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The monitoring of microseismicity during temporary human activities such as fluid injections for hydrofracturing, hydrothermal stimulations or wastewater disposal is a difficult task. The seismic stations often cannot be installed on hard rock, and at quiet places, noise is strongly increased during the operation itself and the installation of sensors in deep wells is costly and often not feasible. The combination of small-aperture seismic arrays with shallow borehole sensors offers a solution. We tested this monitoring approach at two different sites: (1) accompanying a fracking experiment in sedimentary shale at 4 km depth and (2) above a gas field under depletion. The small-aperture arrays were planned according to theoretical wavenumber studies combined with simulations considering the local noise conditions. We compared array recordings with recordings available from shallow borehole sensors and give examples of detection and location performance. Although the high-frequency noise on the 50-m-deep borehole sensors was smaller compared to the surface noise before the injection experiment, the signals were highly contaminated during injection by the pumping activities. Therefore, a set of three small-aperture arrays at different azimuths was more suited to detect small events, since noise recorded on these arrays is uncorrelated with each other. Further, we developed recommendations for the adaptation of the monitoring concept to other sites experiencing induced seismicity.
Wydawca
Czasopismo
Rocznik
Tom
Strony
311--326
Opis fizyczny
Bibliogr. 38 poz.
Twórcy
autor
- GFZ German Research Centre for Geosciences, Potsdam, Germany
- University of Potsdam, Potsdam, Germany
autor
- GFZ German Research Centre for Geosciences, Potsdam, Germany
- NORSAR, Kjeller, Norway
autor
- GFZ German Research Centre for Geosciences, Potsdam, Germany
- University of Potsdam, Potsdam, Germany
autor
- GFZ German Research Centre for Geosciences, Potsdam, Germany
- King Abdullah University of Science and Technology, Thuwal, Kingdom of Saudi Arabia
autor
- GFZ German Research Centre for Geosciences, Potsdam, Germany
autor
- GFZ German Research Centre for Geosciences, Potsdam, Germany
- University of Potsdam, Potsdam, Germany
Bibliografia
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- 5. Cesca S, López-Comino J, Kühn D, Dahm T (2016) Array in Wittewierum, Netherlands. deutsches geoforschungszentrum gfz. other/seismic network. https://doi.org/10.14470/6P7561560569
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- 7. Dost B, Ruigrok E, Spetzler J (2017) Development of seismicity and probabilistic hazard assessment for the Groningen gas field. Neth J Geosci 96(5):s235–s245
- 8. Ellsworth W (2018) Injection-induced earthquakes. Science 341(6142):10.1126/science.1225,942
- 9. Green C, Styles P, Baptie J (2012) Review and recommendations for induced seismicity mitigation. Preese Hall Shale Gas Fracturing—Induced Seismicity Report pp 1–22
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- 15. Hofman L, Ruigrok E, Dost B, Paulssen H (2017) A shallow seismic velocity model for the Groningen area in the Netherlands. J Geophys Res Solid Earth 122(10):8035–8050
- 16. Horton (2012) Disposal of hydrofracking waste fluid by injection into subsurface aquifers triggers earthquake swarm in Central Arkansas with potential for damaging earthquake. Seismol Res Lett 83(2):doi.org/10.1785/gssrl.83.2.250
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- 22. López-Comino J, Cesca S, Jarosławski J, Montcoudiol N, Heimann H, Dahm T, Lasocki S, Gunning A, Capuano P, Ellsworth W (2018) Induced seismicity response of hydraulic fracturing: results of a multidisciplinary monitoring at the Wysin site, Poland. Sci Rep 20:251–267
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- 29. Rubinstein J, Ellsworth W, McGarr A, Benz H (2014) The 2001-present induced earthquake sequence in the Raton Basin of Northern New Mexico and Southern Colorado. Bull Seismol Soc Am 104(5):10.1785/012,014
- 30. Sasaki S (1998) Characteristics of microseismic events induced during hydraulic fracturing experiments at the Hijori hot dry rock geothermal site. Tectonophysics 289:171–188
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- 32. Sick B, Joswig M (2016) Combining network and array waveform coherence for automatic location: examples from induced seismicity monitoring. Geophys J Int 208(3):1373–1388
- 33. Spetzler J, Dost B (2017) Hypocentre estimation of induced earthquakes in Groningen. Geophys J Int 209(1):453–465
- 34. Stipčević J, Kennett BL, Tkalčić H (2017) Simultaneous use of multiple seismic arrays. Geophys J Int 209(2):770–783
- 35. Tadokoro K, Ando M, Nishigami K (2000) Induced earthquakes accompanying the water injection experiment at the Nojima fault zone, Japan: seismicity and its migration. J Geophys Res 105(B3):6089–6104
- 36. Wathelet M, Jongmans D, Ohrnberger M, Bonnefoy-Claudet S (2008) Array performances for ambient vibrations on a shallow structure and consequences over Vss inversion. J Seismol 12(1):1–19
- 37. Willacy C, van Dedem E, Minisini S, Li J, Blokland J, Das I, Droujinine A (2018) Application of full-waveform event location and moment-tensor inversion for Groningen induced seismicity. Lead Edge 37(2):92–99
- 38. Zywicki DJ (1999) Advanced signal processing methods applied to engineering analysis of seismic surface waves. Ph.D. thesis, Georgia Institute of Technology
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-8ac478ff-5545-4b4e-9a99-402a03bdda36