Utah FORGE: Temperature-Dependent Fracture Seismicity from Fluid Injection Experiments
This dataset contains experimental data from fluid injection experiments conducted to investigate the influence of temperature on fracture seismicity. The experiments were performed on granite samples from Utah FORGE. The samples were prepared with a 30-degree inclined fracture and subjected to controlled stress and temperature conditions. Data were collected under three distinct temperature settings: 24 C, 78 C, and 137 C.
During the experiments, a constant confining pressure of 10 MPa and a constant shear stress at 80% of the shear strength of the sample were maintained. Pore pressure was incrementally increased at a rate of 300 kPa every three minutes to simulate fluid injection. Temperature was raised rapidly and then stabilized for the duration of each test. The dataset includes shear stress and displacement measurements under each temperature condition, along with supplementary figures illustrating the experimental setup and time-series plots of pressures and temperature.
Citation Formats
Pennsylvania State University. (2024). Utah FORGE: Temperature-Dependent Fracture Seismicity from Fluid Injection Experiments [data set]. Retrieved from https://dx.doi.org/10.15121/2483881.
Wang, Junpeng, Elsworth, Derek, and Eijsink, Agathe. Utah FORGE: Temperature-Dependent Fracture Seismicity from Fluid Injection Experiments. United States: N.p., 29 Feb, 2024. Web. doi: 10.15121/2483881.
Wang, Junpeng, Elsworth, Derek, & Eijsink, Agathe. Utah FORGE: Temperature-Dependent Fracture Seismicity from Fluid Injection Experiments. United States. https://dx.doi.org/10.15121/2483881
Wang, Junpeng, Elsworth, Derek, and Eijsink, Agathe. 2024. "Utah FORGE: Temperature-Dependent Fracture Seismicity from Fluid Injection Experiments". United States. https://dx.doi.org/10.15121/2483881. https://gdr.openei.org/submissions/1696.
@div{oedi_6450, title = {Utah FORGE: Temperature-Dependent Fracture Seismicity from Fluid Injection Experiments}, author = {Wang, Junpeng, Elsworth, Derek, and Eijsink, Agathe.}, abstractNote = {This dataset contains experimental data from fluid injection experiments conducted to investigate the influence of temperature on fracture seismicity. The experiments were performed on granite samples from Utah FORGE. The samples were prepared with a 30-degree inclined fracture and subjected to controlled stress and temperature conditions. Data were collected under three distinct temperature settings: 24 C, 78 C, and 137 C.
During the experiments, a constant confining pressure of 10 MPa and a constant shear stress at 80% of the shear strength of the sample were maintained. Pore pressure was incrementally increased at a rate of 300 kPa every three minutes to simulate fluid injection. Temperature was raised rapidly and then stabilized for the duration of each test. The dataset includes shear stress and displacement measurements under each temperature condition, along with supplementary figures illustrating the experimental setup and time-series plots of pressures and temperature. }, doi = {10.15121/2483881}, url = {https://gdr.openei.org/submissions/1696}, journal = {}, number = , volume = , place = {United States}, year = {2024}, month = {02}}
https://dx.doi.org/10.15121/2483881
Details
Data from Feb 29, 2024
Last updated Dec 27, 2024
Submitted Dec 11, 2024
Organization
Pennsylvania State University
Contact
Junpeng Wang
814.826.5497
Authors
Original Source
https://gdr.openei.org/submissions/1696Research Areas
Keywords
geothermal, energy, EGS, temperature, fracture seismicity, fluid injection, shear stress, displacement, pore pressure, experimental geomechanics, geomechanics, high temperature rock mechanics, raw data, seismicity, granite, Utah FORGE, fracture mechanics, stimulationDOE Project Details
Project Name Utah FORGE
Project Lead Lauren Boyd
Project Number EE0007080