| Name |
Format |
Description |
Link |
|
21 |
Stimulation data from Experiment 1 of EGS Collab, which occurred on the 4850 ft level of the Sanford Underground Research Facility (SURF). |
https://gdr.openei.org/submissions/1229 |
|
21 |
The Newberry Volcano EGS Demonstration in central Oregon, a 5 year project started in 2010, tests recent technological advances designed to reduce the cost of power generated by EGS in a hot, dry well (NWG 55-29) drilled in 2008. This submission includes all of the files and reports associated with the geophysical exploration, stimulation, and monitoring included in the scope of the project. |
https://gdr.openei.org/submissions/271 |
|
21 |
The Newberry Volcano EGS Demonstration in central Oregon, a 5 year project started in 2010, tests recent technological advances designed to reduce the cost of power generated by EGS in a hot, dry well (NWG 55-29) drilled in 2008. This submission includes all of the files and reports associated with the stimulation, pressure testing, and monitoring included in the scope of the project. |
https://gdr.openei.org/submissions/508 |
|
33 |
In this paper, we develop a hybrid machine learning (ML) model to visualize in situ permeability evolution for an intermediate-scale (~10 m) hydraulic stimulation experiment. This model includes an ML model that was trained using the well history of flow rate and wellhead pressure and MEQ (microearthquake) data from the first three stimulation episodes to predict average permeability from the statistical features of the MEQs alone for later episodes. Moreover, a physics-inspired model is integrated to estimate in situ fracture permeability spatially. This method relates fracture permeability to fracture dilation and scales dilation to the equivalent MEQ magnitude, according to laboratory observations. The seismic data are then applied to define incremental changes in permeability in both space and time. Our results confirm the excellent agreement between the ground truth and model- predicted permeability evolution. The resulting permeability map defines and quantifies flow paths in the reservoir with the averaged permeability comparing favorably with the ground truth of permeability. |
https://gdr.openei.org/files/1311/Induced%20microearthquakes%20predict%20permeability%20creation%20in%20the%20brittle%20crust.pdf |