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A Summary of Recent Study on the Initial State of the Matsukawa Geothermal Reservoir

M. Hanano and G. Matsuo

Location
Matsukawa, Japan; Sengan geothermal area
Conference
Stanford Geothermal Workshop
Year
1990
Session
Field Results
Language
English

Full text

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Abstract

Feed point pressures of some of the earliest production wells i n Matsukawa were reconstructed from water levels and temperature profiles measured during warm up of the wells immediately after drilling . Although most of the wells currently produce dry superheated steam, the reconstructed pressures indicate that the pressure gradient of the production zone was super-hydrostatic and was similar to that of Kakkonda. which is a liquid-dominated system. It implies that the current production zone of the Matsukawa reservoir was induced to produce dry superheated steam mainly by little water recharge and high heat flow.

Copyright 1990, 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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