Author/Authors :
Thornton، نويسنده , , Blair and Ohnishi، نويسنده , , Seiki and Ura، نويسنده , , Tamaki and Odano، نويسنده , , Naoteru and Sasaki، نويسنده , , Shun and Fujita، نويسنده , , Tsuneo and Watanabe، نويسنده , , Tomowo and Nakata، نويسنده , , Kaoru and Ono، نويسنده , , Tsuneo and Ambe، نويسنده , , Daisuke، نويسنده ,
Abstract :
An estimated 3.5 ± 0.7 × 1015 Bq of 137Cs is thought to have been discharged into the ocean following the melt down at Fukushima Dai-ichi Nuclear Power Plant (F1NPP). While efforts have been made to monitor seafloor radiation levels, the sampling techniques used cannot capture the continuous distribution of radionuclides. In this work, we apply in situ measurement techniques using a towed gamma ray spectrometer to map the continuous distribution of 137Cs on the seafloor within 20 km of the F1NPP. The results reveal the existence of local 137Cs anomalies, with levels of 137Cs an order of magnitude higher than the surrounding seafloors. The sizes of the anomalies mapped in this work range from a few meters to a few hundreds of meters in length, and it is demonstrated that the distribution of these anomalies is strongly influenced by meter scale features of the terrain.
Keywords :
Fukushima Dai-ichi Nuclear Power Plant , Radioactive cesium , Towed gamma ray spectrometer , marine sediment , Terrain features