Dispersion and fate of 90Sr in the Northwestern Pacific and adjacent seas: Global fallout and the Fukushima Dai-ichi accident
Creators
- 1. Institute of Mathematical Machine and System Problems, Glushkov av., 42, Kiev 03187 (Ukraine)
- 2. Korea Institute of Ocean Science and Technology, 787, Haean-ro, Ansan 426-744 (Korea, Republic of)
- 3. Ukrainian Center of Water and Environmental Projects, Glushkov av., 42, Kiev 03187 (Ukraine)
- 4. NRG, Utrechtseweg 310, 6800 ES Arnhem (Netherlands)
- 5. First Institute of Oceanography, 6 Xianxialing Road, Qingdao 266061 (China)
- 6. Laboratory of Ion Beam Physics, ETH-Zurich, Schafmattstrasse 20, 8093 Zurich (Switzerland)
- 7. Institut de Ciència i Tecnologia Ambientals and Departament de Física, Universitat Autònoma de Barcelona, 08193 Bellaterra (Spain)
Description
The 3D compartment model POSEIDON-R was applied to the Northwestern Pacific and adjacent seas to simulate the transport and fate of 90Sr in the period 1945–2010 and to perform a radiological assessment on the releases of 90Sr due to the Fukushima Dai-ichi nuclear accident for the period 2011–2040. The contamination due to runoff of 90Sr from terrestrial surfaces was taken into account using a generic predictive model. A dynamical food-chain model describes the transfer of 90Sr to phytoplankton, zooplankton, molluscs, crustaceans, piscivorous and non-piscivorous fishes. Results of the simulations were compared with observation data on 90Sr for the period 1955–2010 and the budget of 90Sr activity was estimated. It was found that in the East China Sea and Yellow Sea the riverine influx was 1.5% of the ocean influx and it was important only locally. Calculated concentrations of 90Sr in water, bottom sediment and marine organisms before and after the Fukushima Dai-ichi accident are in good agreement with available experimental measurements. The concentration of 90Sr in seawater would return to the background levels within one year after leakages were stopped. The model predicts that the concentration of 90Sr in fish after the Fukushima Dai-ichi accident shall return to the background concentrations only 2 years later due to the delay of the transfer throughout the food web and specific accumulation of 90Sr. The contribution of 90Sr to the maximal dose rate due to the FDNPP accident was three orders of magnitude less than that due to 137Cs, and thus well below the maximum effective dose limits for the public. - Highlights: • A box model with a dynamical food-chain model for the NW Pacific was applied. • The transport and fate of 90Sr in sea were simulated for the period 1945–2040. • Marine exposure pathways for 90Sr were assessed for the Fukushima Dai-ichi accident. • Simulations confirm the presence of leak of 90Sr with a 90Sr/137Cs ratio of about 1. • 90Sr human dose was 3 orders of magnitude less than that from 137Cs
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2014.06.136Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2014.06.136;
- PII
- S0048-9697(14)01009-2;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 494-495
- Journal Issue
- Complete
- Journal Page Range
- p. 261-271
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 47012594
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- AQUATIC ORGANISMS; CESIUM 137; DOSE LIMITS; DOSE RATES; ECOLOGICAL CONCENTRATION; FOOD CHAINS; FUKUSHIMA DAIICHI NUCLEAR POWER STATION; GLOBAL FALLOUT; REACTOR ACCIDENTS; SEAWATER; SIMULATION; STRONTIUM 90; THREE-DIMENSIONAL CALCULATIONS
- Descriptors DEC
- ACCIDENTS; ALKALINE EARTH ISOTOPES; BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; CESIUM ISOTOPES; EVEN-EVEN NUCLEI; FALLOUT; HYDROGEN COMPOUNDS; INTERMEDIATE MASS NUCLEI; ISOTOPES; NUCLEI; ODD-EVEN NUCLEI; OXYGEN COMPOUNDS; RADIOISOTOPES; REACTOR SITES; SAFETY STANDARDS; STANDARDS; STRONTIUM ISOTOPES; WATER; YEARS LIVING RADIOISOTOPES
Optional Information
- Copyright
- Copyright (c) 2014 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.