Published November 2016 | Version v1
Journal article

Numerical study of sediment and 137Cs discharge out of reservoirs during various scale rainfall events

  • 1. Japan Atomic Energy Agency (JAEA), Sector of Fukushima Research and Development, 10-2 Fukasaku, Miharu-machi, Tamura-gun, Fukushima 963-7700 (Japan)
  • 2. Japan Atomic Energy Agency (JAEA), Center for Computational Science & e-Systems, University of Tokyo Kashiwanoha Campus Satellite, 178-4-4 Wakashiba, Kashiwa, Chiba 277-0871 (Japan)
  • 3. Yasuo Onishi Consulting, LLC, Richland, WA 99354 (United States)

Description

Contamination of reservoirs with radiocesium is one of the main concerns in Fukushima Prefecture, Japan. We performed simulations using the three-dimensional finite volume code FLESCOT to understand sediment and radiocesium transport in generic models of reservoirs with parameters similar to those in Fukushima Prefecture. The simulations model turbulent water flows, transport of sediments with different grain sizes, and radiocesium migration both in dissolved and particulate forms. To demonstrate the validity of the modeling approach for the Fukushima environment, we performed a test simulation of the Ogaki Dam reservoir over Typhoon Man-yi in September 2013 and compared the results with field measurements. We simulated a set of generic model reservoirs systematically varying features such as flood intensity, reservoir volume and the radiocesium distribution coefficient. The results ascertain how these features affect the amount of sediment or 137Cs discharge downstream from the reservoirs, and the forms in which 137Cs is discharged. Silt carries the majority of the radiocesium in the larger flood events, while the clay-sorbed followed by dissolved forms are dominant in smaller events. The results can be used to derive indicative values of discharges from Fukushima reservoirs under arbitrary flood events. For example the generic model simulations indicate that about 30% of radiocesium that entered the Ogaki Dam reservoir over the flood in September 2015 caused by Typhoon Etau discharged downstream. Continued monitoring and numerical predictions are necessary to quantify future radiocesium migration in Fukushima Prefecture and evaluate possible countermeasures since reservoirs can be a sink of radiocesium. - Highlights: • Systematic analysis of sediment and 137Cs discharge from generic models of reservoirs. • Parameters employed (flood intensity, reservoir volume and Kd) are similar to those occurring in Fukushima. • Simulations determine the effect of these parameters on radiocesium discharge. • 137Cs mainly discharges in silt-sorbed form in larg floods, while clay-sorbed and dissolved forms dominate in small events. • Results can be used to estimate 137Cs discharges from reservoirs in arbitrary flood events.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.jenvrad.2016.07.004

Additional details

Identifiers

DOI
10.1016/j.jenvrad.2016.07.004;
PII
S0265-931X(16)30234-X;

Publishing Information

Journal Title
Journal of Environmental Radioactivity
Journal Volume
164
Journal Page Range
p. 73-83
ISSN
0265-931X
CODEN
JERAEE

Optional Information

Copyright
Copyright (c) 2016 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.