Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4984
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dc.contributor.authorallPatella, D.; Dipartimento di Fisica, Università degli Studi di Napoli «Federico II», Napoli, Italyen
dc.date.accessioned2009-03-26T14:27:54Zen
dc.date.available2009-03-26T14:27:54Zen
dc.date.issued2008-02en
dc.identifier.urihttp://hdl.handle.net/2122/4984en
dc.description.abstractIt is illustrated that IP phenomena in rocks can be described using conductivity dispersion models deduced as solutions to a 2nd-order linear differential equation describing the motion of a charged particle immersed in an external electrical field. Five dispersion laws are discussed, namely: the non-resonant positive IP model, which leads to the classical Debye-type dispersion law and by extension to the Cole-Cole model, largely used in current practice; the non-resonant negative IP model, which allows negative chargeability values, known in metals at high frequencies, to be explained as an intrinsic physical property of earth materials in specific field cases; the resonant flat, positive or negative IP models, which can explain the presence of peak effects at specific frequencies superimposed on flat, positive or negative dispersion spectra.en
dc.language.isoEnglishen
dc.relation.ispartofAnnals of Geophysicsen
dc.relation.ispartofseries1/51 (2008)en
dc.subjectinduced polarizationen
dc.subjectelectrical dispersion spectraen
dc.subjectgeophysical applicationsen
dc.titleModeling electrical dispersion phenomena in Earth materialsen
dc.typearticleen
dc.description.status159 - 165en
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.99. General or miscellaneousen
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WARD (Editors) (1990): Induced polarization: applications and case histories, in Investigations in Geophysics, Society of Exploration Geophysicists, Tulsa, Oklahoma, vol. 4, pp. 414. GIAMMETTI, S., D. PATELLA, A. SINISCALCHI and A. TRAMACERE (1996): The Siena Graben: Combined interpretation of DES and MT soundings, Ann. Geofis., XXXIX (1), 189-200. MADDEN, T.R. and T. CANTWELL (1967): Induced polarization, a review, in Mining Geophysics, Society of Exploration Geophysicists, Tulsa, Oklahoma, vol. 2, 373-400. MAURIELLO, P., D. PATELLA and A. SINISCALCHI (1996): The magnetotelluric response over two-dimensional media with resistivity frequency dispersion, Geophys. Prosp., 44, 789-818. MAURIELLO, P., D. PATELLA, Z. PETRILLO and A. SINISCALCHI (2000): An integrated magnetotelluric study of the Mt. Etna volcanic structure, Ann. Geofis., 43 (2), 325-342. MAURIELLO, P., D. PATELLA, Z. PETRILLO, A. SINISCALCHI, T. IULIANO and C. DEL NEGRO (2004): A geophysical study of the Mt. Etna volcanic area, in Mt. Etna: Volcano Laboratory, edited by A. BONACCORSO, S. CALVARI, M. COLTELLI, C. DEL NEGRO and S. FALSAPERLA, American Geophysical Union, Geophysical Monograph Series, 143, 273-291. NABIGHIAN, M.N., and C.L. ELLIOT (1976): Negative induced polarization effects from layered media, Geophysics, 41, 1235-1255. PATELLA, D. (1987): Tutorial: Interpretation of magnetotelluric measurements over an electrically dispersive onedimensional earth, Geophys. Prosp., 35, 1-11. PATELLA, D. (1993): I principi metodologici della magnetotellurica su mezzi generalmente dispersivi (in Italian), Ann. Geofis., XXXVI (5/6), 147-160. PATELLA, D. (2003): On the role of the J-E constitutive relationship in applied geoelectromagnetism, Ann. Geophys., 46, 589-597. PATELLA, D. and R. DI MAIO (1989): On the analysis of Cole-Cole relaxations transients in the induced polarization prospecting method, in Inverse Modeling in Exploration Geophysics, edited by A. VOGEL, R. GORENFLO, B. KUMMER and C.O. OFOEGBU (F. Vieweg & Sohn, Braunschweig/Wiesbaden), 205-219. PATELLA, D., A. TRAMACERE, R. DI MAIO and A. SINISCALCHI (1991): Experimental evidence of resistivity frequency-dispersion in magnetotellurics in the Newberry (Oregon), Snake River Plain (Idaho) and Campi Flegrei (Italy) volcano-geothermal areas, J. Volcanol. Geoth. Res., 48, 61-75. PELTON, W.H., S.H. WARD, P.G. HALLOF, W.R. SILL and P.H. NELSON (1978): Mineral discrimination and removal of inductive coupling with multi-frequency IP, Geophysics, 43, 588-603. PELTON, W.H., W.R. SILL and B.D. SMITH (1983): Interpretation of complex resistivity and dielectric data. Part I, Geophys. Trans., 29, 297-330. SAFONOV, A.S., I.A. MUSHIN, E.S. KISELEV and A.S. GORYUNOV (1996): A structural-formation model as the physical-geological basis for high-resolution electroprospecting, Geofizika, 2, 12-23. SEIGEL, H.O. (1959): Mathematical formulation and type curves for induced polarization, Geophysics, 24, 547- 565. STOYER, C.H. (1976): Consequences of induced polarization in magnetotelluric interpretation, Pure Appl. Geophys., 114, 435-449. STRATTON, J. (1941): Electromagnetic Theory (McGraw- Hill, New York). SUMNER, J.S. (1967): The problem of negative IP anomalies, in Proc. of the Symposium on Induced Electrical Polarization, Engineering Geoscience, Department of Mineral, Technical University of California, Berkeley, 32-50. SUMNER, J.S. (1976): Principles of Induced Polarization for Geophysical Exploration (Elsevier, Amsterdam). SVETOV, B.S. and V.V. AGEEV, (1999): High resolution electromagnetic methods and low fequency dispersion of rock conductivity, Ann. Geofis., 42 (4), 699-713. WAIT, J.R. (Editor) (1959): Overvoltage Research and Geophysical Applications (Pergamon, Oxford). WAIT, J.R. (1982): Geo-electromagnetism (Academic Press, New York).en
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorPatella, D.en
dc.contributor.departmentDipartimento di Fisica, Università degli Studi di Napoli «Federico II», Napoli, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze Fisiche, Università «Federico II», Napoli, Italy-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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