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La Vigna, F.
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- PublicationOpen AccessGroundwater of Rome(2016)
; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ;; ; ; ; ;; ; ; ; ; ; ; ; ; ; ; ; ;; ;; ; ;This paper describes the contents of the new Hydrogeological Map of the City of Rome (1:50,000 scale). The map extends to the entire municipality (1285 km2) and is based on both the most recent scientific studies on the groundwater field and new survey activities carried out in order to fill the data gaps in several areas of the examined territory. The map is the result of a combination of different urban groundwater expertise and Geographic Information System (GIS)-based mapping performed using the most recent available data and has been produced with the intention of furnishing the City of Rome with the most recent and updated information regarding groundwater691 122 - PublicationRestrictedIntermediate-field hydrogeological response induced by L'Aquila earthquake: the Acque Albule hydrothermal system (Central Italy)(2012)
; ; ; ; ; ; ; ; ;La Vigna, F.; Università degli Studi Roma Tre ;Carucci, V.; Università degli Sudi dell'Aquila ;Mariani, I.; Università degli Studi Roma Tre ;Minelli, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia ;Pascale, F.; Università degli Studi Roma Tre ;Mattei, M.; Università degli Studi Roma Tre ;Mazza, R.; Università degli Studi Roma Tre ;Tallini, M.; Università degli Sudi dell'Aquila; ; ; ; ; ; ; The 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.357 39