| Project/Area Number |
05232103
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| Research Category |
Grant-in-Aid for Scientific Research on Priority Areas
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| Allocation Type | Single-year Grants |
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| Research Institution | Tohoku University |
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Principal Investigator |
HAYASHI Kazuo Tohoku University, Institute of Fluid Science, Professor, 流体科学研究所, 教授 (30111256)
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| Co-Investigator(Kenkyū-buntansha) |
MATSUKI Kohji Tohoku University Faculty of Engineering, Professor, 工学部, 教授 (10108475)
SATO Kazuhiko Muroran University of Technology, Faculty of Engineering, Professor, 工学部, 教授 (30002009)
NIITSUMA Hiroaki Tohoku University Faculty of Engineering, Professor, 工学部, 教授 (90108473)
MIZUTA Yoshiaki Yamaguchi University, Faculty of Engineering, Professor, 工学部, 教授 (20107733)
OGINO Fumimaru Kyoto University, Faculty of Engineering, Professor, 工学部, 教授 (50026069)
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| Project Period (FY) |
1993 – 1995
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| Project Status |
Completed (Fiscal Year 1996)
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| Budget Amount *help |
¥132,300,000 (Direct Cost: ¥132,300,000)
Fiscal Year 1995: ¥34,100,000 (Direct Cost: ¥34,100,000)
Fiscal Year 1994: ¥40,600,000 (Direct Cost: ¥40,600,000)
Fiscal Year 1993: ¥57,600,000 (Direct Cost: ¥57,600,000)
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| Keywords | Geothermal Reservoir / Artificial Crack / Fluid Flow in a Crack / Heat Transfer in a Crack / Characteristic of a Crack Surface / Acoustic Emission / Fractal Crack Surface / Crack Stiffness |
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| Research Abstract |
The main objective of the present project is to clarify the mechanical response of geothermal engineered reservoirs, such as HDR/HWR reservoirs, within a rock mass with many planes of weakness. To this end, we have constructed models for the case that the reservoir consists of innumerable joints and for the case that the reservoir consists of predominant reservoir cracks. We have clarified the basic characteristics of such reservoirs. Then, we have applied them successfully to the results of massive hydraulic fracturing/stimulation conducted at the Fenton Hill HDR field and at the Yunomori HWR field. It is preferable that the basic characteristics of the models can be estimated by using the geometrical and mechanical characteristics of fracture surfaces of fractures within core samples retrieved from the depth of boreholes. Therefore, we developed new methods for estimating the hydraulic properties of fractures from the fractal characteristics of fracture surfaces based on the laborato
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ry experiments under tri-axial stress conditions. Furthermore, we conducted mini-hydraulic fracturings in a driftway at the Kamioka mine to make a man-made fracture and to characterize the fractal characteristics of the surfaces created by hydraulic fracturing to find that the fractal characteristics are different from those of surfaces of fractures made by explosion and of slicken sides which are the surfaces subjected to shear movements. We have also developed new techniques on crosshole seismic measurement, borehole radar measurement and precise AE measurement for estimating the structure of multicrack geothermal reservoirs and the in-situ stress state of surrounding rocks. We have analyzed data sets observed at geothermal fields and have estimated reservoir characteristics by using these new techniques. It was found that it is highly probable that man-made reservoir cracks are accompanied by many-small secondary cracks generally. The hydraulic and heat transfer properties have been investigated for reservoir cracks accompanied by the secondary cracks by conducting laboratory experiments, where the rock with secondary cracks is simulated by a packed cube bed. Less
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