Phase changes of filled ice Ih methane hydrate under low temperature and high pressure

Low-temperature and high-pressure experiments were performed with filled ice Ih structure of methane hydrate under 2.0–77.0 GPa and 30–300 K using diamond anvil cells and a helium-refrigeration cryostat. In situ X-ray diffractometry revealed distinct changes in the compressibility of the axial ratio...

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Published in:The Journal of Chemical Physics
Main Authors: Tanaka, Takehiko, Hirai, Hisako, Matsuoka, Takahiro, Ohishi, Yasuo, Yagi, Takehiko, Ohtake, Michika, Yamamoto, Yoshitaka, Nakano, Satoshi, Irifune, Tetsuo
Format: Article in Journal/Newspaper
Language:English
Published: AIP Publishing 2013
Subjects:
Online Access:http://dx.doi.org/10.1063/1.4820358
https://pubs.aip.org/aip/jcp/article-pdf/doi/10.1063/1.4820358/13572751/104701_1_online.pdf
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spelling craippubl:10.1063/1.4820358 2024-09-09T19:52:09+00:00 Phase changes of filled ice Ih methane hydrate under low temperature and high pressure Tanaka, Takehiko Hirai, Hisako Matsuoka, Takahiro Ohishi, Yasuo Yagi, Takehiko Ohtake, Michika Yamamoto, Yoshitaka Nakano, Satoshi Irifune, Tetsuo 2013 http://dx.doi.org/10.1063/1.4820358 https://pubs.aip.org/aip/jcp/article-pdf/doi/10.1063/1.4820358/13572751/104701_1_online.pdf en eng AIP Publishing The Journal of Chemical Physics volume 139, issue 10 ISSN 0021-9606 1089-7690 journal-article 2013 craippubl https://doi.org/10.1063/1.4820358 2024-07-18T04:05:43Z Low-temperature and high-pressure experiments were performed with filled ice Ih structure of methane hydrate under 2.0–77.0 GPa and 30–300 K using diamond anvil cells and a helium-refrigeration cryostat. In situ X-ray diffractometry revealed distinct changes in the compressibility of the axial ratios of the host framework with pressure. Raman spectroscopy showed a split in the C–H vibration modes of the guest methane molecules, which was previously explained by the orientational ordering of the guest molecules. The pressure and temperature conditions at the split of the vibration modes agreed well with those of the compressibility change. The results indicate the following: (i) the orientational ordering of the guest methane molecules from an orientationally disordered state occurred at high pressures and low temperatures; and (ii) this guest ordering led to anisotropic contraction in the host framework. Such guest orientational ordering and subsequent anisotropic contraction of the host framework were similar to that reported previously for filled ice Ic hydrogen hydrate. Since phases with different guest-ordering manners were regarded as different phases, existing regions of the guest disordered-phase and the guest ordered-phase were roughly estimated by the X-ray study. In addition, above the pressure of the guest-ordered phase, another high-pressure phase developed in the low-temperature region. The deuterated-water host samples were also examined, and the influence of isotopic effects on guest ordering and phase transformation was observed. Article in Journal/Newspaper Methane hydrate AIP Publishing Anvil ENVELOPE(-64.267,-64.267,-65.239,-65.239) The Journal of Chemical Physics 139 10 104701
institution Open Polar
collection AIP Publishing
op_collection_id craippubl
language English
description Low-temperature and high-pressure experiments were performed with filled ice Ih structure of methane hydrate under 2.0–77.0 GPa and 30–300 K using diamond anvil cells and a helium-refrigeration cryostat. In situ X-ray diffractometry revealed distinct changes in the compressibility of the axial ratios of the host framework with pressure. Raman spectroscopy showed a split in the C–H vibration modes of the guest methane molecules, which was previously explained by the orientational ordering of the guest molecules. The pressure and temperature conditions at the split of the vibration modes agreed well with those of the compressibility change. The results indicate the following: (i) the orientational ordering of the guest methane molecules from an orientationally disordered state occurred at high pressures and low temperatures; and (ii) this guest ordering led to anisotropic contraction in the host framework. Such guest orientational ordering and subsequent anisotropic contraction of the host framework were similar to that reported previously for filled ice Ic hydrogen hydrate. Since phases with different guest-ordering manners were regarded as different phases, existing regions of the guest disordered-phase and the guest ordered-phase were roughly estimated by the X-ray study. In addition, above the pressure of the guest-ordered phase, another high-pressure phase developed in the low-temperature region. The deuterated-water host samples were also examined, and the influence of isotopic effects on guest ordering and phase transformation was observed.
format Article in Journal/Newspaper
author Tanaka, Takehiko
Hirai, Hisako
Matsuoka, Takahiro
Ohishi, Yasuo
Yagi, Takehiko
Ohtake, Michika
Yamamoto, Yoshitaka
Nakano, Satoshi
Irifune, Tetsuo
spellingShingle Tanaka, Takehiko
Hirai, Hisako
Matsuoka, Takahiro
Ohishi, Yasuo
Yagi, Takehiko
Ohtake, Michika
Yamamoto, Yoshitaka
Nakano, Satoshi
Irifune, Tetsuo
Phase changes of filled ice Ih methane hydrate under low temperature and high pressure
author_facet Tanaka, Takehiko
Hirai, Hisako
Matsuoka, Takahiro
Ohishi, Yasuo
Yagi, Takehiko
Ohtake, Michika
Yamamoto, Yoshitaka
Nakano, Satoshi
Irifune, Tetsuo
author_sort Tanaka, Takehiko
title Phase changes of filled ice Ih methane hydrate under low temperature and high pressure
title_short Phase changes of filled ice Ih methane hydrate under low temperature and high pressure
title_full Phase changes of filled ice Ih methane hydrate under low temperature and high pressure
title_fullStr Phase changes of filled ice Ih methane hydrate under low temperature and high pressure
title_full_unstemmed Phase changes of filled ice Ih methane hydrate under low temperature and high pressure
title_sort phase changes of filled ice ih methane hydrate under low temperature and high pressure
publisher AIP Publishing
publishDate 2013
url http://dx.doi.org/10.1063/1.4820358
https://pubs.aip.org/aip/jcp/article-pdf/doi/10.1063/1.4820358/13572751/104701_1_online.pdf
long_lat ENVELOPE(-64.267,-64.267,-65.239,-65.239)
geographic Anvil
geographic_facet Anvil
genre Methane hydrate
genre_facet Methane hydrate
op_source The Journal of Chemical Physics
volume 139, issue 10
ISSN 0021-9606 1089-7690
op_doi https://doi.org/10.1063/1.4820358
container_title The Journal of Chemical Physics
container_volume 139
container_issue 10
container_start_page 104701
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