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The objective of this field test is to validate several technologies for non-invasive well integrity assessment using existing wells with a known completion. The tests were made at the Cymric oil field, which is a steam flood operation. The wells therefore undergo similar downhol...
Wang, J. Lawrence Berkeley National Laboratory (2019)
Feb 21, 2019
The coaxial-cable experiment conducted in the lab was with 80 m coaxial cable( RG-85). This experiment compares the TDR response between damaged and undamaged cable. For the damaged cable, the damaged section is in the middle (40 m). The amplitude of the data is mV.
Wu, Y. and Wang, J. Lawrence Berkeley National Laboratory (2018)
Mar 15, 2018
This experiment is testing the tube waves reflected from the bottom of the well. We put six single-channel geophones on the surface and a 24-channel downhole hydrophone into the well. The well is about 30 meters deep. Just a steel casing in the sand formation, no cement.
Wu, Y. et al Lawrence Berkeley National Laboratory (2018)
Apr 25, 2018
Thermal profile data acquired using Silixa Ultima Distributed Temperature Sensor (DTS) at Cranfield, MS field test
Lawrence Berkeley National Laboratory (2015)
Jan 19, 2015
This archive contains an Excel spreadsheet with pressure and temperature logs from PacifiCorp well 71-10. This well is in the Blundell Power Plant geothermal well field near Roosevelt Hot Springs, Beaver County, Utah. The spreadsheet also contains UTM coordinates for the location ...
Foster, K. Energy and Geoscience Institute at the University of Utah (2018)
Oct 08, 2018
As part of the geophysical characterization suite for the first EGS Collab tesbed, here are the baseline cross-well seismic data and resultant models. The campaign seismic data have been organized, concatenated with geometry and compressional (P-) & and shear (S-) wave picks, and ...
Schwering, P. et al Lawrence Berkeley National Laboratory (2018)
Apr 30, 2018
This zipped data set includes Schlumberger FMI logs DLIS and XML files from Utah FORGE deep well 58-32. These include runs 1 (2226-7550 ft) and 2 (7440-7550 ft). Run 3 (7390-7527ft) was acquired during phase 2c.
Nash, G. and Moore, J. Energy and Geoscience Institute at the University of Utah (2017)
Nov 17, 2017
This is the set of earthquake catalogs developed for the Utah FORGE project. These are discussed in the "Utah FORGE Phase 2B Final Topical Report", which can be found on GDR under id: 1038 (See link 'Final Topical Report' in resources below). The details are in section: 'TASK 2B....
Pankow, K. Energy and Geoscience Institute at the University of Utah (2018)
Mar 21, 2018
These are data from soil CO2 flux surveys done in the Utah FORGE study area near Roosevelt Hot Springs.
Rahilly, K. Energy and Geoscience Institute at the University of Utah (2018)
Mar 12, 2018
This submission contains the following data associated with Utah FORGE Phase 2C within the Roosevelt Hot Springs geothermal area: - An ArcGIS shapefile with well locations for wells 58-32, 78-32, 68-32, OH-3, OH-4, WOW-2, and WOW-3. Well 58-32 is the deep test well, wells 68-32 a...
Abraham, S. et al Energy and Geoscience Institute at the University of Utah (2019)
Mar 26, 2019