Evaluation of Low-Temperature Geothermal Potential in Cache Valley, Utah
The purpose of this research was to continue the assessment of the low-temperature geothermal resources of Cache Valley, Utah initiated by the Utah Geological and Mineral Survey. Field work consisted of locating 90 wells and springs throughout the study area, collecting water samples for later labor...
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| Format: | Others |
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DigitalCommons@USU
1982
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| Online Access: | https://digitalcommons.usu.edu/etd/5048 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=6090&context=etd |
| Summary: | The purpose of this research was to continue the assessment of the low-temperature geothermal resources of Cache Valley, Utah initiated by the Utah Geological and Mineral Survey. Field work consisted of locating 90 wells and springs throughout the study area, collecting water samples for later laboratory analyses, and field measurement of pH, temperature, bicarbonate alkalinity, and electrical conductivity. Na+, K+, Ca+2 , Mg+2 , SiO2, Fe, SO4-2, Cl-, F-, and total dissolved solids were determined in the laboratory.
Temperature profiles were measured in 12 additional, unused wells. Thermal gradients calculated from the profiles were approximately the same as the average for the Basin and Range province, about 35°C/km. One well produced a gradient of 297°C/k.m, most probably as a result of a near-surface occurrence of warm water.
Possible warm water reservoir temperatures were calculated using both the silica and the Na-K-Ca geothermometers, with the results averaging about 50-100°C. If mixing calculations were applied, taking into account the temperatures and silica contents of both warm springs or wells and the cold groundwater, reservoir temperatures up to about 200°C were obtained.
Considering measured surface water temperatures, calculated reservoir temperatures, thermal gradients, and the local geology, most of the Cache Valley, Utah area is unsuited for geothermal development. However, the areas of North Logan, Benson, and Trenton were found to have anomalously warm groundwater in comparison to the background temperature of 13.0°C for the study area. The warm water has potential for isolated energy development but is not warm enough for major commercial development. |
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