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• W2996571850 endingPage "1181" @default.
• W2996571850 startingPage "1167" @default.
• W2996571850 abstract "A sustained increase in spring discharges was monitored after the 2016 Central Italy seismic sequence in the fractured carbonate aquifer of Valnerina–Sibillini Mts. The groundwater surplus recorded between August 2016 and November 2017 was determined to be between 400 and 500 × 106 m3. In fractured aquifers, the post-seismic rise in spring discharges is generally attributed to an increase in bulk permeability caused by the fracture cleaning effect, which is induced by pore pressure propagation. In the studied aquifers, the large amount of additional discharge cannot only be attributed to the enhanced permeability, which was evaluated to be less than 20% after each main seismic event. A detailed analysis of the spring discharge hydrographs and of the water level at five gauging stations was carried out to determine the possible causes of this sudden increase in groundwater outflow. Taking into account the geological and structural framework, a conceptual model of a basin-in-series has been adopted to describe the complex hydrogeological setting, where the thrusts and extensional faults have clearly influenced the groundwater flow directions before and after the seismic sequence. The prevalent portion of the total post-seismic discharge surplus not explained by the increase in permeability has been attributed to changes in the hydraulic gradient that caused seismogenic fault rupture and the disruption in the upgradient sector of the aquifer. The additional flow calculated through the breach of the pre-existing hydrostructural barrier corresponds to approximately 470 × 106 m3. This value is consistent with the total discharge increase measured in the whole study area, validating the proposed conceptual model. Consequently, a shift in the piezometric divide of the hydrogeological system has been induced, causing a potentially permanent change that lowers the discharge amount of the eastern springs." @default.
• W2996571850 created "2019-12-26" @default.
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• W2996571850 date "2019-12-10" @default.
• W2996571850 modified "2023-09-23" @default.
• W2996571850 title "Sustained post‐seismic effects on groundwater flow in fractured carbonate aquifers in Central Italy" @default.
• W2996571850 cites W1684180267 @default.
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• W2996571850 cites W1970413401 @default.
• W2996571850 cites W1973378173 @default.
• W2996571850 cites W1983523676 @default.
• W2996571850 cites W1985173691 @default.
• W2996571850 cites W1990497385 @default.
• W2996571850 cites W1993233923 @default.
• W2996571850 cites W2003595959 @default.
• W2996571850 cites W2015056451 @default.
• W2996571850 cites W2018957105 @default.
• W2996571850 cites W2028177037 @default.
• W2996571850 cites W2035825320 @default.
• W2996571850 cites W2042558191 @default.
• W2996571850 cites W2042630214 @default.
• W2996571850 cites W2054238627 @default.
• W2996571850 cites W2061373259 @default.
• W2996571850 cites W2061707839 @default.
• W2996571850 cites W2066209327 @default.
• W2996571850 cites W2066880729 @default.
• W2996571850 cites W2070364254 @default.
• W2996571850 cites W2077656237 @default.
• W2996571850 cites W2079740787 @default.
• W2996571850 cites W2080555924 @default.
• W2996571850 cites W2085216393 @default.
• W2996571850 cites W2098992336 @default.
• W2996571850 cites W2101685721 @default.
• W2996571850 cites W2102861978 @default.
• W2996571850 cites W2103437663 @default.
• W2996571850 cites W2105611715 @default.
• W2996571850 cites W2108755903 @default.
• W2996571850 cites W2110527274 @default.
• W2996571850 cites W2110686004 @default.
• W2996571850 cites W2120026917 @default.
• W2996571850 cites W2129777446 @default.
• W2996571850 cites W2149268277 @default.
• W2996571850 cites W2150517102 @default.
• W2996571850 cites W2154983301 @default.
• W2996571850 cites W2160400194 @default.
• W2996571850 cites W2165746064 @default.
• W2996571850 cites W2200946045 @default.
• W2996571850 cites W2252653953 @default.
• W2996571850 cites W2314621101 @default.
• W2996571850 cites W2329887915 @default.
• W2996571850 cites W24179842 @default.
• W2996571850 cites W2560761138 @default.
• W2996571850 cites W2579138762 @default.
• W2996571850 cites W2584490967 @default.
• W2996571850 cites W2604220874 @default.
• W2996571850 cites W2626943559 @default.
• W2996571850 cites W2732375979 @default.
• W2996571850 cites W2754256356 @default.
• W2996571850 cites W2754268221 @default.
• W2996571850 cites W2768402950 @default.
• W2996571850 cites W2784630782 @default.
• W2996571850 cites W2789754823 @default.
• W2996571850 cites W2792804554 @default.
• W2996571850 cites W2794077518 @default.
• W2996571850 cites W2807030849 @default.
• W2996571850 cites W2885490588 @default.
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• W2996571850 cites W2901159730 @default.
• W2996571850 cites W2902997498 @default.
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• W2996571850 doi "https://doi.org/10.1002/hyp.13662" @default.
• W2996571850 hasPublicationYear "2019" @default.
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