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Heat Extracted from the Long Term Flow Test in the Fenton Hill HDR Reservoir

P. Kruger, B. Robinson

Location
Fenton Hill, New Mexico; Valles Caldera, New Mexico
Conference
Stanford Geothermal Workshop
Year
1994
Session
Production
Language
English

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Abstract

A long-term flow test was carried out in the Fenton Hill HDR Phase-2 reservoir for 14 months during 1992-1993 to examine the potential for supplying thermal energy at a sustained rate as a commercial demonstration of HDR technology. The test was accomplished in several segments with changes in mean flowrate due to pumping conditions. Re-test estimates of the extractable heat content above a minimum useful temperature were based on physical evidence of the size of the Fenton Hill reservoir. A numerical model was used to estimate the extent of heat extracted during the individual flow segments from the database of measured production data during the test. For a reservoir volume of 6.5~106 m3, the total heat content above a minimum temperature of 150" C was 1.5~10'~ J. For the total test period at the three sustained mean flowrates, the integrated heat extracted was 0.088~10'~ J, with no discernable temperature decline of the produced fluid. The fraction of energy extracted above the abandonment temperature was 5.9 %. On the basis of a constant thermal energy extraction rate, the lifetime of the reservoir (without reservoir growth) to the abandonment temperature would be 13.3 years, in good agreement with the pre-test estimate of 15.0 years for the given reservoir volume.

Copyright 1994, 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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