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DCIF Westerly Granite AE Stress Effect Test (Task 3-1)

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Directional Cooling-Induced Fracturing (DCIF) experiments were conducted on rectangular Westerly granite blocks (width=depth=4.0", height=2.0"). Liquid nitrogen was poured in a small, 1"-diameter copper cup attached to the top of the sample, and the resulting acoustic emissions (AEs) and temperature changes on the surface of the sample were monitored. Several confining stresses were applied bi-axially to the sides of the samples so that the onset of AE activity and the stress applied to the sample were correlated. The obtained AEs were used to determine the microcracking source locations and amplitude, and the associated moment tensors. Included in this submission are the animations of the AE locations and graphics displaying the measured temperature-AE activity changes for different stresses.

Citation Formats

Lawrence Berkeley National Laboratory. (2021). DCIF Westerly Granite AE Stress Effect Test (Task 3-1) [data set]. Retrieved from https://dx.doi.org/10.15121/1829305.
Export Citation to RIS
Nakagawa, Seiji, Trzeciak, Maciej. DCIF Westerly Granite AE Stress Effect Test (Task 3-1). United States: N.p., 08 Jul, 2021. Web. doi: 10.15121/1829305.
Nakagawa, Seiji, Trzeciak, Maciej. DCIF Westerly Granite AE Stress Effect Test (Task 3-1). United States. https://dx.doi.org/10.15121/1829305
Nakagawa, Seiji, Trzeciak, Maciej. 2021. "DCIF Westerly Granite AE Stress Effect Test (Task 3-1)". United States. https://dx.doi.org/10.15121/1829305. https://gdr.openei.org/submissions/1343.
@div{oedi_4550, title = {DCIF Westerly Granite AE Stress Effect Test (Task 3-1)}, author = {Nakagawa, Seiji, Trzeciak, Maciej.}, abstractNote = {Directional Cooling-Induced Fracturing (DCIF) experiments were conducted on rectangular Westerly granite blocks (width=depth=4.0", height=2.0"). Liquid nitrogen was poured in a small, 1"-diameter copper cup attached to the top of the sample, and the resulting acoustic emissions (AEs) and temperature changes on the surface of the sample were monitored. Several confining stresses were applied bi-axially to the sides of the samples so that the onset of AE activity and the stress applied to the sample were correlated. The obtained AEs were used to determine the microcracking source locations and amplitude, and the associated moment tensors. Included in this submission are the animations of the AE locations and graphics displaying the measured temperature-AE activity changes for different stresses. }, doi = {10.15121/1829305}, url = {https://gdr.openei.org/submissions/1343}, journal = {}, number = , volume = , place = {United States}, year = {2021}, month = {07}}
https://dx.doi.org/10.15121/1829305

Details

Data from Jul 8, 2021

Last updated Nov 8, 2021

Submitted Oct 21, 2021

Organization

Lawrence Berkeley National Laboratory

Contact

Seiji Nakagawa

510.486.7894

Authors

Seiji Nakagawa

Lawrence Berkeley National Laboratory

Maciej Trzeciak

Department of Geoscience - University of Wisconsin-Madison

Research Areas

DOE Project Details

Project Name DEVELOPMENT OF A DIRECTIONAL COOLING INDUCED FRACTURING (DCIF) TECHNOLOGY FOR NEAR-WELLBORE STRESS ESTIMATION IN GEOTHERMAL RESERVOIRS

Project Lead Zachary Frone

Project Number EE0009033

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