- 著者
-
武山 詳
坂口 清敏
渡邉 則昭
土屋 範芳
- 出版者
- 一般社団法人 資源・素材学会
- 雑誌
- Journal of MMIJ (ISSN:18816118)
- 巻号頁・発行日
- vol.135, no.3, pp.25-30, 2019-03-31 (Released:2019-03-29)
- 参考文献数
- 26
Gypsum aggregate specimens have been used in the present study, because brittle, semi-brittle and ductile stress-strain behaviors of the specimen can be controlled only with confining stress level at the room temperature. At confining stresses up to 40 MPa, tri-axial compression and fluid flow experiments have been conducted on the intact specimens and single fracture specimens. It has been indicated that stress-strain behavior is independent of existence of fracture. Moreover, permeability of the single fracture specimen is much higher than intact specimen at conditions of brittle, semi-brittle, intermediate state between semi-brittle and ductile and ductile condition. On the other hand, permeability of the single fracture specimen is not so different from that of the intact specimen at conditions of a transitional behavior between semi-brittle and ductile stress-strain behaviors. As for the geothermal reservoir in the semi-brittle and ductile region, it was suggested that the fracture is retained and permeability is maintained when fracturing occurs due to hydraulic crushing or the like.