Utah FORGE: GIS Well Temperature Data

Gwynn, Mark; Hill, Jay; Allis, Rick

doi:10.15121/1452744

Title: Utah FORGE: GIS Well Temperature Data

Dataset
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Abstract

This is a GIS point feature shapefile representing wells, and their temperatures, that are located in the general Utah FORGE area near Milford, Utah. There are also fields that represent interpolated temperature values at depths of 200 m, 1000 m, 2000 m, 3000 m, and 4000 m. in degrees Fahrenheit. The temperature values at specific depths as mentioned above were derived as follows. In cases where the well reached a given depth (200 m and 1, 2, 3, or 4 km), the temperature is the measured temperature. For the shallower wells (and at deeper depths in the wells reaching one or more of the target depths), temperatures were extrapolated from the temperature-depth profiles that appeared to have stable (re-equilibrated after drilling) and linear profiles within the conductive regime (i.e. below the water table or other convective influences such as shallow hydrothermal outflow from the Roosevelt Hydrothermal System). Measured temperatures/gradients from deeper wells (when available and reasonably close to a given well) were used to help constrain the extrapolation to greater depths. Most of the field names in the attribute table are intuitive, however HF = heat flow, intercept = the temperature at the surface (x-axis of the temperature-depth plots) basedmore »« less

Authors:: Gwynn, Mark; Hill, Jay; Allis, Rick

Publication Date:: Wed Feb 28 00:00:00 EST 2018

Other Number(s):: 1012

DOE Contract Number:: EE0007080

Research Org.:: USDOE Geothermal Data Repository (United States); Energy and Geoscience Institute at the University of Utah

Sponsoring Org.:: USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Program (EE-2C)

Collaborations:: Energy and Geoscience Institute at the University of Utah

Subject:: 15 Geothermal Energy

Keywords:: geothermal; energy; Utah FORGE; Roosevelt Hot Springs; FORGE; Well Temperatures; heat flow; geospatial data; GIS data; shapefile; Utah FORGE well temperatures; ArcGIS; Utah; temperature; well data; resource; characterization; Milford; interpolated; processed data; EGS

Geolocation:: 38.535085801141,-112.83408584595|38.402856824972,-112.83408584595|38.402856824972,-112.97110061646|38.535085801141,-112.97110061646|38.535085801141,-112.83408584595

OSTI Identifier:: 1452744

DOI:: https://doi.org/10.15121/1452744

Project Location:

Citation Formats


                    Gwynn, Mark, Hill, Jay, and Allis, Rick. Utah FORGE: GIS Well Temperature Data.  United States: N. p., 2018. 
        Web.  doi:10.15121/1452744.

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                    Gwynn, Mark, Hill, Jay, & Allis, Rick. Utah FORGE: GIS Well Temperature Data.  United States.  doi:https://doi.org/10.15121/1452744

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                    Gwynn, Mark, Hill, Jay, and Allis, Rick. 2018.  
"Utah FORGE: GIS Well Temperature Data".  United States.  doi:https://doi.org/10.15121/1452744.  https://www.osti.gov/servlets/purl/1452744. Pub date:Wed Feb 28 00:00:00 EST 2018

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@article{osti_1452744,

  title        = {Utah FORGE: GIS Well Temperature Data},

  author       = {Gwynn, Mark and Hill, Jay and Allis, Rick},

  abstractNote = {This is a GIS point feature shapefile representing wells, and their temperatures, that are located in the general Utah FORGE area near Milford, Utah. There are also fields that represent interpolated temperature values at depths of 200 m, 1000 m, 2000 m, 3000 m, and 4000 m. in degrees Fahrenheit. The temperature values at specific depths as mentioned above were derived as follows. In cases where the well reached a given depth (200 m and 1, 2, 3, or 4 km), the temperature is the measured temperature. For the shallower wells (and at deeper depths in the wells reaching one or more of the target depths), temperatures were extrapolated from the temperature-depth profiles that appeared to have stable (re-equilibrated after drilling) and linear profiles within the conductive regime (i.e. below the water table or other convective influences such as shallow hydrothermal outflow from the Roosevelt Hydrothermal System). Measured temperatures/gradients from deeper wells (when available and reasonably close to a given well) were used to help constrain the extrapolation to greater depths. Most of the field names in the attribute table are intuitive, however HF = heat flow, intercept = the temperature at the surface (x-axis of the temperature-depth plots) based on the linear segment of the plot that was used to extrapolate the temperature profiles to greater depths, and depth_m is the total well depth. This information is also present in the shapefile metadata.},

  doi          = {10.15121/1452744},

  journal      = {},

  number       = ,

  volume       = ,

  place        = {United States},

  year         = {Wed Feb 28 00:00:00 EST 2018},

  month        = {Wed Feb 28 00:00:00 EST 2018}

}

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DOI: https://doi.org/10.15121/1452744

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