Induced change of electric self-potential and magnetic field at the artificial explosion

被引:0
作者
Sakai H. [1 ]
Kobayashi T. [1 ]
Izumi Y. [2 ]
Nakayama T. [2 ]
Hattori K. [2 ]
机构
[1] Department of Earth Sciences, University of Toyama, 3190 Gofuku, Toyama
[2] Disaster Prevention Research Institute, Kyoto University, Uji
基金
日本学术振兴会;
关键词
Apparent resistivity; Electric self-potential; Explosion seismic experiment; Magnetic field;
D O I
10.1541/ieejfms.136.291
中图分类号
学科分类号
摘要
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 32.2-75 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 to 100 m. Induced SP changes consisted of two portions, namely, fluctuations with shorter periods (∼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. Further, 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. © 2016 The Institute of Electrical Engineers of Japan.
引用
收藏
页码:291 / 296
页数:5
相关论文
共 18 条
[1]  
Fraser-Smith A.C., Bernardi A., McGill P.R., Ladd M.E., Helliwell R.A., Villard O.G., Low frequency magnetic field measurements near the epicenter of the Ms 7.1 Loma Prieta earthquake, Geophys. Res. Lett., 17, pp. 1465-1468, (1990)
[2]  
Nagao T., Hattori K., Sayanagi K., Application for earthquake prediction research: Relationship between earthquakes and magnetic field changes (The Special Issue on geomagnetism: Earth and planetary science), J. JSAEM, 9, 4, pp. 435-442, (2001)
[3]  
Okubo K., Takeuchi A., Nakamura Y., Takeuchi N., Underground electric signal at the occurrence of the niigataken chuetsu-oki earthquake in 2007, Jpn, Phys. & Chemi. Earth, 34, pp. 373-379, (2009)
[4]  
Widarto D.S., Mogi T., Tanaka Y., Nagao T., Hattori K., Uyeda S., Co-seismic geoelectrical potential changes associated with the June 4, 2000's earthquake (Mw7.9) in Bengkulu, Indonesia, IEICE Trans. Electron, E95C, 1, pp. 110-114, (2012)
[5]  
Nagata T., Kinoshita H., Studies of piezo-magnetization, J. Geomag. Geoelectr., 17, pp. 121-135, (1965)
[6]  
Mizutani H., Ishido T., Yokokura T., Ohnishi S., Electrokinetic phenomena associated with earthquakes, Geophys. Res. Lett., 33, pp. 365-368, (1976)
[7]  
Ogawa T., Oike K., Miura T., Electromagnetic radiation from rocks, ? International Conf. Atmospheric Elect., pp. 504-507, (1984)
[8]  
Yoshida S., Uyeshima M., Nakatani M., Electric potential changes associated with slip failure of granite: Preseismic and coseismic signals, J. Geophys. Res., 102, pp. 14883-14897, (1997)
[9]  
Freund F.T., Pre-earthquake signals - Part I: Deviatoric stresses turn rocks into a source of electric currents, Natural Hazards & Earth Syst. Sci., 7, pp. 535-541, (2007)
[10]  
Sakai H., Oda H., Nakayama T., Doi H., Electromagnetic changes at explosion seismic experiment, J. Phys. Earth, 40, pp. 447-458, (1992)