JpGU-AGU Joint Meeting 2017

Presentation information

[JJ] Poster

S (Solid Earth Sciences) » S-SS Seismology

[S-SS17] [JJ] Fault Rheology and Earthquake Physics

Sun. May 21, 2017 1:45 PM - 3:15 PM Poster Hall (International Exhibition Hall HALL7)

convener:Takanori Matsuzawa(National Research Institute for Earth Science and Disaster Resilience), Takeshi Iinuma(National Research and Development Agency Japan Agency for Marine-Earth Science and Technology), Wataru Tanikawa(Japan Agency for Marine-Earth Science and Technology, Kochi Instutute for Core Sample Research), Hideki Mukoyoshi(Department of Geoscience Interdisciplinary Graduate School of Science and Engineering, Shimane University)

[SSS17-P11] Moment tensor analysis of acoustic emissions induced by hydraulic fracturing in laboratory experiments

*Makoto Naoi1, Kengo Nishihara1, Kazune Yamamoto1, Shunsuke Yano1, Wataru Fujito1, Youqing CHEN1, Tsuyoshi Ishida1, Hironori Kawakata2, Takashi Akai3, Isao Kurosawa3 (1.Kyoto University, 2.Ritsumeikan University, 3.Japan Oil, Gas and Metals National Corporation)

Keywords:Acoustic Emission, Hydraulic fracturing, Moment tensor

Hydraulic fracturing has been used for the development of Enhanced Geothermal reservoirs and Shale Gas/Oil reservoirs in order to stimulate reservoirs by producing artificial fractures. Microseismic observation is often employed to monitor the hydraulic fracturing. Some field observations suggested that shear events were dominated (e.g., Maxwell, 2013), although an open crack along the maximum compression axis is predicted by stress concentration around a circular hole in elastic medium. Focal mechanisms of earthquakes induced by hydraulic fracturing is important because, for example, proppants are injected so as to prevent closing cracks in Shale Gas/Oil Reservoirs and they should enter open cracks more easily. It is however difficult to constrain focal mechanisms of induced earthquakes in such fields due to insufficient network coverage.
In the present study, we conducted hydraulic fracturing laboratory experiments under uniaxial loading by using 7 granite samples, and monitored acoustic emissions (AE) by a 16-channel AE monitoring system, estimating their seismic moment tensors. Generally, moment tensor analysis, in which accurate measurements of waveform amplitudes are necessary, is difficult for AE data owing to unknown and complex sensor characteristics such as sensor sensitivity depending on sensor coupling. In this study, we estimated the influence of coupling of individual AE sensors in each experiment by using an approach similar to Kwiatek et al. (2013), and estimated moment tensors by using calibrated AE amplitudes. We classified the obtained moment tensor solutions into isotropic, double couple and CLVD dominant solutions on the basis of the decomposition method of Knopoff and Randall (1970). The shear-dominated events occupied 20%-55% whereas CLVD dominated events indicating open-mode cracks occupied 10–20%. In addition, T-axes of the CLVD dominated events (corresponds to open axis of the corresponding open cracks) were consistent with that of the open cracks predicted by stress concentration nearby a circular hole.