{"refrec":{"BRefID":362428,"RR":"<b>Vespasiano, G.; Cianflone, G.; Marini, L.; de Rosa, R.; Polemio, M.; Walraevens, K.; Vaselli, O.; Pizzino, L.; Cinti, D.; Capecchiacci, F.; Barca, D.; Dominici, R.; Apollaro, C.</b> (2023). Hydrogeochemical and isotopic characterization of the Gioia Tauro coastal Plain (Calabria-southern Italy): a multidisciplinary approach for a focused management of vulnerable strategic systems. <i>Sci. Total Environ. 862</i>: 160694. <a href=\"https://dx.doi.org/10.1016/j.scitotenv.2022.160694\" target=\"_blank\">https://dx.doi.org/10.1016/j.scitotenv.2022.160694</a>","BEntID":360145,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Sci. Total Environ. 862</i>: 160694. <a href=\"https://dx.doi.org/10.1016/j.scitotenv.2022.160694\" target=\"_blank\">https://dx.doi.org/10.1016/j.scitotenv.2022.160694</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vespasiano, G.; Cianflone, G.; Marini, L.; de Rosa, R.; Polemio, M.; Walraevens, K.; Vaselli, O.; Pizzino, L.; Cinti, D.; Capecchiacci, F.; Barca, D.; Dominici, R.; Apollaro, C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vespasiano, G. <i>et al.</i>","Englishabstract":"This work pursues the hydro-geochemical and isotopic characterization of the complex groundwater system of the Gioia Tauro Plain, one of the most important industrialized and agricultural coastal areas of southern Italy. The an-thropic pressure exposes the water resources at risk of depletion and quality degradation making the plain groundwa-ter a system of high scientific and social interest.The plain is characterized by a shallow aquifer, mostly recharged by local rains and a deep aquifer apparently less in-fluenced by local precipitation. Both aquifers are mainly Ca-HCO3 waters except for localized sectors where Na-HCO3, Na-Cl and Ca-SO4 waters are present. In deep aquifer, both prolonged interaction with sedimentary rocks, mainly de-riving from the erosion of crystalline rocks, and direct cation exchange represent the primary factors controlling the formation of Na-HCO3 waters. Mixing processes between these waters and either connate brine and/or deep thermal waters contribute to the formation of isolated high salinity Na-Cl-rich waters. In shallow aquifer, inputs of N-rich sew-age and agriculture-related contaminants, and SOx emissions in proximity of the harbor are responsible of the increasing nitrate and sulphate concentrations, respectively. The Cl/Br and NO3/Cl ratios highlight contamination mainly linked to agricultural activities and contribution of wastewater.Along the northern boundary, the warmest groundwater (Na-Cl[SO4]) were found close to a bend of the main strike -slip fault system, locally favouring the rising of B-and Li-rich deep waters, testifying the influence of geological -structural features on deep water circulation. Despite the high-water demand, a direct marine intrusion is localized in a very restricted area, where we observed an incipient groundwater-seawater mixing (seawater contribution <= 7 %). The qualitative and quantitative conditions of the shallow aquifer still have acceptable levels because of the relatively high recharge inflow. A reliable hydrogeo-chemical conceptual model, able to explain the compositional variability of the studied waters, is proposed.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Hydrogeochemical and isotopic characterization of the Gioia Tauro coastal Plain (Calabria-southern Italy): a multidisciplinary approach for a focused management of vulnerable strategic systems","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-24 01:33:17.990302","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Coastal aquifers; Hydrogeochemistry; Water isotopes; Conceptual hydrogeochemical model; Calabria; Southern Italy","OtherDescriptors":null,"Notes":null,"AnaPub":2023,"MonPub":null,"DateUpdate":"2023-03-27","DateCreate":"2023-03-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000901674200011","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.scitotenv.2022.160694"},"refs":null,"anarec":{"AnaID":362428,"PubliDate":2023,"Pagination":"160694","XtraPublOfAnaID":null,"ISBN":null,"Volume":"862","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43780,"SerRR":"Science of the Total Environment. 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