H089-0023
The transfer of fallout radionuclides by Fukushima Daiichi Nuclear Power Plant Accident revealed by intensive monitoring network
Abstract:
We started sediment and Cs-137 outflow from plot scale monitoring (Wakiyama et al., 2019), headwater catchments (Iwagami et al., 2019), Paddy field (Wakahara et al. 2014). Also, we install river monitoring sites at six sites from June 2011 to quantify radiocesium fluxes by measuring discharge and turbidity, and sampling bulk suspended sediment and water. From December 2012, we installation of a further 24 monitoring sites to give 30 stations in total to cover most of the rivers in an 80-km radius from FDNPP (Taniguchi et al., 2019).
The factors controlling different declining trends between watersheds across the fallout zone were investigated and found that both radiocesium flux and the rate of decline in activity concentrations in rivers were an order of magnitude higher than rates measured after Chernobyl. In Fukushima, the initial fallout and vertical movement of radionuclide in the land and forest, and subsequent transport and redistribution through hydrological and geomorphological processes in cropland, Urban area, Paddy field, and forested area. Our finding revealed that land use is a key control of the sources of suspended particulate matter entering river networks, contributing to declining rates of radiocesium flux.
Wakiyama et al. (2015) J. Environ. Radioact. DOI: 10.1016/j.jenvrad.2019.105990
Iwagami et al. (2019) J. Environ. Radioact. DOI: 10.1016/j.jenvrad.2019.106001
Wakahara et al (2014) Environ. Sci. Process. Impacts DOI: 10.1039/c4em00262h
Taniguchi et al (2019) Environ. Sci. Technol. DOI:10.1021/acs.est.9b02890