The Fukushima accident remains, to date, the largest accidental release of radionuclides into the marine environment. It resulted in particularly high concentrations in water, living species, and sediments, which will be measurable in the medium and long term near the coast and across the entire North Pacific. This accident highlights the need for operational tools to quickly model and predict the fate of radionuclides released into the sea in order to assess the impact of radioactivity on marine ecosystems. Developing reliable methods to evaluate the impact of an accidental release on the marine environment requires improving our knowledge on: (1) processes at the land-ocean interface; (2) the dispersion of radionuclides in water masses; (3) the fixation and transport of radionuclides by particulate matter on various spatio-temporal scales; (4) the transfer of radionuclides within food chains; and (5) the sensitivity and vulnerability of affected ecosystems. These five research areas form the framework of the ANR AMORAD project (Improvement of prediction models for radionuclide dispersion and impact assessment in the environment; ANR-11-RSNR-0002), to which the TRAMAT campaign is attached.
The evolution of concentrations measured in the marine environment near the accident site confirms what has been observed in the English Channel and the Irish Sea: the medium- and long-term persistence of pollutant concentrations is largely controlled by the dynamics of sediment transport. Once pollutants are fixed by suspended matter, sedimenting particles can retain traces for years, with transport dynamics unique to them. Radionuclides released under controlled conditions by industry can serve as valuable markers to track these movements.
Understanding the transport of radionuclides via particulate matter involves: (1) hydro-sedimentary modeling in regions close to contamination sources (in the short term) or further away (in the long term); (2) improving models by incorporating processes observed in situ that are still poorly understood; (3) comparing model results with in situ measurements. In situ observation of particulate matter now benefits from many punctual or integrated measurement tools such as the DYSPI (Dynamic Sediment Profiler Imagery developed jointly by IFREMER and IRSN) (Blanpain et al., 2009), the AQUASCAT (suspended sediment profiler, AQUATEC GROUP®) (Moore et al., 2013), the LISST (in situ granulometer, SEQUOIA®) (Pedocchi and García, 2006), particle tracing via the measurement of radionuclides they carry (Boust, 1999), or stratified sampling in facies at hydro-sedimentary equilibrium (sampling by divers).
References :
Blanpain, O., du Bois, P.B., Cugier, P., Lafite, R., Lunven, M., Dupont, J., Le Gall, E., Legrand, J., Pichavant, P., 2009. Dynamic sediment profile imaging (DySPI): a new field method for the study of dynamic processes at the sediment-water interface. Limnology and Oceanography: Methods, 7, 8-20.
Boust, D., 1999. Distribution and inventories of some artificial and naturally occurring radionuclides in medium to coarse-grained sediments of the channel. Continental Shelf Research, 19, 1959-1975.
Moore, S.A., Dramais, G., Dussouillez, P., Le Coz, J., Rennie, C., Camenen, B., 2013. Acoustic measurements of the spatial distribution of suspended sediment at three sites on the Lower Mekong River. The Journal of the Acoustical Society of America, 133, 3227-3227.
Pedocchi, F., García, M.H., 2006. Evaluation of the LISST-ST instrument for suspended particle size distribution and settling velocity measurements. Continental Shelf Research, 26, 943-958.