Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)

This work shows the result of an electrical resistivity tomography (ERT) survey carried out for imaging and characterizing the shallow subsurface affected by the coseismic effects of the Mw = 6.1 Emilia-Romagna (northern Italy) earthquake that occurred on 20 May 2012. The most characteristic coseism...

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Main Authors: A. Giocoli, B. Quadrio, J. Bellanova, V. Lapenna, S. Piscitelli
Format: Article
Language:English
Published: Copernicus Publications 2014-04-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/14/731/2014/nhess-14-731-2014.pdf
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spelling doaj-4a7fc57468384e68b9edc186fffad1112020-11-24T22:32:39ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812014-04-0114473173710.5194/nhess-14-731-2014Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)A. Giocoli0B. Quadrio1J. Bellanova2V. Lapenna3S. Piscitelli4CNR-IMAA, Tito, Potenza, ItalyCNR-IGAG, Rome, ItalyCNR-IMAA, Tito, Potenza, ItalyCNR-IMAA, Tito, Potenza, ItalyCNR-IMAA, Tito, Potenza, ItalyThis work shows the result of an electrical resistivity tomography (ERT) survey carried out for imaging and characterizing the shallow subsurface affected by the coseismic effects of the Mw = 6.1 Emilia-Romagna (northern Italy) earthquake that occurred on 20 May 2012. The most characteristic coseismic effects were ground failure, lateral spreading and liquefaction that occurred extensively along the paleo-Reno River in the urban areas of San Carlo and Mirabello (southwestern portion of Ferrara Province). In total, six electrical resistivity tomographies were performed and calibrated with surface geological surveys, exploratory boreholes and aerial photo interpretations. This was one of first applications of the electrical resistivity tomography method in investigating coseismic liquefaction.http://www.nat-hazards-earth-syst-sci.net/14/731/2014/nhess-14-731-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Giocoli
B. Quadrio
J. Bellanova
V. Lapenna
S. Piscitelli
spellingShingle A. Giocoli
B. Quadrio
J. Bellanova
V. Lapenna
S. Piscitelli
Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)
Natural Hazards and Earth System Sciences
author_facet A. Giocoli
B. Quadrio
J. Bellanova
V. Lapenna
S. Piscitelli
author_sort A. Giocoli
title Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)
title_short Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)
title_full Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)
title_fullStr Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)
title_full_unstemmed Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw = 6.1, northern Italy)
title_sort electrical resistivity tomography for studying liquefaction induced by the may 2012 emilia-romagna earthquake (mw = 6.1, northern italy)
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2014-04-01
description This work shows the result of an electrical resistivity tomography (ERT) survey carried out for imaging and characterizing the shallow subsurface affected by the coseismic effects of the Mw = 6.1 Emilia-Romagna (northern Italy) earthquake that occurred on 20 May 2012. The most characteristic coseismic effects were ground failure, lateral spreading and liquefaction that occurred extensively along the paleo-Reno River in the urban areas of San Carlo and Mirabello (southwestern portion of Ferrara Province). In total, six electrical resistivity tomographies were performed and calibrated with surface geological surveys, exploratory boreholes and aerial photo interpretations. This was one of first applications of the electrical resistivity tomography method in investigating coseismic liquefaction.
url http://www.nat-hazards-earth-syst-sci.net/14/731/2014/nhess-14-731-2014.pdf
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