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
2019 ◽  
Vol 34 (5) ◽  
pp. 1167-1181 ◽  
Author(s):  
Lucia Mastrorillo ◽  
Michele Saroli ◽  
Stefano Viaroli ◽  
Francesca Banzato ◽  
Daniela Valigi ◽  
...  

2018 ◽  
Vol 26 (4) ◽  
pp. 1009-1026 ◽  
Author(s):  
Marco Petitta ◽  
Lucia Mastrorillo ◽  
Elisabetta Preziosi ◽  
Francesca Banzato ◽  
Marino Domenico Barberio ◽  
...  

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

Author(s):  
Giuseppe Sappa ◽  
Sibel Ergul ◽  
Flavia Ferranti

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).


2014 ◽  
Vol 50 (6) ◽  
pp. 4858-4876 ◽  
Author(s):  
A. Amoruso ◽  
L. Crescentini ◽  
S. Martino ◽  
M. Petitta ◽  
M. Tallini

2008 ◽  
Vol 16 (6) ◽  
pp. 1057-1064 ◽  
Author(s):  
Gino Naclerio ◽  
Emma Petrella ◽  
Valentina Nerone ◽  
Vincenzo Allocca ◽  
Pantaleone De Vita ◽  
...  

Water ◽  
2021 ◽  
Vol 13 (10) ◽  
pp. 1374
Author(s):  
Daniela Valigi ◽  
Costanza Cambi ◽  
Roberto Checcucci ◽  
Lucio Di Matteo

Transmissivity estimates can be obtained by different approaches, mainly analytical and empirical. The application of analytical methods requires checking non-linear well losses due to turbulence and vertical flow related to partial penetration. The empirical approach relates transmissivity values to specific capacity data measured in the same well. The interpretation of available pumping tests highlights porous media solutions’ applicability in most of the step-drawdown curves analyzed. Double or triple porosity approaches are more appropriate only for wells located close to fault systems. In this work, a new relationship to estimate transmissivity by specific capacity data in some Italian carbonate aquifers is proposed. The comparison with other relationships available in the literature for similar aquifers worldwide confirms the validity of a general equation for carbonate aquifers, helping the spatial characterization of aquifer transmissivity in scarce data regions. Nonetheless, the use of equations of the same kind with different coefficients allows good results on our set of data. Results can improve the knowledge of fractured–karst aquifers by also including data from Central Italy.


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