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Well Testing and Reservoir Engineering Studies at the Tendaho Geothermal Field, Ethiopia

Yiheyis Amdeberhan and Grimur Bjornsson

Key words
Tendaho geothermal field
Location
Tendaho, Ethiopia
Conference
World Geothermal Congress
Year
2000
Session
Exploration and Development
Language
English
Paper number
R0071

Full text

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Abstract

In this paper the 6 wells drilled in the Tendaho geothermal field are briefly described. Formation temperatures and initial pressures for each well are estimated and a conceptual reservoir model presented. The Tendaho reservoir is divided into a shallow sedimentary reservoir of 220-250oC temperature and a deep one in volcanic basalts, ranging from 220-270oC in temperature. Inflow comes from depth in the east and flows diagonally to the surface, causing reversed temperatures in the present wellfield. Production data analysis indicates permeability-thickness in the range of 3-10 Dm in the shallow reservoir. A wellbore simulator study show that the present wells maintain high flowrates despite either a 5 bars reservoir drawdown or a 20oC reservoir cooling. Both volumetric reservoir assessment and TOUGH2 reservoir model indicate that the present wellfield can sustain 70 kg/s production rate for 20 years.

Copyright 2000, International Geothermal Association. 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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