NUKLEONIKA 2006, 51(Suppl. 2):s39-s44
Abdallah Z. Al-Zamel1, Firyal Bou-Rabee1, Mohammad A. Al-Sarawi1, Marcin Olszewski2, Henryk Bem2
1 Faculty of Science, Department of Earth and Environmental Sciences,
University of Kuwait, P. O. Box 5969, Safat 13060, Kuwait
2 Institute of Applied Radiation Chemistry,
Department of Chemistry, Technical University of £ódŸ,
36 ¯wirki Str., 90-924 £ódŸ, Poland
Five bottom sediment cores from the Kuwait Bay were dated using 210Pb and 137Cs
radionuclides. For evaluating the sedimentation rate two methods were applied: geochronology with
the constant rate of supply unsupported 210Pb (CRS model) and the Weibull distribution of
anthropogenic 137Cs. The sedimentation rates in this region, calculated by the first method
ranged from 0.24 to 0.39 cm/year, while the same rates obtained from 137Cs distribution were
slightly lower: from 0.1 to 0.25 cm/year. These relatively small differences can be explained by
additional input of the Chernobyl accident to the 137Cs inventory in the bottoms sediments
of the Northern Hemisphere.