Article
Methane Hydrate Behavior under High Pressure
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Abstract
Phases changes in a water−methane system were investigated in a pressure range from 0.2 to 5.5 GPa using a diamond anvil cell. In-situ X-ray diffractometry and optical microscopy revealed methane hydrate behavior from growth to decomposition into high-pressure ice and solid methane at room temperature. Methane hydrate crystallized at 0.2−0.3 GPa from liquid, and it was compressed continuously until 2.3 GPa, maintaining structure I. Below 0.7 GPa the cage occupancy was unchanged. At 1.5 GPa methane hydrate partly decomposed to ice IV and fluid methane. The remaining methane hydrate kept structure I, but the cage occupancy was changed; i.e., small cages became vacant. At 2.1 GPa, coexisting ice VI transformed to ice VII and fluid methane solidified to phase I, while methane hydrate remained. At this pressure, structure I of methane hydrate was still maintained, and an additional change of cage occupancy occurred. The change in the cage occupancy is consistent with the change in compressibility observed on the compression curve. At 2.3 GPa, all of the methane hydrate decomposed into ice VII and phase I of solid methane.
Citing Articles
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This article has been cited by 11 ACS Journal articles (5 most recent appear below).

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Molecular Models for the Intercalation of Methane Hydrate Complexes in Montmorillonite Clay
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Randall T. Cygan, Stephen Guggenheim, and August F. Koster van GroosThe Journal of Physical Chemistry B2004 108 (39), 15141-15149Molecular simulations were performed to determine the structure and behavior of methane and H2O in the interlayer of various montmorillonite clays. Molecular dynamics using NPT ensembles and large simulation supercellscomprised of Na-, K-, Ca-, and Mg-...
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History
- Published In Issue February 24, 2000
- Received July 28, 1999
Revised November 10, 1999
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