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University of Illinois Campus Deep Direct-Use Feasibility Study - Subsurface Temperature Profile
High resolution fiber-optic distributed temperature sensing logs from the Illinois Basin Decatur Project (IBDP) in Decatur, IL were used to model the thermal profile in the Illinois Basin.
Resources
5 resources available
-
Basin Scale Modeling for CO2 Sequestration in the Basal Sandstone Reservoir
317 -
Groundwater Discharge in the Illinois Basin as Suggested by Temperature Anomalies
HTML -
Deep Well Monitoring and Veritification at the Illinois Basin Decatur Project
3366031 -
Bottom-Hole Temperature Data.xlsx
XLSX -
Geothermal Gradient Map of North America
HTML
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Complete Metadata
| @type | dcat:Dataset |
|---|---|
| accessLevel | public |
| bureauCode |
[ "019:20" ] |
| contactPoint |
{ "fn": "Yu-Feng Lin", "@type": "vcard:Contact", "hasEmail": "mailto:yflin@illinois.edu" } |
| dataQuality |
true
|
| description | High resolution fiber-optic distributed temperature sensing logs from the Illinois Basin Decatur Project (IBDP) in Decatur, IL were used to model the thermal profile in the Illinois Basin. |
| distribution |
[ { "@type": "dcat:Distribution", "title": "Basin Scale Modeling for CO2 Sequestration in the Basal Sandstone Reservoir", "format": "317", "accessURL": "https://doi.org/10.1016/j.egypro.2014.11.317", "mediaType": "application/octet-stream", "description": "This paper describes the development of a basin-scale model of geologic carbon sequestration (GCS) in the basal sandstone of the Illinois Basin." }, { "@type": "dcat:Distribution", "title": "Groundwater Discharge in the Illinois Basin as Suggested by Temperature Anomalies", "format": "HTML", "accessURL": "https://doi.org/10.1029/WR006i003p00912", "mediaType": "text/html", "description": "This paper identifies areas where ground water in the Illinois basin is moving vertically should be reflected by temperature anomalies. To test this hypothesis, an isothermal map for a depth of 500 feet was constructed, based on bottom hole temperatures of deep wells. This map was compared with a theoretical isothermal map for a depth of 500 feet that was made by projecting temperature gradients (calculated from the thermal conductivities of the rock) downward from the surface where mean annual air temperatures were known. The residual temperature map that was made on the basis of this comparison (calculated minus observed temperature) shows several warm and cool anomalies that are postulated to be discharge and recharge areas, respectively. Analysis of the curvature of the earth's thermal profile calculated for the basin suggests that approximately 59,000 acre‐feet of ground water per year are discharged upward from the deep rocks in the Illinois basin." }, { "@type": "dcat:Distribution", "title": "Deep Well Monitoring and Veritification at the Illinois Basin Decatur Project", "format": "3366031", "accessURL": "https://dx.doi.org/10.2139/ssrn.3366031", "mediaType": "application/octet-stream", "description": "Summary of research undertaken at Illinois Basin - Decatur Project" }, { "@type": "dcat:Distribution", "title": "Bottom-Hole Temperature Data.xlsx", "format": "xlsx", "accessURL": "https://gdr.openei.org/files/1059/bottomhole_temperature_data_il_basin__20180208%20%282%29.xlsx", "mediaType": "application/vnd.openxmlformats-officedocument.spreadsheetml.sheet", "description": "Bottom-hole temperatures from the Illinois Basin in central Illinois. From this data analysis we found the large variation in temperature at each depth interval prohibited us from using this data alone to determine the thermal gradient. Most temperature records lacked information about when the measurement was taken in reference to the drilling operation or injection and extraction activities. This information is critical so that measurements affected by heating from drilling and brine flow can be disregarded. Includes formation temperature versus depth plot." }, { "@type": "dcat:Distribution", "title": "Geothermal Gradient Map of North America", "format": "HTML", "accessURL": "https://ngmdb.usgs.gov/Prodesc/proddesc_66065.htm", "mediaType": "text/html", "description": "Geothermal gradients of North America based on corrected bottom-hole temperatures." } ] |
| DOI | 10.15121/1458560 |
| identifier | https://data.openei.org/submissions/8346 |
| issued | 2018-06-13T06:00:00Z |
| keyword |
[ "DDU", "DTS", "Deep Direct-Use", "Illinois Basin", "University of Illinois", "distributed temperature sensing", "energy", "geothermal", "temperature gradient", "temperature profile" ] |
| landingPage | https://gdr.openei.org/submissions/1059 |
| license | https://creativecommons.org/licenses/by/4.0/ |
| modified | 2025-02-17T17:45:03Z |
| programCode |
[ "019:006" ] |
| projectLead | Arlene Anderson |
| projectNumber | EE0008106 |
| projectTitle | Geothermal Heat Recovery Complex: Large-scale, Deep Direct-Use System in a Low-Temperature Sedimentary Basin |
| publisher |
{ "name": "University of Illinois", "@type": "org:Organization" } |
| spatial |
"{"type":"Polygon","coordinates":[[[-167.7267,13.518],[-53.8316,13.518],[-53.8316,75.0714],[-167.7267,75.0714],[-167.7267,13.518]]]}"
|
| title | University of Illinois Campus Deep Direct-Use Feasibility Study - Subsurface Temperature Profile |
