Víctor Manuel Arellano, Rosa María Barragán, Alfonso Aragón, Marco Helio Rodríguez, Alfredo Pérez
Geothermics, Volume 40, Issue 3, September 2011, Pages 190-198
The CerroPrietoIV (CP IV) reservoir, located in the northeastern part of the CerroPrieto (Mexico) geothermal field, was studied in order to define its pre-exploitation conditions and initial (2000–2005) response to exploitation. Bottomhole thermodynamic conditions were estimated by modeling heat and fluid flows using the WELLSIM program and well production data. Produced fluid chemical and isotopic data were also analyzed to investigate characteristic patterns of behavior over time, which were then compared against simulation results to obtain a conceptual model of the CP IV reservoir. According to the proposed model, two zones in the reservoir – separated by Fault H and producing fluids of different characteristics – were identified under pre-exploitation conditions. Wells in the area to the east-southeast (south block) produce very high-enthalpy fluids (≥2000 kJ/kg), with very low chloride (≤7000 mg/kg) and high CO2 (>6‰ molar) and δD (<−94‰). In contrast, wells toward the west-northwest (north block) show moderate-enthalpy fluids (1400–1800 kJ/kg), with high chloride (∼12,000 mg/kg) and relatively low CO2 (<6‰ molar) and δD (<−94‰). Dilution caused by cooler water entry, boiling due to steam gain, both occurring in the north block, and steam condensation in the south block were identified as the three main reservoir processes associated with exploitation. Also, it was found that the dynamics of the CP IV reservoir is controlled by the Fault H system.
- Chemical and production data of CP IV geothermal reservoir (Mexico) were interpreted.
- CP IV pre-exploitation conditions revealed fluid production from two different zones.
- 2000–2005 reservoir processes included: cooler water entry, boiling and condensation.
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