日本地球惑星科学連合2019年大会

講演情報

[J] 口頭発表

セッション記号 H (地球人間圏科学) » H-SC 社会地球科学・社会都市システム

[H-SC07] 地球温暖化防止と地学(CO2地中貯留・有効利用、地球工学)

2019年5月29日(水) 10:45 〜 12:15 301B (3F)

コンビーナ:徂徠 正夫(国立研究開発法人産業技術総合研究所地圏資源環境研究部門)、薛 自求(公益財団法人 地球環境産業技術研究機構)、愛知 正温(東京大学大学院新領域創成科学研究科)、座長:薛 自求(公益財団法人地球環境産業技術研究機構)

11:00 〜 11:15

[HSC07-08] Monitoring hydromechanical responses in aquifer by distributed fiber-optic strain sensing: From lab to field

*張 毅1,2薛 自求1,2橋本 励1,2朴 赫1,2 (1.二酸化炭素地中貯留技術研究組合、2.公益財団法人地球環境産業技術研究機構)

キーワード:分布型光ファイバひずみセンサ、帯水層透水試験、ハイドロメカニカル変形、CO2地中貯留

Pore fluids control deformation of porous media by the fluid-to-solid hydromechanical (HM) coupling in which a change in fluid pressure can modify the effective stress and deform the porous medium (Wang, 2000). The HM coupling mechanism provides a possibility that to understand aquifer characteristics and fluid activities during fluid extraction and/or injection operations, e.g., in geological CO2 storage (GCS), by monitoring rock strain changes. We successfully measured such HM deformations using a high-resolution distributed fiber optic strain sensing (DFOSS) tool in both laboratory and field scale studies. From the DFOSS-obtained HM information, we are able to track the pressure impact zone, understand the permeability structure of the aquifer formation and identify the preferential flow layers. Moreover, we can track the fluid migration front during CO2 displacing water and the mechanical response of CO2 breaking through to a low-permeability layer or caprock. The application of DFOSS would be beneficial to guide the aquifer pressure management for safe GCS with prior or simultaneous water extraction (Buscheck et al., 2012).