Japan Geoscience Union Meeting 2015

Presentation information

International Session (Oral)

Symbol S (Solid Earth Sciences) » S-TT Technology & Techniques

[S-TT13] Recent Advances in Exploration Geophysics (RAEG2015)

Wed. May 27, 2015 2:15 PM - 4:00 PM 102A (1F)

Convener:*Hitoshi Mikada(Kyoto University), Junichi Takekawa(Graduate School of Science, Kyoto University), Junzo Kasahara(University of Shizuoka, Faculty of Earth Scieces), Yoshihisa Iio(Disater Prevention Research Institute, Kyoto University), Yasuo Ogawa(Volcanic Fluid Research Center Tokyo Institute of Technology), Nobukazu Seama(Department of Earth and Planetary Sciences, Graduate School of Science, Kobe University), Tatsuya Sato(Geothermal Energy Research & Development Co., LTD.), Eiichi Asakawa(JGI, Incorporated), Chair:Ehsan Jamali Hondori(JGI, Inc.), Hitoshi Mikada(Kyoto University)

3:00 PM - 3:15 PM

[STT13-04] An experiment of subsidence monitoring in the quarry area by a seismic source during two months: near source observation

*Aya KAMIMURA1, Junzo KASAHARA1, Naoyuki FUJII1, Motoyuki USHIYAMA1 (1.Shizuoka Univ.)

Keywords:time lapse, artificial seismic sourcce, subsidence, seismic method, disaster prevention

We tested to monitor temporal changes in the subsurface at the quarry area. At this quarry, there is a subsidence warning system to detect micro-earthquakes associated with the subsidence measured by seismometers. At the past subsidence, seismic vibrations were repeatedly observed during several months, but the 2014 subsidence showed only four vibration events preceding to the subsidence. It is thought that if we can observe any other temporal changes of the subsurface before the vibration, we could help to find subsidence. Therefore we carried out "seismic time-lapse observation". We used a control seismic source on the ground at fix location, and tested whether any changes of the subsurface changes during the observation period was caught or not.
Field test
We carried out one-week experiments twice in July and August of 2014. The first and the second experiments were from 16 to 21 in July and from 21 to 25 in August, respectively. We used electro-magnetic vibrator developed by Kawasaki Geological Engineering Co. Ltd as the seismic source. We set 100-second sweep from 10 to 50 Hz and 5-second rest with the GPS time accuracy and repeated 32 sweeps with 5 second rest in an hour. We operated the vibrator 12 hours consecutively at night (20:00 - 08:00).
We recorded accelerations signals of reaction-mass and base-plate with desired signals, and seismic waves at east of the source, south of the source, and near the source. Local warning system of 97 geophones also recorded these artificial seismic data.
We carried out FFT conversions of observed data. We transformed two sweep sequences of seismic records to the frequency domain and stacked 16 sets of data in 1 hour. We calculated source signature using the reaction-mass and the baseplate accelerations of the vibrator. The transfer functions between the source and a receiver were obtained by the division of observed spectra by source signature. After applied window function in spectral domain, we inverse-transformed the data into a time domain.
In this paper we report the characteristics near the source. When we set the amplitude of seismometer beside the source was 100, that of eastern seismometer (ca. 35m east of source) was 5, and that of southern seismometer (ca. 45m south of source) was 2 (vertical axis). The transfer function of 18 and 19 of July showed a change in comparison with others periods. There were few changes of the transfer functions during an experiment period of August.
Discussion and conclusions
We checked the weather condition during experimental periods. On July 18 03:00-04:00, 28mm/hour rainfalls measured by the neighboring precipitation observatory, and intense thunderstorm was recorded at the test field. In other periods, such heavy rainfalls were not observed. From these data, it is thought that the near surface layers including the water by rainfalls changed the transfer function of the test field.
This study was supported by the Center for Integrated Research and Education of Natural Hazard, of Shizuoka University. The field experiments was carried out by Kawasaki Geological Engineering Co., Ltd.
Kasahara, J., et al., Real time Imaging of CO2 storage zone by very accurate-stable-long term seismic source, Energy Precedia, 2013d.
Kasahara, J., et al., Observation of very larger temporal changes due to the near surface effects and importance on the time-lapse study, Proc. Soc. #130 Exploration Geophysicists of Japan, 212-215, 2014.
Kubota, R., et al., Development of the Seismic ACROSS using electro-magnetic vibrator, Proc. "2nd KACST-KCUST-JCCP international workshop on Surface and Subsurface 4D Monitoring", KAUST Feb. 2014.
Kunitomo, T., et al., Active monitoring of the Earth's structure by the seismic ACROSS - Transmitting and receiving technologies of the seismic ACROSS, Proc. 1st International Workshop "Active Monitoring in the Solid Earth Geophysics", in Mizunami, Japan, S4-04., 2004.