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Published bySamuel Atkins Modified over 5 years ago
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A remote, wireless microseismic monitoring system
Henry C. Bland, Robert R. Stewart, Malcolm B. Bertram, Eric V. Gallant, and Jeff Thurston Funded by Coordinated University Research for Synergy & Effectiveness, Alberta Energy Research Institute, Government of Alberta Alberta Community Development
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Microseismic / Passive Seismic Monitoring Applications
Reservoir monitoring Microfractures Fluid containment Tomography Landslide prediction Structural integrity monitoring Mine Stability Nuclear blast detection Military / Border patrol
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Passive seismic for reservoir monitoring
Seismic emanations come from fracturing rock, reservoir pressurization changes or fluid-induced microfracturing (Maxwell et al. 2003) Microseismic hypocentres are mapped in 4-D Reservoir changes may be inferred from maps Regional seismic monitoring may used to resolve public complaints of oilfield-induced seismicity.
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Landslide detection / prediction
Increased microseismic activity may be a predictor for large-scale slides Hypocentre concentrations may indicate new fractures or fault slip 30 million cubic meters of rock fell at Randa Switzerland in 1991. Randa, Switzerland
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Remote, wireless microseismic recording system
Remote data collection centre GPS 3-C geophone time stamp 3-C A/D converter Microcontroller WLAN Radio digital waveform data packets
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Passive Seismic Monitoring Network
Remote Station 1 Remote Station 2 Data Collection Centre Remote Station 3 Remote Station 4 Remote Station 5
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System components Power controller A/D converter Microcontroller
Solar panel Time source (GPS) WLAN Radio Directional antenna Battery
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System Construction GPS Antenna Solar panel (active side on back)
Geophones Electronics Box Post secured with guy wire, turnbuckle, bolt hanger, rock bolt Battery Box Base mount
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3-C Microvibrator Arrow
Handle contains 2 AA batteries and drive electronics Spike 3-C vibrator Cable connected to output of blaster (used to start vibration sequence)
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3-C Microvibrator Cube 3 cm Y X Z
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Pancake vibrators
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Summary 3-C recording is frequently used for passive seismic recording as it help provide directional information for received microseismic events Current technology for remote monitoring based requires a large power infrastructure, particularly for northern latitudes We will continue our efforts to reduce power consumption, complexity, size and cost as we strive to make a portable wireless geophone 3-C Microvibrator technology may prove useful for automated testing of 3-C geophones
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