日本地球惑星科学連合2018年大会

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[JJ] 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-SC05] 地球温暖化防止と地学(CO2地中貯留・有効利用、地球工学)

2018年5月23日(水) 10:45 〜 12:15 201B (幕張メッセ国際会議場 2F)

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:徂徠 正夫(国立研究開発法人産業技術総合研究所)

11:00 〜 11:15

[HSC05-08] Saturation dependency of Bishop’s effective stress coefficient strongly affects strain behavior of rocks under two-phase flow condition

*後藤 宏樹1愛知 正温2徳永 朋祥2 (1.産業技術総合研究所、2.東京大学)

キーワード:Bishopの有効応力係数、二相流、変形、室内実験、数値シミュレーション

Understanding the strain behavior of rocks under two-phase flow condition is important to discuss a variety of subsurface processes including geological sequestration of carbon dioxide. Bishop’s effective stress coefficient (χ) is a parameter which defines “equivalent” fluid pressure in the stress-strain-fluid pressure relationships for porous media in two-phase fluid system (Coussy, 2007), and is commonly expressed as a function of the wetting-phase saturation. In this study, laboratory experiments and numerical simulations were conducted to investigate the effects of saturation dependency of χ on the strain behavior of rocks. In the experiment, compressed air was injected into a water-saturated cylindrical Berea sandstone sample from the bottom under hydrostatic external stress condition. During the experiment, confining pressure, air pressure at the bottom, and water pressure at the top were kept constant at 0.55, 0.35, 0.20 MPa, respectively, and axial and circumferential strains at half the height of the sample were monitored. Numerical simulation was conducted to reproduce the measured data by using a simulator which can solve coupled two-phase flow and deformation in porous media (Aichi, 2010). The measured strain behaviors before air breakthrough were reproduced well by assuming χ to be equal to water saturation, while those after the breakthrough was not. Non-linear relationships between χ and wetting-phase saturation explained both the measured strain behaviors before and after the breakthrough. It is concluded that saturation dependency of χ is an important parameter for understanding the strain behavior of rocks in two-phase fluid system.

References:
Aichi, M. (2010), Thermodynamically consistent multiphase poroelasticity and its application to water-dissolved gas reservoir simulation, PhD thesis, Univ. of Tokyo.
Coussy, O. (2007), Revisiting the constitutive equations of unsaturated porous solids using a Lagrangian saturation concept, Int. J. Numer. Anal. Meth. Geomech., 31, 1675-1694.