JpGU-AGU Joint Meeting 2020

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)

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)、今野 義浩(東京大学)

[HSC07-06] CO2/H2O/Muscovite系の圧力増加による接触角変化のメカニズムについて

*志賀 正茂1,2徂徠 正夫1愛知 正温2本田 博巳2 (1.産業技術総合研究所、2.東京大学)

キーワード:CO2地中貯留、濡れ性、接触角

CO2 Geological Storage (CGS) is one of the most promising technologies designed for reducing the amount of CO2 emissions into the atmosphere. The trapping mechanisms are classified into four types; structural, residual, dissolution, and mineral trapping.

The sealing performance of the caprock is affected by wettability, which derives from the interfacial tensions related to CO2, brine, and mineral phases. In the reservoir condition, the pressure and temperature are about 10MPa and 313K. Physical properties of CO2 are likely to change drastically because it changes from gaseous phase to the supercritical phase. Therefore, the pressure dependence of the contact angle of CO2/Brine/Mineral system has been investigated by a number of experimental measurements. Among them, the largest amount of experimental data has been obtained for muscovite (Iglauer et al. (2015)). Most data shows that the contact angle increases with increasing pressure. This indicates that the sealing performance is likely to decrease at the target PT conditions compared with the ambient condition. However, the mechanism of this trend has not been quantitatively revealed yet. This study calculated the effect of intermolecular forces by the augmented Young Laplace equation which is based on van der Waals forces, electrostatic forces, and hydration forces. Results shows that the increase in CO2 density and the surface charge reversal are crucial factors for the wettability alteration.