Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs
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
TY - DATA
AB - 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.
AU - Moore, Joe
DB - Open Energy Data Initiative (OEDI)
DP - Open EI | National Renewable Energy Laboratory
DO - 10.15121/1406605
KW - geothermal
KW - triaxial
KW - testing
KW - egi
KW - forge
KW - egs
KW - fracture
KW - stress
KW - compression
KW - permeability
KW - utah
KW - milford
KW - test
KW - horizontal
KW - Moore
KW - GNS
KW - sample
KW - data
KW - vertical
KW - geomechanics
KW - geomechanical
KW - Utah FORGE
KW - core
KW - strain
KW - core data
KW - resource
KW - characterization
KW - well data
KW - Roosevelt Hot Springs
KW - 52-21
LA - English
DA - 2016/03/01
PY - 2016
PB - Energy and Geoscience Institute at the University of Utah
T1 - Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs
UR - https://doi.org/10.15121/1406605
ER -
Moore, Joe. Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs. Energy and Geoscience Institute at the University of Utah, 1 March, 2016, GDR. https://doi.org/10.15121/1406605.
Moore, J. (2016). Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs. [Data set]. GDR. Energy and Geoscience Institute at the University of Utah. https://doi.org/10.15121/1406605
Moore, Joe. Utah FORGE: Milford Triaxial Test Data and Summary from EGI labs. Energy and Geoscience Institute at the University of Utah, March, 1, 2016. Distributed by GDR. https://doi.org/10.15121/1406605
@misc{OEDI_Dataset_6951,
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. },
url = {https://gdr.openei.org/submissions/732},
year = {2016},
howpublished = {GDR, Energy and Geoscience Institute at the University of Utah, https://doi.org/10.15121/1406605},
note = {Accessed: 2025-05-28},
doi = {10.15121/1406605}
}
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
Original Source
https://gdr.openei.org/submissions/732Research Areas
Keywords
geothermal, triaxial, testing, egi, forge, egs, fracture, stress, compression, permeability, utah, milford, test, horizontal, Moore, GNS, sample, data, vertical, geomechanics, geomechanical, Utah FORGE, core, strain, core data, resource, characterization, well data, Roosevelt Hot Springs, 52-21DOE Project Details
Project Name Frontier Observatory for Research in Geothermal Energy: Milford, UT
Project Lead Lauren Boyd
Project Number EE0007080
