TY - JOUR
T1 - Anomalous changes in atmospheric radon concentration before and after the 2011 northern Wakayama earthquake (Mj 5.5)
AU - Goto, Mikako
AU - Yasuoka, Yumi
AU - Nagahama, Hiroyuki
AU - Muto, Jun
AU - Omori, Yasutaka
AU - Ihara, Hayato
AU - Mukai, Takahiro
N1 - Publisher Copyright:
© The Author 2016.
PY - 2017
Y1 - 2017
N2 - A significant increase in atmospheric radon concentration was observed in the area around the epicentre before and after the occurrence of the shallow inland earthquake in the northern Wakayama Prefecture on 5 July 2011 (Mj 5.5, depth 7 km) in Japan. The seismic activity in the sampling site was evaluated to identify that this earthquake was the largest near the sampling site during the observation period. To determine whether this was an anomalous change, the atmospheric daily minimum radon concentration measured for a 13-year period was analysed. When the residual radon concentration values without the seasonal radon variation and the linear trend was > 3 standard deviations of the residual radon variation corresponding to the normal period, the values were deemed as anomalous. As a result, an anomalous increase in radon concentration was determined before and after the earthquake. In conclusion, anomalous change related to earthquakes with at least Mj 5.5 can be detected by monitoring atmospheric radon near the epicentre.
AB - A significant increase in atmospheric radon concentration was observed in the area around the epicentre before and after the occurrence of the shallow inland earthquake in the northern Wakayama Prefecture on 5 July 2011 (Mj 5.5, depth 7 km) in Japan. The seismic activity in the sampling site was evaluated to identify that this earthquake was the largest near the sampling site during the observation period. To determine whether this was an anomalous change, the atmospheric daily minimum radon concentration measured for a 13-year period was analysed. When the residual radon concentration values without the seasonal radon variation and the linear trend was > 3 standard deviations of the residual radon variation corresponding to the normal period, the values were deemed as anomalous. As a result, an anomalous increase in radon concentration was determined before and after the earthquake. In conclusion, anomalous change related to earthquakes with at least Mj 5.5 can be detected by monitoring atmospheric radon near the epicentre.
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M3 - Article
C2 - 27412515
AN - SCOPUS:85020074455
SN - 0144-8420
VL - 174
SP - 376
EP - 381
JO - Radiation Protection Dosimetry
JF - Radiation Protection Dosimetry
IS - 3
M1 - ncw220
ER -