The
March 2011 Fukushima Dai-ichi Nuclear Power Plant accident
in Japan released 520 PBq of radionuclides compared to a total release
of 5300 PBq from the Chornobyl Nuclear Power Plant accident. Both
nuclear accidents resulted in deposition of radiocesium throughout
the northern hemisphere, and a plethora of studies have been performed
regarding radiocesium (137Cs) behavior. However, few studies
have assessed the impact of precipitation on 137Cs deposition
in forests. Wide-scale environmental measurements from 2011 and 2016
were used to determine the differences in 137Cs deposition
because of precipitation following the Fukushima accident. In areas
where wet deposition processes were dominant, dense forests generally
had lower ambient dose rates and levels of contamination on forest
floors than other stands with fewer stems per hectare in 2011. Similar
tendencies were not observed in areas that were primarily subject
to dry deposition nor were any trends observed in 2016. 137Cs was retained in dense forest canopies for an extended period regardless
of the deposition mode. Additionally, it was found that the initial
retention of radionuclides by forest canopies is in general higher
for areas with predominantly dry deposition. Incorporation of radiocesium
into wood tissues was the same for both wet and dry deposition.