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Natural State Simulation of the Kakkonda Geothermal Field, Japan

Yukihiro Sakagawa, Kengo Aoyama, Ken Ikeuchi, Masahiro Takahashi, Osamu Kato, Nobuo Doi, Toshiyuki Tosha, Takao Ominato and Kazuo Koide

Key words
geothermal, natural state simulation, Kakkonda field, NEDOĆ­s project
Location
Kakkonda, Japan; Sengan Geothermal Area
Conference
World Geothermal Congress
Year
2000
Session
Reservoir Evaluation
Language
English
Paper number
R0452

Full text

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Abstract

A numerical study of the Kakkonda field which consisted of three-dimensional natural state simulation, history matching and future prediction, is being carried out. Among them, the natural state simulation with porous models is presented here. Satisfactory fits on temperature in the natural state were obtained. The result implies that the heat source at the depth drives the fluid which originates from the meteoric water to form the current hydrothermal system, and that the temperature gap between the deep reservoir and the shallow reservoir may be caused by the permeability difference between both reservoirs. A sketch of the geological structure, the outline of the numerical model and results of the natural state simulation are presented.

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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