研究報告20 - 1 解説 - Review
トリチウムの環境動態
Environmental Tritium
百島則幸
熊本大学理学部
〒860-8555熊本市黒髪2丁目39-1
Noriyuki Momoshima
Faculty of Science, Kumamoto University, Kurokami 2-39-1, Kumamoto 860-8555
Abstract
Environmental tritium was first observed in a helium fraction
at a liquid air production facility in Germany in 1949. During the 1950s
and early 1960s, huge amounts of artificial tritium were released into
the atmosphere by nuclear testing. The environmental tritium level increased
to more than 200 times the natural tritium level. Since the signing of
a test ban treaty in 1963, the environmental tritium level has decreased,
and analysis of recent Japanese rain samples has shown that the environmental
tritium level is close to that before the nuclear testing. Tritium released
from nuclear bombs into the atmosphere has been used as a global-scale
tracer in studies on water mass movement in the ocean, groundwater flow
and atmospheric air mass movement. Useful and valuable results have been
obtained in those studies. In the atmosphere, tritium exists in three different
chemical forms: hydrogen (HT), water vapor (HTO) and hydrocarbons (CH3T).
The concentration of HT the highest, followed by those of CH3T
and HTO. The most interesting feature of these chemical species is their
significantly different specific activities. HT has 106 TU,
CH3T has 104 TU and HTO has 10 TU, suggesting that
HT and CH3T have been released from nuclear facilities. Vegetation
is sensitively responds to a change in environmental HTO level by rapid
exchange of water molecules between leaf water and atmospheric water vapor.
HTO vapor released into the air slowly contaminates soil water. A nuclear
fusion facility is planed to use a large quantity of tritium that is comparable
to natural tritium on the earth, indicating the necessity to maintain tritium
in a nuclear fusion facility and the necessity to carefully monitor the
environmental tritium level.