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(137)Cs activity distribution in the Lithuanian coastal waters of the Baltic Sea

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The main (137)Cs accumulation zone in the study area was found to be located at depths below the 50-metre isobath, i.e. below the layer of hydrodynamic activity. In coastal waters not influenced by the fresh water discharge from the Curonian Lagoon, (137)Cs occurs mostly in soluble form. The particulate 137Cs activity concentration in the marine area affected by Curonian Lagoon water can make up 10% of the total (137)Cs activity concentration. The circulation model was developed to assess the distribution of artificial radionuclides in Lithuanian territorial waters. The model was validated on the basis of data acquired during the measurement campaign in the Lithuanian part of the Baltic Sea and the Curonian Lagoon in the years 1999-2001. The model enables the (137)Cs activity concentration to be simulated as a passive admixture (error within c. 15%).
Czasopismo
Rocznik
Strony
71--90
Opis fizyczny
bibliogr. 19 poz., tab., wykr.
Twórcy
autor
autor
autor
autor
Bibliografia
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  • [3].Davuliene L., Dailidiene I., Dick S., Trinkunas G., Valkunas L., 2002, Validation of Circulation Model for Lithuanian coastal waters, Environ. Chem. Phys., 24 (4), 226-231.
  • [4].Davuliene L., Trinkunas G., Valkunas L., 2002a, Analysis of salinity variation in Lithuanian marine waters, Lithuan. J. Phys., 42 (4), 309-314.
  • [5].Dick S., Kleine E., M¨uller-Navarra S., Klein H., Komo H., 2001, The Operational Circulation Model of BSH (BSHcmod), Ber. BSH, 29, 48 pp.
  • [6].Dubra J., Dubra V., 1998, Calculation of the water changes in the Lithuanian nearshore of the Baltic Sea, Centr. Mar. Res., Sci. Inf. Publ., Klaipeda, 49-56, (in Lithuanian).
  • [7].Gavrilov V.M., Gritchenko Z. G., Ivanova L. M., Orlova T.E., Tiskov V. P., Tiskova N.A., 1990, Strontium-90, Caesium-137 and Caesium-137 in the water basins of the Baltic States at Soviet Union (1986-1988), Radiochemistry, 3, 171-179, (in Russian).
  • [8].Galkus A., Jokˇsas K., 1997, Sedimentary material in the transitional aquasystem, Inst. Geogr., Vilnius, 198 pp.
  • [9].Kleine E., 1994, Das operationelle Modell des BSH f¨ur Nordsee und Ostsee. Konzeption und ¨Ubersicht, BSH, Hamburg, 132 pp.
  • [10].Lujaniene G., Vilimaite-Silobritiene B., Joksas K., 2005, Accumulation of 137Cs in bottom sediments of the Curonian Lagoon, Nukleonika, 50 (1), 23-29.
  • [11].Nielsen S.P., 1997, A comparison between predicted and observed levels of 137Cs and 90Sr in the Baltic Sea, Radioprotection -Colloq., 32 (C2), 387-394.
  • [12].NATO - North Atlantic Treaty Organization, 1998, Cross-border environmental problems emanating from defence-related installations and activities. Phase II: 1995-1998, Final Report Vol. 2. Radioactive contamination of rivers and transport through rivers, deltas and estuaries to the sea, Rep. No 225, 105 pp.
  • [13].Osvath I., Samiel M., Valkunas L., Zlatnansky J., 2001, Dynamic waters of the Baltic Sea, IAEA Bull., 43( 2), 9-15.
  • [14].Styro D., Bumelien˙e ˇZ., Lukinskien˙e M., Mork¯unien˙e R., 2001, 137Cs and 90Sr behavioural regularities in the southeastern part of the Baltic Sea, J. Environ. Radioactiv., 53( 1), 27-39.
  • [15].Szefer P., 2002, Metal pollutants and radionuclides in the Baltic Sea - an overview, Oceanologia, 44 (2), 129-178.
  • [16].Špirkauskaité N., Tarasiuk N., Stelingis K., Lujaniene G., Lujanas V., 1994, The use of 137Cs tracer in the estimation of the pollution accumulation processes in the Gdańsk Bay (BAEX-ONE data), Proc. 19th Conf. Baltic Oceanogr., Vol. I, 43-46.
  • [17].Tarasiuk N., Špirkauskaité N., 1994, Radioactive contamination of the coastal zone of the Baltic Sea of Lithuania, Atmos. Phys., 16, 85-89.
  • [18].Tarasiuk N., Špirkauskaité N., Lujaniene G., 1999, The formation of 137Cs concentrations in the Nemunas river accumulation zone, Environ. Chem. Phys., 21 (2), 27-32.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS5-0003-0056
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