1980 年 15 巻 1 号 p. 47-53
222Rn escape-to-production ratio of soil is estimated based on the 226Ra concentration determined by using NaI(Tl) detector and the 222Rn emanating power of soil (the 222Rn emanating power of soil is the activity of 222Rn that escapes into soil gas per gram of dry soil at equilibrium state). The value for it is 32.2±5.9% for the soil of the campus of Nagoya University. The dependence of 222Rn escape-to-production ratio of this soil on the water content of soil is observed.
The measurement of the 222Rn escape-to-production ratio is also carried out by using Ge(Li) detector. In measuring the sampled soils, they are not dried because of the dependence of 222Rn escape-to-production ratio of the soil on the water content of soil. The measured value for the soil of the campus of Nagoya University is 38.9±5.0% and agrees with that measured by the above-mentioned technique.
In contrast to the method hitherto used, the method presented in this work enables us to evaluate exposure rate from the sources of 238U-series precisely and easily in a laboratory.