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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8676
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dc.contributor.authorallLa Vigna, F.; Università degli Studi Roma Treen
dc.contributor.authorallCarucci, V.; Università degli Sudi dell'Aquilaen
dc.contributor.authorallMariani, I.; Università degli Studi Roma Treen
dc.contributor.authorallMinelli, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallPascale, F.; Università degli Studi Roma Treen
dc.contributor.authorallMattei, M.; Università degli Studi Roma Treen
dc.contributor.authorallMazza, R.; Università degli Studi Roma Treen
dc.contributor.authorallTallini, M.; Università degli Sudi dell'Aquilaen
dc.date.accessioned2013-04-24T13:32:53Zen
dc.date.available2013-04-24T13:32:53Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/8676en
dc.description.abstractThe intermediate-field hydrological response to the 6th April 2009 L’Aquila earthquake (Mw 6.3) has been studied using groundwater level data that were recorded by six piezometers in the Acque Albule Basin (Tivoli travertine quarry area) and in the Cornicolani Mountains (Pozzo del Merro shaft). The hydrogeological setting of the Tivoli area is characterised by two superimposed aquifers: a deep aquifer in carbonate and a shallow aquifer in travertine. At the time of the L’Aquila earthquake, the groundwater level at five piezometers located in the travertine quarry area began to decrease, while the water level slightly increased in the Pozzo del Merro karst lake that is located in the carbonate aquifer. To explain these variations, a possible conceptual model is proposed that assumes that ground - water-level variations are caused by a change in aquifer permeability principally due to the dynamic stress associated with the passing of the earthquake’s seismic waves.en
dc.language.isoEnglishen
dc.relation.ispartofItalian Journal of Geosciencesen
dc.relation.ispartofseries/131(2012)en
dc.subjectearthquake hydrologyen
dc.subjectgrounwater level changesen
dc.subjectdynamic stressen
dc.subjectcentral italyen
dc.titleIntermediate-field hydrogeological response induced by L'Aquila earthquake: the Acque Albule hydrothermal system (Central Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber475-485en
dc.subject.INGV03. Hydrosphere::03.02. Hydrology::03.02.03. Groundwater processesen
dc.identifier.doi10.3301/IJG.2012.05en
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.contributor.authorLa Vigna, F.en
dc.contributor.authorCarucci, V.en
dc.contributor.authorMariani, I.en
dc.contributor.authorMinelli, L.en
dc.contributor.authorPascale, F.en
dc.contributor.authorMattei, M.en
dc.contributor.authorMazza, R.en
dc.contributor.authorTallini, M.en
dc.contributor.departmentUniversità degli Studi Roma Treen
dc.contributor.departmentUniversità degli Sudi dell'Aquilaen
dc.contributor.departmentUniversità degli Studi Roma Treen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentUniversità degli Studi Roma Treen
dc.contributor.departmentUniversità degli Studi Roma Treen
dc.contributor.departmentUniversità degli Studi Roma Treen
dc.contributor.departmentUniversità degli Sudi dell'Aquilaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità degli Studi Roma Tre-
crisitem.author.deptUniversità degli Sudi dell'Aquila-
crisitem.author.deptUniversità degli Studi Roma Tre-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptUniversità degli Studi Roma Tre-
crisitem.author.deptUniversità degli studi di Roma TRE-
crisitem.author.deptUniversità degli Studi Roma Tre-
crisitem.author.orcid0000-0002-9395-3905-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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