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Study on Thermal Processes Beneath Kuju Volcano, Japan: A Step to Volcano Energy Utilization

Ehara, Sachio

Key words
Exploration; General; Japan; Kyushu; Magma; Fumaroles; Heat Flow; Curie Point; Volcanics; Convective Systems; Permeability; Solfatara
Location
Kuju Volcano, Japan
Conference
Geothermal Resources Council Transactions
Year
1992
Session
Exploration; Heat flow; Reservoir modeling; Volcanism
Language
English

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Abstract

Thermal state beneath Kuju volcano, central Kyushu, Japan is investigated as a first step to volcano energy utilization. Simulation of the regional high heat flow around Kuju volcano shows that most of the underlying magma reservoir is not molten at present but maintains high temperatures of 400-700°C. Simulation of the thermal processes beneath the solfatara field which is above the central part of the cooling magma suggests that the geothermal reservoir is a two phase reservoir heated by magmatic fluids.

Copyright 1992, Geothermal Resources Council. 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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