222Rn fluxes from the ground surface and
226Ra contents in soil were measured on Hachijo-jima Island, which is a solitary island in the Pacific Ocean located about 200 km to the south of the main island of Japan, to evaluate fractional contributions of the locally exhaled
222Rn and the long-range transported one to the surface air concentration measured on this island. Averages of
222Rn flux and
226Ra content in dry soil were evaluated to be 0.9 ± 0.4 mBq m
-2 s
-1 and 6.8 ± 0.2 Bq kg
-1, respectively. These are considerably smaller than the respective values of 9.7 ± 0.8 mBq m
-2 s
-1 and 23.2 ± 0.4 Bq kg
-1 measured at Nagoya as a reference. The lower value of the
226Ra content and the even lower
222Rn flux on this island can be attributed to the basaltic geology and the soil's coarse texture and high moisture, respectively. A simple model calculation assuming a typical nocturnal condition showed that the measured
222Rn flux would cause only a small increase in the surface air concentration by 0.035 to 0.072 Bq m
-3 (relative contribution of 1 to 12%) in addition to the long-range transported
222Rn under a typical nocturnal condition. The contribution of the local flux would be smaller than that under nocturnal condition. This local
222Rn component is negligible as compared with the concentration of the long-range transported
222Rn (0.6 to 3.6 Bq m
-3). It is, therefore, concluded that Hachijo-jima Island is suitable for measuring the long-range transported atmospheric
222Rn in East Asia region.
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