Biogeochemical behaviour of 137Cs and 90Sr in the artificial reservoirs of Mayak PA, Russia

The Mayak Production Association (PA) in the southern Urals, Russia was the site of the first weapons-grade plutonium production reactor complex in Russia. The site and surrounding area have been significantly contaminated by direct discharges of radionuclides for over 40 years, the Techa River alone having received more than 100 PBq of waste in the period 1949–1956. The aim of this study was to consider the levels of 90Sr and 137Cs in water, sediment and biota samples for two industrial reservoirs in the Mayak PA area, thus allowing a biogeochemical assessment of the behaviour of radionuclides in the system. Four sediment cores were collected and sectioned along with four water samples and seven fish samples (pike, perch and roach). Samples were analysed using (i) standard gamma-spectrometric techniques (HPGe and NaI(Tl) detectors) for 137Cs determination; and (ii) radiochemical separation and beta-counting (low-background, anti-coincidence and Geiger–Muller counters) for 90Sr determination. Maximum specific activities (dry weight) of 3350 kBq kg−1 137Cs and 720 kBq kg−1 90Sr were measured in sediments from Reservoir 10. Activity levels of sediment-bound radionuclides in Reservoir 11 were 403 kBq kg−1 137Cs and 670 kBq kg−1 90Sr. Water concentrations in Reservoir 10 were as high as 100 Bq l−1 137Cs and 8.4–14 kBq l−1 90Sr. A dramatic decrease in 137Cs concentrations was observed in Reservoir 11, i.e. 1.1–1.5 Bq l−1, but 90Sr levels fell to a lesser extent, i.e. 1.9–2.4 kBq l−1. Sediment and water activity data allowed the calculation of distribution coefficients (Kd values). This parameter fluctuated for both radionuclides reflecting the heterogeneous nature of the sediment deposits in the reservoirs. Caesium-137 Concentration Factors (CFs) as high as 1400 l kg−1 were calculated for pike from Reservoir 10. A pronounced ‘trophic level’ effect was evident in Reservoir 11 (pike CF=1000, roach CF=240).

[1]  V. Komov,et al.  137Cs in fish of some lakes and rivers of the Bryansk region and north-west Russia in 1990–1992 , 1994 .

[2]  H. A. Das,et al.  Mobilization of radiocaesium in pore water of lake sediments , 1989, Nature.

[3]  E. Häsänen,et al.  BIOLOGICAL HALF-TIMES OF 137Cs AND 22Na IN DIFFERENT FISH SPECIES AND THEIR TEMPERATURE DEPENDENCE , 1968 .

[4]  F. Livens,et al.  Particle size and radionuclide levels in some west Cumbrian soils , 1988 .

[5]  J. M. Elliott,et al.  Sources of variation in post-Chernobyl radiocaesium in fish from two Cumbrian lakes (north-west England) , 1992 .

[6]  M. Meili 2.9. Radiocaesium as Ecological Tracer in Aquatic Systems A Review , 1994 .

[7]  I. Kryshev Radioactive contamination of aquatic ecosystems following the Chernobyl accident , 1995 .

[8]  A. Akleyev,et al.  Environmental and medical effects of nuclear weapon production in the southern Urals. , 1994, The Science of the total environment.

[9]  A. Aarkrog,et al.  Evidence of 99Tc in Ural river sediments , 1997 .

[10]  P. Strand Environmental radioactivity in the arctic , 1997 .

[11]  A. Aarkrog,et al.  Radioactive contamination of the Techa River, the Urals. , 1993, Health physics.

[12]  B. G. Blaylock,et al.  Radionuclide data bases available for bioaccumulation factors for freshwater biota , 1982 .

[13]  Frank Oldfield,et al.  Radionuclides in coastal and estuarine sediments from Wirral and Lancashire , 1988 .

[14]  Brenda J. Howard,et al.  Nordic Radioecology. The transfer of radionuclides through Nordic ecosystems to man , 1995 .