Four of the wells drilled for production (PGM-02, PGM-06, PGM-07, PGM-19) in Miravalles geothermal field of Costa Rica discharge acid fluids. They are located along the eastern boundary of the field close to the Miravalles volcano. Analysis of the existing chemical and isotopic data for the acidic wells in comparison with those for the pH-neutral production wells and surface natural manifestations allowed us to refine the geochemical models of geothermal field present in the literature. Two types of acidic fluids, a shallower one and a deeper one have been postulated.

Preliminary notes on the acid fluids of the Miravalles geothermal field (Guanacaste, Costa Rica)

Gherardi F;
2005

Abstract

Four of the wells drilled for production (PGM-02, PGM-06, PGM-07, PGM-19) in Miravalles geothermal field of Costa Rica discharge acid fluids. They are located along the eastern boundary of the field close to the Miravalles volcano. Analysis of the existing chemical and isotopic data for the acidic wells in comparison with those for the pH-neutral production wells and surface natural manifestations allowed us to refine the geochemical models of geothermal field present in the literature. Two types of acidic fluids, a shallower one and a deeper one have been postulated.
2005
Istituto di Geoscienze e Georisorse - IGG - Sede Pisa
Inglese
Use of isotope techniques to trace the origin of acidic fluids in geothermal systems
61
81
197
92-0-102805-9
Sì, ma tipo non specificato
4
02 Contributo in Volume::02.01 Contributo in volume (Capitolo o Saggio)
268
none
Gherardi, F; Panichi, C; Yock, Fung; Gerardoabaya, J
info:eu-repo/semantics/bookPart
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/161158
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