Deep carbon degassing in the Matese massif chain (Southern Italy) inferred by geochemical and isotopic data.

Autor: Rufino F; Department of Environmental, Biological and Pharmaceutical Sciences and Technologies, University of Campania 'Luigi Vanvitelli', Via Vivaldi 43, 81100, Caserta, Italy. francesco.rufino@unicampania.it., Cuoco E; Department of Environmental, Biological and Pharmaceutical Sciences and Technologies, University of Campania 'Luigi Vanvitelli', Via Vivaldi 43, 81100, Caserta, Italy.; Istituto Nazionale di Geofisica e Vulcanologia, sezione di Napoli - Osservatorio Vesuviano, Via Diocleziano 328, 80124, Naples, Italy., Busico G; Department of Geology, Laboratory of Engineering Geology & Hydrogeology, Aristotle University of Thessaloniki, 54124, Thessaloniki, Greece., Caliro S; Istituto Nazionale di Geofisica e Vulcanologia, sezione di Napoli - Osservatorio Vesuviano, Via Diocleziano 328, 80124, Naples, Italy., Maletic EL; School of Earth Sciences, The Ohio State University, 125 South Oval Mall, Columbus, OH, 43210, USA., Avino R; Istituto Nazionale di Geofisica e Vulcanologia, sezione di Napoli - Osservatorio Vesuviano, Via Diocleziano 328, 80124, Naples, Italy., Darrah TH; School of Earth Sciences, The Ohio State University, 125 South Oval Mall, Columbus, OH, 43210, USA.; Global Water Institute, 190 North Oval Mall, Columbus, OH, 43210, USA., Tedesco D; Department of Environmental, Biological and Pharmaceutical Sciences and Technologies, University of Campania 'Luigi Vanvitelli', Via Vivaldi 43, 81100, Caserta, Italy.; Istituto Nazionale di Geofisica e Vulcanologia, sezione di Napoli - Osservatorio Vesuviano, Via Diocleziano 328, 80124, Naples, Italy.
Jazyk: angličtina
Zdroj: Environmental science and pollution research international [Environ Sci Pollut Res Int] 2021 Sep; Vol. 28 (34), pp. 46614-46626. Date of Electronic Publication: 2020 Oct 10.
DOI: 10.1007/s11356-020-11107-1
Abstrakt: The Italian Apennines are among the most important sources of freshwater for several Italian regions. With evidences of deep CO 2 -rich fluids intruding into aquifers in the nearby central-southern Apennines, a thorough investigation into the geochemistry of groundwater became critical to ensure the water quality in the area. Here, we show the main hydrogeochemical processes occurring in the Matese Massif (MM) aquifer through the investigation of 98 water samples collected from springs and water wells. All waters were classified as HCO 3 type with Ca dominance (from 50% up to 97%) and variable amount of Mg (from 1% up to 49%). A multivariate statistical approach through the application of the factor analysis (FA) highlighted three main hydrogeochemical processes: (i) water-carbonate rock interactions mostly enhanced in peripheral areas of the MM by CO 2 deep degassing; (ii) addition of NaCl-rich components linked to recharging process and to water mixing processes of the groundwater with a thermal component relatively rich in Cl, Na, and CO 2 ; (iii) anthropogenic activities influencing groundwater composition at the foothills of MM. Furthermore, the first detailed TDIC, pCO 2 , and δ 13 C-TDIC distribution maps of the MM area have been created, which track chemical and isotopic anomalies in several peripheral areas (Pratella, Ailano, and Telese) throughout the region. These maps systematically highlight that the greater the amount of dissolved carbon occurs the heavier the C isotope enrichment, especially in the peripheral areas. Conversely, spring waters emerging at higher altitudes within MM are only slightly mineralized and associated with δ 13 C-TDIC values mainly characterized by recharging processes with the addition of biogenic carbon during the infiltration process through the soil.
(© 2020. Springer-Verlag GmbH Germany, part of Springer Nature.)
Databáze: MEDLINE
Externí odkaz: