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Use of Rapid Temperature Measurements at a 2-meter Depth to Augment Deeper Temperature Gradient Drilling

Mark F. Coolbaugh, Chris Sladek, James E. Faulds, Richard E. Zehner, and Gary L. Oppliger

Key words
shallow, temperature, gradients, geothermal, two, meter, structure, faults
Location
Desert Peak, Nevada; Desert Queen, Nevada
Conference
Stanford Geothermal Workshop
Year
2007
Session
Field Studies
Language
English

Full text

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Abstract

Temperature gradient drilling has historically been a key tool in the exploration for geothermal resources in the Great Basin, USA, but regulatory, environmental, and accessibility issues, as well as the expense of drilling, are increasingly limiting its use. In cases where thermal groundwater is not overlain by near-surface cold aquifers, it is possible to augment temperature gradient drilling with temperatures measured from a 2-meter depth. We discuss the development of a rapid, efficient, and portable 2-meter-deep temperature measurement system that obtains accurate temperatures within an hour of emplacing hollow steel probes into the ground, making it possible to map results on a daily basis so that temperature surveys can rapidly vector towards thermal anomalies. As an example, a thermal anomaly related to a 60 m (200 ft) deep thermal aquifer at the Desert Queen geothermal area, near Desert Peak, Churchill County, Nevada, USA was mapped in much greater detail with 2-meter-deep measurements than possible with previous temperature gradient drilling, demonstrating that this technique can reduce the number of temperature gradient wells needed to identify zones of thermal upwelling.

Copyright 2007, Stanford Geothermal Program. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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