Author/Authors :
Takuya Matsumoto، نويسنده , , Teruyuki Maruoka، نويسنده , , Gen Shimoda، نويسنده , , Hajime Obata، نويسنده , , Hiroyuki Kagi، نويسنده , , Katsuhiko Suzuki، نويسنده , , Koshi Yamamoto، نويسنده , , Takehiro Mitsuguchi، نويسنده , , Kyoko Hagino، نويسنده , , Naotaka Tomioka، نويسنده , , Chinmaya Sambandam، نويسنده , , Daniela Brummer، نويسنده , , Philipp Martin Klaus، نويسنده , , Pradeep Aggarwal، نويسنده ,
Abstract :
Tritium concentrations in Japanese precipitation samples collected after the March 2011 accident at the Fukushima Dai-ichi Nuclear Power Plant (FNPP1) were measured. Values exceeding the pre-accident background were detected at three out of seven localities (Tsukuba, Kashiwa and Hongo) southwest of the FNPP1 at distances varying between 170 and 220 km from the source. The highest tritium content was found in the first rainfall in Tsukuba after the accident; however concentrations were 500 times less than the regulatory limit for tritium in drinking water. Tritium concentrations decreased steadily and rapidly with time, becoming indistinguishable from the pre-accident values within five weeks. The atmospheric tritium activities in the vicinity of the FNPP1 during the earliest stage of the accident was estimated to be 1.5 × 103 Bq/m3, which is potentially capable of producing rainwater exceeding the regulatory limit, but only in the immediate vicinity of the source.
Keywords :
Fukushima , Radionuclide , tritium , Hydrology