Utah FORGE: Fluid Injection-Rate Controls on Seismic Moment from Laboratory Fault Reactivation Experiments
This dataset contains experimental and acoustic data from shear reactivation tests that investigate the relationship between fluid-injection rate, pore pressure distribution, and seismic moment during laboratory fault slip. It includes raw mechanical data and acoustic emission recordings from fifteen experiments performed on 2.5-3 inch granitoid cores from the Utah FORGE enhanced geothermal systems (EGS) site. Each sample contains a single inclined fracture with small-scale surface roughness.
Experiments were conducted in an aluminum triaxial pressure vessel (TEMCO) equipped with three independently servo-controlled pumps using distilled water as the working fluid. The pumps regulated confining, upstream pore, and axial pressures, with each connected to a LabView interface to record applied pressures, cumulative injected volumes, and flow rates. The downstream outlet was closed to allow pressurization, monitored by an external pressure transducer. Axial displacement was measured by a linear variable differential transformer (LVDT) attached to the axial piston and converted to shear displacement along the fracture. Acoustic emissions were recorded using P-wave transducers, with event timing, amplitude, and cumulative amplitude compared against seismic moment and shear slip velocity.
Fluid injection rates of 0.05, 0.25, and 0.75 mL/min were applied under constant shear stress conditions, with both uniform and non-uniform along-fault pressure distributions. Samples were fully saturated with deionized water. Axial and confining stresses were increased to 3 MPa in 500 kPa increments, while pore pressure was held at 200 kPa prior to initiating shear mobilization. Axial stress was then increased to induce shear slip and subsequently reduced to approximately 60%, 80%, or 90% of the peak shear stress, depending on the experiment. The raw mechanical data files include time-series measurements of confining, pore, and axial pressures; pump volumes and flow rates; time (in hours:minutes:seconds); axial displacement (in millimeters); and downstream pressure (in psi).
Citation Formats
TY - DATA
AB - This dataset contains experimental and acoustic data from shear reactivation tests that investigate the relationship between fluid-injection rate, pore pressure distribution, and seismic moment during laboratory fault slip. It includes raw mechanical data and acoustic emission recordings from fifteen experiments performed on 2.5-3 inch granitoid cores from the Utah FORGE enhanced geothermal systems (EGS) site. Each sample contains a single inclined fracture with small-scale surface roughness.
Experiments were conducted in an aluminum triaxial pressure vessel (TEMCO) equipped with three independently servo-controlled pumps using distilled water as the working fluid. The pumps regulated confining, upstream pore, and axial pressures, with each connected to a LabView interface to record applied pressures, cumulative injected volumes, and flow rates. The downstream outlet was closed to allow pressurization, monitored by an external pressure transducer. Axial displacement was measured by a linear variable differential transformer (LVDT) attached to the axial piston and converted to shear displacement along the fracture. Acoustic emissions were recorded using P-wave transducers, with event timing, amplitude, and cumulative amplitude compared against seismic moment and shear slip velocity.
Fluid injection rates of 0.05, 0.25, and 0.75 mL/min were applied under constant shear stress conditions, with both uniform and non-uniform along-fault pressure distributions. Samples were fully saturated with deionized water. Axial and confining stresses were increased to 3 MPa in 500 kPa increments, while pore pressure was held at 200 kPa prior to initiating shear mobilization. Axial stress was then increased to induce shear slip and subsequently reduced to approximately 60%, 80%, or 90% of the peak shear stress, depending on the experiment. The raw mechanical data files include time-series measurements of confining, pore, and axial pressures; pump volumes and flow rates; time (in hours:minutes:seconds); axial displacement (in millimeters); and downstream pressure (in psi).
AU - Elsworth, Derek
A2 - Eijsink, Agathe
A3 - Marone, Chris
A4 - Shokouhi, Parisa
A5 - Riviere, Jacques
A6 - Wang, Junpeng
A7 - Yu, Jiayi
DB - Geothermal Data Repository
DP - Open EI | National Laboratory of the Rockies
DO -
KW - geothermal
KW - energy
KW - induced seismicity
KW - EGS
KW - geomechanics
KW - Utah FORGE
KW - granitoid
KW - laboratory experiments
KW - fault reactivation
KW - shear slip
KW - fluid injection
KW - injection rate
KW - pore pressure
KW - pore pressure distribution
KW - seismic moment
KW - acoustic emissions
KW - permeability
KW - triaxial testing
KW - shear stress
KW - axial displacement
KW - pressure vessel
KW - mechinical data
KW - time-series data
KW - raw data
KW - processed data
KW - MATLAB
LA - English
DA - 2025/09/16
PY - 2025
PB - Pennsylvania State University
T1 - Utah FORGE: Fluid Injection-Rate Controls on Seismic Moment from Laboratory Fault Reactivation Experiments
UR - https://gdr.openei.org/submissions/1775
ER -
Elsworth, Derek, et al. Utah FORGE: Fluid Injection-Rate Controls on Seismic Moment from Laboratory Fault Reactivation Experiments. Pennsylvania State University, 16 September, 2025, Geothermal Data Repository. https://gdr.openei.org/submissions/1775.
Elsworth, D., Eijsink, A., Marone, C., Shokouhi, P., Riviere, J., Wang, J., & Yu, J. (2025). Utah FORGE: Fluid Injection-Rate Controls on Seismic Moment from Laboratory Fault Reactivation Experiments. [Data set]. Geothermal Data Repository. Pennsylvania State University. https://gdr.openei.org/submissions/1775
Elsworth, Derek, Agathe Eijsink, Chris Marone, Parisa Shokouhi, Jacques Riviere, Junpeng Wang, and Jiayi Yu. Utah FORGE: Fluid Injection-Rate Controls on Seismic Moment from Laboratory Fault Reactivation Experiments. Pennsylvania State University, September, 16, 2025. Distributed by Geothermal Data Repository. https://gdr.openei.org/submissions/1775
@misc{GDR_Dataset_1775,
title = {Utah FORGE: Fluid Injection-Rate Controls on Seismic Moment from Laboratory Fault Reactivation Experiments},
author = {Elsworth, Derek and Eijsink, Agathe and Marone, Chris and Shokouhi, Parisa and Riviere, Jacques and Wang, Junpeng and Yu, Jiayi},
abstractNote = {This dataset contains experimental and acoustic data from shear reactivation tests that investigate the relationship between fluid-injection rate, pore pressure distribution, and seismic moment during laboratory fault slip. It includes raw mechanical data and acoustic emission recordings from fifteen experiments performed on 2.5-3 inch granitoid cores from the Utah FORGE enhanced geothermal systems (EGS) site. Each sample contains a single inclined fracture with small-scale surface roughness.
Experiments were conducted in an aluminum triaxial pressure vessel (TEMCO) equipped with three independently servo-controlled pumps using distilled water as the working fluid. The pumps regulated confining, upstream pore, and axial pressures, with each connected to a LabView interface to record applied pressures, cumulative injected volumes, and flow rates. The downstream outlet was closed to allow pressurization, monitored by an external pressure transducer. Axial displacement was measured by a linear variable differential transformer (LVDT) attached to the axial piston and converted to shear displacement along the fracture. Acoustic emissions were recorded using P-wave transducers, with event timing, amplitude, and cumulative amplitude compared against seismic moment and shear slip velocity.
Fluid injection rates of 0.05, 0.25, and 0.75 mL/min were applied under constant shear stress conditions, with both uniform and non-uniform along-fault pressure distributions. Samples were fully saturated with deionized water. Axial and confining stresses were increased to 3 MPa in 500 kPa increments, while pore pressure was held at 200 kPa prior to initiating shear mobilization. Axial stress was then increased to induce shear slip and subsequently reduced to approximately 60\%, 80\%, or 90\% of the peak shear stress, depending on the experiment. The raw mechanical data files include time-series measurements of confining, pore, and axial pressures; pump volumes and flow rates; time (in hours:minutes:seconds); axial displacement (in millimeters); and downstream pressure (in psi).
},
url = {https://gdr.openei.org/submissions/1775},
year = {2025},
howpublished = {Geothermal Data Repository, Pennsylvania State University, https://gdr.openei.org/submissions/1775},
note = {Accessed: 2026-05-04}
}
Details
Data from Sep 16, 2025
Last updated Oct 9, 2025
Submitted Sep 17, 2025
Organization
Pennsylvania State University
Contact
Matthew Roseboom
610.790.7402
Authors
Keywords
geothermal, energy, induced seismicity, EGS, geomechanics, Utah FORGE, granitoid, laboratory experiments, fault reactivation, shear slip, fluid injection, injection rate, pore pressure, pore pressure distribution, seismic moment, acoustic emissions, permeability, triaxial testing, shear stress, axial displacement, pressure vessel, mechinical data, time-series data, raw data, processed data, MATLABDOE Project Details
Project Name Utah FORGE
Project Lead Lauren Boyd
Project Number EE0007080

