Induced Change of Electric Self‐Potential and Magnetic Field at the Artificial Explosion

SUMMARY Study of the electric self‐potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The explosion was induced by 450‐kg gun powder placed at a depth of 32.2 m to 75 m. The SP was measured by four electrodes arranged in a line cross...

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Published inElectronics and communications in Japan Vol. 100; no. 3; pp. 68 - 75
Main Authors SAKAI, HIDEO, KOBAYASHI, TSUYOSHI, IZUMI, YOSHINORI, NAKAYAMA, TAKESHI, HATTORI, KATSUMI
Format Journal Article
LanguageEnglish
Published Hoboken Wiley Subscription Services, Inc 01.03.2017
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Abstract SUMMARY Study of the electric self‐potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The explosion was induced by 450‐kg gun powder placed at a depth of 32.2 m to 75 m. The SP was measured by four electrodes arranged in a line crossing the explosion point, where the distance of each electrode from the explosion ranged from 10 m to 100 m. Induced SP changes consisted of two portions, namely, fluctuations with shorter period (∼10 ms) and fluctuations with longer periods (∼50 ms). Regarding the latter, the amplitude was in proportion to the span length of electrode couples and the fluctuations arrived faster at the electrode couples nearer to the explosion. Furthermore, the increment of ground level in SP was observed in each electrode couple after the explosion, which was concordant with the distribution of apparent resistivity underground studied by the survey. The magnetic field measured by the fluxgate magnetometer at the site 35 m north from the explosion also showed change of a few nT after the explosion. This may have been caused by change of magnetic properties underground.
AbstractList SUMMARY Study of the electric self‐potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The explosion was induced by 450‐kg gun powder placed at a depth of 32.2 m to 75 m. The SP was measured by four electrodes arranged in a line crossing the explosion point, where the distance of each electrode from the explosion ranged from 10 m to 100 m. Induced SP changes consisted of two portions, namely, fluctuations with shorter period (∼10 ms) and fluctuations with longer periods (∼50 ms). Regarding the latter, the amplitude was in proportion to the span length of electrode couples and the fluctuations arrived faster at the electrode couples nearer to the explosion. Furthermore, the increment of ground level in SP was observed in each electrode couple after the explosion, which was concordant with the distribution of apparent resistivity underground studied by the survey. The magnetic field measured by the fluxgate magnetometer at the site 35 m north from the explosion also showed change of a few nT after the explosion. This may have been caused by change of magnetic properties underground.
Study of the electric self-potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The explosion was induced by 450-kg gun powder placed at a depth of 32.2 m to 75 m. The SP was measured by four electrodes arranged in a line crossing the explosion point, where the distance of each electrode from the explosion ranged from 10 m to 100 m. Induced SP changes consisted of two portions, namely, fluctuations with shorter period (10 ms) and fluctuations with longer periods (50 ms). Regarding the latter, the amplitude was in proportion to the span length of electrode couples and the fluctuations arrived faster at the electrode couples nearer to the explosion. Furthermore, the increment of ground level in SP was observed in each electrode couple after the explosion, which was concordant with the distribution of apparent resistivity underground studied by the survey. The magnetic field measured by the fluxgate magnetometer at the site 35 m north from the explosion also showed change of a few nT after the explosion. This may have been caused by change of magnetic properties underground.
SUMMARY Study of the electric self-potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The explosion was induced by 450-kg gun powder placed at a depth of 32.2 m to 75 m. The SP was measured by four electrodes arranged in a line crossing the explosion point, where the distance of each electrode from the explosion ranged from 10 m to 100 m. Induced SP changes consisted of two portions, namely, fluctuations with shorter period (10 ms) and fluctuations with longer periods (50 ms). Regarding the latter, the amplitude was in proportion to the span length of electrode couples and the fluctuations arrived faster at the electrode couples nearer to the explosion. Furthermore, the increment of ground level in SP was observed in each electrode couple after the explosion, which was concordant with the distribution of apparent resistivity underground studied by the survey. The magnetic field measured by the fluxgate magnetometer at the site 35 m north from the explosion also showed change of a few nT after the explosion. This may have been caused by change of magnetic properties underground.
Author HATTORI, KATSUMI
IZUMI, YOSHINORI
KOBAYASHI, TSUYOSHI
SAKAI, HIDEO
NAKAYAMA, TAKESHI
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10.1111/j.1365-246X.2011.05309.x
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10.1029/GL003i007p00365
10.5194/nhess-7-535-2007
10.4294/jpe1952.40.447
10.1093/gji/ggu435
10.1029/GL017i009p01465
10.1029/97JB00729
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Snippet SUMMARY Study of the electric self‐potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The...
SUMMARY Study of the electric self-potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The...
Study of the electric self-potential (SP) and the magnetic field was conducted at the explosion seismic experiment in Ooyama, Toyama Prefecture. The explosion...
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SubjectTerms apparent resistivity
Couples
Electric potential
electric self‐potential
Electrical resistivity
Electrodes
Electronics
explosion seismic experiment
Explosions
Fluctuation
Fluxgate magnetometers
Ground level
magnetic field
Magnetic fields
Magnetic properties
Underground explosions
Title Induced Change of Electric Self‐Potential and Magnetic Field at the Artificial Explosion
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