scholarly journals Sustained post‐seismic effects on groundwater flow in fractured carbonate aquifers in Central Italy

2019 ◽  
Vol 34 (5) ◽  
pp. 1167-1181 ◽  
Author(s):  
Lucia Mastrorillo ◽  
Michele Saroli ◽  
Stefano Viaroli ◽  
Francesca Banzato ◽  
Daniela Valigi ◽  
...  
Keyword(s):  
Groundwater Flow ◽  
Central Italy ◽  
Seismic Effects ◽  
Carbonate Aquifers ◽  
Fractured Carbonate

Correlation between groundwater flow and deformation in the fractured carbonate Gran Sasso aquifer (INFN underground laboratories, central Italy)

2014 ◽  
Vol 50 (6) ◽  
pp. 4858-4876 ◽  
Author(s):  
A. Amoruso ◽  
L. Crescentini ◽  
S. Martino ◽  
M. Petitta ◽  
M. Tallini
Keyword(s):  
Groundwater Flow ◽  
Central Italy ◽  
Fractured Carbonate

scholarly journals Fractured carbonate aquifers of Sibillini Mts. (Central Italy)

2021 ◽  
Vol 17 (2) ◽  
pp. 140-149
Author(s):  
Stefano Viaroli ◽  
Francesco Mirabella ◽  
Lucia Mastrorillo ◽  
Serafino Angelini ◽  
Daniela Valigi
Keyword(s):  
Central Italy ◽  
Carbonate Aquifers ◽  
Fractured Carbonate

scholarly journals 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

2018 ◽  
Vol 26 (4) ◽  
pp. 1009-1026 ◽  
Author(s):  
Marco Petitta ◽  
Lucia Mastrorillo ◽  
Elisabetta Preziosi ◽  
Francesca Banzato ◽  
Marino Domenico Barberio ◽  
...  
Keyword(s):  
Conceptual Model ◽  
Water Table ◽  
Central Italy ◽  
Seismic Sequence ◽  
Carbonate Aquifers ◽  
Fractured Carbonate ◽  
Hydrogeological Data

Groundwater dynamics in fossil fractured carbonate aquifers in Eastern Arabian Peninsula: A preliminary investigation

2019 ◽  
Vol 571 ◽  
pp. 460-470 ◽  
Author(s):  
Abotalib.Z. Abotalib ◽  
Essam Heggy ◽  
Giovanni Scabbia ◽  
Annamaria Mazzoni
Keyword(s):  
Arabian Peninsula ◽  
Preliminary Investigation ◽  
Carbonate Aquifers ◽  
Groundwater Dynamics ◽  
Fractured Carbonate

scholarly journals Characterisation of fractured carbonate aquifers using ambient borehole dilution tests

2020 ◽  
Vol 589 ◽  
pp. 125191
Author(s):  
Prodeo Yao Agbotui ◽  
Landis Jared West ◽  
Simon Henry Bottrell
Keyword(s):  
Carbonate Aquifers ◽  
Fractured Carbonate

scholarly journals Regional groundwater flow and interactions with deep fluids in western Apennine: the case of Narni-Amelia chain (Central Italy)

Geofluids ◽  
2011 ◽  
Vol 12 (2) ◽  
pp. 182-196 ◽  
Author(s):  
F. FRONDINI ◽  
C. CARDELLINI ◽  
S. CALIRO ◽  
G. CHIODINI ◽  
N. MORGANTINI
Keyword(s):  
Groundwater Flow ◽  
Central Italy ◽  
Regional Groundwater

scholarly journals Geochemical evolution of groundwater in carbonate aquifers of southern Latium region, central Italy

2013 ◽  
Author(s):  
Giuseppe Sappa ◽  
Sibel Ergul ◽  
Flavia Ferranti
Keyword(s):  
Seawater Intrusion ◽  
Coastal Area ◽  
Alkaline Earth ◽  
Geochemical Modeling ◽  
Central Italy ◽  
Mineral Weathering ◽  
Geochemical Evolution ◽  
Positive Trend ◽  
Rock Interaction ◽  
Carbonate Aquifers

Spring and well water samples, from carbonate aquifers of Latium region, have been characterized to determine the hydrochemical processes governing the evolution of the groundwater. Most of the spring samples, issuing from Lepini, Ausoni and Aurunci Mts., are characterized as alkaline earth HCO3 waters, however, some samples show a composition of Cl--SO4 -- alkaline earth waters. Groundwater samples from Pontina Plain shows three different hydrochemical facies: alkaline earth HCO3 type, Cl-- SO4 -- alkaline earth type and Cl--SO4 -- alkaline type waters. Geochemical modeling and saturation index computation of the sampled waters show an interaction with calcareous and calcareous-dolomitic lithologies. Most of the springs and wells was kinetically saturated with respect to calcite and dolomite, and all the samples were below the equilibrium state with gypsum. This indicates that the groundwater has capacity to dissolve the gypsum along the flow paths. The electrical conductivity and Cl- concentrations of the sampled waters show a positive trend with the decrease in the distance from the coast, highlighting seawater intrusion in the coastal area. According to hydrochemistry results and geochemical modeling, the dominant factors in controlling the hydrochemical characteristics of groundwater are: (i) water rock interaction with calcareous and calcareous-dolomitic lithologies; (ii) seawater intrusion in the coastal area; (iii) dissolution and/or precipitation of carbonate and (i.e. dolomite and calcite) evaporate minerals (gypsum) determined by saturation indexes; (iv) mineral weathering process; (the high Mg/Ca ratio due to the weathering of Mg-rich dolomite).

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