1. Chernobyl fallout in the uppermost (0–3 cm) humus layer of forest soil in Finland, North East Russia and the Baltic countries in 2000–2003
- Author
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Ylipieti, J., Rissanen, K., Kostiainen, E., Salminen, R., Tomilina, O., Täht, K., Gilucis, A., and Gregorauskiene, V.
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ENVIRONMENTAL research , *RADIOACTIVE fallout , *COMPARATIVE studies , *NUCLEAR accidents , *HUMUS , *GAMMA rays , *NUCLIDES , *CESIUM isotopes , *CHERNOBYL Nuclear Accident, Chornobyl, Ukraine, 1986 - Abstract
The situation resulting from the Chernobyl fallout in 1987 was compared to that in 2000–2001 in Finland and NW Russia and that in 2003 in the Baltic countries. 786 humus (0–3 cm layer) samples were collected during 2000–2001 in the Barents Ecogeochemistry Project, and 177 samples in the Baltic countries in 2003. Nuclides emitting γ-radiation in the 0–3 cm humus layer were measured by the Radiation and Nuclear Safety Authority–STUK in Finland. In 1987 the project area was classified by the European Commission into four different fallout classes. 137Cs inventory Bg/m2 levels measured in 2000–2003 were compared to the EU''s class ranges. Fitting over the whole project area was implemented by generalizing the results for samples from the Baltic countries, for which Bq/m2 inventories could be calculated. A rough estimation was made by comparing the mass of organic matter and humus with 137Cs concentrations in these two areas. Changes in 137Cs concentration levels are illustrated in both thematic maps and tables. Radionuclide 137Cs concentrations (Bq/kg d.w.) were detected in the humus layer at all the 988 sampling sites. 134Cs was still present in 198 sites 15 years after the nuclear accident in Chernobyl. No other anthropogenic nuclides emitting γ-radiation were detected, but low levels of 60Co, 125Sb and 154Eu isotopes were found in 14 sites. Fifteen years after the Chernobyl accident, the radioactive nuclide 137Cs was and still is the most significant fallout radionuclide in the environment and in food chains. The results show that the fallout can still be detected in the uppermost humus layer in North East Europe. [Copyright &y& Elsevier]
- Published
- 2008
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