Research Article| July 04, 2018 Persistent Noise Signal in the FairfieldNodal Three‐Component 5‐Hz Geophones Jamie Farrell; Jamie Farrell aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Search for other works by this author on: GSW Google Scholar Sin‐Mei Wu; Sin‐Mei Wu aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Search for other works by this author on: GSW Google Scholar Kevin M. Ward; Kevin M. Ward aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Search for other works by this author on: GSW Google Scholar Fan‐Chi Lin Fan‐Chi Lin aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Jamie Farrell aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Sin‐Mei Wu aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Kevin M. Ward aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Fan‐Chi Lin aDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112 U.S.A., jamie.farrell@utah.edu Publisher: Seismological Society of America First Online: 04 Jul 2018 Online Issn: 1938-2057 Print Issn: 0895-0695 © Seismological Society of America Seismological Research Letters (2018) 89 (5): 1609–1617. https://doi.org/10.1785/0220180073 Article history First Online: 04 Jul 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jamie Farrell, Sin‐Mei Wu, Kevin M. Ward, Fan‐Chi Lin; Persistent Noise Signal in the FairfieldNodal Three‐Component 5‐Hz Geophones. Seismological Research Letters 2018;; 89 (5): 1609–1617. doi: https://doi.org/10.1785/0220180073 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search ABSTRACT Data from deployments of the FairfieldNodal three‐component nodes were used to analyze a persistently observed noise signal. The noise signal is most prominent in the 20‐ to 40‐Hz range but has been observed anywhere in the 10‐ to 100‐Hz range. Interestingly, the signal is affected by air temperature and moves to higher frequencies in colder temperatures. Nodes that were deployed in seismic vaults directly on flat concrete slabs do not show the noise signal, and nodes that were buried in the ground or covered in snow show a significant decrease in the noise signal. This suggests that whatever is causing this signal may be mitigated by better coupling to the ground. Spectral analysis of hydrothermal tremor in the Upper Geyser Basin, Yellowstone, suggests this noise signal can interfere with the true ground vibration and can impede the ability to accurately characterize these signals. It is our recommendation to always bury the nodes if it is possible to reduce this noise signal that can interfere with natural signals of interest in a similar frequency band. In addition, tests to better estimate the best gain setting were done, and results show that above 12 dB, the waveforms of teleseismic events on the three‐component nodes are very similar, suggesting that there is no advantage to using a gain setting higher than 18 dB for recording teleseismic events. If background noise is of interest in addition to teleseismic events, we see no adverse effects on the waveforms of teleseismic events using the max gain setting of 36 dB. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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