日本地熱学会誌

高温岩体からの熱抽出実験と人工貯留層のモデル化

山口勉, 厨川道雄, 佐藤嘉晃, 及川寧己, 小林秀男, 松永烈, ジョージジボロスキー

1991 年 13 巻 2 号 p. 73-93
発行日: 1991/04/25
公開日: 2009/08/07

DOIhttps://doi.org/10.11367/grsj1979.13.73

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The field tests for extracting the energy from Hot Dry Rock had been conducted at Hijiori test field in Yamagata Prefecture since 1984. In 1989, a 1-month flow test (Exp. 8902) was conducted using a injection well (SKG-2) and production wells (HDR-1 and HDR-2). In Exp. 8902, 40°C water was injected at the flow rate of 17 kg/s and 170°C hot water was recovered from production wells. The production rate from HDR-1 was 1.5 to 1.6 kg/s and that from HDR-2 was 4.2 to 4.9 kg/s. Although these production rates was not so high but the thermal output during the experiment reached to as high as 6 MW. This experiment was modeled by WBHT (Wellbore Heat Tranfer Code) and FEHM (Finite Element Heat and Mass Transfer Code), The simulation results showed that the permeability between SKG-1 and HDR-1 had 2 orders of magnitude more than the surrounding rocks. The calculated pressure distribution around the injection well showed that there was a high degree of pressure drop at the vicinity of injection well. The Gringarten's model was also used to estimate the area of heat transfer using the temperature draw down during the experiment.

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断裂型地熱貯留層におけるトレーサー応答解析

小倉啓明, 新堀雄一, 千田佶

1991 年 13 巻 2 号 p. 95-105
発行日: 1991/04/25
公開日: 2009/08/07

DOIhttps://doi.org/10.11367/grsj1979.13.95

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This paper proposes a new numerical model on tracer response analysis of a fractured geothermal reservoir. The multiple paths model has been generally used for analysis of tracer response. However, such a model is so complex that it has a lot of parameters to be determined. The model proposed in the paper has only one main path, composed of fracture and semi-fracture layers, and has fewer number of parameters to be specified than the multiple paths model does.The conclusions are as follows:(1) Good agreements are found between calculations by this model and observation data of tracer response in a geothermal reservoir.(2) It is possible to say that flow path in the reservoir is not always made up of multiple paths but of one main path composed of fracture and semi-fracture layers.

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講演要旨

1991 年 13 巻 2 号 p. 107-143
発行日: 1991/04/25
公開日: 2009/08/07

DOIhttps://doi.org/10.11367/grsj1979.13.107

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