Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7070
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dc.contributor.authorallCusano, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallBobbio, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallFesta, G.; Università degli Studi di Napoli «Federico II», Dipartimento di Scienze Fisiche, Naples, Italyen
dc.contributor.authorallPetrosino, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallRombetto, S.; Istituto di Cibernetica «Eduardo Caianiello», Consiglio Nazionale delle Ricerche, Naples, Italyen
dc.date.accessioned2011-07-15T08:58:39Zen
dc.date.available2011-07-15T08:58:39Zen
dc.date.issued2011-07-06en
dc.identifier.urihttp://hdl.handle.net/2122/7070en
dc.description.abstractWe have investigated the mechanical response of a magnetically shielded room that hosts a magnetoencephalography system that is subject to external vibrations. This is a superconducting quantum interference device, which are the most sensitive sensors for magnetic flux variations. When the magnetoencephalography operates with people inside the room, the spectrum of the flux of the magnetic field shows anomalous peaks at several frequencies between 1 Hz and 20 Hz, independent of the experiment that is being run. As the variations in the flux of the magnetic field through the sensors might not only be related to the electrical currents circulating inside the brain, but also to non-damped mechanical oscillations of the room, we installed seismic instrumentation to measure the effective motion inside the room and to compare it to the external motion. For this analysis, we recorded the ambient seismic noise at two very close stations, one inside the magnetically shielded room, the other one outside in the room in which the magnetically shielded room is itself located. Data were collected over four days, including a week-end, to study the response of the magnetically shielded room subjected to different energy levels of external vibrations. The root mean square, Fourier spectra and power spectral density show significant differences between the signal recorded inside and outside the magnetically shielded room, with several anomalous peaks in the frequency band of 1 Hz to 20 Hz. The normalized spectral quantities (horizontal to vertical spectral ratio, and ratio between the internal and external spectra) show large amplification at several frequencies, reaching in some cases one order of magnitude. We concluded that the magnetically shielded room does not dampen the external vibrations, but it instead appears to amplify these across a broad frequency range.en
dc.language.isoEnglishen
dc.publisher.nameIstituto Nazionale di Geofisica e Vulcanologiaen
dc.relation.ispartofAnnals of geophysicsen
dc.relation.ispartofseries3/54 (2011)en
dc.subjectSeismic noiseen
dc.subjectSpectral ratio analysesen
dc.subjectMagnetoencephalographyen
dc.titleAnalysis of seismic noise to check the mechanical isolationen
dc.title.alternativeMECHANICAL DISTURBANCE ON A MEDICAL DEVICEen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber223-233en
dc.identifier.URLhttp://www.annalsofgeophysics.eu/index.php/annals/article/view/4774en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.04. Ground motionen
dc.identifier.doi10.4401/ag-4774en
dc.description.obiettivoSpecifico4.1. Metodologie sismologiche per l'ingegneria sismicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorCusano, P.en
dc.contributor.authorBobbio, A.en
dc.contributor.authorFesta, G.en
dc.contributor.authorPetrosino, S.en
dc.contributor.authorRombetto, S.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentUniversità degli Studi di Napoli «Federico II», Dipartimento di Scienze Fisiche, Naples, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto di Cibernetica «Eduardo Caianiello», Consiglio Nazionale delle Ricerche, Naples, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptDipartimento di Scienze Fisiche Università di Napoli Federico II-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto di Cibernetica «Eduardo Caianiello», Consiglio Nazionale delle Ricerche, Naples, Italy-
crisitem.author.orcid0000-0002-6266-6225-
crisitem.author.orcid0000-0003-2386-8737-
crisitem.author.orcid0000-0002-2588-8160-
crisitem.author.orcid0000-0002-5042-0244-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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