chernobyl period. The time constants of exponential functions were determined and the forecast of 90Sr and 137Cs concentrations reduction to the pre-accident levels in the components of the ecosystem of the Sevastopol bay was made. The estimations of the balance components of these radionuclides in the Black Sea were obtained. It is shown that to the present time the steady-state equilibrium between entry and elimination of 90Sr and 137Cs in the oxygen zone of the Black Sea was formed, at the same time their accumulation in the hydrogen-sulphidous zone has been increasing. By 2013 the 90Sr and 137Cs content in the Black Sea was evaluated as 1670 and 2843 TBq, respectively, that was in 3.6–6.4 and in 1.2–1.6 times higher, than the content of these radionuclides at the sea in 2000. At the same time 66% of 137Cs and 67% of 90Sr of the total content of radionuclides in the whole water column was in the hydrogen-sulphidous zone of the Black Sea. The period of circulation of 137Cs and 90Sr in the oxygen and hydrogen-sulphidous zones of the Black Sea is about 14 and 94 years, respectively.
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Mirzoyeva, N.Y., Egorov, V.N., Gulin, S.B. (2018). Radionuclides 137Cs and 90Sr in Components of the Black Sea Ecosystems: Contemporary Status and Prognosis. In: Finkl, C., Makowski, C. (eds) Diversity in Coastal Marine Sciences. Coastal Research Library, vol 23. Springer, Cham. https://doi.org/10.1007/978-3-319-57577-3_17
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