Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9695
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dc.contributor.authorallGreco, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallBiolcati, E.; Istituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.authorallPistorio, A.; Dipartimento di Ingegneria Elettrica, Elettronica e Informatica, Università di Catania, Italyen
dc.contributor.authorallD'Agostino, G.; Istituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.authorallGermak, A.; Istituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.authorallOriglia, C.; Istituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.authorallDel Negro, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.date.accessioned2015-06-01T06:39:23Zen
dc.date.available2015-06-01T06:39:23Zen
dc.date.issued2015en
dc.identifier.urihttp://hdl.handle.net/2122/9695en
dc.description.abstractThe performances of two absolute gravimeters at three different sites in Italy between 2009 and 2011 is presented. The measurements of the gravity acceleration g were performed using the absolute gravimeters Micro-g LaCoste FG5#238 and the INRiM prototype IMGC-02, which represent the state of the art in ballistic gravimeter technology (relative uncertainty of a few parts in 10 9 ). For the comparison, the measured g values were reported at the same height by means of the vertical gravity gradient estimated at each site with relative gravimeters. The consistency and reliability of the gravity observations, as well as the performance and efficiency of the instruments, were assessed by measurements made in sites charac- terized by different logistics and environmental conditions. Furthermore, the various factors affecting the measurements and their uncertainty were thoroughly investigated. The measurements showed good agree- ment, with the minimum and maximum differences being 4.0 and 8.3 µGal. The normalized errors are very much lower than 1, ranging between 0.06 and 0.45, confirming the compatibility between the results. This excellent agreement can be attributed to several factors, including the good working order of gravimeters and the correct setup and use of the instruments in different conditions. These results can contribute to the standardization of absolute gravity surveys largely for applications in geophysics, volcanology and other branches of geosciences, allowing achieving a good trade-off between uncertainty and efficiency of gravity measurements.en
dc.language.isoEnglishen
dc.publisher.nameSpringer Berlin Heidelbergen
dc.relation.ispartofThe European Physical Journal Plusen
dc.relation.ispartofseries/130 (2015)en
dc.subjectabsolute gravimeteren
dc.subjectgravity accelerationen
dc.subjectcomparison of absolute gravimetersen
dc.titleAbsolute gravity measurements at three sites characterized by different environmental conditions using two portable ballistic gravimetersen
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber38en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniquesen
dc.identifier.doi10.1140/epjp/i2015-15038-0en
dc.description.obiettivoSpecifico2V. Dinamiche di unrest e scenari pre-eruttivien
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.eissn2190-5444en
dc.contributor.authorGreco, F.en
dc.contributor.authorBiolcati, E.en
dc.contributor.authorPistorio, A.en
dc.contributor.authorD'Agostino, G.en
dc.contributor.authorGermak, A.en
dc.contributor.authorOriglia, C.en
dc.contributor.authorDel Negro, C.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.departmentDipartimento di Ingegneria Elettrica, Elettronica e Informatica, Università di Catania, Italyen
dc.contributor.departmentIstituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.departmentIstituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.departmentIstituto Nazionale di Ricerca Metrologica, Torino, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Ricerca Metrologica, INRiM, Torino, Italy,-
crisitem.author.deptIstituto Nazionale di Ricerca Metrologica, INRiM, Torino, Italy,-
crisitem.author.deptIstituto Nazionale di Ricerca Metrologica, INRiM, Torino, Italy,-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.orcid0000-0002-0265-5073-
crisitem.author.orcid0000-0001-5734-9025-
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-
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