Japan Geoscience Union Meeting 2024

Presentation information

[J] Oral

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

[M-AG34] Radioisotope migration: New Development of Environmental Dynamics Research on the 1FNPS Accident

Fri. May 31, 2024 10:45 AM - 12:00 PM 303 (International Conference Hall, Makuhari Messe)

convener:Daisuke Tsumune(University of Tsukuba), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Akira Kirishima(Tohoku University), Hiroaki Kato(Center for Research in Isotopes and Environmental Dynamics, University of Tsukuba), Chairperson:Daisuke Tsumune(University of Tsukuba), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Akira Kirishima(Tohoku University), Hiroaki Kato(Center for Research in Isotopes and Environmental Dynamics, University of Tsukuba)

11:00 AM - 11:15 AM

[MAG34-02] Effects of shallow groundwater runoff on Cs-137 discharge flux from forest headwater catchment

*Hiroaki Kato1, Yuma Niwano1, Yuichi Onda1 (1.Center for Research in Radiation, Isotopes, and Earth System Sciences, University of Tsukuba)

Keywords:Fukushima Dai-ichi Nuclear Power Plant accident, Cs-137, Forest catchment, Shallow groundwater

In the aftermath of the Fukushima Daiichi Nuclear Power Plant disaster, radiocesium (Cs-137) dispersion through forest ecosystems into aquatic systems has raised environmental concerns. While prior investigations have delineated the augmentation of Cs-137 in surface waters, attributing this to the deposited litter leaching, the role of groundwater runoff on Cs-137 discharge remains underexplored. This research aims to elucidate the role of shallow groundwater, characterized by diverse residence times and pathways on forested slopes, in modulating Cs-137 concentrations within surface waters. Employing detailed hydrological monitoring at a forest hillslope, we discerned elevated Cs-137 levels in shallow groundwater compared to adjacent surface waters. Notably, surface water Cs-137 concentrations surged in conjunction with rainfall events, accompanied by pronounced groundwater flow toward river channels. A significant correlation between the groundwater hydraulic gradient and surface water flow rate was identified, underscoring the pivotal contribution of shallow groundwater discharge to both the enhanced flow and Cs-137 levels in surface waters. This study quantifies shallow groundwater's impact on Cs-137 surface water concentrations, leveraging detailed hydrological data and Cs-137 measurements. Our findings contribute to a deeper understanding of radioactive contaminant dynamics in forested watersheds, highlighting the need for integrated water management strategies post-nuclear accidents.