Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6332
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dc.contributor.authorallLesparre, N.; Institut de Physique du Globe de Paris (UMR CNRS 7154), Sorbonne Paris Cité, Paris, Franceen
dc.contributor.authorallGibert, D.; Institut de Physique du Globe de Paris (UMR CNRS 7154), Sorbonne Paris Cité, Paris, Franceen
dc.contributor.authorallMarteau, J.; Institut de Physique Nucléaire de Lyon (UMR CNRS 5822), Lyon, Franceen
dc.contributor.authorallDéclais, Y.; Institut de Physique Nucléaire de Lyon (UMR CNRS 5822), Lyon, Franceen
dc.contributor.authorallCarbone, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallGalichet, E.; Conservatoire National des Arts et M´etiers, Paris, Franceen
dc.date.accessioned2010-12-13T14:39:08Zen
dc.date.available2010-12-13T14:39:08Zen
dc.date.issued2010-12en
dc.identifier.urihttp://hdl.handle.net/2122/6332en
dc.description.abstractWe study the possibility of muon radiography as a tool to investigate space and time changes in the internal density distribution inside geological structures. Previous work has shown the practical applicability of this method. Nevertheless, quantitative information on factors which impose limitations on it are still sorely lacking in the literature. We discuss the main issues that can influence the final result of a geophysical imaging experiment. In particular, with the view of optimizing the signal-to-noise ratio, we address issues concerning (i) the energy spectrum for muons arriving at different zenith angles, (ii) the muon propagation model through matter and (iii) the characteristics of the muon detector (telescope) that we have designed to perform experiments of muon radiography against the harsh environment usually encountered in the active zone of a volcano. We thus identify factors that can induce either static or dynamic effects and that should be taken into account. We also define a feasibility eq. (32) relating the geometrical characteristics of the telescope and the duration of the experiment to the expected density resolution, in turn a function of the geometrical characteristics of the target structure. This relation is especially important to define the applicability domain of muon radiography and it is utilized to test the suitability of the method to investigate the density distribution inside some candidate target structures.en
dc.language.isoEnglishen
dc.publisher.nameBlackwell Publishingen
dc.relation.ispartofGeophysical Journal Internationalen
dc.relation.ispartofseries3 / 183 (2010)en
dc.subjectInverse theory; Spatial analysis; Tomographyen
dc.titleGeophysical muon imaging: feasibility and limitsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1348-1361en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.07. Instruments and techniquesen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniquesen
dc.identifier.doi10.1111/j.1365-246X.2010.04790.xen
dc.description.obiettivoSpecifico1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attiveen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorLesparre, N.en
dc.contributor.authorGibert, D.en
dc.contributor.authorMarteau, J.en
dc.contributor.authorDéclais, Y.en
dc.contributor.authorCarbone, D.en
dc.contributor.authorGalichet, E.en
dc.contributor.departmentInstitut de Physique du Globe de Paris (UMR CNRS 7154), Sorbonne Paris Cité, Paris, Franceen
dc.contributor.departmentInstitut de Physique du Globe de Paris (UMR CNRS 7154), Sorbonne Paris Cité, Paris, Franceen
dc.contributor.departmentInstitut de Physique Nucléaire de Lyon (UMR CNRS 5822), Lyon, Franceen
dc.contributor.departmentInstitut de Physique Nucléaire de Lyon (UMR CNRS 5822), Lyon, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentConservatoire National des Arts et M´etiers, Paris, Franceen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstitut de Physique du Globe de Paris (UMR CNRS 7154), Sorbonne Paris Cité, Paris, France-
crisitem.author.deptInstitut de Physique du Globe de Paris (UMR CNRS 7154), Sorbonne Paris Cité, Paris, France-
crisitem.author.deptInstitut de Physique Nucléaire de Lyon (UMR CNRS 5822), Lyon, France-
crisitem.author.deptInstitut de Physique Nucléaire de Lyon (UMR CNRS 5822), Lyon, France-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptConservatoire National des Arts et Métiers, Paris, France-
crisitem.author.orcid0000-0003-2566-6290-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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