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Similarity of long-term temporal decrease in atmospheric Cs-137 between Chernobyl and Fukushima

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We compare the atmospheric concentrations of Cs-137 after a decade between Chernobyl and Fukushima cases. We plotted 8 datasets on log-log axes (5 cases in Chernobyl and 3 cases Fukushima) and found that they appear to follow a single function.There have been measured the atmospheric concentration after the Chernobyl accident for more than 30 years [1]. On the other hand, several teams of Japanese researchers have been measured in Fukushima and its vicinity for almost 10 years. [2][3] In this study, we compare 5 sites in Chernobyl (Pripyat, Chernobyl, Baryshevka, Kiev, and Polesskoe) and 3 sites in Fukushima (FDNPP O-6 and O-7, Univ. Fukushima).We adjust the magnitude of the data because it depends on the amount of the initial deposition. After the adjustment, we plot the 8 cases on a log-log plot. We found that the 8 cases collapse together, with the power index of -1.6. Namely,C(t) ~ t^{-1.6}.               …(1)Incidentally, we have been proposed a formula which reproduce the long-term behavior of atmospheric concentration at a fixed location asC(t) = A exp(-bt) t^{-4/3}    …(2)where A is a parameter which relates to the amount of the initial deposition and b as the reaction rate of all the first-order reactions (including the radioactive decay rate, the vegetation uptake rate, the runoff rate, etc). We will investigate the difference in the power-law index in Eq. (1) and (2). The parameter b is highly dependent on the environment. When we take a proper value of b, the apparent decrease of the concentration will change from t^{-4/3}. We may make the apparent power-index close to -1.6. [1] E. K. Garger, et al., J. Env. Radioact., 110 (2012) 53-58.[2] A. Watanabe, et al., Atmos. Chem. Phys. 22 (2022) 675-692.[3] T. Abe, K. Yoshimura, Y. Sanada, Aerosol and Air Quality Research, 21 (2021) 200636.
Title: Similarity of long-term temporal decrease in atmospheric Cs-137 between Chernobyl and Fukushima
Description:
We compare the atmospheric concentrations of Cs-137 after a decade between Chernobyl and Fukushima cases.
We plotted 8 datasets on log-log axes (5 cases in Chernobyl and 3 cases Fukushima) and found that they appear to follow a single function.
There have been measured the atmospheric concentration after the Chernobyl accident for more than 30 years [1].
On the other hand, several teams of Japanese researchers have been measured in Fukushima and its vicinity for almost 10 years.
[2][3] In this study, we compare 5 sites in Chernobyl (Pripyat, Chernobyl, Baryshevka, Kiev, and Polesskoe) and 3 sites in Fukushima (FDNPP O-6 and O-7, Univ.
Fukushima).
We adjust the magnitude of the data because it depends on the amount of the initial deposition.
After the adjustment, we plot the 8 cases on a log-log plot.
We found that the 8 cases collapse together, with the power index of -1.
6.
Namely,C(t) ~ t^{-1.
6}.
               …(1)Incidentally, we have been proposed a formula which reproduce the long-term behavior of atmospheric concentration at a fixed location asC(t) = A exp(-bt) t^{-4/3}    …(2)where A is a parameter which relates to the amount of the initial deposition and b as the reaction rate of all the first-order reactions (including the radioactive decay rate, the vegetation uptake rate, the runoff rate, etc).
We will investigate the difference in the power-law index in Eq.
(1) and (2).
The parameter b is highly dependent on the environment.
When we take a proper value of b, the apparent decrease of the concentration will change from t^{-4/3}.
We may make the apparent power-index close to -1.
6.
 [1] E.
K.
Garger, et al.
, J.
Env.
Radioact.
, 110 (2012) 53-58.
[2] A.
Watanabe, et al.
, Atmos.
Chem.
Phys.
22 (2022) 675-692.
[3] T.
Abe, K.
Yoshimura, Y.
Sanada, Aerosol and Air Quality Research, 21 (2021) 200636.

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