Spatiotemporal distributions of Fukushima-derived radionuclides in nearby marine surface sediments

Spatiotemporal distributions of anthropogenic radionuclides in marine surface sediments off Miyagi, Fukushima, and Ibaraki Prefectures were analyzed on the basis of data collected during the monitoring program launched by the Japanese Ministry of Education, Sports, Science and Technology in 2011 right after the Fukushima Dai-ichi Nuclear Power Plant accident began. Concentrations of 137 Cs in the surface sediments varied spatially by two orders of magnitude, from 1.7 to 580 Bq kg-dry −1 , and there was no obvious correlation between 137 Cs concentration and the proximity of the sampling location to the accident site. The total inventory of 137 Cs accumulated in the upper 3 cm of surface sediments in the monitoring area was estimated to be 3.78 × 10 13 Bq, that is, 0.1–2% of the total 137 Cs flux from the plant to the ocean as a result of the accident (the percentage depends on the model used to estimate the total flux). The spatial variations of 137 Cs concentration and inventory depended on two main factors: the 137 Cs concentration in the overlying water during the first several months after the accident and the physical characteristics of the sediments (water content and bulk density). The temporal variations of the concentrations of other anthropogenic radionuclides ( 90 Sr, 95 Nb, 110 m Ag, 125 Sb, 129 Te, and 129 m Te) in the sediments were also investigated. Activity ratios of these nuclides to 137 Cs suggest that the nuclides themselves were not homogenized before they were removed from seawater to the sediments.