Fiber‐Optic Network Observations of Earthquake Wavefields
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- Nathaniel J. Lindsey
- Earth and Planetary Science Department University of California Berkeley CA USA
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- Eileen R. Martin
- Institute for Computational and Mathematical Engineering Stanford University Stanford CA USA
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- Douglas S. Dreger
- Earth and Planetary Science Department University of California Berkeley CA USA
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- Barry Freifeld
- Energy Geosciences Division Lawrence Berkeley National Laboratory Berkeley CA USA
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- Stephen Cole
- OptaSense, Inc. Brea CA USA
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- Stephanie R. James
- Department of Geological Sciences University of Florida Gainesville FL USA
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- Biondo L. Biondi
- Institute for Computational and Mathematical Engineering Stanford University Stanford CA USA
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- Jonathan B. Ajo‐Franklin
- Energy Geosciences Division Lawrence Berkeley National Laboratory Berkeley CA USA
書誌事項
- 公開日
- 2017-12-08
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#am
- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1002/2017gl075722
- 公開者
- American Geophysical Union (AGU)
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説明
<jats:title>Abstract</jats:title><jats:p>Our understanding of subsurface processes suffers from a profound observation bias: seismometers are sparse and clustered on continents. A new seismic recording approach, distributed acoustic sensing (DAS), transforms telecommunication fiber‐optic cables into sensor arrays enabling meter‐scale recording over tens of kilometers of linear fiber length. We analyze cataloged earthquake observations from three DAS arrays with different horizontal geometries to demonstrate some possibilities using this technology. In Fairbanks, Alaska, we find that stacking ground motion records along 20 m of fiber yield a waveform that shows a high degree of correlation in amplitude and phase with a colocated inertial seismometer record at 0.8–1.6 Hz. Using an L‐shaped DAS array in Northern California, we record the nearly vertically incident arrival of an earthquake from The Geysers Geothermal Field and estimate its backazimuth and slowness via beamforming for different phases of the seismic wavefield. Lastly, we install a fiber in existing telecommunications conduits below Stanford University and show that little cable‐to‐soil coupling is required for teleseismic <jats:italic>P</jats:italic> and <jats:italic>S</jats:italic> phase arrival detection.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 44 (23), 11-, 2017-12-08
American Geophysical Union (AGU)
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詳細情報 詳細情報について
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- CRID
- 1361418520853525504
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- ISSN
- 19448007
- 00948276
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- Web Site
- https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL075722
- https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075722
- https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL075722
- https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1002/2017GL075722
- https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075722
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- データソース種別
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