JpGU-AGU Joint Meeting 2017

Presentation information

[EJ] Oral

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

[M-AG34] [EJ] Dynamics of radionuclides emitted from Fukuchima Dai-ichi Nuclear Power Plant in the environment

Thu. May 25, 2017 10:45 AM - 12:15 PM Convention Hall A (International Conference Hall 2F)

convener:Kazuyuki Kita(Faculty of Science, Ibaraki University), Yuichi Onda(Center for Research on Isotopes and Environmental Dynamics, University of Tsukuba), Yasuhito Igarashi(Atmospheric Environment and Applied Meteorology Research Department, Meteorological Research Institute), Masatoshi Yamada(Institute of Radiation Emergency Medicine, Hirosaki University), Chairperson:Haruka Minowa(The Jikei University School of Medicine), Chairperson:Hiroaki Kato(Tsukuba University)

11:45 AM - 12:00 PM

[MAG34-11] Migration of sediment and 137Cs on decontaminated arable lands

*Yoshifumi Wakiyama1, Yuichi Onda1,2 (1.Institute of Environmental Radioacitivity, Fukushima Universiy, 2.Center for Research in Isotopes and Environmental Dynamics, University of Tsukuba)

Keywords:Decontamination , Soil erosion, Slope, 137Cs

To mitigate radiological risks to residents in Fukushima, decontamination, such as removal of contaminated surface soil and covering contaminated soils with clean soil (i.e., soil dressing), has been conducted in areas of heavy radiological contamination. Although removing and concealing radioactive materials are expected to reduce ambient dose rates, such anthropogenic alteration of soil may result in changes to the hydrological responses and sediment dynamics of the area under the decontamination. Few studies have investigated the dynamics of sediment and 137Cs associated with decontamination efforts. Our research studies the release of sediments and 137Cs from decontaminated lands to elucidate the influence of decontamination. Soil erosion plots were installed on four contaminated land use types (uncultivated farmland, cultivated farmland, grassland, forest) and two decontaminated land use types (uncultivated farmland, cultivated farmland) to observe sediment discharge and 137Cs wash-off. The 137Cs activity concentration of eroded sediments from decontaminated lands were approximately 10 times lower than those from contaminated lands. The amount of sediment eroded from the decontaminated farmland was comparable to those from contaminated farmlands, but higher than those from contaminated grassland and forest. 137Cs wash-off rates on decontaminated lands were lower than those on contaminated farmlands and higher than those on grassland and forest. These results suggest that decontamination results in a decrease of 137Cs wash-off on erodible agricultural lands and increase relative to less erodible lands (grasslands and forests). Surface runoff coefficients and contribution of fine sediment to discharges of both sediment and 137Cs were lower on decontaminated farmlands than those on contaminated farmlands. One possible explanation is that high permeability of decontaminated land resulted in inactive discharge of fine sediment. Elucidation of soil erosion processes on decontaminated lands based on investigation of its soil physical properties, such as permeability and particle size distribution, are required to better understand the influence of the decontamination.