Utah FORGE Hydrothermal Friction-Hydraulic Transmissivity Laboratory Experiments
Submission includes data from laboratory slide-hold-slide tests, combined with flow through tests, conducted on Westerly granite with 30 degree sawcut. Tests were conducted with a constant confining pressure of 30 MPa with an average pore pressure of 10 MPa at temperatures of 23 and 200 degC. Three fluid flow conditions were examined (1) no flow, (2) cycled flow, and (3) continuous flow. Data were collected to asses the effect of temperature and pore fluid on frictional healing rates in granite at geothermal conditions. Data is available in XML and JSON data types.
Citation Formats
U.S. Geological Survey. (2022). Utah FORGE Hydrothermal Friction-Hydraulic Transmissivity Laboratory Experiments [data set]. Retrieved from https://dx.doi.org/10.15121/1879674.
Jeppson, Tamara, Lockner, David. Utah FORGE Hydrothermal Friction-Hydraulic Transmissivity Laboratory Experiments. United States: N.p., 24 Feb, 2022. Web. doi: 10.15121/1879674.
Jeppson, Tamara, Lockner, David. Utah FORGE Hydrothermal Friction-Hydraulic Transmissivity Laboratory Experiments. United States. https://dx.doi.org/10.15121/1879674
Jeppson, Tamara, Lockner, David. 2022. "Utah FORGE Hydrothermal Friction-Hydraulic Transmissivity Laboratory Experiments". United States. https://dx.doi.org/10.15121/1879674. https://gdr.openei.org/submissions/1406.
@div{oedi_5761, title = {Utah FORGE Hydrothermal Friction-Hydraulic Transmissivity Laboratory Experiments}, author = {Jeppson, Tamara, Lockner, David.}, abstractNote = {Submission includes data from laboratory slide-hold-slide tests, combined with flow through tests, conducted on Westerly granite with 30 degree sawcut. Tests were conducted with a constant confining pressure of 30 MPa with an average pore pressure of 10 MPa at temperatures of 23 and 200 degC. Three fluid flow conditions were examined (1) no flow, (2) cycled flow, and (3) continuous flow. Data were collected to asses the effect of temperature and pore fluid on frictional healing rates in granite at geothermal conditions. Data is available in XML and JSON data types.}, doi = {10.15121/1879674}, url = {https://gdr.openei.org/submissions/1406}, journal = {}, number = , volume = , place = {United States}, year = {2022}, month = {02}}
https://dx.doi.org/10.15121/1879674
Details
Data from Feb 24, 2022
Last updated Aug 4, 2022
Submitted Aug 3, 2022
Organization
U.S. Geological Survey
Contact
Tamara Jeppson
Authors
Original Source
https://gdr.openei.org/submissions/1406Research Areas
Keywords
geothermal, experiment, test, failure, flow test, flow through, westerly granite, temperature, pressure, slide hold slide, tests, testing, hydraulic, friction, friction hydraulic transmissivity, lab, laboratory, Utah, FORGE, Utah FORGE, fluid flow, fluid flow conditionsDOE Project Details
Project Name Utah FORGE
Project Lead Lauren Boyd
Project Number EE0007080
