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Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs

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Six samples were evaluated in unconfined and triaxial compression, their data are included in separate excel spreadsheets, and summarized in the word document. Three samples were plugged along the axis of the core (presumed to be nominally vertical) and three samples were plugged perpendicular to the axis of the core. A designation of "V"indicates vertical or the long axis of the plugged sample is aligned with the axis of the core. Similarly, "H" indicates a sample that is nominally horizontal and cut orthogonal to the axis of the core. Stress-strain curves were made before and after the testing, and are included in the word doc. The confining pressure for this test was 2800 psi. A series of tests are being carried out on to define a failure envelope, to provide representative hydraulic fracture design parameters and for future geomechanical assessments. The samples are from well 52-21, which reaches a maximum depth of 3581 ft +/- 2 ft into a gneiss complex.

Citation Formats

Energy and Geoscience Institute at the University of Utah. (2016). Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs [data set]. Retrieved from https://dx.doi.org/10.15121/1406605.
Export Citation to RIS
Moore, Joe. Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs. United States: N.p., 01 Mar, 2016. Web. doi: 10.15121/1406605.
Moore, Joe. Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs. United States. https://dx.doi.org/10.15121/1406605
Moore, Joe. 2016. "Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs". United States. https://dx.doi.org/10.15121/1406605. https://data.openei.org/submissions/3460.
@div{oedi_3460, title = {Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs}, author = {Moore, Joe.}, abstractNote = {Six samples were evaluated in unconfined and triaxial compression, their data are included in separate excel spreadsheets, and summarized in the word document. Three samples were plugged along the axis of the core (presumed to be nominally vertical) and three samples were plugged perpendicular to the axis of the core. A designation of "V"indicates vertical or the long axis of the plugged sample is aligned with the axis of the core. Similarly, "H" indicates a sample that is nominally horizontal and cut orthogonal to the axis of the core. Stress-strain curves were made before and after the testing, and are included in the word doc. The confining pressure for this test was 2800 psi. A series of tests are being carried out on to define a failure envelope, to provide representative hydraulic fracture design parameters and for future geomechanical assessments. The samples are from well 52-21, which reaches a maximum depth of 3581 ft +/- 2 ft into a gneiss complex. }, doi = {10.15121/1406605}, url = {https://data.openei.org/submissions/3460}, journal = {}, number = , volume = , place = {United States}, year = {2016}, month = {03}}
https://dx.doi.org/10.15121/1406605

Details

Data from Mar 1, 2016

Last updated Mar 16, 2020

Submitted Mar 25, 2016

Organization

Energy and Geoscience Institute at the University of Utah

Contact

Joe Moore

Authors

Joe Moore

Energy and Geoscience Institute at the University of Utah

DOE Project Details

Project Name Frontier Observatory for Research in Geothermal Energy: Milford, UT

Project Lead Lauren Boyd

Project Number EE0007080

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