Evaluation of radioactive cesium impact from atmospheric deposition and direct release fluxes into the North Pacific from the Fukushima Daiichi nuclear power plant
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文摘

The atmospheric deposition is essential to reproduce the distribution of 134Cs activity in the North Pacific after the Fukushima Nuclear accident.

134Cs activities observed north of 42°N in 2012 originated from atmospheric deposition.

134Cs from atmospheric deposition (direct release) was transported to the Central Mode Water(CMW) since April 2011 (during the winter of 2012).

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