摘要
We measured the concentrations of 131I, 134Cs, and 137Cs released from the Fukushima nuclear accident in soil and rainwater samples collected March 30-31, 2011, in Ibaraki Prefecture, Kanto district, bordering Fukushima Prefecture to the south. Column experiments revealed that all 131I in rainwater samples was adsorbed onto an anion-exchange resin. However, 30%of 131I was not retained by the resin after it passed through a soil layer, suggesting that a portion of 131I became bound to organic matter from the soil. The 137Cs migration rate was estimated to be approximately 0.6聽mm/y in the Kanto area, which indicates that contamination of groundwater by 137Cs is not likely to occur in rainwater infiltrating into the surface soil after the Fukushima accident.