Utah FORGE: Fluid Injection-Rate Controls on Seismic Moment from Laboratory Fault Reactivation Experiments

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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 -
Export Citation to RIS
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

Derek Elsworth

Pennsylvania State University

Agathe Eijsink

Pennsylvania State University

Chris Marone

Pennsylvania State University

Parisa Shokouhi

Pennsylvania State University

Jacques Riviere

Pennsylvania State University

Junpeng Wang

Pennsylvania State University

Jiayi Yu

Pennsylvania State University

DOE Project Details

Project Name Utah FORGE

Project Lead Lauren Boyd

Project Number EE0007080

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