日本地球惑星科学連合2024年大会

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[J] 口頭発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS18] 結晶成⻑、溶解における界⾯・ナノ現象

2024年5月31日(金) 15:30 〜 16:45 101 (幕張メッセ国際会議場)

コンビーナ:木村 勇気(北海道大学低温科学研究所)、三浦 均(名古屋市立大学大学院理学研究科)、佐藤 久夫(日本原燃株式会社埋設事業部)、塚本 勝男(東北大学)、座長:山﨑 智也(北海道大学低温科学研究所)、三浦 均(名古屋市立大学大学院理学研究科)

16:00 〜 16:15

[MIS18-06] 高圧力環境で氷から生成するクラスレートハイドレートの透過電子顕微鏡観察

*山﨑 智也1内田 努2木村 勇気1 (1.北海道大学低温科学研究所、2.北海道大学大学院工学研究院)

キーワード:クラスレートハイドレート、透過電子顕微鏡法、氷、環境セル、高圧環境

Clathrate hydrates are crystals that form a cage-like structure of water molecules and incorporate a free molecule into the cage. Their formation temperature and pressure vary depending on the type of molecules incorporated into the cage, but the environment is basically low temperature and high pressure. In particular, gas hydrates, which are clathrate hydrates that incorporate gas molecules, have potential applications in a variety of fields, such as energy storage and gas separation [1]. The conditions for the formation of clathrate hydrates were applied to the environments in space, suggesting the presence of them in icy bodies in the solar system [2]. Thus, clathrate hydrate has the potential to exist in the universe, where water and gas molecules are present and under appropriate temperature and pressure conditions. For such applications and discussions, it is important to clarify the fundamental properties of clathrate hydrates, such as their formation environment, morphology, and formation kinetics.
Recently, an observation system that can cool an environmental cell by Peltier devices was developed for transmission electron microscopy [3]. The environmental cell can isolate a volatile sample from a high vacuum environment by sandwiching it between two thin electron-transparent membranes. Observations of ice crystallization from water have been achieved with this system [3]. During observation of ices the system, we discovered that crystals with clathrate hydrate structure were forming. Here we will report on the results of analysis of the crystals and discuss their formation process inside the environmental cell. This method has the potential to enable in situ observation of the formation of clathrate hydrates from ice in nanoscale and is expected to be a new approach for studying clathrate hydrate [4].

[1] A. Hassanpouryouzband et al. Chem. Soc. Rev. 49, (2021) 5225.
[2] W. L. Mao et al., Science 297 (2002) 2247.
[3] T. Yamazaki & Y. Kimura, Microsc. Microanal. 29 (2023) 1940.
[4] This work was supported by JSPS KAKENHI Grant Numbers JP20H05657 and JP21K18901.