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(Article of periodic en Anglais - 2012)

Document title

Intermediate-field hydrogeological response induced by L’Aquila earthquake : the Acque Albule hydrothermal system (Central Italy)

Authors(s) and Affiliation(s)

LA VIGNA F. ;

Abstract

The intermediate-field hydrological response to the 6th April 2009 L’Aquila earthquake has been studied using groundwater level data that were recorded by 6 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 2 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 5 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. - (NF)

Source

Article of periodic

published at : Italian Journal of Geosciences / ISSN 2038-1719

Editor : Società Geologica Italiana, Roma - ITALIE (2009)

Millesime : 2012, vol. 131, no3 [pp. 475-485]

Bibliographic references : 1 p.

Collation : 7 fig., 1 tabl.

Language

Anglais

INIST-CNRS, Cote INIST : 5205

Digital Object Identifier

Go to electronic document thanks to its DOI : doi:10.3301/IJG.2012.05

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2013
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