Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5207
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dc.contributor.authorallPesci, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallCasula, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallLoddo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallBianchi, M.G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallTeza, G.; Dipartimento di Geoscienze - Univ. di Padovaen
dc.date.accessioned2009-10-21T15:10:36Zen
dc.date.available2009-10-21T15:10:36Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5207en
dc.description.abstractThe OptecTM ILRIS-3D Terrestrial Laser Scanner (TLS) has been recently acquired by the Istituto Nazionale di Geofisica e Vulcanologia (INGV) Sezione di Bolgna in the context of a TTC program for volcanoes monitoring (TTC 1.3 Controllo Geodetico delle Aree Vulcaniche Attive) supported by the Dipartimento di Protezione Civile. Several experiments were performed by INGV since 2004 to study the level of precision for surface modelling by means of laser scanner long range instruments, in order to detect the best suitable standard for rapid and simple acquisition in volcanic area (Pesci et al., 2007). In particular, during the MESIMEX experiment (October 2006), a national exercitation organized by the Dipartimento di Protezione Civile (DPC) exploited to simulate a volcanic eruption in Naples, the second TLS survey of the whole Vesuvius crater was executed and a large mass variations were estimated revealing the collapse of a portion of the crater. The alignment and comparison of point clouds (2006–2005) show high variations over a large portion of the NE slope and a volume variation of about 6850 m3 was computed. The analysis was performed in almost real time by means of direct comparisons between scans, indicating the laser scanning as one of the most reliable technique for fast monitoring in crisis time (Pesci et al. 2008a). The main characteristics recommended for surveying in volcanic areas were the laser device eyes safety, the achievable very long range (> 1 km), the precision of measurements and final accuracy in data modelling, the acquisition velocity, the instrument portability in terms of weight and size and the ability to manage scanner by means of PC pocket. The ILRIS-3D scanner was chosen based on the previously described recommended points. The simple operation needed for scan execution and the possibility to plan and realize a complete survey by means of only two operators confirmed ILRIS-3D as the best choice for volcanic applications. This technical report is a simple and effective user guide for laser scanner management providing all the necessary instruction from instrument settings, remote connection, data storage, downloading and preprocessing. Authors proposal is to make operators independent enough to scan and carry out survey in interested areas also without a specific experiences in LIDAR (Light Detection And Ranging) monitoring.en
dc.description.sponsorshipIstituto Nazionale di Geofisica e Vulcanologia (INGV)en
dc.language.isoEnglishen
dc.relation.ispartofseries2009en
dc.relation.ispartofseries109en
dc.subjectTerrestrial Laser Scanneren
dc.subjectUser Guideen
dc.titleOPTECHTM ILRIS-3D TERRESTRIAL LASER SCANNER: SHORT USER GUIDEen
dc.typereporten
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniquesen
dc.relation.referencesOPTECTM ILRIS-3D Operation Manual (2006). Optech Incorporated Industrial & 3D Imaging Division, 0040170/Rev A, 1-147. Pesci, A., Loddo, F., Conforti, D. (2007). The first terrestrial laser scanner survey OVER VESUVIUS: the high resolution model of VOLCANO crater (Napoli, Italy). International Journal of Remote Sensing, 28, 1, 203-219. Pesci A., Teza G., and Ventura G. (2008a). Remote sensing of volcanic terrains by terrestrial laser scanner: preliminary reflectance and RGB implications for studying Vesuvius crater (Italy). Annals of Geophysics, Vol. 51, Num. 4, August 2008, pp. 633-653. Pesci A., and Teza G. (2008b). Effects of surface irregularities on intensity data from laser scanning: an experimental approach. Annals of Geophysics, Vol. 51, 839-848. Franceschi, M., Teza, G., Preto, N., Pesci, A., Galgaro, A., Girardi, S. (2009). Discrimination between marls and limestones using intensity data from terrestrial laser scanner. ISPRS Journal of Photogrammetry and Remote Sensing, in press.en
dc.description.obiettivoSpecifico1.10. TTC - Telerilevamentoen
dc.description.fulltextopenen
dc.contributor.authorPesci, A.en
dc.contributor.authorCasula, G.en
dc.contributor.authorLoddo, F.en
dc.contributor.authorBianchi, M.G.en
dc.contributor.authorTeza, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentDipartimento di Geoscienze - Univ. di Padovaen
item.openairetypereport-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_93fc-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptDipartimento di Geoscienze - Univ. di Padova-
crisitem.author.orcid0000-0003-1863-3132-
crisitem.author.orcid0000-0001-7934-2019-
crisitem.author.orcid0000-0002-1153-1021-
crisitem.author.orcid0000-0002-7269-123X-
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.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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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