1. Water-table and discharge changes associated with the 2016–2017 seismic sequence in central Italy. Hydrogeological data and a conceptual model for fractured carbonate aquifers
- Author
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Elisabetta Preziosi, Francesca Banzato, Michele Saroli, T. Nanni, Gaetano De Luca, Daniela Valigi, Andrea Billi, Cristina Di Salvo, Sergio Rusi, Marino Domenico Barberio, Alberto Tazioli, Stefano Palpacelli, Giuseppe Di Carlo, Lucia Mastrorillo, Marco Tallini, Costanza Cambi, Carlo Doglioni, Diego Di Curzio, Marco Petitta, Paola Vivalda, Petitta, Marco, Mastrorillo, Lucia, Preziosi, Elisabetta, Banzato, Francesca, Barberio, Marino Domenico, Billi, Andrea, Cambi, Costanza, De Luca, Gaetano, Di Carlo, Giuseppe, Di Curzio, Diego, Di Salvo, Cristina, Nanni, Torquato, Palpacelli, Stefano, Rusi, Sergio, Saroli, Michele, Tallini, Marco, Tazioli, Alberto, Valigi, Daniela, Vivalda, Paola, and Doglioni, Carlo
- Subjects
010504 meteorology & atmospheric sciences ,Water table ,carbonate rocks ,co-seismic effects ,earthquake ,groundwater monitoring ,Italy ,water science and technology ,earth and planetary sciences ,Aquifer ,010502 geochemistry & geophysics ,01 natural sciences ,Hydraulic conductivity ,Streamflow ,Earth and Planetary Sciences (miscellaneous) ,Geomorphology ,0105 earth and related environmental sciences ,Water Science and Technology ,geography ,Hydrogeology ,geography.geographical_feature_category ,Subsidence ,Groundwater recharge ,Earthquake . Groundwater monitoring . Italy . Co-seismic effects . Carbonate rocks ,earthquake, groundwater monitoring, Italy, co-seismic effects, carbonate rocks ,Geology ,Groundwater - Abstract
A seismic sequence in central Italy from August 2016 to January 2017 affected groundwater dynamics in fractured carbonate aquifers. Changes in spring discharge, water-table position, and streamflow were recorded for several months following nine Mw 5.0–6.5 seismic events. Data from 22 measurement sites, located within 100 km of the epicentral zones, were analyzed. The intensity of the induced changes were correlated with seismic magnitude and distance to epicenters. The additional post-seismic discharge from rivers and springs was found to be higher than 9 m3/s, totaling more than 0.1 km3 of groundwater release over 6 months. This huge and unexpected contribution increased streamflow in narrow mountainous valleys to previously unmeasured peak values. Analogously to the L’Aquila 2009 post-earthquake phenomenon, these hydrogeological changes might reflect an increase of bulk hydraulic conductivity at the aquifer scale, which would increase hydraulic heads in the discharge zones and lower them in some recharge areas. The observed changes may also be partly due to other mechanisms, such as shaking and/or squeezing effects related to intense subsidence in the core of the affected area, where effects had maximum extent, or breaching of hydraulic barriers.
- Published
- 2018
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