Soil radon in winter months under snowpack in Hokkaido, Japan

摘要

Soil radon (~(222)Rn) has been monitored during winter months under cool-temperate deciduous stands of different surface geology in Tomakomai and in Sapporo, Hokkaido, Japan. Radon level was lower in Tomakomai of immature soil of porous volcanic ash emitted from an active volcano (Mt. Tarumae), compared with those in Sapporo of alluvial sediments. In Tomakomai, mean value of the ~(222)Rn activity concentration was higher in winter (570 Bq m~(-3))than in summer (350 Bq m~(-3))at a depth of 1 m, which is consistent with the results in cold and dry winter reported in the literature. In contrast, soil radon decreasing with decreasing soil temperature from mid-September (5.0 kBq m~(-3)) remained low (2.6 kBq m~(-3)) under persistent snow in Sapporo, which had already been observed in the same location. Measurements of the activity concentrations of ~(222)Rn in snow and in snow air as well as in soil air indicate that the small amount of ~(222)Rn is released from the ground surface to the overlying snowpack with a ~(222)Rn flux density of 0.4 mBq m~(-2) s~(-1) under thick snow cover in Sapporo.