Analysis of pressure transient data from the Sumikawa geothermal field
Abstract
The permeability structure of the Sumikawa geothermal field in northern Japan has been the subject of an extensive pressure-transient testing investigation since 1986. In this paper, various pertinent data sets are presented and analyzed, including results showing reservoir heterogeneity (i.e. boundary) effects and apparent double porosity behavior. Interference tests between wells SB-3 and SD-2 (both of which have feedpoints in dacitic layers in the ''marine-volcanic complex'' formation) were carried out during 1990. The results have been interpreted to indicate the presence of a moderately high permeability ({approx} 4 darcy-meters) layer with two impermeable boundaries intersecting at a right angle. The 1988 pressure buildup data for well SN-7D are also explained by assuming two impermeable boundaries in a high transmissivity reservoir within the deep ''granodiorite'' formation. Interference tests between wells S-4 and KY-1 have suggested that a very permeable north-south channel is present in the ''altered andesite'' layer. Although the response was successfully interpreted using an ''anisotropic line-source model'' by Garg et al. (1991), a ''double porosity channel model'' seems to be particularly applicable for explaining both the short-term and long-term behavior observed in this series of tests.
- Authors:
- Publication Date:
- Research Org.:
- Geological Survey of Japan, Tsukuba, Ibaraki, JP; Mitsubishi Materials Corporation, Kazuno, Akita, JP
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 888723
- Report Number(s):
- SGP-TR-141-26
TRN: US200619%%253
- Resource Type:
- Conference
- Resource Relation:
- Conference: Seventeenth Workshop on Geothermal Reservoir Engineering: Proceedings, Stanford University, Stanford, CA, January 29-31, 1992
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 02 PETROLEUM; 15 GEOTHERMAL ENERGY; BUILDUP; GEOTHERMAL FIELDS; JAPAN; PERMEABILITY; POROSITY; RESERVOIR ENGINEERING; TESTING; TRANSIENTS; Geothermal Legacy
Citation Formats
Ishido, T, Kikuchi, T, yano, Y, Miyazaki, Y, Nakao, S, and Hatakeyama, K. Analysis of pressure transient data from the Sumikawa geothermal field. United States: N. p., 1992.
Web.
Ishido, T, Kikuchi, T, yano, Y, Miyazaki, Y, Nakao, S, & Hatakeyama, K. Analysis of pressure transient data from the Sumikawa geothermal field. United States.
Ishido, T, Kikuchi, T, yano, Y, Miyazaki, Y, Nakao, S, and Hatakeyama, K. 1992.
"Analysis of pressure transient data from the Sumikawa geothermal field". United States. https://www.osti.gov/servlets/purl/888723.
@article{osti_888723,
title = {Analysis of pressure transient data from the Sumikawa geothermal field},
author = {Ishido, T and Kikuchi, T and yano, Y and Miyazaki, Y and Nakao, S and Hatakeyama, K},
abstractNote = {The permeability structure of the Sumikawa geothermal field in northern Japan has been the subject of an extensive pressure-transient testing investigation since 1986. In this paper, various pertinent data sets are presented and analyzed, including results showing reservoir heterogeneity (i.e. boundary) effects and apparent double porosity behavior. Interference tests between wells SB-3 and SD-2 (both of which have feedpoints in dacitic layers in the ''marine-volcanic complex'' formation) were carried out during 1990. The results have been interpreted to indicate the presence of a moderately high permeability ({approx} 4 darcy-meters) layer with two impermeable boundaries intersecting at a right angle. The 1988 pressure buildup data for well SN-7D are also explained by assuming two impermeable boundaries in a high transmissivity reservoir within the deep ''granodiorite'' formation. Interference tests between wells S-4 and KY-1 have suggested that a very permeable north-south channel is present in the ''altered andesite'' layer. Although the response was successfully interpreted using an ''anisotropic line-source model'' by Garg et al. (1991), a ''double porosity channel model'' seems to be particularly applicable for explaining both the short-term and long-term behavior observed in this series of tests.},
doi = {},
url = {https://www.osti.gov/biblio/888723},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Wed Jan 01 00:00:00 EST 1992},
month = {Wed Jan 01 00:00:00 EST 1992}
}