Japan Geoscience Union Meeting 2022

Presentation information

[J] Oral

M (Multidisciplinary and Interdisciplinary) » M-AG Applied Geosciences

[M-AG39] Radioisotope migration: New development for dynamics study of radionuclides from 1F NPP accident

Mon. May 23, 2022 1:45 PM - 3:15 PM 202 (International Conference Hall, Makuhari Messe)

convener:Daisuke Tsumune(Central Research Institute of Electric Power Industry), convener:Yuichi Onda(Center for Research on Isotopes and Environmental Dynamics, University of Tsukuba), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), convener:Akira Kirishima(Tohoku University), Chairperson:Daisuke Tsumune(Central Research Institute of Electric Power Industry), Akira Kirishima(Tohoku University)

2:30 PM - 2:45 PM

[MAG39-04] 137Cs of decontamination effect and temporal changes in an urban pond

*Honoka Kurosawa1, Kenji Nanba2,3, Toshihiro Wada2, Yoshifumi Wakiyama2 (1.Major of Environmental Radioactivity, Graduate school of Symbiotic System Science and Technology, Fukushima University, 2.Institute of Environmental Radioactivity, Fukushima University, 3.Faculty of Symbiotic System Science, Fukushima University)

Keywords:Fukushima Dai-ichi Nuclear Power Plant accident, 137Cs, pond, decontamination, δ15N

There are more than 4,000 ponds in Fukushima Prefecture, and many ponds were contaminated by radiocesium (134Cs+137Cs) due to the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident. The decontamination and/or countermeasures against radioactive materials were considered for ponds heavily contaminated by radiocesium, higher than 8 kBq/kg in bottom sediment as a criteria based on the Act on Special Measures Concerning the Handling of Radioactive Materials Contamination. The bottom sediment removal, one of the countermeasures, is an effective way to decrease the radiocesium concentration in bottom sediment and water body. The previous studies have been shown that 137Cs accumulate in ponds and dam reservoirs due to its secondary inflow from catchments. Therefore, it is necessary to understand how and how much 137Cs accumulates after decontamination. However, there are few studies on the effects of decontamination and the temporal changes in the pond. The objectives of this study were to reveal the effect of decontamination on the 137Cs and water quality and to elucidate accumulation process of 137Cs after decontamination, based on long-term investigation on an urban pond.
The investigated pond is located in Koriyama City. The water was taken from the Asaka- canal and the Minami River, and flowed into the pond through culvert and open culvert. The amount of 137Cs deposited around the investigated pond was 0.170 MBq/m2. The investigated pond was decontaminated by dredging of bottom sediment in 2017. The bottom sediment, pond water, inflow water, and outflow water were collected in 2015, 2018-2021, and analyzed for 137Cs concentration, particle size distribution, nitrogen and carbon stable isotope ratio, and water quality.
Compared between 2015 and 2018, the 137Cs inventory and the 137Cs concentration in the top layer of bottom sediment at 7 points were decreased by 78 % and 72 %, respectively. Since the 137Cs inventory and the 137Cs concentration in the bottom sediment were decreased, it was said that the decontamination had an effect. After decontamination, there was no change in the average 137Cs inventory, however, the 137Cs inventory was increased due to the deposition of fine particles at points where the water flow was stagnant. There was a significant positive correlation between δ15N and 137Cs concentrations in 0-1 cm of bottom sediment after decontamination. It was suggested that 137Cs concentrations tend to be higher at points where the contribution of particles from urban areas was larger, since δ15N is reported to increase with human activity. The total 137Cs concentration (dissolved 137Cs concentration + particulate 137Cs concentration) in pond water before and after decontamination was decreased by 33 %. The 137Cs concentration in SS of pond water was significantly decreased by decontamination, however, the 137Cs concentration in SS of pond water was remained at 8 kBq/kgDW after decontamination. The 137Cs concentration in SS of the inflow water were exceeded 8 kBq/kgDW under high-flow condition. The 137Cs concentration in SS of the inflow water at the investigated pond was higher than that in soil of the cultivated farmland and paddy fields. It was suggested that the infow of SS with high 137Cs concentrations from urban areas is a factor in remain high concentrations of 137Cs in SS of pond water and bottom sediment. The total 137Cs concentration in the outflow water was higher than that in the inflow and pond water, suggesting that 137Cs tended to be discharged. The δ15N of the outflow water was between the bottom sediment and the ponded water, suggesting that the bottom sediment and the ponded water were mixing and flowing out. In the investigated pond, the 137Cs concentration after decontamination was higher than that in the pond located in forests and farmlands, reflecting the fact that the catchment area in the investigated pond was an urban area.