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Title: The structure of CO 2 hydrate between 0.7 and 1.0 GPa

Journal Article · · Journal of Chemical Physics
DOI:https://doi.org/10.1063/1.4899265· OSTI ID:1387495

A deuterated sample of CO2 structure I (sI) clathrate hydrate (CO2·8.3 D2O) has been formed and neutron diffraction experiments up to 1.0 GPa at 240 K were performed. The sI CO2 hydrate transformed at 0.7 GPa into the high pressure phase that had been observed previously by Hirai et al. [J. Phys. Chem. 133, 124511 (2010)] and Bollengier et al. [Geochim. Cosmochim. Acta 119, 322 (2013)], but which had not been structurally identified. The current neutron diffraction data were successfully fitted to a filled ice structure with CO2 molecules filling the water channels. This CO2+water system has also been investigated using classical molecular dynamics and density functional ab initio methods to provide additional characterization of the high pressure structure. Both models indicate the water network adapts a MH-III “like” filled ice structure with considerable disorder of the orientations of the CO2 molecule. Furthermore, the disorder appears to be a direct result of the level of proton disorder in the water network. In contrast to the conclusions of Bollengier et al., our neutron diffraction data show that the filled ice phase can be recovered to ambient pressure (0.1 MPa) at 96 K, and recrystallization to sI hydrate occurs upon subsequent heating to 150 K, possibly by first forming low density amorphous ice. Unlike other clathrate hydrate systems, which transform from the sI or sII structure to the hexagonal structure (sH) then to the filled ice structure, CO2 hydrate transforms directly from the sI form to the filled ice structure.

Research Organization:
Energy Frontier Research Centers (EFRC) (United States). Energy Frontier Research in Extreme Environments (EFree)
Sponsoring Organization:
USDOE Office of Science (SC), Basic Energy Sciences (BES)
DOE Contract Number:
SC0001057
OSTI ID:
1387495
Journal Information:
Journal of Chemical Physics, Vol. 141, Issue 17; Related Information: EFree partners with Carnegie Institution of Washington (lead); California Institute of Technology; Colorado School of Mines; Cornell University; Lehigh University; Pennsylvania State University; ISSN 0021-9606
Publisher:
American Institute of Physics (AIP)
Country of Publication:
United States
Language:
English

References (33)

Molecular dynamics study of the stability of methane structure H clathrate hydrates journal March 2007
Generalized Gradient Approximation Made Simple journal October 1996
A potential model for the study of ices and amorphous water: TIP4P/Ice journal June 2005
Phase equilibria in the H2O–CO2 system between 250–330K and 0–1.7GPa: Stability of the CO2 hydrates and H2O-ice VI at CO2 saturation journal October 2013
Transformations in methane hydrates journal November 2000
'Arctic Armageddon' Needs More Science, Less Hype journal August 2010
Structural systematics in the clathrate hydrates under pressure journal January 2003
A new clathrate hydrate structure journal January 1987
Hoover NPT dynamics for systems varying in shape and size journal February 1993
Ocean methane hydrates as a slow tipping point in the global carbon cycle journal November 2008
Stable methane hydrate above 2 GPa and the source of Titan's atmospheric methane journal April 2001
High-pressure gas hydrates journal January 2008
From ultrasoft pseudopotentials to the projector augmented-wave method journal January 1999
Phase Behaviour of Ices and Hydrates journal March 2010
Phase changes of CO2 hydrate under high pressure and low temperature journal September 2010
Rapid and Extensive Surface Changes Near Titan's Equator: Evidence of April Showers journal March 2011
Transition from Cage Clathrate to Filled Ice: The Structure of Methane Hydrate III journal October 2001
Cage occupancies in the high pressure structure H methane hydrate: A neutron diffraction study journal February 2012
Extensive Methane Venting to the Atmosphere from Sediments of the East Siberian Arctic Shelf journal March 2010
The PVT equation of state of D 2 O ice VI determined by neutron powder diffraction in the range 0 < P < 2.6 GPa and 120 < T < 330 K, and the isothermal equation of state of D 2 O ice VII from 2 to 7 GPa at room temperature journal May 2012
Isothermal equation of state for gold with a He-pressure medium journal September 2008
Ab initiomolecular dynamics for liquid metals journal January 1993
Stability of rare gas structure H clathrate hydrates journal September 2006
Escape of methane gas from the seabed along the West Spitsbergen continental margin: ARCTIC METHANE GAS PLUMES journal August 2009
An optimized molecular potential for carbon dioxide journal June 2005
High-pressure structures of methane hydrate observed up to 8 GPa at room temperature journal October 2001
A unified formulation of the constant temperature molecular dynamics methods journal July 1984
Structure, Composition, and Thermal Expansion of CO 2 Hydrate from Single Crystal X-ray Diffraction Measurements journal May 2001
Guest disorder and high pressure behavior of argon hydrates journal January 2010
Synthesis and characterization of a new structure of gas hydrate journal March 2009
Rising Arctic Ocean temperatures cause gas hydrate destabilization and ocean acidification: ARCTIC OCEAN GAS HYDRATES journal April 2011
Phase Diagram and High-Pressure Boundary of Hydrate Formation in the Carbon Dioxide−Water System journal May 2009
Methane Hydrate Behavior under High Pressure journal February 2000

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