Development of a Downhole Tool Measuring Real-Time Concentration of Ionic Tracers and pH in Geothermal Reservoirs
For enhanced or Engineered Geothermal Systems (EGS) geothermal brine is pumped to the surface via the production wells, the heat extracted to turn a turbine to generate electricity, and the spent brine re-injected via injection wells back underground. If designed properly, the subsurface rock formations will lead this water back to the extraction well as heated brine. Proper monitoring of these geothermal reservoirs is essential for developing and maintaining the necessary level of productivity of the field. Chemical tracers are commonly used to characterize the fracture network and determine the connectivity between the injection and production wells. Currently, most tracer experiments involve injecting the tracer at the injection well, manually collecting liquid samples at the wellhead of the production well, and sending the samples off for laboratory analysis. While this method provides accurate tracer concentration data at very low levels of detection, it does not provide information regarding the location of the fractures which were conducting the tracer between wellbores. Sandia is developing a high-temperature electrochemical sensor capable of measuring tracer concentrations and pH downhole on a wireline tool. The goal of this effort is to collect real-time pH and ionic tracer concentration data at temperatures up to 225 degrees C and pressures up to 3000 psi.
In this paper, a prototype electrochemical sensor and the initial data obtained will be presented detailing the measurement of iodide tracer concentrations at high temperature and pressure in a newly developed laboratory scale autoclave.
Citation Formats
TY - DATA
AB - For enhanced or Engineered Geothermal Systems (EGS) geothermal brine is pumped to the surface via the production wells, the heat extracted to turn a turbine to generate electricity, and the spent brine re-injected via injection wells back underground. If designed properly, the subsurface rock formations will lead this water back to the extraction well as heated brine. Proper monitoring of these geothermal reservoirs is essential for developing and maintaining the necessary level of productivity of the field. Chemical tracers are commonly used to characterize the fracture network and determine the connectivity between the injection and production wells. Currently, most tracer experiments involve injecting the tracer at the injection well, manually collecting liquid samples at the wellhead of the production well, and sending the samples off for laboratory analysis. While this method provides accurate tracer concentration data at very low levels of detection, it does not provide information regarding the location of the fractures which were conducting the tracer between wellbores. Sandia is developing a high-temperature electrochemical sensor capable of measuring tracer concentrations and pH downhole on a wireline tool. The goal of this effort is to collect real-time pH and ionic tracer concentration data at temperatures up to 225 degrees C and pressures up to 3000 psi.
In this paper, a prototype electrochemical sensor and the initial data obtained will be presented detailing the measurement of iodide tracer concentrations at high temperature and pressure in a newly developed laboratory scale autoclave.
AU - Hess, Ryan F.
A2 - Boyle, Timothy J.
A3 - Limmer, Steven
A4 - Yelton, William G.
A5 - Bingham, Samuel
A6 - Stillman, Greg
A7 - Lindblom, Scott
A8 - Cieslewski, Grzegorz
DB - Open Energy Data Initiative (OEDI)
DP - Open EI | National Renewable Energy Laboratory
DO -
KW - geothermal
KW - EGS
KW - downhole tool
KW - reservoir monitoring
KW - chemical tracers
KW - high temperature electrochemical sensor
KW - high temp
KW - high temperature
KW - electrochemical sensor
KW - ionic tracers
KW - Engineered Geothermal Systems EGS
KW - Sandia National Labs
KW - SNL
KW - doi 10.1117/12.2051151
KW - tracer
KW - downhole
KW - high pressure
LA - English
DA - 2014/03/31
PY - 2014
PB - Sandia National Laboratories
T1 - Development of a Downhole Tool Measuring Real-Time Concentration of Ionic Tracers and pH in Geothermal Reservoirs
UR - https://data.openei.org/submissions/6726
ER -
Hess, Ryan F., et al. Development of a Downhole Tool Measuring Real-Time Concentration of Ionic Tracers and pH in Geothermal Reservoirs. Sandia National Laboratories, 31 March, 2014, GDR. https://gdr.openei.org/submissions/413.
Hess, R., Boyle, T., Limmer, S., Yelton, W., Bingham, S., Stillman, G., Lindblom, S., & Cieslewski, G. (2014). Development of a Downhole Tool Measuring Real-Time Concentration of Ionic Tracers and pH in Geothermal Reservoirs. [Data set]. GDR. Sandia National Laboratories. https://gdr.openei.org/submissions/413
Hess, Ryan F., Timothy J. Boyle, Steven Limmer, William G. Yelton, Samuel Bingham, Greg Stillman, Scott Lindblom, and Grzegorz Cieslewski. Development of a Downhole Tool Measuring Real-Time Concentration of Ionic Tracers and pH in Geothermal Reservoirs. Sandia National Laboratories, March, 31, 2014. Distributed by GDR. https://gdr.openei.org/submissions/413
@misc{OEDI_Dataset_6726,
title = {Development of a Downhole Tool Measuring Real-Time Concentration of Ionic Tracers and pH in Geothermal Reservoirs},
author = {Hess, Ryan F. and Boyle, Timothy J. and Limmer, Steven and Yelton, William G. and Bingham, Samuel and Stillman, Greg and Lindblom, Scott and Cieslewski, Grzegorz},
abstractNote = {For enhanced or Engineered Geothermal Systems (EGS) geothermal brine is pumped to the surface via the production wells, the heat extracted to turn a turbine to generate electricity, and the spent brine re-injected via injection wells back underground. If designed properly, the subsurface rock formations will lead this water back to the extraction well as heated brine. Proper monitoring of these geothermal reservoirs is essential for developing and maintaining the necessary level of productivity of the field. Chemical tracers are commonly used to characterize the fracture network and determine the connectivity between the injection and production wells. Currently, most tracer experiments involve injecting the tracer at the injection well, manually collecting liquid samples at the wellhead of the production well, and sending the samples off for laboratory analysis. While this method provides accurate tracer concentration data at very low levels of detection, it does not provide information regarding the location of the fractures which were conducting the tracer between wellbores. Sandia is developing a high-temperature electrochemical sensor capable of measuring tracer concentrations and pH downhole on a wireline tool. The goal of this effort is to collect real-time pH and ionic tracer concentration data at temperatures up to 225 degrees C and pressures up to 3000 psi.
In this paper, a prototype electrochemical sensor and the initial data obtained will be presented detailing the measurement of iodide tracer concentrations at high temperature and pressure in a newly developed laboratory scale autoclave.
},
url = {https://gdr.openei.org/submissions/413},
year = {2014},
howpublished = {GDR, Sandia National Laboratories, https://gdr.openei.org/submissions/413},
note = {Accessed: 2025-05-03}
}
Details
Data from Mar 31, 2014
Last updated Jun 18, 2024
Submitted May 1, 2014
Organization
Sandia National Laboratories
Contact
Grzegorz Cieslewski
505.284.2532
Authors
Original Source
https://gdr.openei.org/submissions/413Research Areas
Keywords
geothermal, EGS, downhole tool, reservoir monitoring, chemical tracers, high temperature electrochemical sensor, high temp, high temperature, electrochemical sensor, ionic tracers, Engineered Geothermal Systems EGS, Sandia National Labs, SNL, doi 10.1117/12.2051151, tracer, downhole, high pressureDOE Project Details
Project Name High Temperature Chemical Sensing Tool for Distributed Mapping of Fracture Flow in EGS
Project Lead Greg Stillman
Project Number FY14 AOP 1.1.5.1