Utah FORGE: Well 16A(78)-32 Core-Flooding Experiment Results
This dataset contains core-flood experimental results from the Utah FORGE project, generated through laboratory tests at Lawrence Livermore National Laboratory. The experiments were conducted at temperatures of 100C and 200C using core samples from the 16A(78)-32 well. The primary objectives of these tests were to determine the change in calculated hydraulic fracture and permeability over time, under constant confining pressure, in predominantly constant flowrate conditions, while monitoring effluent chemistry as a function of time. The dataset includes measurements related to elapsed time, sample pH, elemental concentrations, and pressure conditions at different core depths. Additional data captures inlet and outlet pressures, pump flowrate, brine temperature, reactor pressure, and calculated hydraulic parameters.
Citation Formats
Lawrence Livermore National Laboratory. (2024). Utah FORGE: Well 16A(78)-32 Core-Flooding Experiment Results [data set]. Retrieved from https://gdr.openei.org/submissions/1722.
Smith, Megan, Davila Ordonez, Maria Gabriela, Kottkamp, Wayne, and Kroll-Whitesides, Kayla. Utah FORGE: Well 16A(78)-32 Core-Flooding Experiment Results. United States: N.p., 04 Apr, 2024. Web. https://gdr.openei.org/submissions/1722.
Smith, Megan, Davila Ordonez, Maria Gabriela, Kottkamp, Wayne, & Kroll-Whitesides, Kayla. Utah FORGE: Well 16A(78)-32 Core-Flooding Experiment Results. United States. https://gdr.openei.org/submissions/1722
Smith, Megan, Davila Ordonez, Maria Gabriela, Kottkamp, Wayne, and Kroll-Whitesides, Kayla. 2024. "Utah FORGE: Well 16A(78)-32 Core-Flooding Experiment Results". United States. https://gdr.openei.org/submissions/1722.
@div{oedi_1722, title = {Utah FORGE: Well 16A(78)-32 Core-Flooding Experiment Results}, author = {Smith, Megan, Davila Ordonez, Maria Gabriela, Kottkamp, Wayne, and Kroll-Whitesides, Kayla.}, abstractNote = {This dataset contains core-flood experimental results from the Utah FORGE project, generated through laboratory tests at Lawrence Livermore National Laboratory. The experiments were conducted at temperatures of 100C and 200C using core samples from the 16A(78)-32 well. The primary objectives of these tests were to determine the change in calculated hydraulic fracture and permeability over time, under constant confining pressure, in predominantly constant flowrate conditions, while monitoring effluent chemistry as a function of time. The dataset includes measurements related to elapsed time, sample pH, elemental concentrations, and pressure conditions at different core depths. Additional data captures inlet and outlet pressures, pump flowrate, brine temperature, reactor pressure, and calculated hydraulic parameters. }, doi = {}, url = {https://gdr.openei.org/submissions/1722}, journal = {}, number = , volume = , place = {United States}, year = {2024}, month = {04}}
Details
Data from Apr 4, 2024
Last updated Mar 13, 2025
Submitted Mar 12, 2025
Organization
Lawrence Livermore National Laboratory
Contact
Megan M. Smith
925.423.7970
Authors
Keywords
geothermal, energy, coreflood, Utah FORGE, core testing, geochemistry, permeability, EGS, core-flood experiment, hydraulic fracture, confining pressure, effluent chemistry, brine chemistry, pressure measurements, flowrate, core sample, 16A78-32, fluids, pH, temperature, fracture evolution, concentration, Processed dataDOE Project Details
Project Name Utah FORGE
Project Lead Lauren Boyd
Project Number EE0007080
