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Research Article| February 28, 2018 Laboratory Tests of Three Z‐Land Fairfield Nodal 5‐Hz, Three‐Component Sensors A. T. Ringler; A. T. Ringler aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov Search for other works by this author on: GSW Google Scholar R. E. Anthony; R. E. Anthony aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov Search for other works by this author on: GSW Google Scholar M. S. Karplus; M. S. Karplus bUniversity of Texas El Paso, 500 West University Avenue, El Paso, Texas 79968 U.S.A. Search for other works by this author on: GSW Google Scholar A. A. Holland; A. A. Holland aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov Search for other works by this author on: GSW Google Scholar D. C. Wilson D. C. Wilson aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov Search for other works by this author on: GSW Google Scholar Author and Article Information A. T. Ringler aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov R. E. Anthony aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov M. S. Karplus bUniversity of Texas El Paso, 500 West University Avenue, El Paso, Texas 79968 U.S.A. A. A. Holland aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov D. C. Wilson aU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque, New Mexico 87198‐2010 U.S.A., aringler@usgs.gov Publisher: Seismological Society of America First Online: 28 Feb 2018 Online Issn: 1938-2057 Print Issn: 0895-0695 © Seismological Society of America Seismological Research Letters (2018) 89 (5): 1601–1608. https://doi.org/10.1785/0220170236 Article history First Online: 28 Feb 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation A. T. Ringler, R. E. Anthony, M. S. Karplus, A. A. Holland, D. C. Wilson; Laboratory Tests of Three Z‐Land Fairfield Nodal 5‐Hz, Three‐Component Sensors. Seismological Research Letters 2018;; 89 (5): 1601–1608. doi: https://doi.org/10.1785/0220170236 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 We conduct a number of laboratory tests at the Albuquerque Seismological Laboratory to verify the self‐noise and fidelity in which 3 three‐component Fairfield Nodal Z‐Land, Generation 2, 5‐Hz sensors are able to record seismic signals. In addition to the incoherent self‐noise of the sensors, we estimate the sensitivity of the units in digital volts/m/s, the damping, and the free period. These three parameters allow us to completely characterize the response of the instruments. We find that the responses of all components match a mean‐derived response to within 5% of amplitude and 0.03 radians in phase. This close agreement suggests that for most applications a nominal response is suitable. We also checked the timing of the units as compared to a Quanterra Q330HR and found good agreement up to 200 samples/s. Finally, we compared the results of our noise tests on these sensors to a couple of nodal sensors recently deployed at the Community Wavefield Demonstration Experiment in north‐central Oklahoma and found that local site noise and not the sensor self‐noise is a fundamental limiter in the resolution of these deployed sensors at frequencies above ∼0.1 Hz. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Ringler et al. (Wed,) studied this question.