Tuesday, October 2, 2018 5:06 pm

This submission includes meteorological data recorded by National Weather Service at University of Illinois Willard Airport, Savoy IL for period 1972 to 2018. This data is for use in parameterizing the demand and life-cycle assessments associated with the project, and provides information about energy loads for the buildings being included in the DDU applications. This includes how energy demand fluctuates with seasonal changes in climate, which is used to model expected demand for the DDU system.

*Note: All times are reported in local standard time.
NC: Wind Chill/Heat Index do not meet the required thresholds to be calculated.
cli-MATE: MRCC Application Tools Environment
Generated at: 2/7/2018 8:52:33 AM CST
m = missing data
Date = year-month-day
Time = 24 hour clock
Temp_F = temperature (deg. fahrenheit)
RH_pct = relative humidity (percent)
Dewpt_F = dew point (deg. fahrenheit)
WindSpeed_mph = wind speed (miles/hour)
WindDir_deg = wind direction (deg. from north)
PeakWindGust_mph = peak wind gust (miles/hour)
Visibility_mi = visibility (miles)
AtmPress_hPa = atmospheric pressure (hectopascals)
Precip_in = precipitation (inches) Excel File with meteorological data recorded by National Weather Service at University of Illinois — Willard Airport for period 1972 to 2018.

Media file
Tuesday, October 2, 2018 5:06 pm

This submission includes 3-D geocellular model files with formation top and formation thickness data for the St. Peter and Mt. Simon Sandstones in University of Illinois Deep Direct-Use project area. An input parameters file is also included for the St. Peter Sandstone. Elevation (m) of the top of St. Peter Sandstone in University of Illinois DDU project area.

Media file
Tuesday, October 2, 2018 5:06 pm

This submission includes 3-D geocellular model files with formation top and formation thickness data for the St. Peter and Mt. Simon Sandstones in University of Illinois Deep Direct-Use project area. An input parameters file is also included for the St. Peter Sandstone. Input parameters for the St. Peter Sandstone in the geocellular model.

Media file
Tuesday, October 2, 2018 5:06 pm

This is a zipped archive containing an ArcGIS shapefile and a text file containing gravity data covering the Cove Fort and Dog Valley areas in central Utah. Part of the data was acquired by the Utah Geological Survey and part came from PACES (University of Texas El Paso). The attribute fields in the datasets are included in the README file below.

*A 2.67 g/cm^3 reduction density was used for the Bouguer correction. This is a zipped archive containing an ArcGIS shapefile and a text file containing gravity data covering the Cove Fort and Dog Valley areas in central Utah.

Media file
Tuesday, October 2, 2018 5:06 pm

This submission includes 3-D geocellular model files with formation top and formation thickness data for the St. Peter and Mt. Simon Sandstones in University of Illinois Deep Direct-Use project area. An input parameters file is also included for the St. Peter Sandstone. Thickness of St. Peter Sandstone in model area.

Media file
Tuesday, October 2, 2018 5:06 pm

This submission includes 3-D geocellular model files with formation top and formation thickness data for the St. Peter and Mt. Simon Sandstones in University of Illinois Deep Direct-Use project area. An input parameters file is also included for the St. Peter Sandstone. Thickness of Mt. Simon Sandstone in model area.

Media file
Tuesday, October 2, 2018 5:06 pm

This submission includes meteorological data recorded by National Weather Service at University of Illinois Willard Airport, Savoy IL for period 1972 to 2018. This data is for use in parameterizing the demand and life-cycle assessments associated with the project, and provides information about energy loads for the buildings being included in the DDU applications. This includes how energy demand fluctuates with seasonal changes in climate, which is used to model expected demand for the DDU system.

*Note: All times are reported in local standard time.
NC: Wind Chill/Heat Index do not meet the required thresholds to be calculated.
cli-MATE: MRCC Application Tools Environment
Generated at: 2/7/2018 8:52:33 AM CST
m = missing data
Date = year-month-day
Time = 24 hour clock
Temp_F = temperature (deg. fahrenheit)
RH_pct = relative humidity (percent)
Dewpt_F = dew point (deg. fahrenheit)
WindSpeed_mph = wind speed (miles/hour)
WindDir_deg = wind direction (deg. from north)
PeakWindGust_mph = peak wind gust (miles/hour)
Visibility_mi = visibility (miles)
AtmPress_hPa = atmospheric pressure (hectopascals)
Precip_in = precipitation (inches) Microsoft Access database file with meteorological data recorded by National Weather Service at University of Illinois — Willard Airport for period 1972 to 2018.

Media file
Tuesday, October 2, 2018 5:06 pm

This submission contains 167 deviatoric moment tensor (MT) solutions for the seismicity observed two years prior and three years post start of injection activities at The Geysers Prati 32 EGS Demonstration. Also included is a statistical representation of the properties of 751 fractures derived from the analysis of seismicity observed two years prior and three years post start of injection activities at The Geysers Prati 32 EGS Demonstration Project. The locations of the fractures are taken from microseismic hypocenters, the fracture areas are derived from moment magnitudes via scaling relationships, and the azimuths (sigma 1) and dips (sigma 3) are derived from the results of stress analyses. This file contains 167 deviatoric moment tensor (MT) solutions for the seismicity observed two years prior and three years post start of injection activities.

Media file
Tuesday, October 2, 2018 5:06 pm

This is the final report for the second phase of geological, geophysical, and geochemical data collection and processing for the Eastern Great Basin Geothermal Play Fairway Analysis project. This is the Phase 2 final report for the Eastern Great Basin Geothermal Play Fairway Analysis project.

Media file
Tuesday, September 11, 2018 2:28 pm

The site characterization data used to develop the conceptual geologic model for the Snake River Plain site in Idaho, as part of phase 1 of the Frontier Observatory for Research in Geothermal Energy (FORGE) initiative. This collection includes data on seismic events, groundwater, geomechanical models, gravity surveys, magnetics, resistivity, magnetotellurics (MT), rock physics, stress, the geologic setting, and supporting documentation, including several papers. Also included are 3D models (Petrel and Jewelsuite) of the proposed site.

Data for wells INEL-1, WO-2, and USGS-142 have been included as links to separate data collections.

These data have been assembled by the Snake River Geothermal Consortium (SRGC), a team of collaborators that includes members from national laboratories, universities, industry, and federal agencies, lead by the Idaho National Laboratory (INL). Other contributors include the National Renewable Energy Laboratory (NREL), Lawrence Livermore National Laboratory (LLNL), the Center for Advanced Energy Studies (CEAS), the University of Idaho, Idaho State University, Boise State University, University of Wyoming, University of Oklahoma, Energy and Geoscience Institute-University of Utah, US Geothermal, Baker Hughes

Campbell Scientific Inc., Chena Power, US Geological Survey (USGS), Idaho Department of Water Resources, Idaho Geological Survey, and Mink GeoHydro. Dobson et al, 2015. "He Isotopic Evidence for Undiscovered Geothermal Systems in the Snake River Plain." from the 40th Stanford Geothermal Workshop.

Media file
Tuesday, September 11, 2018 2:28 pm

The site characterization data used to develop the conceptual geologic model for the Snake River Plain site in Idaho, as part of phase 1 of the Frontier Observatory for Research in Geothermal Energy (FORGE) initiative. This collection includes data on seismic events, groundwater, geomechanical models, gravity surveys, magnetics, resistivity, magnetotellurics (MT), rock physics, stress, the geologic setting, and supporting documentation, including several papers. Also included are 3D models (Petrel and Jewelsuite) of the proposed site.

Data for wells INEL-1, WO-2, and USGS-142 have been included as links to separate data collections.

These data have been assembled by the Snake River Geothermal Consortium (SRGC), a team of collaborators that includes members from national laboratories, universities, industry, and federal agencies, lead by the Idaho National Laboratory (INL). Other contributors include the National Renewable Energy Laboratory (NREL), Lawrence Livermore National Laboratory (LLNL), the Center for Advanced Energy Studies (CEAS), the University of Idaho, Idaho State University, Boise State University, University of Wyoming, University of Oklahoma, Energy and Geoscience Institute-University of Utah, US Geothermal, Baker Hughes

Campbell Scientific Inc., Chena Power, US Geological Survey (USGS), Idaho Department of Water Resources, Idaho Geological Survey, and Mink GeoHydro. Smith et al, 1996. "Paleoseismology and seismic hazards evaluations in extensional volcanic terrains." Extensional structures in volcanic terrains are the surface expression of shallow dike intrusion and can be misinterpreted as structures associated with major tectonic faults...

Media file
Tuesday, September 11, 2018 2:27 pm

The site characterization data used to develop the conceptual geologic model for the Snake River Plain site in Idaho, as part of phase 1 of the Frontier Observatory for Research in Geothermal Energy (FORGE) initiative. This collection includes data on seismic events, groundwater, geomechanical models, gravity surveys, magnetics, resistivity, magnetotellurics (MT), rock physics, stress, the geologic setting, and supporting documentation, including several papers. Also included are 3D models (Petrel and Jewelsuite) of the proposed site.

Data for wells INEL-1, WO-2, and USGS-142 have been included as links to separate data collections.

These data have been assembled by the Snake River Geothermal Consortium (SRGC), a team of collaborators that includes members from national laboratories, universities, industry, and federal agencies, lead by the Idaho National Laboratory (INL). Other contributors include the National Renewable Energy Laboratory (NREL), Lawrence Livermore National Laboratory (LLNL), the Center for Advanced Energy Studies (CEAS), the University of Idaho, Idaho State University, Boise State University, University of Wyoming, University of Oklahoma, Energy and Geoscience Institute-University of Utah, US Geothermal, Baker Hughes

Campbell Scientific Inc., Chena Power, US Geological Survey (USGS), Idaho Department of Water Resources, Idaho Geological Survey, and Mink GeoHydro. 2010 annual report detailing seismic events in the Snake River Plain and within a 100 mile radius of the Idaho National Lab (Intended to supplement the broken link associated with "INL Seismic Monitoring 2010 Annual Report - UNAVAILABLE")

Media file
Tuesday, September 11, 2018 2:27 pm

The site characterization data used to develop the conceptual geologic model for the Snake River Plain site in Idaho, as part of phase 1 of the Frontier Observatory for Research in Geothermal Energy (FORGE) initiative. This collection includes data on seismic events, groundwater, geomechanical models, gravity surveys, magnetics, resistivity, magnetotellurics (MT), rock physics, stress, the geologic setting, and supporting documentation, including several papers. Also included are 3D models (Petrel and Jewelsuite) of the proposed site.

Data for wells INEL-1, WO-2, and USGS-142 have been included as links to separate data collections.

These data have been assembled by the Snake River Geothermal Consortium (SRGC), a team of collaborators that includes members from national laboratories, universities, industry, and federal agencies, lead by the Idaho National Laboratory (INL). Other contributors include the National Renewable Energy Laboratory (NREL), Lawrence Livermore National Laboratory (LLNL), the Center for Advanced Energy Studies (CEAS), the University of Idaho, Idaho State University, Boise State University, University of Wyoming, University of Oklahoma, Energy and Geoscience Institute-University of Utah, US Geothermal, Baker Hughes

Campbell Scientific Inc., Chena Power, US Geological Survey (USGS), Idaho Department of Water Resources, Idaho Geological Survey, and Mink GeoHydro. Nadine McQuarrie and David Rogers, 1998. "Subsidence of a volcanic basin by flexure and crustal flow: The eastern Snake River Plain, Idaho."

Media file
Tuesday, September 11, 2018 2:27 pm

The site characterization data used to develop the conceptual geologic model for the Snake River Plain site in Idaho, as part of phase 1 of the Frontier Observatory for Research in Geothermal Energy (FORGE) initiative. This collection includes data on seismic events, groundwater, geomechanical models, gravity surveys, magnetics, resistivity, magnetotellurics (MT), rock physics, stress, the geologic setting, and supporting documentation, including several papers. Also included are 3D models (Petrel and Jewelsuite) of the proposed site.

Data for wells INEL-1, WO-2, and USGS-142 have been included as links to separate data collections.

These data have been assembled by the Snake River Geothermal Consortium (SRGC), a team of collaborators that includes members from national laboratories, universities, industry, and federal agencies, lead by the Idaho National Laboratory (INL). Other contributors include the National Renewable Energy Laboratory (NREL), Lawrence Livermore National Laboratory (LLNL), the Center for Advanced Energy Studies (CEAS), the University of Idaho, Idaho State University, Boise State University, University of Wyoming, University of Oklahoma, Energy and Geoscience Institute-University of Utah, US Geothermal, Baker Hughes

Campbell Scientific Inc., Chena Power, US Geological Survey (USGS), Idaho Department of Water Resources, Idaho Geological Survey, and Mink GeoHydro. 3D model of the INL site. Model 2 shows the same system of calderas shifted to the south, beyond the boundaries of the GRRA. Here we assume that the boundary between volcanics and Paleozoic rocks is defined by a flexural surface that was formed in response to the emplacement of a dense mid-crustal sill beneath the ESRP. This model is supported by the attitudes of ancient fold hinges within the mountains north of the plain. Fold hinges near the boundary of the plain plunge towards the plain at around 30 degrees. North of the plain, the plunge angles decrease in a more or less uniform manner. Thus, in this model, the base of the volcanic system is defined by a planar feature dipping 30 degrees to the south.

Media file
Tuesday, September 11, 2018 2:27 pm

The site characterization data used to develop the conceptual geologic model for the Snake River Plain site in Idaho, as part of phase 1 of the Frontier Observatory for Research in Geothermal Energy (FORGE) initiative. This collection includes data on seismic events, groundwater, geomechanical models, gravity surveys, magnetics, resistivity, magnetotellurics (MT), rock physics, stress, the geologic setting, and supporting documentation, including several papers. Also included are 3D models (Petrel and Jewelsuite) of the proposed site.

Data for wells INEL-1, WO-2, and USGS-142 have been included as links to separate data collections.

These data have been assembled by the Snake River Geothermal Consortium (SRGC), a team of collaborators that includes members from national laboratories, universities, industry, and federal agencies, lead by the Idaho National Laboratory (INL). Other contributors include the National Renewable Energy Laboratory (NREL), Lawrence Livermore National Laboratory (LLNL), the Center for Advanced Energy Studies (CEAS), the University of Idaho, Idaho State University, Boise State University, University of Wyoming, University of Oklahoma, Energy and Geoscience Institute-University of Utah, US Geothermal, Baker Hughes

Campbell Scientific Inc., Chena Power, US Geological Survey (USGS), Idaho Department of Water Resources, Idaho Geological Survey, and Mink GeoHydro. William Leeman, Derek Schutt, and Scott Hughes, 2009. "Thermal structure beneath the Snake River Plain: Implications for the Yellowstone hotspot."

Media file

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