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Origin of enriched uranium contained in Japanese atmospheric deposits
1Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
Research Laboratory for Nuclear Reactors, Tokyo Institute of Technology, Tokyo, Japan
Atomic Energy Research Laboratory, Tokyo City University, Kawasaki, Japan
Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
Meteorological Research Institute, Tsukuba, Japan
- 1 1Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
- 2 Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
- 3 Research Laboratory for Nuclear Reactors, Tokyo Institute of Technology, Tokyo, Japan
- 4 Atomic Energy Research Laboratory, Tokyo City University, Kawasaki, Japan
- 5 Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
- 6 Department of Materials and Life Sciences, Sophia University, Tokyo, Japan;
- 7 Meteorological Research Institute, Tsukuba, Japan
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Abstract
The chemical compositions of atmospheric deposits collected in Fukuoka, Japan, in 1964 and 2000, which are known to have high 235 U/ 238 U uranium isotope ratio were determined. High uranium contents relative to that of continental crust were observed for the deposition samples in 1964 together with the high 235 U/ 238 U ratios, which indicated that the origin of uranium is fallout materials due to the large-scale 1961- 1962 nuclear explosions conducted by US and former USSR. The deposits in 2000 were mainly composed of dusts from the East Asia. This suggested that uranium with a high 235 U/ 238 U ratio in the deposits in 2000 has been transported as a component of mineral dust particles contaminated with nuclear debris from nuclear test sites from the East Asian deserts and arid regions by the prevailing wind.
KeywordsAtmospheric DepositEnriched UraniumUranium Isotope RatioNuclear TestAnthropogenic Radionuclides
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