Gas geochemistry of the Cerro Pabellón geothermal plant: protocol constraining thermal and redox conditions

Abstract Geothermal heat extraction at a binary plant, and associated plant lifetime, can be optimized through fluid monitoring of geothermal gases and natural system gas discharges. A novel gas monitoring tool for geothermal exploration and production-stage decision-making is presented, based on research conducted at Cerro Pabellón, Chile, following its internationally celebrated opening in 2017. The gas phase was studied over a period of 5 years using direct gas condensate sampling and an innovative application of principal component analysis combined with the uniform manifold approximation and projection (UMAP) method. Monitoring results show that gas composition varies during cooling of the vapor phase, with oxidation state (RH) increasing as vapor fraction (%) decreases. A subsequent increase in HCO₃ 2 ⁻ concentration was detected in condensate liquids measured by ion chromatography, reflecting progressive gas–liquid interaction. According to UMAP clustering and gas composition analysis, the N₂/Ar ratio in gas samples represents an effective pathfinder to monitor geothermal plant physico-chemical parameters. Gas compositional clusters of CO₂-rich gases (> 96.0%), mainly represented by the N₂/Ar ratio (N 2 /O 2 :CH 4 /CO 2 ), show two clear trends in gas mixture fluctuations: cooling associated with a relatively hot (315 ± 45 °C) Apacheta-like gas mixture derived from the hydrothermal reservoir, relatively cooler fluids (Md = 252 ± 78 °C) varying in redox conditions (Md (LogH 2 /H 2 O) = − 3.33 ± 0.64 RH). These estimated thermo-redox conditions in tandem with vapor N₂/Ar ratio fluctuate distinctly along each vapor separation line segments (C, F, J, M), correlating strongly on vapor fraction (19–100 vol.%), with progressive cooling until reaching temperatures of 140–160 °C at the plant steam–brine separators. Gas compounds in equilibrium with CO₂-rich fluids represent critical indicators of reservoir and plant-scale processes. Monitoring and control of these gas compounds at geothermal plants can improve long-term maintenance strategies and sustainability of binary power plants through integration of condensate liquid surveillance and improved geostatistical analysis.

Authors

Publication Details

Journal
Geothermal Energy
Published
2026-04-06
DOI
https://doi.org/10.1186/s40517-026-00382-9
Primary Topic
Geothermal Energy Systems and Applications
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Gas geochemistry of the Cerro Pabellón geothermal plant: protocol constraining thermal and redox conditions

Diego Morata, Santiago Maza, Gianni Volpi, Verónica Moreno-Rodríguez et al.
Geothermal Energy
Geothermal Energy Systems and Applications
article

Gas geochemistry of the Cerro Pabellón geothermal plant: protocol constraining thermal and redox conditions

Diego Morata, Santiago Maza, Gianni Volpi, Verónica Moreno-Rodríguez, Fausto Grassa, Manfredi Longo, Pierangelo Romano, Philippe Robidoux, M. Salvá Cárdenas, Germain Rivera, Marianno Tantillo, Marco Cecioni
article en

Abstract

Abstract Geothermal heat extraction at a binary plant, and associated plant lifetime, can be optimized through fluid monitoring of geothermal gases and natural system gas discharges. A novel gas monitoring tool for geothermal exploration and production-stage decision-making is presented, based on research conducted at Cerro Pabellón, Chile, following its internationally celebrated opening in 2017. The gas phase was studied over a period of 5 years using direct gas condensate sampling and an innovative application of principal component analysis combined with the uniform manifold approximation and projection (UMAP) method. Monitoring results show that gas composition varies during cooling of the vapor phase, with oxidation state (RH) increasing as vapor fraction (%) decreases. A subsequent increase in HCO₃ 2 ⁻ concentration was detected in condensate liquids measured by ion chromatography, reflecting progressive gas–liquid interaction. According to UMAP clustering and gas composition analysis, the N₂/Ar ratio in gas samples represents an effective pathfinder to monitor geothermal plant physico-chemical parameters. Gas compositional clusters of CO₂-rich gases (> 96.0%), mainly represented by the N₂/Ar ratio (N 2 /O 2 :CH 4 /CO 2 ), show two clear trends in gas mixture fluctuations: cooling associated with a relatively hot (315 ± 45 °C) Apacheta-like gas mixture derived from the hydrothermal reservoir, relatively cooler fluids (Md = 252 ± 78 °C) varying in redox conditions (Md (LogH 2 /H 2 O) = − 3.33 ± 0.64 RH). These estimated thermo-redox conditions in tandem with vapor N₂/Ar ratio fluctuate distinctly along each vapor separation line segments (C, F, J, M), correlating strongly on vapor fraction (19–100 vol.%), with progressive cooling until reaching temperatures of 140–160 °C at the plant steam–brine separators. Gas compounds in equilibrium with CO₂-rich fluids represent critical indicators of reservoir and plant-scale processes. Monitoring and control of these gas compounds at geothermal plants can improve long-term maintenance strategies and sustainability of binary power plants through integration of condensate liquid surveillance and improved geostatistical analysis.

Geothermal Energy
Agencia Nacional de Investigación y Desarrollo
Openalex Percentile: Top 34%
Geothermal Energy Systems and Applications
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.