| Project/Area Number |
26249138
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| Research Category |
Grant-in-Aid for Scientific Research (A)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Earth system and resources engineering
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| Research Institution | The University of Tokyo |
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Principal Investigator |
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| Co-Investigator(Kenkyū-buntansha) |
山本 肇 大成建設株式会社技術センター, 土木技術研究所 地盤・岩盤研究室, チームリーダー (10417090)
愛知 正温 東京大学, 新領域創成科学研究科, 講師 (40645917)
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| Research Collaborator |
HIGUCHI Kohei 東京大学, 大学院新領域創成科学研究科, 特任研究員
MOGI Katsuro 東京大学, 大学院工学系研究科, 技術専門職員
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| Project Period (FY) |
2014-04-01 – 2017-03-31
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| Project Status |
Completed (Fiscal Year 2016)
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| Budget Amount *help |
¥35,490,000 (Direct Cost: ¥27,300,000、Indirect Cost: ¥8,190,000)
Fiscal Year 2016: ¥6,760,000 (Direct Cost: ¥5,200,000、Indirect Cost: ¥1,560,000)
Fiscal Year 2015: ¥12,090,000 (Direct Cost: ¥9,300,000、Indirect Cost: ¥2,790,000)
Fiscal Year 2014: ¥16,640,000 (Direct Cost: ¥12,800,000、Indirect Cost: ¥3,840,000)
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| Keywords | 地殻工学 / 光ファイバ歪センサ / 室内実験 / 多相流れ / 地殻変動計測 |
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| Outline of Final Research Achievements |
The behavior of rock masses under the existence of multi-phase fluid was analyzed through the usage of newly developed ultra-high resolution fiber optic strain sensors. We conducted both in-situ measurements and laboratory experiments for this study. Scale/time dependent rock mass behavior was analyzed through the long-term measurements of in-situ strains in the vault, and characteristic rock deformation behavior under the extremely slow non-wetting phase fluid movement was discovered by laboratory experiments.
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