Validation of Play Fairway Analysis of the geothermal potential of Camas Prairie, south-central Idaho, by an exploration well

Lachmar, Thomas E.; Neupane, Ghanashyam; Garg, Sabodh K.; Dobson, Patrick F.; Smith, Connor J.; Newell, Dennis L.; Shervais, John W.; Evans, James P.; Mink, Leland L.

doi:10.1186/s40517-023-00264-4

Validation of Play Fairway Analysis of the geothermal potential of Camas Prairie, south-central Idaho, by an exploration well

Journal Article · Fri Aug 04 00:00:00 EDT 2023 · Geothermal Energy

DOI:https://doi.org/10.1186/s40517-023-00264-4· OSTI ID:1993886

; Neupane, Ghanashyam; Garg, Sabodh K.; Dobson, Patrick F.; Smith, Connor J.; Newell, Dennis L.; Shervais, John W.; Evans, James P.; Mink, Leland L.

Abstract

Play Fairway Analysis (PFA) methodology was adapted for geothermal exploration at Camas Prairie, Idaho. Geophysical data, structural and geologic mapping, volcanic rock ages and vent locations, and the distribution of thermal springs and wells all indicated a relatively high geothermal potential along the southern margin of the Prairie. An exploration well (USU Camas-1) was drilled to a depth of 618.3 m to validate the PFA. A permeable zone was encountered at ~ 357.5 m with a maximum measured temperature of ~ 80 °C, which was suppressed following the injection of cold water. A moderate transmissivity of ~ 0.25–1 cm ² /s estimated from an injection test as well a seasonal artesian flow at ~ 0.7 L/s corroborate the presence of a permeable zone. The existence of a lacustrine clay seal was confirmed near the bottom of the basin-fill sediment occupying the upper 314 m of the well. Geothermometers suggest the USU Camas-1 well water equilibrated at a reservoir temperature of ~ 120 °C. Based on the locations of both thermal and cold wells, geothermal fluids appear to be flowing upward along one or both of two fault systems. The presence of young basalts and elevated helium isotope ratios suggest that the heat source of Camas Prairie is magmatic. However, the faults may be acting as a conduit for geothermal fluids to rise from great depth without a shallow magmatic source being present. Camas Prairie is a promising area for geothermal development, but the relatively low reservoir temperatures indicate this resource may not be suitable for electric generation. Perhaps the best use would be for heating.

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Sponsoring Organization:: USDOE

OSTI ID:: 1993886

Journal Information:: Geothermal Energy, Journal Name: Geothermal Energy Journal Issue: 1 Vol. 11; ISSN 2195-9706

Publisher:: Springer Science + Business MediaCopyright Statement

Country of Publication:: Germany

Language:: English

References (19)

Continuous flow2H/1H and18O/16O analysis of water samples with dual inlet precision Gehre, M.; Geilmann, H.; Richter, J. Rapid Communications in Mass Spectrometry, Vol. 18, Issue 22 https://doi.org/10.1002/rcm.1672	journal	January 2004
An empirical NaKCa geothermometer for natural waters Fournier, R. O.; Truesdell, A. H. Geochimica et Cosmochimica Acta, Vol. 37, Issue 5 https://doi.org/10.1016/0016-7037(73)90060-4	journal	May 1973
Magnesium correction to the NaKCa chemical geothermometer Fournier, R. O.; Potter, R. W. Geochimica et Cosmochimica Acta, Vol. 43, Issue 9 https://doi.org/10.1016/0016-7037(79)90147-9	journal	September 1979
Geothermal solute equilibria. Derivation of Na-K-Mg-Ca geoindicators Giggenbach, Werner F. Geochimica et Cosmochimica Acta, Vol. 52, Issue 12 https://doi.org/10.1016/0016-7037(88)90143-3	journal	December 1988
Regional implications of heat flow of the Snake River Plain, Northwestern United States Blackwell, D. D. Tectonophysics, Vol. 164, Issue 2-4 https://doi.org/10.1016/0040-1951(89)90025-5	journal	August 1989
Chemical geothermometers and mixing models for geothermal systems Fournier, R. O. Geothermics, Vol. 5, Issue 1-4 https://doi.org/10.1016/0375-6505(77)90007-4	journal	January 1977
The Yellowstone hotspot Smith, Robert B.; Braile, Lawrence W. Journal of Volcanology and Geothermal Research, Vol. 61, Issue 3-4 https://doi.org/10.1016/0377-0273(94)90002-7	journal	July 1994
Comparison of circulation times of thermal waters discharging from the Idaho batholith based on geothermometer temperatures, helium concentrations, and 14C measurements Mariner, Robert H.; Evans, William C.; Young, H. William Geothermics, Vol. 35, Issue 1 https://doi.org/10.1016/j.geothermics.2005.08.002	journal	February 2006
Geodynamics of the Yellowstone hotspot and mantle plume: Seismic and GPS imaging, kinematics, and mantle flow Smith, Robert B.; Jordan, Michael; Steinberger, Bernhard Journal of Volcanology and Geothermal Research, Vol. 188, Issue 1-3 https://doi.org/10.1016/j.jvolgeores.2009.08.020	journal	November 2009
A graphic procedure in the geochemical interpretation of water-analyses Piper, Arthur M. Transactions, American Geophysical Union, Vol. 25, Issue 6 https://doi.org/10.1029/TR025i006p00914	journal	January 1944
Isotopic Evolution of the Idaho Batholith and Challis Intrusive Province, Northern US Cordillera Gaschnig, Richard M.; Vervoort, Jeffrey D.; Lewis, Reed S. Journal of Petrology, Vol. 52, Issue 12 https://doi.org/10.1093/petrology/egr050	journal	November 2011
Isotopic Variations in Meteoric Waters Craig, H. Science, Vol. 133, Issue 3465 https://doi.org/10.1126/science.133.3465.1702	journal	May 1961
Geothermal play Fairway Analysis of the Snake River Plain, Idaho Shervais, John W.; Glen, Jonathan; Nielson, Dennis GSA Annual Meeting in Seattle, Washington, USA - 2017, Geological Society of America Abstracts with Programs https://doi.org/10.1130/abs/2017AM-305209	conference	January 2017
Play Fairway Analysis in Geothermal Exploration: case Study in Snake River Plain Volcanic Province Shervais, John W.; Glen, Jonathan Geological Society of America Abstracts with Programs https://doi.org/10.1130/abs/2019AM-335425	conference	January 2019
Evaluation of the Geothermal Potential of the Camas Prairie, South-Central Idaho Smith, Connor; Lachmar, Thomas Geological Society of America Abstracts with Programs https://doi.org/10.1130/abs/2021AM-365166	conference	January 2021
Effect of an 860-m thick, cold, freshwater aquifer on geothermal potential along the axis of the eastern Snake River Plain, Idaho Lachmar, Thomas E.; Freeman, Thomas G.; Sant, Christopher J. Geothermal Energy, Vol. 5, Issue 1 https://doi.org/10.1186/s40517-017-0086-8	journal	December 2017
Evaluation of the geothermal potential of the western Snake River Plain based on a deep corehole on the Mountain Home AFB near Mountain Home, Idaho Lachmar, Thomas E.; Freeman, Thomas G.; Kessler, James A. Geothermal Energy, Vol. 7, Issue 1 https://doi.org/10.1186/s40517-019-0142-7	journal	September 2019
Snake River Plain Play Fairway Analysis Phase 1 Favorability Model (DE EE0006733) DeAngelo, Jacob; Shervais, John W.; Glen, Jonathan M. U.S. Geological Survey https://doi.org/10.5066/P95EULTI	dataset	January 2021
Snake River Plain Play Fairway Analysis Phase 2 Favorability Model (DE EE0006733) DeAngelo, Jacob; Shervais, John W.; Glen, Jonathan M. U.S. Geological Survey https://doi.org/10.5066/P9Y8MEZY	dataset	January 2021

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