Normal seasonal variations for atmospheric radon concentration: a sinusoidal model

2015 ◽  
Vol 139 ◽  
pp. 149-153 ◽  
Author(s):  
Koseki Hayashi ◽  
Yumi Yasuoka ◽  
Hiroyuki Nagahama ◽  
Jun Muto ◽  
Tetsuo Ishikawa ◽  
...  
2006 ◽  
Vol 21 (6) ◽  
pp. 1064-1072 ◽  
Author(s):  
Yumi Yasuoka ◽  
George Igarashi ◽  
Testuo Ishikawa ◽  
Shinji Tokonami ◽  
Masaki Shinogi

2018 ◽  
Vol 8 (1) ◽  
Author(s):  
Daichi Iwata ◽  
Hiroyuki Nagahama ◽  
Jun Muto ◽  
Yumi Yasuoka

2007 ◽  
Vol 7 (5) ◽  
pp. 629-635 ◽  
Author(s):  
Y. Omori ◽  
Y. Yasuoka ◽  
H. Nagahama ◽  
Y. Kawada ◽  
T. Ishikawa ◽  
...  

Abstract. Anomalous emanation of radon (222Rn) was observed preceding large earthquakes and is considered to be linked to preseismic electromagnetic phenomena (e.g. great changes of atmospheric electric field and ionospheric disturbances). Here we analyze atmospheric radon concentration and estimate changes of electrical conditions in atmosphere due to preseismic radon anomaly. The increase of radon emanation obeys crustal damage evolution, following a power-law of time-to-earthquake. Moreover, the radon emanation decreases the atmospheric electric field by 40%, besides influencing the maximum strength of atmospheric electric field by 104–105 V/m enough to trigger ionospheric disturbances. These changes are within the ranges observed or explaining electromagnetic phenomena associated with large earthquakes.


2005 ◽  
Vol 40 (2-6) ◽  
pp. 686-694 ◽  
Author(s):  
F. Bochicchio ◽  
G. Campos-Venuti ◽  
S. Piermattei ◽  
C. Nuccetelli ◽  
S. Risica ◽  
...  

2009 ◽  
Vol 34 (6-7) ◽  
pp. 431-434 ◽  
Author(s):  
Yumi Yasuoka ◽  
Yusuke Kawada ◽  
Hiroyuki Nagahama ◽  
Yasutaka Omori ◽  
Tetsuo Ishikawa ◽  
...  

2007 ◽  
Vol 14 (2) ◽  
pp. 123-130 ◽  
Author(s):  
Y. Kawada ◽  
H. Nagahama ◽  
Y. Omori ◽  
Y. Yasuoka ◽  
T. Ishikawa ◽  
...  

Abstract. Prior to large earthquakes (e.g. 1995 Kobe earthquake, Japan), an increase in the atmospheric radon concentration is observed, and this increase in the rate follows a power-law of the time-to-earthquake (time-to-failure). This phenomenon corresponds to the increase in the radon migration in crust and the exhalation into atmosphere. An irreversible thermodynamic model including time-scale invariance clarifies that the increases in the pressure of the advecting radon and permeability (hydraulic conductivity) in the crustal rocks are caused by the temporal changes in the power-law of the crustal strain (or cumulative Benioff strain), which is associated with damage evolution such as microcracking or changing porosity. As the result, the radon flux and the atmospheric radon concentration can show a temporal power-law increase. The concentration of atmospheric radon can be used as a proxy for the seismic precursory processes associated with crustal dynamics.


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