2011 Volume 60 Issue 8 Pages 323-328
Concentration profiles of 134Cs and 137Cs were obtained in an undisturbed paddy field before plowing in Fukushima prefecture on May 24th, 2011, about two month after explosions of Fukushima Daiichi nuclear power plant. Top soil of 0 - 15cm was sampled, by separating it into 6 layers of 1 - 5cm thick. Resulting concentration profile indicates that 88% of 134Cs+137Cs existed within 0 - 3cm and 96% within 0 - 5cm layer. However, although most of radioactive Cs stays within a few cm surface layer, a part of it already reached 10 - 15cm layer. Mean travel distance of 134Cs and 137Cs were calculated from the profile to be 1.74cm;on the other hand, mean travel distance of water molecules during the 70days was also estimated as [precipitation - evaporation]/[volumetric water content] to be about 20cm. Therefore, convective velocity of Cs was 1/10 of water due to sorption of Cs on soil. However, this ratio of Cs velocity is 2 - 3 order greater than that calculated from soil-soil solution distribution coefficients(Kd) for soils of Japanese paddy field shown in a literature, indicating that the movement of Cs in the field occurs in condition far from sorption equilibrium.