Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/14804
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dc.date.accessioned2021-08-31T06:31:55Z-
dc.date.available2021-08-31T06:31:55Z-
dc.date.issued2021-04-23-
dc.identifier.urihttp://hdl.handle.net/2122/14804-
dc.description.abstractIn this paper, we analyse the seismic noise at Ischia Island (Italy) with the objective of detecting the hydrothermal source signals taking advantage of the Covid-19 quiescence due to lockdown (strong reduction of anthropogenic noise). We compare the characteristics of the background noise in pre-, during and post-lockdown in terms of spectral content, energy release (RMS) and statistical moments. The continuous noise is decomposed into two independent signals in the 1-2 Hz and 2-4 Hz frequency bands, becoming sharpened around 1 Hz and 3 Hz respectively in lockdown. We propose a conceptual model according to which a dendritic system of fluid-permeated fractures plays as neighbour closed organ pipes, for which the fundamental mode provides the persistent whisper and the first higher mode is activated in concomitance with energy increases. By assuming reasonable values for the sound speed in low vapor-liquid mass fraction for a two-phase fluid and considering temperatures and pressures of the shallow aquifer fed by sea, meteoric and deep hydrothermal fluids, we estimate pipe lengths in the range 200-300 m. In this scheme, Ischia organ-like system can play both continuous whisper and transients, depending on the energy variations sourced by pressure fluctuations in the hydrothermal fluids.en_US
dc.language.isoEnglishen_US
dc.publisher.nameNature PGen_US
dc.relation.ispartofScientific Reportsen_US
dc.relation.ispartofseries/11 (2021)en_US
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.titlePicking up the hydrothermal whisper at Ischia Island in the Covid-19 lockdown quieten_US
dc.typearticleen
dc.description.statusPublisheden_US
dc.description.pagenumber8871en_US
dc.identifier.doi10.1038/s41598-021-88266-9en_US
dc.description.obiettivoSpecifico4V. Processi pre-eruttivien_US
dc.description.journalTypeJCR Journalen_US
dc.contributor.authorFalanga, Mariarosaria-
dc.contributor.authorCusano, Paola-
dc.contributor.authorDe Lauro, Enza-
dc.contributor.authorPetrosino, Simona-
dc.contributor.departmentDipartimento Di Ingegneria Dell’Informazione Ed Elettrica E Matematica Applicata/DIEM, Università Degli Studi Di Salernoen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italiaen_US
dc.contributor.departmentMinistry of Education, Universities and Research, Rome, Italyen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italiaen_US
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 Salerno-
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.orcid0000-0002-6266-6225-
crisitem.author.orcid0000-0002-8841-1861-
crisitem.author.orcid0000-0002-5042-0244-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.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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