Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6250
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dc.contributor.authorallPalangio, P. G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallDi Lorenzo, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.date.accessioned2010-11-23T09:09:10Zen
dc.date.available2010-11-23T09:09:10Zen
dc.date.issued2010-04-11en
dc.identifier.urihttp://hdl.handle.net/2122/6250en
dc.description.abstractThe vectorial gradiometry offers many advantages compared to scalar gradiometry in the exploration of the subsoil. The introduction of new differential quantities adds a new dimension for the identification of magnetic sources. The direct measurement of the differential tensor quantities in the process of inversion can significantly increase the quality of solutions and the ability to separate more effectively the various magnetic sources in the regions where the magnetic field is derivable from a simple scalar potential. This paper describes the development of a magnetic tensorial gradiometer system and its capabilities with emphasis on the design, testing and operation. The system has been constructed by employing two independent cubic coil sensors at a distance of 50cm. The system measures the nine tensor components Tij as well as the magnitude of the six magnetic components Bhk, in the range of +/-50000 nT with a bandwidth from DC to 10 Hz and a sensitivity of 10 pT/m. The sampling rate can be set from 1 Hz to 20 Hz. It has been shown that a gradiometer sensitivity of 10 pT/m is sufficient to detect even weak magnetic contrasts such as in archaeological applications.en
dc.language.isoEnglishen
dc.relation.ispartofEGM 2010en
dc.subjectFull tensor gradiometryen
dc.titleMagnetic Tensorial Gradiometeren
dc.typePoster sessionen
dc.description.statusUnpublisheden
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.description.ConferenceLocationCapri, Italyen
dc.relation.referencesCooper, G. R. J., 2004, Euler deconvolution applied to potential field gradients: Exploration Geophysics, 35, 165–170. Florio G, Fedi M. and Pasteka R.,2006, On the application of Euler deconvolution to the analytic signal: Geophysics, 71, 87-93. Keating, P., and M. Pilkington, 2004, Euler deconvolution of the analytic signal and its application to magnetic interpretation: Geophysical Prospecting, 52, 165–182 Palangio P.,1998, A broad band two axis flux-gate magnetometer: Annali di Geofisica, Vol. 41, N. 3, August.en
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.fulltextrestricteden
dc.contributor.authorPalangio, P. G.en
dc.contributor.authorDi Lorenzo, C.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
item.openairetypePoster session-
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 Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-5092-3669-
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.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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