Carbon-14 (14 C) is of great interest in the assessment of dose due to the nuclear industry because of the biological importance of carbon. We collected atmospheric CO 2 , rice grain, leafy vegetable, and Japanese mugwort samples at various locations at different time intervals, and measured their 14 C concentrations to show the spatiotemporal distribution of 14 C around the Tokai reprocessing plant (TRP). The results consistently gave the picture of a 14 C dispersion pattern brought about by the prevailing wind in this area, which conveys the 14 C plume, and as a result, caused elevated 14 C concentrations in the area 2-3 km southwest of the main stack of the TRP. The increases in 14 C concentration were, however, quite temporary, and the baseline concentration remained at the background level even in the elevated area. The 14 C concentrations in vegetations generally followed those in atmospheric CO 2 , but seemed different in 14 C uptake response between vegetation types, emphasizing the importance of this nature not only in its application as bioindicators in environmental monitoring but also in establishing a more realistic dose evaluation model for 14 C. Through a series of investigations, we found the highest 14 C concentrations of 374, 287, and 361 Bq kg-C À1 in atmospheric CO 2 , rice grains, and leafy vegetables, respectively. They corresponded to a maximum of $110 Bq kg-C À1 excess above the background. The annual effective dose delivered from the concentrations was estimated to be around 0.7 mSv yr À1 , only 0.07% of the annual effective dose limit for the public. Thus, we conclude that the 14 C releases from the TRP have a very slight impact both on the environment and on the public.