Radon concentrations in soil gas,considering radioactive equilibrium conditions with application to estimating fault-zone geometry |
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Authors: | Katsuaki Koike Tohru Yoshinaga Hisafumi Asaue |
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Institution: | (1) Graduate School of Science and Technology, Kumamoto University, 2-39-1 Kurokami, Kumamoto 860-8555, Japan;(2) Technical Division, Faculty of Engineering, Kumamoto University, 2-39-1 Kurokami, Kumamoto 860-8555, Japan;(3) Institute for Geo-Resources and Environment, Geological Survey of Japan, AIST, 1-1-3 Higashim Tsukuba, Tsukuba Ibaraki, 305-8567, Japan |
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Abstract: | A calculation method for determining the amount of Rn isotopes and daughter products at the start of measurement (CRAS) is
proposed as a more accurate means of estimating the initial Rn concentration in soil gas. The CRAS utilizes the decay law
between 222Rn and 220Rn isotopes and the daughter products 218Po and 216Po, and is applicable to α-scintillation counter measurements. As Rn is both inert and chemically stable, it is useful for
fault investigation based on the soil gas geochemistry. However, the total number of α particles emitted by the decay of Rn
has generally been considered to be proportional to the initial Rn concentration, without considering the gas condition with
respect to radioactive equilibrium. The CRAS method is shown to be effective to derive Rn concentration for soil gases under
both nonequilibrium conditions, in which the total number of decays increases with time, and equilibrium conditions, which
are typical of normal soil under low gas flux. The CRAS method in conjunction with finite difference method simulation is
applied to the analysis of two active fault areas in Japan, and it is demonstrated that this combination could detect the
sharp rises in 222Rn concentrations associated with faults. The method also allows the determination of fault geometry near the surface based
on the asymmetry variation of the Rn concentration distribution when coupled with a numerical simulation of 222Rn transport. The results for the new method as applied to the two case studies are consistent with the data collected from
the geological survey. It implies that the CRAS method is suitable for investigating the fault system and interstitial gas
mobility through fractures. The present analyses have also demonstrated that high Rn concentrations require the recent and
repeated accumulation of 222Rn parents (230Th and 226Ra) in fault gouges through deep gas release during fault movement. |
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Keywords: | Radon-222 α -scintillation counter Radioactive equilibrium Active fault Fault geometry Finite difference method |
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