Published October 1, 2017 | Version v1
Journal article

Transition mechanism of sH to filled-ice Ih structure of methane hydrate under fixed pressure condition

  • 1. Geodynamics Research Center, Ehime University, Matsuyama, Ehime 790-8577 (Japan)
  • 2. Japan Synchrotron Radiation Research Institute, Hyogo 679-5198 (Japan)
  • 3. The National Institute of Advanced Industrial Science and Technology, Tsukuba, Ibaraki 305-8568 (Japan)

Description

The phase transition mechanism of methane hydrate from sH to filled-ice Ih structure was examined using a combination of time-resolved X-ray diffractometry (XRD) and Raman spectroscopy in conjunction with charge-coupled device (CCD) camera observation under fixed pressure conditions. Prior to time-resolved Raman experiments, the typical C-H vibration modes and their pressure dependence of three methane hydrate structures, fluid methane and solid methane were measured using Raman spectroscopy to distinguish the phase transitions of methane hydrates from decomposition to solid methane and ice VI or VII. Experimental results by XRD, Raman spectroscopy and CCD camera observation revealed that the structural transition of sH to filled-ice Ih occurs through a collapse of the sH framework followed by the release of fluid methane that is then gradually incorporated into the filled-ice Ih to reconstruct its structure. These observations suggest that the phase transition of sH to filled-ice Ih takes place by a typical reconstructive mechanism. (paper)

Availability note (English)

Available from http://dx.doi.org/10.1088/1742-6596/950/4/042044

Additional details

Publishing Information

Journal Title
Journal of Physics. Conference Series (Online)
Journal Volume
950
Journal Issue
4
Journal Page Range
[6 p.]
ISSN
1742-6596

Conference

Title
53. Joint International Conference on High Pressure Science and Technology
Acronym
Joint AIRAPT-25th and EHPRG
Dates
30 Aug - 4 Sep 2015
Place
Madrid (Spain)