Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5562
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dc.contributor.authorallWang, J.; University of Cambridge, Bullard Laboratoriesen
dc.contributor.authorallFrederick, T.; University of Cambridge, Bullard Laboratoriesen
dc.contributor.authorallWhite, R. S.; University of Cambridge, Bullard Laboratoriesen
dc.contributor.authorallBordoni, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.date.accessioned2010-01-13T14:04:22Zen
dc.date.available2010-01-13T14:04:22Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5562en
dc.description.abstractHydraulic-fracture induced microseismic events are usually small, and noise levels are high at the surface due to the activities associated with a producing oil field. Similarly, local arrays for the detection of local earthquakes will also benefit from reduced noise levels and detect smaller events. We present a frequency-dependent multi-channel Wiener filtering technique with linear constraints, which employs an adaptive least-squares technique to remove coherent noise in seismic array data. The noise records on a number of reference channels is used to predict the noise on a primary channel, which can then be subtracted. We implement and test first an unconstrained version of this filter, where maximal noise suppression can lead to signal distortion. Two methods of imposing constraints are then introduced to achieve signal preservation. We test this technique with two case studies. First, synthetic signals are added to actual noise from a pilot deployment of a hexagonal array (9 three-component seismometers, approximate size 150 m × 150 m) in an oil field; noise levels are suppressed by up to 11 dB (at 1 - 6 Hz). Secondly we use natural seismicity recorded at a dense array (∼10 m spacing) in Italy where the application of the filter reduces the signal-to-noise ratio by more than 20 dB (at 8 - 15 Hz), using 35 stations. In both cases, the performance of the multi-channel Wiener filters is significantly better than stacking, especially at lower frequency where stacking does not help to suppress the coherent noise. The unconstrained version of the filter yielded the best improvement in the signal-to-noise ratio, but the constrained filter is useful when waveform distortion is not acceptable.en
dc.language.isoEnglishen
dc.publisher.nameSociety of Exploration Geophysicistsen
dc.relation.ispartofGeophysicsen
dc.relation.ispartofseries6/74 (2009)en
dc.subjectWeiner filters, noise suppression, cavola arrayen
dc.titleApplication of frequency-dependent multichannel Wiener filters to detect events in 2D three-component seismometer arraysen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberv133-v141en
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.08. Instruments and techniquesen
dc.identifier.doi10.1190/1.3256282en
dc.relation.referencesBackus, M. M., J. P. Burg, D. Baldwin, and E. Bryan, 1964, Wide-band extraction of mantle P waves from ambient noise: Geophysics, 5, 672–692. Bordoni, P., J. Haines, G. D. Giulio, G. Milana, P. Augliera, L. Martelli, F. Cara, and the Cavola Experiment Team, 2007, Cavola experiment site: geophysical investigations and deployment of a dense seismic array on a landslide: Ann. Geophys., 50, 100–125. Crawford, W. C. and S. C. Webb, 2000, Identifying and removing tilt noise from low- frequency (< 0.1 Hz) seafloor vertical seismic data: Bull. Seism. Soc. Am., 90, 952–963. Dahm, T., F. Tilmann, and J. P. Morgan, 2006, Seismic broadband ocean-bottom data and noise observed with free-fall stations: experiences from long-term deployments in the North Atlantic and the Tyrrhenian Sea: Bull. Seism. Soc. Am., 96, 647–664. Douglas, A., 1998, Making the most of the recordings from short-period seismometer arrays: Bull. Seism. Soc. Am., 88, 1155–1170. ¨ Ozbek, A., 1999, Noise filtering method for seismic data: United States Patent 5971095. ——–, 2000, Adaptive beamforming with generalized linear constraints: SEG 70th Annual Meeting, 19, 2081–2084. Shen, W., 1979, A constrained minimum power adaptive beamformer with time-varying adaptation rate: Geophysics, 44, 1088–1096. Wang, J., F. Tilmann, R. S. White, H. Soosalu, and P. Bordoni, 2008, Suppression of ambient seismic noise in 2D arrays using multi-channel Wiener filters: The Leading Edge, 27, 232–238.en
dc.description.obiettivoSpecifico1.11. TTC - Osservazioni e monitoraggio macrosismico del territorio nazionaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorWang, J.en
dc.contributor.authorFrederick, T.en
dc.contributor.authorWhite, R. S.en
dc.contributor.authorBordoni, P.en
dc.contributor.departmentUniversity of Cambridge, Bullard Laboratoriesen
dc.contributor.departmentUniversity of Cambridge, Bullard Laboratoriesen
dc.contributor.departmentUniversity of Cambridge, Bullard Laboratoriesen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversity of Cambridge, Bullard Laboratories-
crisitem.author.deptUniversity of Cambridge, Bullard Laboratories-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-3391-4402-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent01. Atmosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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