Influence of hydrostratigraphy and structural setting on the arsenic occurrence in groundwater of the Cimino-Vico volcanic area (central Italy) | Influence des paramètres hydrostatiques et structuraux sur la présence d’arsenic dans les eaux souterraines dans la région volcanique de Cimino-Vico (Italie centrale) Influencia del esquema hidroestratigráfico y estructural sobre la existencia de arsénico en las aguas subterráneas del área volcánica de Cimino – Vico (Italia central) 水文地层和构造对Cimino-Vico火山岩地区 (意大利中部) 地下水中砷分布的影响 Influenza dell’assetto idrostratigrafico e strutturale sulla presenza dell’arsenico nelle acque sotterranee dell’area vulcanica del Cimino-Vico (Italia centrale) Influência da hidrostratigrafia e do enquadramento estrutural na ocorrência de arsénio nas água subterrâneas da zona vulcânica de Cimino-Vico (Itália central)
2009
Angelone, Massimo | Cremisini, Carlo | Piscopo, Vincenzo | Proposito, Marco | Spaziani, Fabio
Arsenic occurrence in groundwater near the Cimino-Vico volcanoes (central Italy) was analysed considering the hydrostratigraphy and structural setting and the shallow and deep flows interacting within the Quaternary volcanics. Groundwater is the local source of drinking water. As documented in the past, arsenic in the groundwater has become a problem, and the European maximum allowable contaminant level was recently lowered to 10 μg/L. Chemical analyses of groundwater were conducted, sampled over an area of about 900 km², from 65 wells and springs representative of the volcanic aquifer and thermal waters. Considering the type of aquifer, the nature of the aquifer formation and its substratum, the hydrochemical data highlight that the arsenic content of the groundwater is mainly connected with the hydrothermal processes in the volcanic area. Thermal waters (54–60°C) fed from deep-rising fluids show higher arsenic concentrations (176–371 μg/L). Cold waters sampled from the volcanic aquifer are characterized by a wide variability in their arsenic concentration (1.6–195 μg/L), and about 62% exceed the limit of 10 μg/L. Where the shallow volcanic aquifer is open to deep-rising thermal fluids, relatively high arsenic concentrations (20–100 μg/L) are found. This occurs close to areas of the more recent volcano-tectonic structures.
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