TY - JOUR
T1 - Temperature estimation of the Nevado del Ruiz Volcano geothermal reservoir
T2 - Insight from western hot springs hydrogeochemistry
AU - Taborda, Alejandra
AU - Portela, Juan Pablo
AU - Lopez-Sanchez, Jacqueline
AU - Daniele, Linda
AU - Moreno, David
AU - Blessent, Daniela
N1 - Funding Information:
The authors would like to thank the Universidad de Medellín (Colombia) for the research project funded in collaboration with FONDAP-ACE210005 (Centro de Excelencia en Geotermia de los Andes, CEGA) and ANID-FONDEQUIP project EQM120098 for the trace element data obtained using the iCap Q-ICP-MS equipment which supported the laboratory analysis samples. The International Geoscience Programme of the UNESCO is acknowledged since this work is part of the project “IGCP 636-Geothermal resources for energy transition”. Finally, the authors are grateful to the SGC (Colombian Geological Survey) for the National Inventory of Hydrothermal Manifestation, Juan Pablo Ávila, and Universidad Pedagógica y Tecnológica de Colombia for the GQAnalyzer software, Daniel Ceballos Gutiérrez from CHEC for his help during fieldwork, and Esteban Gómez Díaz and Daniel Balzan for comments and suggestions provided about this manuscript.
Publisher Copyright:
© 2022 Elsevier B.V.
PY - 2022/9
Y1 - 2022/9
N2 - Geochemical surveying is one of the techniques of geothermal exploration that include geothermometry to estimate the temperature of deep reservoirs. This work provides the temperature estimation of geothermal resources, geochemical analysis, and a conceptual model of the geothermal reservoir located to the western flank of the Nevado del Ruiz Volcano (NRV), a mayor geothermal target for energy production in Colombia. Hydrogeochemical data (pH, temperature, electrical conductivity, major, minor, and trace elements) were obtained from water samples collected at several hot springs located to the west of the NRV between 2017 and 2019. The data available from the Colombian Geological Survey database were also included in the analysis to better characterize the hot spring behavior. The hydrogeochemical tools Liquid analysis Powell and Cumming and GQAnalyzer software were used to draw ternary diagrams and to use geothermometers. The results allowed separating the hot springs into two groups, according with their chemical characteristics and spatial location: Nereidas 1, Nereidas 2, Nereidas Pozo, and Chorro Negro hot springs belong to Group 1 (G1), located closer to the NRV; on the other hand, Geysers, El Bosque-La Piscina, Quebrada Negra, and Rio Claro, which are located further from NRV, belong to Group 2 (G2). The latter is made of mature and chloride waters, indicating a water-rock equilibrated interaction with most of ions. The results of this study contribute to the future Colombian geothermal development, and the methodology and analysis can be applied to geothermal systems with similar geological characteristics to infer a conceptual model useful for geothermal exploration.
AB - Geochemical surveying is one of the techniques of geothermal exploration that include geothermometry to estimate the temperature of deep reservoirs. This work provides the temperature estimation of geothermal resources, geochemical analysis, and a conceptual model of the geothermal reservoir located to the western flank of the Nevado del Ruiz Volcano (NRV), a mayor geothermal target for energy production in Colombia. Hydrogeochemical data (pH, temperature, electrical conductivity, major, minor, and trace elements) were obtained from water samples collected at several hot springs located to the west of the NRV between 2017 and 2019. The data available from the Colombian Geological Survey database were also included in the analysis to better characterize the hot spring behavior. The hydrogeochemical tools Liquid analysis Powell and Cumming and GQAnalyzer software were used to draw ternary diagrams and to use geothermometers. The results allowed separating the hot springs into two groups, according with their chemical characteristics and spatial location: Nereidas 1, Nereidas 2, Nereidas Pozo, and Chorro Negro hot springs belong to Group 1 (G1), located closer to the NRV; on the other hand, Geysers, El Bosque-La Piscina, Quebrada Negra, and Rio Claro, which are located further from NRV, belong to Group 2 (G2). The latter is made of mature and chloride waters, indicating a water-rock equilibrated interaction with most of ions. The results of this study contribute to the future Colombian geothermal development, and the methodology and analysis can be applied to geothermal systems with similar geological characteristics to infer a conceptual model useful for geothermal exploration.
KW - Colombia
KW - Faults
KW - Fluid circulation
KW - Outflow
KW - Upflow
UR - http://www.scopus.com/inward/record.url?scp=85134883395&partnerID=8YFLogxK
U2 - 10.1016/j.gexplo.2022.107049
DO - 10.1016/j.gexplo.2022.107049
M3 - Artículo
AN - SCOPUS:85134883395
VL - 240
JO - Journal of Geochemical Exploration
JF - Journal of Geochemical Exploration
SN - 0375-6742
M1 - 107049
ER -