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Simulating Fenton Hill HDR Test Results Using the GEOTH3D Code

Takeshi Yamamoto, Yuzuru Eguchi, Kouichi Kitano, Donald Brown, Dave Duchane, Michael Fehler, Hiroshi Ohnishi

Key words
Fenton Hill
Location
Fenton Hill, New Mexico; Valles Caldera, New Mexico
Conference
Stanford Geothermal Workshop
Year
1998
Session
HOT DRY ROCK/DEEP-SEATED RESERVOIRS
Language
English

Full text

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Abstract

At the Fenton Hill hot dry rock (HDR) Test Site, the Long-Term Flow Test (LTFT) of the deeper reservoir was conducted h April 1992 through April 1993, following a multi-year period of reservoir pressurization at 15.6 MPa . At an injection pressure of 27.3 MPa, the steady-state fluid recovery at the
production well (not including the additional production flow up the annulus at the injection well) was 80% at a backpressure of 12.4 MPa and 73% at a
backpressure of 15.2 MPa.

The reservoir simulation code GEOTH3D, a model based on an assumed relationship between the distribution of permeability and the corresponding distribution of acoustic emissions (AE) throughout the pressure-stimulated reservoir region, was applied to the LTFT data to determine the applicability of this code to a second HDR reservoir. The principal model output, the percent recovery of fluid at the production well under two different steady-state operating conditions, was obtained by specifying the surface injection pressure and backpressure as boundary conditions. At an injection pressure of 27.3 MPa, the computed fluid recoveries were 81% and 75%, respectively, at the two different backpressure levels of 12.4 MPa and 15.2 MPa, in good agreement with the measured LTFT results. Therefore, the proposed three-dimensional reservoir modeling method, coupling the permeability values to the AE data, appears to be very effective in simulating the Fenton Hill HDR reservoir.

Copyright 1998, 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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