JpGU-AGU Joint Meeting 2020

講演情報

[J] ポスター発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS32] ガスハイドレートと地球環境・資源科学

コンビーナ:戸丸 仁(千葉大学理学部地球科学科)、八久保 晶弘(北見工業大学)、後藤 秀作(産業技術総合研究所地圏資源環境研究部門)、谷 篤史(神戸大学 大学院人間発達環境学研究科 人間環境学専攻)

[MIS32-P12] ガスハイドレートの水和数の直接測定の試み

*鎌田 諒也1木村 宏海1杉森 笑海1八久保 晶弘1竹谷 敏2 (1.北見工業大学、2.産業技術総合研究所)

キーワード:ガスハイドレート、水和数、アルゴン、メタン

Hydration number of gas hydrates is an important parameter, and it decides quality of natural gas hydrates. In the case of full occupancy of methane, hydration number of the crystallographic structure I becomes 5.75, however, hydration number of methane hydrate has been reported as 6, indicating that empty cages exist. Hydration number depends on temperature and pressure at the formation process (Cady, 1981; 1983) as van der Waals & Platteeuw model predicts. In this study, we tried to obtain hydration number of gas hydrates directly by a gravimetric determination. We selected argon as a guest gas, forms the crystallographic structure II. Theoretical value of hydration number is 5.67 in the case of full occupancy. We put 5 g of fine ice powder into a pressure chamber (volume: 42 mL), and introduced pure argon (purity: 99.999%, Air Water Inc.). Temperature was controlled at around 273 K to form argon hydrate. After completion of formation, the residual gas was evacuated at 77 K without dissociation of hydrate. Then, we weighed the cell before and after degasification and calculated weights of gas and water. Purity of the argon hydrate sample was checked by PXRD and it is confirmed that contamination of ice was less than 1%. Besides this, argon hydrate was synthesized in another cell (volume: 30 mL) and measured its equilibrium pressure from 270 K to 276 K. Hydration number at the quadruple point was estimated using Clausius-Clapeyron equation. Hydration number of argon hydrate obtained by gravimetric determination decreased with increasing pressure at the formation process; 6.7 at 10.2 MPa and 5.8 at 18.7 MPa. Hydration number at the quadruple point (273.2 K and 8.27 MPa) was 6.9, agrees with the data by gravimetric determination.

References

Cady GH (1981) Composition of clathrate gas hydrates of CHClF2, CCl3F, Cl2, ClO3F, H2S, and SF6. J Phys Chem 85: 3225-3230

Cady GH (1983) Composition of Clathrate Gas Hydrates of H2S, Xe, SO2, Cl2, CH3Cl, CH3Br, CHClF2, CCl2F2, and C3H8. J Phys Chem 87: 4437-4441