Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)

An integrated research approach consisting of hydrogeologic and geochemical methods was applied to a coastal aquifer in the Ostia Antica archaeological park, Roma, Italy, to describe freshwater–saltwater interactions. The archaeological park of Ostia Antica is located on the left bank of the Tevere...

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Main Authors: Margherita Bonamico, Paola Tuccimei, Lucia Mastrorillo, Roberto Mazza
Format: Article
Language:English
Published: MDPI AG 2021-07-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/13/1866
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author Margherita Bonamico
Paola Tuccimei
Lucia Mastrorillo
Roberto Mazza
author_facet Margherita Bonamico
Paola Tuccimei
Lucia Mastrorillo
Roberto Mazza
author_sort Margherita Bonamico
collection DOAJ
description An integrated research approach consisting of hydrogeologic and geochemical methods was applied to a coastal aquifer in the Ostia Antica archaeological park, Roma, Italy, to describe freshwater–saltwater interactions. The archaeological park of Ostia Antica is located on the left bank of the Tevere River delta which developed on a morphologically depressed area. The water monitoring program included the installation of multiparametric probes in some wells inside the archaeological area, with continuous measurement of temperature, electrical conductivity, and water table level. Field surveys, water sampling, and major elements and bromide analyses were carried out on a seasonal basis in 2016. In order to understand the detailed stratigraphic setting of the area, three surface boreholes were accomplished. Two distinct circulations were identified during the dry season, with local interaction in the rainy period: an upper one within the archaeological cover, less saline and with recharge inland; and a deeper one in the alluvial materials of Tevere River, affected by salinization. Oxygen and carbon isotopic signature of calcite in the sediments extracted from the boreholes, along with major elements and Br concentration, allowed us to recognize the sources of salinity (mainly, local interaction with Roman salt pans and agricultural practices) and the processes of gas–water–rock interaction occurring in the area. All these inferences were confirmed and strengthened by PCA analysis of physicochemical data of groundwater.
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spelling doaj.art-cad2fb141d3f4c1fbc1fbdf5a96f14e22023-11-22T02:55:33ZengMDPI AGWater2073-44412021-07-011313186610.3390/w13131866Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)Margherita Bonamico0Paola Tuccimei1Lucia Mastrorillo2Roberto Mazza3Dipartimento di Scienze, Università “Roma Tre”, 00146 Roma, ItalyDipartimento di Scienze, Università “Roma Tre”, 00146 Roma, ItalyDipartimento di Scienze, Università “Roma Tre”, 00146 Roma, ItalyDipartimento di Scienze, Università “Roma Tre”, 00146 Roma, ItalyAn integrated research approach consisting of hydrogeologic and geochemical methods was applied to a coastal aquifer in the Ostia Antica archaeological park, Roma, Italy, to describe freshwater–saltwater interactions. The archaeological park of Ostia Antica is located on the left bank of the Tevere River delta which developed on a morphologically depressed area. The water monitoring program included the installation of multiparametric probes in some wells inside the archaeological area, with continuous measurement of temperature, electrical conductivity, and water table level. Field surveys, water sampling, and major elements and bromide analyses were carried out on a seasonal basis in 2016. In order to understand the detailed stratigraphic setting of the area, three surface boreholes were accomplished. Two distinct circulations were identified during the dry season, with local interaction in the rainy period: an upper one within the archaeological cover, less saline and with recharge inland; and a deeper one in the alluvial materials of Tevere River, affected by salinization. Oxygen and carbon isotopic signature of calcite in the sediments extracted from the boreholes, along with major elements and Br concentration, allowed us to recognize the sources of salinity (mainly, local interaction with Roman salt pans and agricultural practices) and the processes of gas–water–rock interaction occurring in the area. All these inferences were confirmed and strengthened by PCA analysis of physicochemical data of groundwater.https://www.mdpi.com/2073-4441/13/13/1866freshwater–saltwater interactionsmultilayer coastal aquiferhydro-geochemistryTevere River deltaOstia Antica archaeological park
spellingShingle Margherita Bonamico
Paola Tuccimei
Lucia Mastrorillo
Roberto Mazza
Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)
Water
freshwater–saltwater interactions
multilayer coastal aquifer
hydro-geochemistry
Tevere River delta
Ostia Antica archaeological park
title Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)
title_full Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)
title_fullStr Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)
title_full_unstemmed Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)
title_short Freshwater–Saltwater Interactions in a Multilayer Coastal Aquifer (Ostia Antica Archaeological Park, Central ITALY)
title_sort freshwater saltwater interactions in a multilayer coastal aquifer ostia antica archaeological park central italy
topic freshwater–saltwater interactions
multilayer coastal aquifer
hydro-geochemistry
Tevere River delta
Ostia Antica archaeological park
url https://www.mdpi.com/2073-4441/13/13/1866
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