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The geothermal system of Ischia Island (southern Italy): Critical review and sustainability analysis of geothermal resource for electricity generation
Affiliation:1. Department of Civil, Architectural and Environmental Engineering, University of Naples Federico II, P/le Tecchio 80, 80125 Napoli, Italy;2. DiSTAR, University of Naples Federico II, Largo San Marcellino, 10 80138 Napoli, Italy;3. Institute for Coastal Marine Environment (CNR), Calata Porta di Massa, 80133 Napoli, Italy;1. Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Via Diocleziano 328, I-80124 Napoli, Italy;2. Dipartimento di Scienze della Terra, dell''Ambiente e delle Risorse, Università di Napoli “Federico II”, Via Mezzocannone 8, I-80134 Napoli, Italy;3. Institut für Geologie und Paläontologie, Westfälische Wilhelms-Universität Münster, Corrensstraβe 24, D-48149 Münster, Germany
Abstract:In this paper we analyze the main available data related to the geothermal system of Ischia Island, starting from the first geothermal exploration in 1939. Our aim is to define a conceptual model of the geothermal reservoir, according to geological, geochemical, geophysical and stratigraphic data. In recent times, the interest on geothermal exploitation for electricity generation in Italy is rapidly increasing and the Ischia Island is one of the main targets for future geothermal exploitation. Nowadays, one of the main economic resources of the island is the tourism, mainly driven by the famous thermal springs; so, it is crucial to study the possible interaction between geothermal exploitation and thermal spring activities. To this aim, we also analyze the possible disturbance on temperature and pressure in the shallow geothermal reservoir, due to the heat withdrawal for electric production related to small power plant size (1–5 MWe). Such analysis has been performed by using numerical simulations based on a well known thermofluid-dynamical code (TOUGH2®). Obtained results show that such geothermal exploitation generates a perturbation of temperature and pressure field which, however, is confined in a small volume around the well. At shallow level (0–100 m) the exploitation does not produce any appreciable disturbance, and can be made compatible with thermal spring exploitation. Moreover, such results are crucial both for the evaluation of volcanological processes in the island and for the general assessment of geothermal resource sustainability.
Keywords:Ischia Island  Geothermal resource  Sustainable energy  Heat flow  Fluid advection  Brittle–ductile transition
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