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$$^{137}$$Cs in lichens after the Fukushima Nuclear Accident

Dohi, Terumi   ; Omura, Yoshihito*; Fujiwara, Kenso ; Iijima, Kazuki  

Large quantity of radionuclides, including $$^{134}$$Cs and $$^{137}$$Cs, were released into the atmosphere caused by the Fukushima Dai-chi Nuclear Power Plant (FDNPP) accident on March 11, 2011. As lichens are known to be effective tools to monitor environmental radioelements in both time and space, lichen samples are expected to be used to examine and monitor radiocaesium fallout from FDNPP in Japan. The purpose of this study is to discuss the estimation of radiocaesium fallout in the ecosystem based on the following examinations using lichens. Fifty-eight samples including foliose and fruticose lichens were collected from northern to central Japan especially focusing on Fukushima Prefecture during 2012 and 2013. After correction for radioactive decay (on each sampling date), the detected radiocaesium concentrations ranged from 16.1 Bq kg$$^{-1}$$ (d.w.) to 510,000 Bq kg$$^{-1}$$ for $$^{134}$$Cs and from 33.8 to 880,000 Bq kg$$^{-1}$$ for $$^{137}$$Cs in lichens. $$^{137}$$Cs concentration in the lichen samples generally increased with increase in the amount of fallout estimated by the $$^{137}$$Cs deposition in soil. The positive correlation was supported between $$^{137}$$Cs in lichens collected from Fukushima Prefecture and $$^{137}$$Cs inventories on soil calculated by Inverse Distance Weighted with Spearman's rank correlation coefficient (0.90, p $$<$$ 0.01). The activity ratios of $$^{134}$$Cs and $$^{134}$$Cs for the lichen samples (${it n}$ = 44) collected within Fukushima Prefecture (decay corrected to March 11, 2011) were between 0.95$$pm$$0.04 and 1.08$$pm$$0.41. The ratios are consistent with those for radiocaesium derived from the FDNPP accident (reported as 0.89 to 1.2). The ratios obtained from lichen samples collected in outside of Fukushima Prefecture were 0.75$$pm$$0.23 to 1.48$$pm$$0.48. They were consistent with those from Fukushima. But one sample showing significantly small value, 0.48$$pm$$0.16, might be influenced by different origin from Fukushima.

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