Impacts of anthropogenic source from the nuclear fuel reprocessing plants on global atmospheric iodine-129 cycle: A model analysis

Publication date: July 2018
Source:Atmospheric Environment, Volume 184
Author(s): Masanao Kadowaki, Genki Katata, Hiroaki Terada, Takashi Suzuki, Hidenao Hasegawa, Naofumi Akata, Hideki Kakiuchi
The long-lived radioactive iodine (¹²⁹I) is a useful geochemical tracer of radioactivity in the atmospheric environment. Although the behavior of ¹²⁹I in the atmosphere is still not fully known because of lack of continuous monitoring, we recently observed clear seasonal trends in air concentration and deposition of ¹²⁹I in Japan. Using these data, we developed a global atmospheric ¹²⁹I transport model to reveal key processes for the global atmospheric ¹²⁹I cycle. The physical and chemical processes of advection, turbulent diffusion, dry and wet deposition, atmospheric photolysis, gas–particle conversion in the atmosphere, anthropogenic sources of ¹²⁹I discharged from operating nuclear fuel reprocessing plants, and natural sources of ¹²⁹I volatilized from ocean and land were included into the model. The model generally reproduced the observed seasonal change in monthly air concentration and deposition of ¹²⁹I in Japan, and the global distribution of ¹²⁹I concentration in rain as presented in past literature. Numerical experiments changing the intensity of anthropogenic and natural sources were conducted to quantify the impact of anthropogenic sources on the global ¹²⁹I cycle. The results indicated that the atmospheric ¹²⁹I from the anthropogenic sources was readily deposited in winter and can be accumulated mainly in the northern part of Eurasia. In contrast, the atmospheric ¹²⁹I from the natural sources dominated the deposition in summer. These results suggested that the re-emission process of ¹²⁹I from the Earth's surface may be important as a secondary impact of ¹²⁹I in the global-scaled environment. Furthermore, although wet deposition dominated the total deposition in the Northern hemisphere, dry deposition regionally and seasonally contributed to the total deposition over arctic and northern part of Eurasia in winter, suggesting that the dry deposition may play a key role in the seasonal change of ¹²⁹I deposition in the high latitudes of the Northern hemisphere.



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