Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5337
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dc.contributor.authorallFaggioni, O.; Istituto Nazionale di Geofisica e Vulcanologiaen
dc.contributor.authorallSoldani, M.; Istituto Nazionale di Geofisica e Vulcanologiaen
dc.contributor.authorallLeoncini, D.; Defence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italyen
dc.contributor.authorallZunino, R.; Defence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italyen
dc.contributor.authorallGastaldo, P.; Defence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italyen
dc.contributor.authorallDi Gennaro, E.; Italian Navy, Naval Logistic Inspectorate, Piazza della Marina 4, 00196 Roma, Italyen
dc.contributor.authorallLamberti, L. O.; Italian Navy, Istituto Idrografico della Marina, Passo dell’Osservatorio 4, 16134 Genova, Italyen
dc.contributor.authorallMaggiani, P. V.; Italian Navy, COMFORDRAG, Viale Giovanni Amendola 1, 19122 La Spezia, Italyen
dc.date.accessioned2009-12-15T08:49:18Zen
dc.date.available2009-12-15T08:49:18Zen
dc.date.issued2009-10-21en
dc.identifier.urihttp://hdl.handle.net/2122/5337en
dc.description.abstractSeafloor clearance methods based on acoustic, direct-inspection, and single-sensor magnetic approaches suffer from limitations in controlling the target-sensor distance, and may prove ineffective when the small size or the dangerous nature of targets requires high accuracy in localization. Moreover, random magnetic variations over time bring about spatial decorrelation phenomena, and hinder the application of double-sensor methods in noisy harbour environments. The new High Definition (HD) magnetic survey protocol tackles the measurement-distance problem in two ways: first, by varying the sensor depth dynamically, and secondly by backprojecting the measured field according to seafloor data and vertical incremental factors associated with the bandwidth characteristics of targets. The method to make up for timeinduced loss in spatial localization ability exploits the local behaviour of a coherence function, which correlates local observations to a set of spatially-stabilized reference stations. The consequent normalization of measured magnetic signals allows one to assign the monitored areas with a specific level of confidence in the detection results, ranging from 100% (certainty) to 0% (random events). The principles of HD detection have been fully applied in the seafloor clearance of the firing test site located south of Cape Teulada (Sardinia, Italy), where very weak signal sources such as cartridge cases, mines, and small objects down to 1 Kg mass values (lobster pots) have been successfully localized, even when covered by extensive colonies of Posidonia.en
dc.language.isoEnglishen
dc.publisher.nameMAST Events Ltden
dc.relation.ispartofProceedings of MAST 2009 Conferenceen
dc.subjectSeafloor clearanceen
dc.subjectmagnetic surveyen
dc.subjectmagnetic detectionen
dc.subjectproton Overhauser magnetometeren
dc.titleHarbour Sea-floor Clearance: “HD” High Definition Magnetic Survey Performanceen
dc.typeConference paperen
dc.description.statusPublisheden
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methodsen
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.07. Instruments and techniquesen
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomaliesen
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniquesen
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.01. Data processingen
dc.description.ConferenceLocationStockolm, Swedenen
dc.relation.references[1] Hill M.N., Mason C.S., 1962, “Diurnal variations of the earth’s magnetic field al sea”, Nature, Vol. 195, 365-366. [2] Faggioni O., Caratori Tontini F., 2002, “Quantitative evaluation of the time-line reduction performance in high definition marine magnetic survey”, Mar. Geoph. Res., Vol. 33, pp. 353-365. [3] Faggioni O., Beverini N., Carmisciano C., 1997, “Geomagnetic time variations and high definition study of space magnetic effects induced by artificial submerged sources”, Boll. Geof. Teor. Appl., Vol XXXVIII, N 3-4, pp. 211-228. [4] E. Di Gennaro, E. Bovio, F. Baralli, O. Faggioni and M. Soldani, 2008, “Clearance operation of Teulada Site (Italy): a novel approach for short term MCM missions in seafloor hard conditions”, CD-ROM Proceedings of UDT Europe 2008 Conference, June 11-13, Glasgow, UK.en
dc.description.obiettivoSpecifico1.6. Osservazioni di geomagnetismoen
dc.description.obiettivoSpecifico2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarinien
dc.description.obiettivoSpecifico3.4. Geomagnetismoen
dc.description.fulltextopenen
dc.contributor.authorFaggioni, O.en
dc.contributor.authorSoldani, M.en
dc.contributor.authorLeoncini, D.en
dc.contributor.authorZunino, R.en
dc.contributor.authorGastaldo, P.en
dc.contributor.authorDi Gennaro, E.en
dc.contributor.authorLamberti, L. O.en
dc.contributor.authorMaggiani, P. V.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologiaen
dc.contributor.departmentDefence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italyen
dc.contributor.departmentDefence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italyen
dc.contributor.departmentDefence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italyen
dc.contributor.departmentItalian Navy, Naval Logistic Inspectorate, Piazza della Marina 4, 00196 Roma, Italyen
dc.contributor.departmentItalian Navy, Istituto Idrografico della Marina, Passo dell’Osservatorio 4, 16134 Genova, Italyen
dc.contributor.departmentItalian Navy, COMFORDRAG, Viale Giovanni Amendola 1, 19122 La Spezia, Italyen
item.openairetypeConference paper-
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 Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptDefence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italy-
crisitem.author.deptUniversità degli Studi di Genova – DITEN Genova, Italy-
crisitem.author.deptDefence Geophysics Group; University of Genoa, DIBE, SEA Lab, Via All’Opera Pia 11a, 16145 Genova, Italy-
crisitem.author.deptItalian Navy; Naval Logistic Inspectorate, Piazza della Marina 4, 00196 Roma, Italy-
crisitem.author.deptItalian Navy, Istituto Idrografico della Marina, Passo dell’Osservatorio 4, 16134 Genova, Italy-
crisitem.author.deptItalian Navy, COMFORDRAG, Viale Giovanni Amendola 1, 19122 La Spezia, Italy-
crisitem.author.orcid0000-0002-9772-3453-
crisitem.author.orcid0000-0001-7039-2781-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
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